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Search Results (483)

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17 pages, 4538 KiB  
Article
Determination of Geochemical Background and Baseline and Research on Geochemical Zoning in the Desert and Sandy Areas of China
by Weiji Wen, Fan Yang, Shuyun Xie, Chengwen Wang, Yuntao Song, Yuepeng Zhang and Weihang Zhou
Appl. Sci. 2024, 14(22), 10612; https://doi.org/10.3390/app142210612 - 18 Nov 2024
Viewed by 300
Abstract
Resources in deserts and sandy landscapes have potential for development, but existing surveys and sampling have not collected desert soil samples. As such, the geochemical background of these spaces remains unexplored due to the vastness and desolation of deserts. Therefore, researching the geochemical [...] Read more.
Resources in deserts and sandy landscapes have potential for development, but existing surveys and sampling have not collected desert soil samples. As such, the geochemical background of these spaces remains unexplored due to the vastness and desolation of deserts. Therefore, researching the geochemical background values and geochemical baseline values of deserts is of long-term significance. Our research indicates that in addition to macrostructural environmental divisions, microelement geochemistry can also be used for geological unit zoning. In this paper, geochemical background and geochemical baseline values of 61 desert elements were calculated using the iterative method, frequency histograms method, and multifractal concentration-area method. It also analyzes the distribution characteristics of major, trace, and rare earth elements, and divides the 12 desert sand regions into different geochemical zones. This paper determines, for the first time, the geochemical background values of elements in Chinese deserts, filling the gap in the study of desert background values. By combining machine learning methods, different deserts have been divided into three geochemical zones. This research will greatly enhance our ability to interpret the geochemical distribution and evolutionary patterns of desert elements in China, and it has important scientific significance and practical value for desert research. Full article
(This article belongs to the Special Issue New Advances, Challenges, and Illustrations in Applied Geochemistry)
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<p>Desert Sampling Location Map (Data and base map sources: Institute of Geophysical and Geochemical Exploration, Chinese Academy of Geological Sciences).</p>
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<p>Schematic Diagram of Method Principles. (<b>a</b>). Schematic Diagram of Frequency Histogram Distribution; (<b>b</b>). Schematic plot of Double Logarithmic Coordinate Curve of Content-Area Method.</p>
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<p>Element Standardized Plots. (<b>a</b>). Element Standardized Plots of Major Element; (<b>b</b>). Element Standardized Plots of Trace Element; (<b>c</b>). Element Standardized Plots of Rare Earth elements.</p>
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<p>Ratio of Geochemical Background Values to Baseline Values in Chinese Deserts.</p>
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<p>Triangular Diagrams of Major Elements. (<b>a</b>). SiO₂/10-Al<sub>2</sub>O<sub>3</sub>-CaO ternary diagram; (<b>b</b>). (K<sub>2</sub>O + Na<sub>2</sub>O)-CaO-TFe<sub>2</sub>O<sub>3</sub> ternary diagram; (<b>c</b>). CaO-K<sub>2</sub>O-Na<sub>2</sub>O ternary diagram.</p>
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<p>Feature Importance Stacked Plot. (<b>a</b>). Feature Importance Stacked Plot of Major Element; (<b>b</b>). Feature Importance Stacked Plot of Trace Element; (<b>c</b>). Feature Importance Stacked Plot of Rare Earth Element.</p>
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<p>Trace Element Background Value Clustering Heatmap.</p>
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<p>Trace Element Factor Weight Distribution Map.</p>
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26 pages, 9716 KiB  
Article
Multiscale Spatiotemporal Variation Analysis of Regional Water Use Efficiency Based on Multifractals
by Tong Zhao, Yanan Wang, Yulu Zhang, Qingyun Wang, Penghai Wu, Hui Yang, Zongyi He and Junli Li
Remote Sens. 2024, 16(22), 4269; https://doi.org/10.3390/rs16224269 - 16 Nov 2024
Viewed by 191
Abstract
Understanding the complex variations in water use efficiency (WUE) is critical for optimizing agricultural productivity and resource management. Traditional analytical methods often fail to capture the nonlinear and multiscale variations inherent in WUE, where multifractal theory offers distinct advantages. Given its limited application [...] Read more.
Understanding the complex variations in water use efficiency (WUE) is critical for optimizing agricultural productivity and resource management. Traditional analytical methods often fail to capture the nonlinear and multiscale variations inherent in WUE, where multifractal theory offers distinct advantages. Given its limited application in WUE studies, this paper analyzes the spatiotemporal characteristics and influencing factors of the WUE in Anhui Province from 2001 to 2022 using a multifractal, multiscale approach. The results indicated that the WUE exhibited significant interannual variation, peaking in summer, especially in August (2.4552 gC·mm−1·m−2), with the monthly average showing an inverted “V” shape. Across different spatial and temporal scales, the WUE displayed clear multifractal characteristics. Temporally, the variation in fractal features between years was not prominent, while inter-seasonal variation was most complex in August during summer. Spatially, the most distinct multifractal patterns were observed in hilly and mountainous areas, particularly in regions with brown soil distribution. Rainfall was identified as the primary natural driver influencing regional WUE changes. This study aims to promote the sustainable use of water resources while ensuring the stability of agricultural production within protected farmlands. Full article
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<p>Location of study area. (<b>a</b>) Location of Anhui Province on the administrative map of China. (<b>b</b>) DEM map of Anhui Province.</p>
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<p>Technical flowchart of the study (Among them, RN is net radiation, LAI is leaf area index, LST is land surface temperature, GPP is total primary productivity, and ET is evapotranspiration).</p>
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<p>Changing WUE, GPP, and ET trends.</p>
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<p>Average WUE over four seasons in Anhui Province.</p>
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<p>Trends in the average monthly WUE in Anhui Province during (<b>a</b>) 2001–2011 and (<b>b</b>) 2012–2021.</p>
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<p>Multiple fractal spectrum of WUE at different time scales in Anhui Province. (<b>a</b>) annual multifractal spectrum (<b>b</b>) monthly multifractal spectrum (<b>c</b>) seasonal multifractal spectrum.</p>
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<p>(<b>a</b>) Spatial distribution of average WUE in Anhui province. (<b>b</b>) Interannual trends in average WUE.</p>
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<p>Seasonal average WUE trends: (<b>a</b>) spring, (<b>b</b>) summer, (<b>c</b>) fall, and (<b>d</b>) winter.</p>
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<p>Trend of average WUE in each month: (<b>a</b>) January, (<b>b</b>) February, (<b>c</b>) March, (<b>d</b>) April, (<b>e</b>) May, (<b>f</b>) June, (<b>g</b>) July, (<b>h</b>) August, (<b>i</b>) September, (<b>j</b>) October, (<b>k</b>) November, and (<b>l</b>) December.</p>
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<p>Temporal trends in WUE, ET, and the GPP in the five regions of Anhui Province: (<b>a</b>) the Huaibei Plain, (<b>b</b>) Jianghuai hilly region, (<b>c</b>) plain alongside the river, (<b>d</b>) Dabie Mountain area in west Anhui Province, and (<b>e</b>) hilly and mountainous region of southern Anhui.</p>
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<p>Fractal dimensions of different natural terrain subdivisions in (<b>a</b>) the Huaibei Plain, (<b>b</b>) Jianghuai hilly region, (<b>c</b>) hilly and mountainous region of southern Anhui, (<b>d</b>) Dabie Mountain area, and (<b>e</b>) plain alongside the river.</p>
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<p>The double logarithmic chart for different natural terrain partitions: (<b>a</b>) the Huaibei Plain, (<b>b</b>) Jianghuai hilly region, (<b>c</b>) hilly and mountainous area of southern Anhui, (<b>d</b>) Dabie Mountains, and (<b>e</b>) plain alongside the river.</p>
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<p>The τ(q)~q curves for different natural terrain subdivisions: (<b>a</b>) the Huaibei Plain, (<b>b</b>) Jianghuai hilly region, (<b>c</b>) hilly and mountainous area of southern Anhui, (<b>d</b>) Dabie Mountains, and (<b>e</b>) plain alongside the river.</p>
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<p>Multiple fractal spectra describing the different natural terrain subdivisions: (<b>a</b>) the Huaibei Plain, (<b>b</b>) Jianghuai hilly region, (<b>c</b>) hilly and mountainous area in southern Anhui, (<b>d</b>) Dabie Mountains, and (<b>e</b>) plain alongside the river.</p>
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<p>WUE by soil type in Anhui Province.</p>
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<p>Fractal dimensions of soil types: (<b>a</b>) moist soil, (<b>b</b>) cinnamon soil, (<b>c</b>) red soils, (<b>d</b>) chrysolite, (<b>e</b>) yellow-brown soils, (<b>f</b>) southern paddy soils, (<b>g</b>) blood paddy soils, (<b>h</b>) brown soils.</p>
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<p>Multiple fractal spectra of eight soil types in Anhui Province: (<b>a</b>) moist soil, (<b>b</b>) cinnamon soil, (<b>c</b>) red soils, (<b>d</b>) chrysolite, (<b>e</b>) yellow-brown soils, (<b>f</b>) southern paddy soils, (<b>g</b>) blood paddy soils (<b>h</b>), brown soils.</p>
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<p>Influence weights of each influencing factor. (<b>a</b>) Influence factors of five topographic regions. (<b>b</b>) Influence factors of eight soils.</p>
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17 pages, 3211 KiB  
Article
Scaling Correlation Analysis of Particulate Matter Concentrations of Three South Indian Cities
by Adarsh Sankaran, Susan Mariam Rajesh, Muraleekrishnan Bahuleyan, Thomas Plocoste, Sumayah Santhoshkhan and Akhila Lekha
Pollutants 2024, 4(4), 498-514; https://doi.org/10.3390/pollutants4040034 - 13 Nov 2024
Viewed by 324
Abstract
Analyzing the fluctuations of particulate matter (PM) concentrations and their scaling correlation structures are useful for air quality management. Multifractal characterization of PM2.5 and PM10 of three cities in India wase considered using the detrended fluctuation procedure from 2018 to 2021. The cross-correlation [...] Read more.
Analyzing the fluctuations of particulate matter (PM) concentrations and their scaling correlation structures are useful for air quality management. Multifractal characterization of PM2.5 and PM10 of three cities in India wase considered using the detrended fluctuation procedure from 2018 to 2021. The cross-correlation of PM concentration in a multifractal viewpoint using the multifractal cross-correlation analysis (MFCCA) framework is proposed in this study. It was observed that PM2.5 was more multifractal and complex than PM10 at all the locations. The PM–gaseous pollutant (GP) and PM–meteorological variable (MV) correlations across the scales were found to be weak to moderate in different cities. There was no definite pattern in the correlation of PM with different meteorological and gaseous pollutants variables. The nature of correlation in the pairwise associations was found to be of diverse and mixed nature across the time scales and locations. All the time series exhibited multifractality when analyzed pairwise using multifractal cross-correlation analysis. However, there was a reduction in multifractality in individual cases during PM–GP and PM–MV paired analyses. The insights gained into the scaling behavior and cross-correlation structure from this study are valuable for developing prediction models for PMs by integrating them with machine learning techniques. Full article
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<p>Overall methodological framework.</p>
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<p>Fluctuation functions of PM2.5 and PM10 for the three cities. Upper panels show the plots of PM2.5 and lower panels show the results of PM10.</p>
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<p>Comparison of Renyi exponent plot and multifractal spectrum of PMs for the three cities.</p>
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<p>Renyi exponent and multifractal spectrum of gaseous pollutant time series for the three cities.</p>
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<p>Renyi exponent and multifractal spectrum of meteorological time series for the three cities.</p>
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<p>MFCCA of PM2.5 with meteorological parameters for Chennai. Last column depicts scaling correlations between the paired variables.</p>
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<p>MFCCA of PM2.5 with gaseous pollutants for Chennai. Last column depicts scaling correlations between the paired variables.</p>
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<p>MFCCA of PM10 with meteorological parameters for Chennai. Last column depicts scaling correlations between the paired variables.</p>
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<p>MFCCA of PM10 with gaseous pollutants for Chennai. Last column depicts scaling correlations between the paired variables.</p>
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<p>Comparison of Renyi exponent plot and multifractal spectrum of precipitation data of the three cities.</p>
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<p>MFCCA of rainfall (R) with PMs for Chennai. Last line depicts scaling correlations between the paired variables.</p>
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18 pages, 3764 KiB  
Article
Multifractal Analysis of Standardized Precipitation Evapotranspiration Index in Serbia in the Context of Climate Change
by Tatijana Stosic, Ivana Tošić, Irida Lazić, Milica Tošić, Lazar Filipović, Vladimir Djurdjević and Borko Stosic
Sustainability 2024, 16(22), 9857; https://doi.org/10.3390/su16229857 - 12 Nov 2024
Viewed by 448
Abstract
A better understanding of climate change impact on dry/wet conditions is crucial for agricultural planning and the use of renewable energy, in terms of sustainable development and preservation of natural resources for future generations. The objective of this study was to investigate the [...] Read more.
A better understanding of climate change impact on dry/wet conditions is crucial for agricultural planning and the use of renewable energy, in terms of sustainable development and preservation of natural resources for future generations. The objective of this study was to investigate the impact of climate change on temporal fluctuations of dry/wet conditions in Serbia on multiple temporal scales through multifractal analysis of the standardized precipitation evapotranspiration index (SPEI). We used the well-known method of multifractal detrended fluctuation analysis (MFDFA), which is suitable for the analysis of scaling properties of nonstationary temporal series. The complexity of the underlying stochastic process was evaluated through the parameters of the multifractal spectrum: position of maximum α0 (persistence), spectrum width W (degree of multifractality) and skew parameter r dominance of large/small fluctuations). MFDFA was applied on SPEI time series for the accumulation time scale of 1, 3, 6 and 12 months that were calculated using the high-resolution meteorological gridded dataset E-OBS for the period from 1961 to 2020. The impact of climate change was investigated by comparing two standard climatic periods (1961–1990 and 1991–2020). We found that all the SPEI series show multifractal properties with the dominant contribution of small fluctuations. The short and medium dry/wet conditions described by SPEI-1, SPEI-3, and SPEI-6 are persistent (0.5<α0<1); stronger persistence is found at higher accumulation time scales, while the SPEI-12 time series is antipersistent (0<α01<0.5). The degree of multifractality increases from SPEI-1 to SPEI-6 and decreases for SPEI-12. In the second period, the SPEI-1, SPEI-3, and SPEI-6 series become more persistent with weaker multifractality, indicating that short and medium dry/wet conditions (which are related to soil moisture and crop stress) become easier to predict, while SPEI-12 changed toward a more random regime and stronger multifractality in the eastern and central parts of the country, indicating that long-term dry/wet conditions (related to streamflow, reservoir levels, and groundwater levels) become more difficult for modeling and prediction. These results indicate that the complexity of dry/wet conditions, in this case described by the multifractal properties of the SPEI temporal series, is affected by climate change. Full article
(This article belongs to the Special Issue The Future of Water, Energy and Carbon Cycle in a Changing Climate)
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<p>Position of Serbia in Europe and map of Serbia with its orography and major rivers.</p>
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<p>Multifractal spectra for SPEI-1 for a sample grid point at latitude 43.15 and longitude 22.45, corresponding to the city of Pirot for the two accumulation periods 1961–1990 and 1991–2020. In the top row, the fluctuation function versus scale on the log-log plot is displayed, together with linear fits for different <math display="inline"><semantics> <mrow> <mi>q</mi> </mrow> </semantics></math> values. In the middle row, the functions <math display="inline"><semantics> <mrow> <mi>H</mi> <mo>(</mo> <mi>q</mi> <mo>)</mo> </mrow> </semantics></math>, <math display="inline"><semantics> <mrow> <mi>τ</mi> <mfenced separators="|"> <mrow> <mi>q</mi> </mrow> </mfenced> </mrow> </semantics></math> and <math display="inline"><semantics> <mrow> <mi>f</mi> <mfenced separators="|"> <mrow> <mi>α</mi> </mrow> </mfenced> </mrow> </semantics></math> are shown (lines serve to guide the eye), and in the bottom row, the maps of the parameter <math display="inline"><semantics> <mrow> <msub> <mrow> <mi>α</mi> </mrow> <mrow> <mn>0</mn> </mrow> </msub> </mrow> </semantics></math> are shown, emphasizing the chosen sample grid point position (bold squares in the southeast) for the period 1961–1990 (<b>bottom left</b>) and 1991–2020 (<b>bottom right</b>).</p>
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<p>Mutifractal parameter <math display="inline"><semantics> <mrow> <msub> <mrow> <mi>α</mi> </mrow> <mrow> <mn>0</mn> </mrow> </msub> </mrow> </semantics></math> for SPEI-1, SPEI-3, SPEI-6 and SPEI-12 across Serbia for the periods 1961–1990 and 1991–2020. To emphasize the difference between the parameters among the two periods, the range of the color bar is adjusted to cover (roughly) <math display="inline"><semantics> <mrow> <mo>±</mo> <mn>2</mn> </mrow> </semantics></math> standard deviations of the mean of <math display="inline"><semantics> <mrow> <msub> <mrow> <mi>α</mi> </mrow> <mrow> <mn>0</mn> </mrow> </msub> </mrow> </semantics></math> for each SPEI accumulation period.</p>
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<p>Mutifractal parameter <math display="inline"><semantics> <mrow> <mi>W</mi> </mrow> </semantics></math> for SPEI-1, SPEI-3, SPEI-6 and SPEI-12 across Serbia for the periods 1961–1990 and 1991–2020.</p>
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<p>Mutifractal parameter <math display="inline"><semantics> <mrow> <mi>r</mi> </mrow> </semantics></math> for SPEI-1, SPEI-3, SPEI-6 and SPEI-12 across Serbia for the periods 1961–1990 and 1991–2020.</p>
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22 pages, 3539 KiB  
Article
Multifractal Methods in Characterizing Pore Structure Heterogeneity During Hydrous Pyrolysis of Lacustrine Shale
by Xiaofei Liang, Qinhong Hu, Xiugang Pu, Wei Li, Qiming Wang, Mengdi Sun and Wenzhong Han
Fractal Fract. 2024, 8(11), 657; https://doi.org/10.3390/fractalfract8110657 - 11 Nov 2024
Viewed by 672
Abstract
By using gas physisorption and multifractal theory, this study analyzes pore structure heterogeneity and influencing factors during thermal maturation of naturally immature but artificially matured shale from the Kongdian Formation after being subjected to hydrous pyrolysis from 250 °C to 425 °C. As [...] Read more.
By using gas physisorption and multifractal theory, this study analyzes pore structure heterogeneity and influencing factors during thermal maturation of naturally immature but artificially matured shale from the Kongdian Formation after being subjected to hydrous pyrolysis from 250 °C to 425 °C. As thermal maturity increases, the transformation of organic matter, generation, retention, and expulsion of hydrocarbons, and formation of various pore types, lead to changes in pore structure heterogeneity. The entire process is divided into three stages: bitumen generation stage (250–300 °C), oil generation stage (325–375 °C), and oil cracking stage (400–425 °C). During the bitumen generation stage, retained hydrocarbons decrease total-pore and mesopore volumes. Fractal parameters ΔD indicative of pore connectivity shows little change, while Hurst exponent H values for pore structure heterogeneity drop significantly, indicating reduced pore connectivity due to bitumen clogging. During the peak oil generation stage, both ΔD and H values increase, indicating enhanced pore heterogeneity and connectivity due to the expulsion of retained hydrocarbons. In the oil cracking stage, ΔD increases significantly, and H value rises slowly, attributed to the generation of gaseous hydrocarbons further consuming retained hydrocarbons and organic matter, forming more small-diameter pores and increased pore heterogeneity. A strongly negative correlation between ΔD and retained hydrocarbon content, and a strongly positive correlation with gaseous hydrocarbon yield, highlight the dynamic interaction between hydrocarbon phases and pore structure evolution. This study overall provides valuable insights for petroleum generation, storage, and production. Full article
(This article belongs to the Special Issue Fractal and Fractional in Geomaterials, 2nd Edition)
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<p>Locations of Cangdong Sag and sampled well G1.</p>
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<p>Changes in geochemical indices of original and artificially matured shale samples.</p>
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<p>Characteristics of retained oil changes during thermal evolution.</p>
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<p>Relationship between remaining hydrocarbon generation potential and maturity.</p>
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<p>Changes in hydrocarbon products during thermal evolution.</p>
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<p>CGP isotherm data and pore volume changes.</p>
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<p>CGP-derived PSD during thermal maturation.</p>
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<p>Adsorption/desorption curves of the samples during hydrous pyrolysis.</p>
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<p>Variation of different types of pore volumes and SSA during hydrous pyrolysis.</p>
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<p>Pore size distribution of the samples during hydrous pyrolysis.</p>
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<p>NMR <span class="html-italic">T</span><sub>2</sub> spectra of samples during thermal simulation.</p>
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<p>Generalized dimension variation of the original sample and artificially matured samples pyrolyzed at 250–425 °C.</p>
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<p>Correlation coefficients between pore structure parameters.</p>
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<p>Pore size distribution of thermal simulation samples before and after extraction.</p>
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<p>Pore size distribution of thermal simulation samples before and after extraction.</p>
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<p>Relationship between multifractal parameters and hydrocarbon generation.</p>
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<p>Pore structure evolution characteristics.</p>
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18 pages, 1149 KiB  
Article
Approaching Multifractal Complexity in Decentralized Cryptocurrency Trading
by Marcin Wątorek, Marcin Królczyk, Jarosław Kwapień, Tomasz Stanisz and Stanisław Drożdż
Fractal Fract. 2024, 8(11), 652; https://doi.org/10.3390/fractalfract8110652 - 11 Nov 2024
Viewed by 737
Abstract
Multifractality is a concept that helps compactly grasp the most essential features of financial dynamics. In its fully developed form, this concept applies to essentially all mature financial markets and even to more liquid cryptocurrencies traded on centralized exchanges. A new element that [...] Read more.
Multifractality is a concept that helps compactly grasp the most essential features of financial dynamics. In its fully developed form, this concept applies to essentially all mature financial markets and even to more liquid cryptocurrencies traded on centralized exchanges. A new element that adds complexity to cryptocurrency markets is the possibility of decentralized trading. Based on the extracted tick-by-tick transaction data from the Universal Router contract of the Uniswap decentralized exchange, from 6 June 2023 to 30 June 2024, the present study using multifractal detrended fluctuation analysis (MFDFA) shows that even though liquidity on these new exchanges is still much lower compared to centralized exchanges, convincing traces of multifractality are already emerging in this new trading as well. The resulting multifractal spectra are, however, strongly left-side asymmetric, which indicates that this multifractality comes primarily from large fluctuations, and small ones are more of the uncorrelated noise type. What is particularly interesting here is the fact that multifractality is more developed for time series representing transaction volumes than rates of return. On the level of these larger events, a trace of multifractal cross-correlations between the two characteristics is also observed. Full article
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<p>The probability distribution (histogram) of the exchange rates ETH/USDT and ETH/USDC log returns <math display="inline"><semantics> <msub> <mi>R</mi> <mrow> <mo>Δ</mo> <mi>t</mi> <mo>=</mo> <mn>12</mn> <mspace width="3.33333pt"/> <mi mathvariant="normal">s</mi> </mrow> </msub> </semantics></math> on Uniswap liquidity pools—versions 2 and 3 with different trading commissions: 0.3% (USDT Uv3_0.3, USDC Uv3_03, USDT Uv2, and USDC Uv2) and 0.05% (USDT Uv3_0.05 and USDC Uv3_0.05).</p>
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<p>Complementary cumulative distribution functions for (<b>a</b>) absolute log returns <math display="inline"><semantics> <mrow> <mrow> <mo>|</mo> </mrow> <msub> <mi>R</mi> <mrow> <mo>Δ</mo> <mrow> <mi mathvariant="normal">t</mi> <mo>=</mo> <mn>5</mn> <mspace width="3.33333pt"/> <mi>min</mi> </mrow> </mrow> </msub> <mrow> <mo>|</mo> </mrow> </mrow> </semantics></math> and (<b>b</b>) volume <math display="inline"><semantics> <msub> <mi>V</mi> <mrow> <mo>Δ</mo> <mrow> <mi mathvariant="normal">t</mi> <mo>=</mo> <mn>5</mn> <mspace width="3.33333pt"/> <mi>min</mi> </mrow> </mrow> </msub> </semantics></math> of ETH expressed in USDT and USDC on Binance and Uniswap. The estimated exponent, <math display="inline"><semantics> <mi>γ</mi> </semantics></math> with standard error, is shown in the insets.</p>
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<p>Autocorrelation function for (<b>a</b>) absolute log returns <math display="inline"><semantics> <mrow> <mrow> <mo>|</mo> </mrow> <msub> <mi>R</mi> <mrow> <mo>Δ</mo> <mrow> <mi mathvariant="normal">t</mi> <mo>=</mo> <mn>5</mn> <mspace width="3.33333pt"/> <mi>min</mi> </mrow> </mrow> </msub> <mrow> <mo>|</mo> </mrow> </mrow> </semantics></math> and (<b>b</b>) volume <math display="inline"><semantics> <msub> <mi>V</mi> <mrow> <mo>Δ</mo> <mrow> <mi mathvariant="normal">t</mi> <mo>=</mo> <mn>5</mn> <mspace width="3.33333pt"/> <mi>min</mi> </mrow> </mrow> </msub> </semantics></math> of ETH expressed in USDT and USDC on Binance and Uniswap exchanges.</p>
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<p>Fluctuation functions <math display="inline"><semantics> <mrow> <msub> <mi>F</mi> <mrow> <mi>R</mi> <mi>R</mi> </mrow> </msub> <mrow> <mo>(</mo> <mi>q</mi> <mo>,</mo> <mi>s</mi> <mo>)</mo> </mrow> </mrow> </semantics></math> with the range of <math display="inline"><semantics> <mrow> <mi>q</mi> <mo>∈</mo> <mo>[</mo> <mo>−</mo> <mn>4</mn> <mo>,</mo> <mn>4</mn> <mo>]</mo> </mrow> </semantics></math> ( <math display="inline"><semantics> <mrow> <mo>Δ</mo> <mi>q</mi> <mo>=</mo> <mn>0.2</mn> </mrow> </semantics></math>) calculated for ETH/USDT and ETH/USDC log returns <math display="inline"><semantics> <msub> <mi>R</mi> <mrow> <mo>Δ</mo> <mi>t</mi> <mo>=</mo> <mn>5</mn> <mspace width="3.33333pt"/> <mi>min</mi> </mrow> </msub> </semantics></math> from Binance (<b>top</b>), Uniswap v3 (<b>middle</b>), and Uniswap v2 (<b>bottom</b>). (Main) Thick green lines represent <math display="inline"><semantics> <mrow> <mi>F</mi> <mo>(</mo> <mi>q</mi> <mo>=</mo> <mn>2</mn> <mo>,</mo> <mi>s</mi> <mo>)</mo> </mrow> </semantics></math>, from the slope of which the Hurst exponent <span class="html-italic">H</span> is estimated together with its standard error. Vertical red dashed lines indicate a scale range, where the family of <math display="inline"><semantics> <mrow> <msub> <mi>F</mi> <mrow> <mi>R</mi> <mi>R</mi> </mrow> </msub> <mrow> <mo>(</mo> <mi>q</mi> <mo>,</mo> <mi>s</mi> <mo>)</mo> </mrow> </mrow> </semantics></math> exhibits a power-law dependence for different values of <span class="html-italic">q</span>. (Insets) The generalized Hurst exponent <math display="inline"><semantics> <mrow> <mi>h</mi> <mo>(</mo> <mi>q</mi> <mo>)</mo> </mrow> </semantics></math> is estimated from the scaling of <math display="inline"><semantics> <mrow> <msub> <mi>F</mi> <mrow> <mi>R</mi> <mi>R</mi> </mrow> </msub> <mrow> <mo>(</mo> <mi>q</mi> <mo>,</mo> <mi>s</mi> <mo>)</mo> </mrow> </mrow> </semantics></math>. Error bars represent the standard error of linear regression.</p>
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<p><math display="inline"><semantics> <mrow> <msub> <mi>F</mi> <mrow> <mi>V</mi> <mi>V</mi> </mrow> </msub> <mrow> <mo>(</mo> <mi>q</mi> <mo>,</mo> <mi>s</mi> <mo>)</mo> </mrow> </mrow> </semantics></math> obtained in the same way as in <a href="#fractalfract-08-00652-f004" class="html-fig">Figure 4</a> but for volume <math display="inline"><semantics> <msub> <mi>V</mi> <mrow> <mo>Δ</mo> <mi>t</mi> <mo>=</mo> <mn>5</mn> <mspace width="3.33333pt"/> <mi>min</mi> </mrow> </msub> </semantics></math>.</p>
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<p>Multifractal spectra <math display="inline"><semantics> <mrow> <mi>f</mi> <mo>(</mo> <mi>α</mi> <mo>)</mo> </mrow> </semantics></math> calculated for ETH/USDT and ETH/USDC log returns <math display="inline"><semantics> <msub> <mi>R</mi> <mrow> <mo>Δ</mo> <mi>t</mi> <mo>=</mo> <mn>5</mn> <mspace width="3.33333pt"/> <mi>min</mi> </mrow> </msub> </semantics></math> (<b>left panels</b>) and volume values <math display="inline"><semantics> <msub> <mi>V</mi> <mrow> <mo>Δ</mo> <mi>t</mi> <mo>=</mo> <mn>5</mn> <mspace width="3.33333pt"/> <mi>min</mi> </mrow> </msub> </semantics></math> (<b>right panels</b>) from Binance, Uniswap v3, and Uniswap v2 in the range <math display="inline"><semantics> <mrow> <mi>q</mi> <mo>∈</mo> <mo>[</mo> <mo>−</mo> <mn>4</mn> <mo>:</mo> <mn>4</mn> <mo>]</mo> </mrow> </semantics></math> and <math display="inline"><semantics> <mrow> <mo>Δ</mo> <mi>q</mi> <mo>=</mo> <mn>0.2</mn> </mrow> </semantics></math>. The original time series (<b>top</b>) are compared with their shuffled surrogates marked with dotted lines and the Fourier surrogates marked with dashed lines (<b>bottom</b>).</p>
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<p>(Main) Fluctuation functions <math display="inline"><semantics> <mrow> <msub> <mi>F</mi> <mrow> <mo>|</mo> <mi>R</mi> <mo>|</mo> <mi>V</mi> </mrow> </msub> <mrow> <mo>(</mo> <mi>q</mi> <mo>,</mo> <mi>s</mi> <mo>)</mo> </mrow> </mrow> </semantics></math> for <math display="inline"><semantics> <mrow> <mi>q</mi> <mo>&gt;</mo> <mn>0</mn> </mrow> </semantics></math> with <math display="inline"><semantics> <mrow> <mo>Δ</mo> <mi>q</mi> <mo>=</mo> <mn>0.2</mn> </mrow> </semantics></math> calculated for volatility <math display="inline"><semantics> <mrow> <mrow> <mo>|</mo> </mrow> <msub> <mi>R</mi> <mrow> <mo>Δ</mo> <mn>5</mn> <mo>=</mo> <mrow> <mn>5</mn> <mspace width="3.33333pt"/> <mi>min</mi> </mrow> </mrow> </msub> <mrow> <mo>|</mo> </mrow> </mrow> </semantics></math> and volume <math display="inline"><semantics> <mrow> <mrow> <mo>|</mo> </mrow> <msub> <mi>V</mi> <mrow> <mo>Δ</mo> <mn>5</mn> <mo>=</mo> <mrow> <mn>5</mn> <mspace width="3.33333pt"/> <mi>min</mi> </mrow> </mrow> </msub> <mrow> <mo>|</mo> </mrow> </mrow> </semantics></math> representing time series from Binance (<b>top</b>), Uniswap version 3 (Uv3, <b>middle</b>), and version 2 (Uv2, <b>bottom</b>). (Insets) The scaling exponent <math display="inline"><semantics> <mrow> <mi>λ</mi> <mo>(</mo> <mi>q</mi> <mo>)</mo> </mrow> </semantics></math> (green line) and the average generalized Hurst exponent <math display="inline"><semantics> <mrow> <msub> <mi>h</mi> <mrow> <mo>|</mo> <mi>R</mi> <mo>|</mo> <mi>V</mi> </mrow> </msub> <mrow> <mo>(</mo> <mi>q</mi> <mo>)</mo> </mrow> </mrow> </semantics></math> (blue line) are estimated from the range of scales marked with the dashed lines. Error bars represent the standard error of linear regression.</p>
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<p>The detrended cross-correlation coefficient <math display="inline"><semantics> <mrow> <mi>ρ</mi> <mo>(</mo> <mi>q</mi> <mo>,</mo> <mi>s</mi> <mo>)</mo> </mrow> </semantics></math>, <math display="inline"><semantics> <mrow> <mi>q</mi> <mo>=</mo> <mn>2</mn> </mrow> </semantics></math>, calculated for volatility <math display="inline"><semantics> <mrow> <mrow> <mo>|</mo> </mrow> <msub> <mi>R</mi> <mrow> <mo>Δ</mo> <mn>5</mn> <mo>=</mo> <mrow> <mn>5</mn> <mspace width="3.33333pt"/> <mi>min</mi> </mrow> </mrow> </msub> <mrow> <mo>|</mo> </mrow> </mrow> </semantics></math> and volume <math display="inline"><semantics> <mrow> <mrow> <mo>|</mo> </mrow> <msub> <mi>V</mi> <mrow> <mo>Δ</mo> <mn>5</mn> <mo>=</mo> <mrow> <mn>5</mn> <mspace width="3.33333pt"/> <mi>min</mi> </mrow> </mrow> </msub> <mrow> <mo>|</mo> </mrow> </mrow> </semantics></math> time series of ETH/USDT and ETH/USDC traded on Binance, Uniswap version 3 (Uv3), and version 2 (Uv2).</p>
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32 pages, 8634 KiB  
Review
Fractal Modelling of Heterogeneous Catalytic Materials and Processes
by Suleiman Mousa and Sean P. Rigby
Materials 2024, 17(21), 5363; https://doi.org/10.3390/ma17215363 - 1 Nov 2024
Viewed by 365
Abstract
This review considers the use of fractal concepts to improve the development, fabrication, and characterisation of catalytic materials and supports. First, the theory of fractals is discussed, as well as how it can be used to better describe often highly complex catalytic materials [...] Read more.
This review considers the use of fractal concepts to improve the development, fabrication, and characterisation of catalytic materials and supports. First, the theory of fractals is discussed, as well as how it can be used to better describe often highly complex catalytic materials and enhance structural characterisation via a variety of different methods, including gas sorption, mercury porosimetry, NMR, and several imaging modalities. The review then surveys various synthesis and fabrication methods that can be used to create catalytic materials that are fractals or possess fractal character. It then goes on to consider how the fractal properties of catalysts affect their performance, especially their overall activity, selectivity for desired products, and resistance to deactivation. Finally, this review describes how the optimum fractal catalyst material for a given reaction system can be designed on a computer. Full article
(This article belongs to the Special Issue Featured Reviews in Catalytic Materials)
Show Figures

Figure 1

Figure 1
<p>Fractal tree branches. Author: John Leszczynski. This image is licensed under the Creative Commons Attribution-Share Alike 2.0 Generic license.</p>
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<p>(<b>a</b>) Regular/exact 3D Menger sponge (pre-)fractal. Reprinted with permission from Ref. [<a href="#B2-materials-17-05363" class="html-bibr">2</a>], 1999, American Chemical Society. The bottom, initial generator structure is used to produce the topmost, next level in the fractal creation process. This process can be repeated to ever-more levels. In contrast, the type of repetition in the middle structure is not fractal. (<b>b</b>) Computer-simulated 2D cluster–cluster aggregate (CCA) random (statistical) fractal model (black = CCA). Reprinted with permission from Ref. [<a href="#B3-materials-17-05363" class="html-bibr">3</a>], 1996, Elsevier (<b>c</b>) An example of the natural occurrence of such a CCA-type fractal in the form of a precipitated silica film (white = silica, black = void). Reprinted with permission from Ref. [<a href="#B4-materials-17-05363" class="html-bibr">4</a>], 2005, American Chemical Society.</p>
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<p>(<b>a</b>) Regular/exact 3D Menger sponge (pre-)fractal. Reprinted with permission from Ref. [<a href="#B2-materials-17-05363" class="html-bibr">2</a>], 1999, American Chemical Society. The bottom, initial generator structure is used to produce the topmost, next level in the fractal creation process. This process can be repeated to ever-more levels. In contrast, the type of repetition in the middle structure is not fractal. (<b>b</b>) Computer-simulated 2D cluster–cluster aggregate (CCA) random (statistical) fractal model (black = CCA). Reprinted with permission from Ref. [<a href="#B3-materials-17-05363" class="html-bibr">3</a>], 1996, Elsevier (<b>c</b>) An example of the natural occurrence of such a CCA-type fractal in the form of a precipitated silica film (white = silica, black = void). Reprinted with permission from Ref. [<a href="#B4-materials-17-05363" class="html-bibr">4</a>], 2005, American Chemical Society.</p>
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<p>Schematic diagram illustrating the molecular sieving effect for rough surfaces depending upon molecular size. The smaller molecules can enter surface convolutions from which the larger molecule is excluded.</p>
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<p>Plot of the logarithm of the monolayer capacities for water (■) and the other (labelled; C3, propane; C4, butane; nC6, n-hexane; cC6, cyclohexane) adsorbates (●) on G1 against the logarithm of the molecular cross-sectional area (<span class="html-italic">σ</span> = <span class="html-italic">r<sup>2</sup></span>). The dashed line shows a straight-line fit (with equation and coefficient of determination shown) to the data for the adsorbates other than water. Reprinted with permission from Ref. [<a href="#B10-materials-17-05363" class="html-bibr">10</a>], 2022, Elsevier.</p>
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<p>Schematic diagram illustrating the impact of rough surfaces on the surface area available for multi-layer build-up. The number of surface sites stays the same in successive layers for a flat surface, while the number of sites declines with each successive layer for concave surfaces.</p>
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<p>Examples of the isotherms obtained from the fractal BET equation for a range of surface-fractal dimensions. <span class="html-italic">V<sub>m</sub></span> is the monolayer capacity, and <span class="html-italic">C</span> is the BET constant. Reprinted with permission from Ref. [<a href="#B8-materials-17-05363" class="html-bibr">8</a>], 2020, Springer-Nature.</p>
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<p>(<b>a</b>) TEM image of SBA-16 silica material. The square array of white dots in the centre of the image corresponds to pore bodies formed by the (subsequently removed) polymer template. Reprinted with permission from Ref. [<a href="#B8-materials-17-05363" class="html-bibr">8</a>], 2020, Springer-Nature. (<b>b</b>) 2D and 3D reconstructed greyscale FIB-SEM images and segmentation result for fresh spray-dried methanol synthesis catalyst pellet. Also shown in the figure is the trench/cavity site. The scale bar corresponds to 3 μm. A denser spheroidal region is evident from the void amidst the scatter of (blue) macropores picked out by image segmentation. (<b>c</b>) 2D radial cross-sections and 3D reconstruction of high-resolution CXT image of spray-dried (SD) feed particle used to make the SD feed catalyst pellet. Also shown on the left side of the figure, for comparison purposes, is a low-resolution image of a whole SD feed pellet, with an arrow indicating a corresponding individual constituent feed particle. The fractal-like nature of the structure is evidenced by the visual similarities of the low- and high-resolution images. Reprinted with permission from Ref. [<a href="#B27-materials-17-05363" class="html-bibr">27</a>], 2023, Elsevier. (<b>d</b>) MRI spin–spin relaxation time images of perpendicular 2D slices through the centre of a sol–gel silica catalyst support pellet. The pixel resolution is 40 μm, and the slice thickness is 250 μm. Reprinted with permission from Ref. [<a href="#B28-materials-17-05363" class="html-bibr">28</a>], 2006, Elsevier.</p>
Full article ">Figure 7 Cont.
<p>(<b>a</b>) TEM image of SBA-16 silica material. The square array of white dots in the centre of the image corresponds to pore bodies formed by the (subsequently removed) polymer template. Reprinted with permission from Ref. [<a href="#B8-materials-17-05363" class="html-bibr">8</a>], 2020, Springer-Nature. (<b>b</b>) 2D and 3D reconstructed greyscale FIB-SEM images and segmentation result for fresh spray-dried methanol synthesis catalyst pellet. Also shown in the figure is the trench/cavity site. The scale bar corresponds to 3 μm. A denser spheroidal region is evident from the void amidst the scatter of (blue) macropores picked out by image segmentation. (<b>c</b>) 2D radial cross-sections and 3D reconstruction of high-resolution CXT image of spray-dried (SD) feed particle used to make the SD feed catalyst pellet. Also shown on the left side of the figure, for comparison purposes, is a low-resolution image of a whole SD feed pellet, with an arrow indicating a corresponding individual constituent feed particle. The fractal-like nature of the structure is evidenced by the visual similarities of the low- and high-resolution images. Reprinted with permission from Ref. [<a href="#B27-materials-17-05363" class="html-bibr">27</a>], 2023, Elsevier. (<b>d</b>) MRI spin–spin relaxation time images of perpendicular 2D slices through the centre of a sol–gel silica catalyst support pellet. The pixel resolution is 40 μm, and the slice thickness is 250 μm. Reprinted with permission from Ref. [<a href="#B28-materials-17-05363" class="html-bibr">28</a>], 2006, Elsevier.</p>
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<p>(<b>a</b>–<b>c</b>) Optimal geometry of square networks with 7 × 7 pores. Pores are represented as black, and the microporous catalytic support is indicated by white. Reprinted with permission from Ref. [<a href="#B79-materials-17-05363" class="html-bibr">79</a>], 2004, John Wiley and Sons.</p>
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<p>Illustrative re-assembled archetypal pore networks: (<b>a</b>) minimum shielding; (<b>b</b>) partial cruciform; (<b>c</b>) fully cruciform; (<b>d</b>) fractal tree. Reprinted with permission from Ref. [<a href="#B80-materials-17-05363" class="html-bibr">80</a>], 2007, Elsevier.</p>
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15 pages, 3030 KiB  
Article
Solar Wind Turbulence and Complexity Probed with Rank-Ordered Multifractal Analysis (ROMA)
by Marius Echim, Costel Munteanu, Gabriel Voitcu and Eliza Teodorescu
Entropy 2024, 26(11), 929; https://doi.org/10.3390/e26110929 - 30 Oct 2024
Viewed by 410
Abstract
The Rank-Ordered Multifractal Analysis (ROMA) is a tool designed to characterize scale (in)variance and multifractality based on rank ordering the fluctuations in “groups” characterized by the same mono-fractal behavior (Hurst exponent). A range-limited structure-function analysis provides the mono-fractal index for each rank-ordered range [...] Read more.
The Rank-Ordered Multifractal Analysis (ROMA) is a tool designed to characterize scale (in)variance and multifractality based on rank ordering the fluctuations in “groups” characterized by the same mono-fractal behavior (Hurst exponent). A range-limited structure-function analysis provides the mono-fractal index for each rank-ordered range of fluctuations. We discuss here two examples of multi-scale solar wind turbulence and complexity where ROMA is applied on the following: (a) data collected by Ulysses spacecraft in the fast solar wind, outside the ecliptic, between 25 and 31 January 2007, at roughly 2.5 Astronomical Units (AU) from the Sun, in the Southern heliosphere, at latitudes between −76.5 and −77.3 degrees, and (b) slow solar wind data collected in the ecliptic plane by Venus Express spacecraft, at 0.72 AU, on 28 January 2007. The ROMA spectrum of fast solar wind derived from ULYSSES data shows a scale-dependent structure of fluctuations: (1) at the smallest/kinetic range of scales (800 to 3200 km), persistent fluctuations are dominant, and (2) at the inertial range of scales (104 to 2 × 105 km), anti-persistent fluctuations are dominant, but less clearly developed and possibly indicative for the development of instabilities with cross-over behavior. The ROMA spectrum of the slow solar wind derived from Venus Express data, suggests a different structure of turbulence: (1) fully developed multifractal turbulence across scales between 5 × 104 and 4 × 105 km, with the Hurst index changing from anti-persistent to persistent values for the larger amplitude magnetic fluctuations; (2) at the smallest scales (400 to 6400 km), fluctuations are mainly anti-persistent, and the ROMA spectrum indicates a tendency towards mono-fractal behavior. Full article
(This article belongs to the Section Complexity)
Show Figures

Figure 1

Figure 1
<p>Illustration of the ROMA procedure applied on Venus Express data in the solar wind. (<b>a</b>) Range limited structure functions (7) computed for the first bin of scaled fluctuations ΔY<sub>1</sub> = [0.05, 0.80], ten orders q, from q = −5 to q = +5 and a value assumed a priori s = 0.25; scales from τ<sub>1</sub> = 2 s to τ<sub>4</sub> = 64 s are considered. (<b>b</b>) Structure-function scaling indices ζ(s,q) computed for <math display="inline"><semantics> <mrow> <mi>s</mi> <mo>∈</mo> <mfenced open="[" close="]" separators="|"> <mrow> <mn>0,0.5</mn> </mrow> </mfenced> </mrow> </semantics></math> and q = 2. The intersection between the computed ζ<sub>q</sub> (in red) and the ζ<sub>q</sub> = sq line (in black) is marked by the vertical dashed gray line at s = 0.25. (<b>c</b>) the slopes ζ(s,q) as a function of q for all values s and for each q for ΔY<sub>1</sub>. The ROMA solution for ΔY<sub>1</sub> is determined from the best linear fit of ζ<sub>q</sub>(q) lines. In this case, the solution is equal to s = 0.25.</p>
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<p>The ROMA approach implemented in INA library [<a href="#B33-entropy-26-00929" class="html-bibr">33</a>,<a href="#B35-entropy-26-00929" class="html-bibr">35</a>] exemplified for a bin of scaled fluctuations ΔY = [0.01,0.189] and all the moment orders q (from −5 to +5). The upper panel shows the magnetic field energy, <math display="inline"><semantics> <mrow> <msup> <mrow> <mfenced open="|" close="|" separators="|"> <mrow> <mi>B</mi> </mrow> </mfenced> </mrow> <mrow> <mn>2</mn> </mrow> </msup> </mrow> </semantics></math>, measured by Ulysses between 25 and 31 January 2007. The lower left panel shows the color-coded two-dimensional map of the function log<sub>10</sub>g(q,s); the “brighter” color indicates the maximum of this function, which identifies the ROMA solution for that corresponding q. The right panel shows the result of the global minimization procedure applied for the fluctuations in the bin ΔY = [0.01,0.189]. The procedure minimizes the function <math display="inline"><semantics> <mrow> <mi>f</mi> <mfenced separators="|"> <mrow> <mi>q</mi> <mo>,</mo> <mi>s</mi> </mrow> </mfenced> <mo>=</mo> <msup> <mrow> <mfenced open="|" close="|" separators="|"> <mrow> <mi>ζ</mi> <mfenced separators="|"> <mrow> <mi>q</mi> <mo>,</mo> <mi>s</mi> </mrow> </mfenced> <mo>−</mo> <mi>q</mi> <mi>s</mi> </mrow> </mfenced> </mrow> <mrow> <mn>2</mn> </mrow> </msup> </mrow> </semantics></math> for 100 values of s between 0 and 1 and all the moments q between −5 and +5.</p>
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<p>Schematic diagram showing the main steps to calculate the ROMA spectrum. The two implementations—INA and ODYN—are illustrated.</p>
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<p>The flatness parameter is computed for the entire time interval and 18 scales, between τ<sub>1</sub> = 2 s and τ<sub>18</sub> = 6 days; the scale is specified as “powers of 2” (in order to get the time scales one needs to raise 2 to each value and multiply with the time resolution, δt = 2 s). The three colored ranges emphasize the scales manifesting specific scaling: Range I (marked with red), between τ<sub>1</sub> = 2 and τ<sub>2</sub> = 8 s, corresponding to spatial scales roughly equal to 1400 to 5600 km (assuming the Taylor hypothesis is satisfied; the average solar wind speed is 700 km/s) where K(τ) decreases as τ decreases; Range II (marked with blue), between τ<sub>3</sub> = 32 s and τ<sub>4</sub> = 2048 s, corresponding to spatial scales roughly equal to 22,400 to 5,734,400 km where K(τ) increases as τ decreases, Range III (marked with yellow) τ<sub>5</sub> = 4.5 h and τ<sub>6</sub> = 72.8 h, corresponding to roughly 11.46 to 183.5 millions kilometers. The inset in the top-right indicates the scales considered to compute the flatness, specified in powers of 2 (left column), number of points (central column), and seconds (right column), respectively.</p>
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<p>(<b>left panel</b>) The full ROMA spectrum computed for magnetic field fluctuations measured by Ulysses in Range I of smallest kinetic scales emphasized in red in <a href="#entropy-26-00929-f004" class="html-fig">Figure 4</a>. (<b>middle panel</b>) the ROMA spectrum of magnetic field fluctuations in Range II, inertial of scales emphasized in blue in <a href="#entropy-26-00929-f004" class="html-fig">Figure 4</a>; (<b>right panel</b>) the ROMA spectrum of magnetic field fluctuations for Range III, injection of scales emphasized in yellow in <a href="#entropy-26-00929-f004" class="html-fig">Figure 4</a>.</p>
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<p>(<b>a</b>) Magnetic field energy, <math display="inline"><semantics> <mrow> <msup> <mrow> <mfenced open="|" close="|" separators="|"> <mrow> <mi>B</mi> </mrow> </mfenced> </mrow> <mrow> <mn>2</mn> </mrow> </msup> </mrow> </semantics></math>, measured by Venus Express in the solar wind on 28 January 2007, between 13:44:30 UT and 19:01:08 UT. (<b>b</b>) the flatness computed for B<sup>2</sup>; three ranges of scales are illustrated, between 2 and 32 s (marked with blue), 64 and 256 s (marked with yellow), 256 and 2048 s (marked with red), respectively. The three ranges exhibit different ROMA spectra as discussed in the text.</p>
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<p>(<b>a</b>) Full ROMA spectrum computed for magnetic energy, <math display="inline"><semantics> <mrow> <msup> <mrow> <mfenced open="|" close="|" separators="|"> <mrow> <mi>B</mi> </mrow> </mfenced> </mrow> <mrow> <mn>2</mn> </mrow> </msup> </mrow> </semantics></math>, measured by Venus Express in the solar wind on 28 January 2007, between 13:44:30 UT and 19:01:08 UT between 1 and 32 s, (<b>b</b>) same as (<b>a</b>) but for scale range between 64 and 256 s, (<b>c</b>) same as (<b>a</b>) but for scale range between 256 and 2048 s.</p>
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16 pages, 5958 KiB  
Article
Dynamic Black–Litterman Portfolios Incorporating Asymmetric Fractal Uncertainty
by Poongjin Cho and Minhyuk Lee
Fractal Fract. 2024, 8(11), 642; https://doi.org/10.3390/fractalfract8110642 - 30 Oct 2024
Viewed by 750
Abstract
This study investigates the profitability of portfolios that integrate asymmetric fractality within the Black–Litterman (BL) framework. It predicts 10-day-ahead exchange-traded fund (ETF) prices using recurrent neural networks (RNNs) based on historical price information and technical indicators; these predictions are utilized as BL views. [...] Read more.
This study investigates the profitability of portfolios that integrate asymmetric fractality within the Black–Litterman (BL) framework. It predicts 10-day-ahead exchange-traded fund (ETF) prices using recurrent neural networks (RNNs) based on historical price information and technical indicators; these predictions are utilized as BL views. While constructing the BL portfolio, the Hurst exponent obtained from the asymmetric multifractal detrended fluctuation analysis is employed to determine the uncertainty associated with the views. The Hurst exponent describes the long-range persistence in time-series data, which can also be interpreted as the uncertainty in time-series predictions. Additionally, uncertainty is measured using asymmetric fractality to account for the financial time series’ asymmetric characteristics. Then, backtesting is conducted on portfolios comprising 10 countries’ ETFs, rebalanced on a 10-day basis. While benchmarking to a Markowitz portfolio and the MSCI world index, profitability is assessed using the Sharpe ratio, maximum drawdown, and sub-period analysis. The results reveal that the proposed model enhances the overall portfolio return and demonstrates particularly strong performance during negative trends. Moreover, it identifies ongoing investment opportunities, even in recent periods. These findings underscore the potential of fractality in adjusting uncertainty for diverse portfolio optimization applications. Full article
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<p>Proposed portfolio model framework using A-MFDFA with predictions.</p>
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<p>The Black–Litterman portfolio model by computing the Hurst exponent.</p>
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<p>Price and Hurst exponent series of an EZA ETF.</p>
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<p>Price and the Hurst exponent series of all ETFs.</p>
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18 pages, 5826 KiB  
Article
A Fractal Study on Random Distribution of Recycled Concrete and Its Influence on Failure Characteristics
by Lixia Guo, Qingxiang Liu, Ling Zhong, Yuqing Yang and Jianwei Zhang
Fractal Fract. 2024, 8(11), 641; https://doi.org/10.3390/fractalfract8110641 - 30 Oct 2024
Viewed by 672
Abstract
In order to quantitatively describe the influence of aggregate distribution on crack development and peak stress of recycled aggregate concrete, a multifractal spectrum theory was proposed to quantitatively characterize aggregate distribution in specimens. A mesomechanical model of reclaimed aggregate concrete mixed with natural [...] Read more.
In order to quantitatively describe the influence of aggregate distribution on crack development and peak stress of recycled aggregate concrete, a multifractal spectrum theory was proposed to quantitatively characterize aggregate distribution in specimens. A mesomechanical model of reclaimed aggregate concrete mixed with natural aggregate and artificial aggregate was constructed. Numerical simulation tests were conducted on the uniaxial compression mechanical behavior of 25 groups of sample models with the same proportion and different aggregate distribution forms. Based on the box dimension theory, the multiple fractal spectrum method was used to quantitatively characterize the aggregate distribution form, and the key factors affecting cracks were explored based on the gray correlation degree. The research results show that the aggregate distribution in recycled aggregate concrete has multifractal characteristics. The multifractal spectrum was used to effectively characterize the aggregate distribution pattern, which can enlarge local details and provide new ideas for the quantitative analysis of the damage mode of recycled concrete. Secondly, by establishing a statistical model of the correlation between the multifractal spectrum width of the aggregate distribution pattern and the crack distribution box dimension, it was found that there was a positive correlation between the two, that is, the greater the multifractal spectrum width of the aggregate distribution pattern, the greater the crack box dimension, and the more complex the crack distribution. The complexity of aggregate distribution is closely related to the irregularity and complexity of mesoscopic failure crack propagation in recycled concrete specimens. In addition, gray correlation theory was applied to analyze the key factors affecting the formation of cracks in the specimens. The results showed that aggregate distribution had a first-order correlation with crack formation, and changes in aggregate distribution were an important factor affecting the performance of recycled concrete. Secondly, the poor mechanical properties of NAITZ led to obvious material damage, while NCA and MZ had a significant impact on the skeleton effect in the stress–strain process due to their large areas. This study deepens people’s understanding of the damage characteristics and cracking failure modes of recycled concrete. The study verifies the feasibility of the application of recycled aggregates and provides a valuable reference for engineering practice. Full article
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<p>The five-phase random aggregate model.</p>
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<p>The mesomechanical model of recycled aggregate concrete. (<b>a</b>) Mesomechanical model of recycled aggregate concrete; (<b>b</b>) Meshing results.</p>
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<p>Twenty-five random aggregate models.</p>
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<p>Twenty-five random aggregate models.</p>
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<p>The crack maps of the 25 random aggregate models.</p>
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<p>The stress–strain curve of the experimental group.</p>
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<p>The aggregate box dimension probability cumulative distribution histogram.</p>
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<p>The <math display="inline"><semantics> <mrow> <msub> <mi>D</mi> <mi mathvariant="normal">q</mi> </msub> <mo>−</mo> <mi>q</mi> </mrow> </semantics></math> relationship of model 1.</p>
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<p>The <math display="inline"><semantics> <mrow> <mi>f</mi> <mfenced> <mi>α</mi> </mfenced> <mo>−</mo> <mi>α</mi> </mrow> </semantics></math> relationship of the 25 models.</p>
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<p>Multifractal–aggregate distribution of the 25 groups.</p>
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<p>Calculation of crack box dimension in Model 1.</p>
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<p>The correlation between the spectrum width and box dimension of the 25 models.</p>
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<p>Calculation diagram of gray correlation degree.</p>
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19 pages, 9305 KiB  
Article
Matrix Compression and Pore Heterogeneity in the Coal-Measure Shale Reservoirs of the Qinshui Basin: A Multifractal Analysis
by Baoyuan Zhong, Yanming Zhu, Guangjun Feng, Jie Xiang and Yang Wang
Fractal Fract. 2024, 8(10), 580; https://doi.org/10.3390/fractalfract8100580 - 30 Sep 2024
Viewed by 527
Abstract
The application of high-pressure fluid induces the closure of isolated pores inside the matrix and promotes the generation of new fractures, resulting in a compressive effect on the matrix. To examine the compressibility of coal-measure shale samples, the compression of the coal–shale matrix [...] Read more.
The application of high-pressure fluid induces the closure of isolated pores inside the matrix and promotes the generation of new fractures, resulting in a compressive effect on the matrix. To examine the compressibility of coal-measure shale samples, the compression of the coal–shale matrix in the high-pressure stage was analyzed by a low-pressure nitrogen gas adsorption and mercury intrusion porosimetry experiment. The quantitative parameters describing the heterogeneity of the pore-size distribution of coal-measure shale are obtained using multifractal theory. The results indicate that the samples exhibit compressibility values ranging from 0.154 × 10−5 MPa−1 to 4.74 × 10−5 MPa−1 across a pressure range of 12–413 MPa. The presence of pliable clay minerals enhances the matrix compressibility, whereas inflexible brittle minerals exhibit resistance to matrix compression. There is a reduction in local fluctuations of pore volume across different pore sizes, an improvement in the autocorrelation of PSD, and a mitigation of nonuniformity after correction. Singular and dimension spectra have advantages in multifractal characterization. The left and right spectral width parameters of the singular spectrum emphasize the local differences between the high- and low-value pore volume areas, respectively, whereas the dimensional spectrum width is more suitable for reflecting the overall heterogeneity of the PSD. Full article
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<p>Outline of geological tectonic framework, sedimentary environment and sampling locations.</p>
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<p>Nitrogen adsorption and desorption curves and their corresponding pore type characteristics. (<b>a</b>) H2-type hysteresis curve; (<b>b</b>) H3-type hysteresis curve.</p>
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<p>Difference of raw and corrected MIP curves for the partial samples.</p>
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<p>Double-log plots of the partition function <span class="html-italic">χ</span>(<span class="html-italic">q, ε</span>) versus measure scale ε for the PSD of shale samples. (<b>a</b>) Sample QS-1 with the worst linear correlation, the <span class="html-italic">R</span><sup>2</sup> is above 0.85 for all fitted linear correlations. (<b>b</b>) Sample QS-8 with the best linear correlation, the <span class="html-italic">R</span><sup>2</sup> is above 0.98 for all fitted linear correlations.</p>
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<p>The relationship between matrix compressibility coefficient and material components. (<b>a</b>) Relationship between compressibility coefficient and quartz. (<b>b</b>) Relationship between compressibility coefficient and feldspar. (<b>c</b>) Relationship between compressibility coefficient and total organic carbon content. (<b>d</b>) Relationship between compressibility coefficient and clay minerals.</p>
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<p>Comparison of multifractal calculations by uncorrected and corrected MIP data. (<b>a</b>) Singularity index, α<sub>0</sub>. (<b>b</b>) Information dimension, <span class="html-italic">D</span><sub>1</sub>. (<b>c</b>) Hurst exponent, <span class="html-italic">H</span>. (<b>d</b>) The width of singularity spectrum, <span class="html-italic">α</span><sub>−10</sub> − <span class="html-italic">α</span><sub>10</sub>. (<b>e</b>) The width of generalized dimension spectrum, <span class="html-italic">D</span><sub>−10</sub> − <span class="html-italic">D</span><sub>10</sub>. (<b>f</b>) the width difference of singularity spectrum, <span class="html-italic">R<sub>d</sub></span>.</p>
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<p>Plots of the Hausdorff dimension <span class="html-italic">f[a(q)]</span> and the singularity exponent a(q). (<b>a</b>) Singular spectra of samples with absolute values of <span class="html-italic">R<sub>d</sub></span> greater than 0.1. (<b>b</b>) Singular spectra of samples with absolute values of <span class="html-italic">R<sub>d</sub></span> less than 0.1.</p>
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<p>Multifractal analysis of PSD by generalized dimension. (<b>a</b>) Plots of mass exponent, <span class="html-italic">τ(q),</span> varying with the moment <span class="html-italic">q</span>; (<b>b</b>) plots of <span class="html-italic">Dq</span> versus <span class="html-italic">q</span>, ranging from <span class="html-italic">q</span> = −10 to <span class="html-italic">q</span> = 10.</p>
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<p>Correlation chord plots of multiple fractal parameters with matrix compression coefficients.</p>
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<p>Schematic of nanopore and micro-fracture variation due to matrix compression effect.</p>
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<p>Correlation between Hurst index (<span class="html-italic">H</span>) and mineral compositions. (<b>a</b>) The relationship between <span class="html-italic">H</span> and quartz; (<b>b</b>) the relationship between <span class="html-italic">H</span> and feldspar; (<b>c</b>) the relationship between <span class="html-italic">H</span> and TOC; (<b>d</b>) the relationship between <span class="html-italic">H</span> and clay.</p>
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20 pages, 3357 KiB  
Article
Multifractal Analysis of the Impact of Fuel Cell Introduction in the Korean Electricity Market
by Seung Eun Ock, Minhyuk Lee and Jae Wook Song
Fractal Fract. 2024, 8(10), 573; https://doi.org/10.3390/fractalfract8100573 - 30 Sep 2024
Viewed by 549
Abstract
This study employs multifractal detrended fluctuation analysis to investigate the impact of fuel cell introduction in the Korean electricity market via the lens of multifractal scaling behavior. Using multifractal analysis, the research delineates discrepancies between peak and off-peak hours, accounting for the daily [...] Read more.
This study employs multifractal detrended fluctuation analysis to investigate the impact of fuel cell introduction in the Korean electricity market via the lens of multifractal scaling behavior. Using multifractal analysis, the research delineates discrepancies between peak and off-peak hours, accounting for the daily cyclicity of the electricity market, and proposes a crossover point detection method based on the Chow test. Furthermore, the impacts of fuel cell introduction are evidenced through various methods that encompass multifractal spectra and market efficiency. The findings initially indicate a higher degree of multifractality during off-peak hours relative to peak hours. In particular, the crossover points emerged solely during off-peak hours, unveiling short- and long-term dynamics predicated on a near-annual cycle. Additionally, the average Hurst exponent for the short-term was 0.542, while the average for the long-term was 0.098, representing a notable discrepancy. The introduction of fuel cells attenuated the heterogeneity in the scaling behavior, which is potentially attributable to the decreased volatility in both the supply and demand spectra. Remarkably, after the introduction of fuel cells, there was a discernible decrease in the influence of long-range correlation within multifractality, and the market exhibited an increased propensity toward random-walk behavior. This phenomenon was also detected in the market deficiency measure, from an average of 0.536, prior to the introduction, to an average of 0.267, following the introduction, signifying an improvement in market efficiency. This implies that the introduction of fuel cells into the market engendered increased supply stability and a consistent increase in demand, mitigating volatility on both the supply and demand sides, thus increasing market efficiency. Full article
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<p>A block diagram of the entire research procedure.</p>
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<p>Heatmap of each hour’s weekly log return correlation matrix.</p>
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<p>Weekly log return series of electricity price.</p>
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<p>Generalized Hurst exponent of entire period at each hour.</p>
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<p>Log–log plots of <math display="inline"><semantics> <mrow> <mo form="prefix">ln</mo> <msub> <mi>F</mi> <mn>2</mn> </msub> <mrow> <mo>(</mo> <mi>s</mi> <mo>)</mo> </mrow> </mrow> </semantics></math> vs. <math display="inline"><semantics> <mrow> <mo form="prefix">ln</mo> <mi>s</mi> </mrow> </semantics></math> with detected crossover point by MFDFA.</p>
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<p>Plots of <math display="inline"><semantics> <mrow> <mi>f</mi> <mo>(</mo> <mi>α</mi> <mo>)</mo> </mrow> </semantics></math> vs <math display="inline"><semantics> <mi>α</mi> </semantics></math> for each period using MFDFA.</p>
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29 pages, 8143 KiB  
Article
Inner Multifractal Dynamics in the Jumps of Cryptocurrency and Forex Markets
by Haider Ali, Muhammad Aftab, Faheem Aslam and Paulo Ferreira
Fractal Fract. 2024, 8(10), 571; https://doi.org/10.3390/fractalfract8100571 - 29 Sep 2024
Viewed by 1079
Abstract
Jump dynamics in financial markets exhibit significant complexity, often resulting in increased probabilities of subsequent jumps, akin to earthquake aftershocks. This study aims to understand these complexities within a multifractal framework. To do this, we employed the high-frequency intraday data from six major [...] Read more.
Jump dynamics in financial markets exhibit significant complexity, often resulting in increased probabilities of subsequent jumps, akin to earthquake aftershocks. This study aims to understand these complexities within a multifractal framework. To do this, we employed the high-frequency intraday data from six major cryptocurrencies (Bitcoin, Ethereum, Litecoin, Dashcoin, EOS, and Ripple) and six major forex markets (Euro, British pound, Canadian dollar, Australian dollar, Swiss franc, and Japanese yen) between 4 August 2019 and 4 October 2023, at 5 min intervals. We began by extracting daily jumps from realized volatility using a MinRV-based approach and then applying Multifractal Detrended Fluctuation Analysis (MFDFA) to those jumps to explore their multifractal characteristics. The results of the MFDFA—especially the fluctuation function, the varying Hurst exponent, and the Renyi exponent—confirm that all of these jump series exhibit significant multifractal properties. However, the range of the Hurst exponent values indicates that Dashcoin has the highest and Litecoin has the lowest multifractal strength. Moreover, all of the jump series show significant persistent behavior and a positive autocorrelation, indicating a higher probability of a positive/negative jump being followed by another positive/negative jump. Additionally, the findings of rolling-window MFDFA with a window length of 250 days reveal persistent behavior most of the time. These findings are useful for market participants, investors, and policymakers in developing portfolio diversification strategies and making important investment decisions, and they could enhance market efficiency and stability. Full article
(This article belongs to the Special Issue Complex Dynamics and Multifractal Analysis of Financial Markets)
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<p>5 min high-frequency returns of cryptocurrency markets.</p>
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<p>5 min high-frequency returns of forex markets.</p>
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<p>Daily jump estimates of cryptocurrency markets derived from 5 min high-frequency data.</p>
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<p>Daily jump estimates of forex markets derived from 5 min high frequency data.</p>
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<p>This figure presents the MFDFA outcomes pertaining to the jumps observed in cryptocurrency markets. In the (<b>top-left</b>) section, fluctuation functions for <span class="html-italic">q</span> = 10, <span class="html-italic">q</span> = 0, and <span class="html-italic">q</span> = −10 are displayed. The (<b>top-right</b>) segment illustrates the GHE corresponding to each <span class="html-italic">q</span> value. Additionally, the (<b>bottom-left</b>) section showcases the Mass exponent, <span class="html-italic">τ</span>(<span class="html-italic">q</span>), while the (<b>bottom-right</b>) portion presents the Multifractal Spectrum.</p>
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<p>This figure presents the MFDFA outcomes pertaining to the jumps observed in forex markets. In the (<b>top-left</b>) section, fluctuation functions for <span class="html-italic">q</span> = 10, <span class="html-italic">q</span> = 0, and <span class="html-italic">q</span> = −10 are displayed. The (<b>top-right</b>) segment illustrates the GHE corresponding to each <span class="html-italic">q</span> value. Additionally, the (<b>bottom-left</b>) section showcases the Mass exponent, <span class="html-italic">τ</span>(<span class="html-italic">q</span>), while the (<b>bottom-right</b>) portion presents the Multifractal Spectrum.</p>
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<p>Dynamic Hurst exponent evolution of the jumps of cryptocurrencies (<math display="inline"><semantics> <mrow> <mi>q</mi> <mo>=</mo> <mn>2</mn> </mrow> </semantics></math>, and <math display="inline"><semantics> <mrow> <mi>w</mi> <mi>i</mi> <mi>n</mi> <mi>d</mi> <mi>o</mi> <mi>w</mi> <mo>=</mo> <mn>250</mn> </mrow> </semantics></math>).</p>
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<p>Dynamic Hurst exponent evolution of the jumps of forex markets (<math display="inline"><semantics> <mrow> <mi>q</mi> <mo>=</mo> <mn>2</mn> </mrow> </semantics></math>, and <math display="inline"><semantics> <mrow> <mi>w</mi> <mi>i</mi> <mi>n</mi> <mi>d</mi> <mi>o</mi> <mi>w</mi> <mo>=</mo> <mn>250</mn> </mrow> </semantics></math>).</p>
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23 pages, 8605 KiB  
Article
Displacement Interval Prediction Method for Arch Dam with Cracks: Integrated STL, MF-DFA and Bootstrap
by Zeyuan Chen, Bo Xu, Linsong Sun, Xuan Wang, Dalai Song, Weigang Lu and Yangtao Li
Water 2024, 16(19), 2755; https://doi.org/10.3390/w16192755 - 27 Sep 2024
Viewed by 451
Abstract
Displacement prediction models based on measured data have been widely applied in structural health monitoring. However, most models neglect the particularity of displacement monitoring for arch dams with cracks, nor do they thoroughly analyze the non-stationarity and uncertainty of displacement. To address this [...] Read more.
Displacement prediction models based on measured data have been widely applied in structural health monitoring. However, most models neglect the particularity of displacement monitoring for arch dams with cracks, nor do they thoroughly analyze the non-stationarity and uncertainty of displacement. To address this issue, the influencing factors of displacement were first considered, with crack opening displacement being incorporated into them, leading to the construction of the HSCT model that accounts for the effects of cracks. Feature selection was performed on the factors of the HSCT model utilizing the max-relevance and min-redundancy (mRMR) algorithm, resulting in the screened subset of displacement influence factors. Next, displacement was decomposed into trend, seasonal, and remainder components applying the seasonal-trend decomposition using loess (STL) algorithm. The multifractal characteristics of these displacement components were then analyzed by multifractal detrended fluctuation analysis (MF-DFA). Subsequently, displacement components were predicted employing the convolutional neural network-long short-term memory (CNN-LSTM) model. Finally, the impact of uncertainty factors was quantified using prediction intervals based on the bootstrap method. The results indicate that the proposed methods and models are effective, yielding satisfactory prediction accuracy and providing scientific basis and technical support for the health diagnosis of hydraulic structures. Full article
(This article belongs to the Special Issue Water Engineering Safety and Management)
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<p>Structure of CNN-LSTM network.</p>
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<p>Schematic diagram of prediction interval.</p>
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<p>Flow chart of displacement interval prediction method.</p>
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<p>Layout diagram of plumb line measuring points.</p>
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<p>Schematic diagram of the arch dam.</p>
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<p>Process lines of water level, temperature, and displacement.</p>
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<p>Crack opening displacement process lines of 19 measuring points: (<b>a</b>) automatic measuring point and (<b>b</b>) manual measuring point.</p>
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<p>Decomposition results of two monitoring points via STL: (<b>a</b>) PL8−U and (<b>b</b>) PL18−U.</p>
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<p>Variation of Hurst exponent at measuring points: (<b>a</b>) PL8−U and (<b>b</b>) PL18−U.</p>
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<p>Variation of Renyi exponent at measuring points: (<b>a</b>) PL8−U and (<b>b</b>) PL18−U.</p>
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<p>Multifractal spectrum of measuring points: (<b>a</b>) PL8−U and (<b>b</b>) PL18−U.</p>
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<p>Fitting curves and statistical indicators of various models at PL8−U: (<b>a</b>) SSA-ELM, (<b>b</b>) LSTM, and (<b>c</b>) CNN-LSTM.</p>
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<p>Fitting curves and statistical indicators of various models at PL18−U: (<b>a</b>) SSA-ELM, (<b>b</b>) LSTM, and (<b>c</b>) CNN-LSTM.</p>
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<p>Prediction intervals at 95% PINC of various models at PL8−U: (<b>a</b>) STL-SSA-ELM, (<b>b</b>) STL-LSTM, and (<b>c</b>) STL-CNN-LSTM.</p>
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<p>Prediction intervals at 95% PINC of various models at PL18−U: (<b>a</b>) STL-SSA-ELM, (<b>b</b>) STL-LSTM, and (<b>c</b>) STL-CNN-LSTM.</p>
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14 pages, 712 KiB  
Article
Correlation between Temperature and the Posture of Transmission Line Towers
by Minzhen Wang, Haihang Gao, Zhigang Wang, Keyu Yue, Caiming Zhong, Guangxin Zhang and Jian Wang
Symmetry 2024, 16(10), 1270; https://doi.org/10.3390/sym16101270 - 26 Sep 2024
Viewed by 490
Abstract
Ensuring the safety of transmission line towers is vital for human safety, power supply, economic development, and environmental protection. This study specifically examines how temperature affects tower inclination. Multifractal detrended cross-correlation analysis (MF-DCCA) is a combination of multifractal detrended fluctuation analysis (MF-DFA) and [...] Read more.
Ensuring the safety of transmission line towers is vital for human safety, power supply, economic development, and environmental protection. This study specifically examines how temperature affects tower inclination. Multifractal detrended cross-correlation analysis (MF-DCCA) is a combination of multifractal detrended fluctuation analysis (MF-DFA) and DCCA that reveals the multifractal features of two cross-correlated non-stationary signals. This paper adopts the MF-DCCA tool to investigate the cross-correlations between the internal temperature of an inclination sensor device and the posture of a transmission line tower. The tilt angle data in the x- and y-axes are used to measure the posture of the transmission line tower. We start by using Pearson correlation to assess the relationship between temperature and two inclination angles, followed by verifying their correlation with a p-value below 0.05 using first-order linear fitting. We initially assess the multifractal features of three time series using MF-DFA before MF-DCCA analysis. All exhibit multifractal traits with H(2)<0.5, indicating negative persistence, especially notable in the temperature series. Finally, we adopt the MF-DCCA approach to examine the multifractal cross-correlation between tilt-angle time series and temperature time series, and the results indicate the negative persistence of the cross-correlation between the time series. Furthermore, the multifractal cross-correlation of temperature and inclination data on the y-axis was also found to be stronger than on the x-axis based on features of the scaling exponent and symmetry exponent. Full article
(This article belongs to the Special Issue Symmetry and Fractals: Theory and Applications)
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<p>Schematic diagram of the inclination angle between the transmission tower and the x/y-axis.</p>
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<p>The original time series of (<b>a</b>) x-axis inclination angle, (<b>b</b>) y-axis inclination angle, and (<b>c</b>) temperature time series.</p>
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<p>The original time series of (<b>a</b>) x-axis inclination angle, (<b>b</b>) y-axis inclination angle, and (<b>c</b>) temperature time series.</p>
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<p>The first-order linear fitting between the temperature data and (<b>a</b>) x-axis tilt angle data, and (<b>b</b>) y-axis tilt angle data. A color version of the figure is available in the web version of the article.</p>
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<p>Cross-correlation statistics <math display="inline"><semantics> <mrow> <mi>l</mi> <mi>o</mi> <mi>g</mi> <mo>(</mo> <msub> <mi>Q</mi> <mrow> <mi>c</mi> <mi>c</mi> </mrow> </msub> <mrow> <mo>(</mo> <mi>m</mi> <mo>)</mo> </mrow> <mo>)</mo> </mrow> </semantics></math> of two time-series pairs. A color version of the figure is available in the web version of the article.</p>
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<p>Double logarithmic curves between the fluctuation value and segment size of (<b>a</b>) x-axis inclination angle, (<b>b</b>) y-axis inclination angle, and (<b>c</b>) temperature time series.</p>
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<p>(<b>a</b>) The generalized Hurst exponent, (<b>b</b>) Renyi exponent, and (<b>c</b>) multifractal spectrum of three time series by MF-DFA.</p>
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<p>Cross-correlations of (<b>a</b>) the generalized Hurst exponent, (<b>b</b>) Renyi exponent, and (<b>c</b>) multifractal spectrum of two time-series pairs by MF-DCCA.</p>
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