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Search Results (295)

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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 263
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
(This article belongs to the Special Issue Stochastic Behavior of Environmental Pollution)
Show Figures

Figure 1

Figure 1
<p>Overall methodological framework.</p>
Full article ">Figure 2
<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 405
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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Figure 1

Figure 1
<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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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 640
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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Figure 1

Figure 1
<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>
Full article ">Figure 3
<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>
Full article ">Figure 4
<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>
Full article ">Figure 5
<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>
Full article ">Figure 6
<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>
Full article ">Figure 7
<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>
Full article ">Figure 8
<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>
Full article ">
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 396
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)
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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>
Full article ">Figure 2
<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>
Full article ">Figure 3
<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 721
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 648
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 519
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 537
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 1039
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 437
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 473
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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21 pages, 5433 KiB  
Article
A Novel Detection Algorithm for the Icing Status of Transmission Lines
by Dongxu Dai, Yan Hu, Hao Qian, Guoqiang Qi and Yan Wang
Symmetry 2024, 16(10), 1264; https://doi.org/10.3390/sym16101264 - 25 Sep 2024
Viewed by 491
Abstract
As more and more transmission lines need to pass through areas with heavy icing, the problem of transmission line faults caused by ice and snow disasters frequently occurs. Existing ice coverage monitoring methods have defects such as the use of a single monitoring [...] Read more.
As more and more transmission lines need to pass through areas with heavy icing, the problem of transmission line faults caused by ice and snow disasters frequently occurs. Existing ice coverage monitoring methods have defects such as the use of a single monitoring type, low accuracy of monitoring results, and an inability to obtain ice coverage data over time. Therefore, this study proposes a new algorithm for detecting the icing status of transmission lines. The algorithm uses two-dimensional multifractal detrended fluctuation analysis (2D MF-DFA) to determine the optimal sliding-window size and wave function and accurately segment and extract local feature areas. Based on the local Hurst exponent (Lh(z)) and the power-law relationship between the fluctuation function and the scale at multiple continuous scales, the ice-covered area of a transmission conductor was accurately detected. By analyzing and calculating the key target pixels, the icing thickness was accurately measured, achieving accurate detection of the icing status of the transmission lines. The experimental results show that this method can accurately detect ice-covered areas and the icing thickness of transmission lines under various working conditions, providing a strong guarantee for the safe and reliable operation of transmission lines under severe weather conditions. Full article
(This article belongs to the Special Issue Symmetry and Fractals: Theory and Applications)
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Figure 1
<p>Common types of conductor icing.</p>
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<p>Illustration of a sliding window with a size of <math display="inline"><semantics> <mrow> <mn>7</mn> <mo>×</mo> <mn>7</mn> </mrow> </semantics></math>.</p>
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<p>Original grayscale icing image.</p>
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<p>(<b>a</b>) Initial state of a sliding window with a size of <math display="inline"><semantics> <mrow> <mn>11</mn> <mo>×</mo> <mn>11</mn> </mrow> </semantics></math> in an icing image; (<b>b</b>) route passing points of the sliding window in the retinal icing image.</p>
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<p>Sub-regions of the sub-images of (<b>a</b>) <math display="inline"><semantics> <mrow> <mi>r</mi> <mo>=</mo> <mn>2</mn> </mrow> </semantics></math>, (<b>b</b>) <math display="inline"><semantics> <mrow> <mi>r</mi> <mo>=</mo> <mn>3</mn> </mrow> </semantics></math>, and (<b>c</b>) <math display="inline"><semantics> <mrow> <mi>r</mi> <mo>=</mo> <mn>4</mn> </mrow> </semantics></math>.</p>
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<p>Double-log plots of the sub-image.</p>
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<p>Values of the local Hurst exponent as the sliding window moves.</p>
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<p><math display="inline"><semantics> <mrow> <mi>q</mi> <mo>=</mo> <mn>6</mn> </mrow> </semantics></math>, <math display="inline"><semantics> <mrow> <mi>w</mi> <mo>=</mo> <mn>7</mn> </mrow> </semantics></math>. Experimenting with a synthetic image. (<b>a</b>) Original image; (<b>b</b>–<b>d</b>) plots of segmentation results with <math display="inline"><semantics> <mrow> <mo>(</mo> <msub> <mi>k</mi> <mn>1</mn> </msub> <mo>,</mo> <msub> <mi>k</mi> <mn>2</mn> </msub> <mo>)</mo> </mrow> </semantics></math> parameters of (13,16), (3,6), and (9,26), respectively.</p>
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<p>Multifractal analysis of (<b>a</b>) the original image, (<b>b</b>) double-logarithm plots, (<b>c</b>) the generalized Hurst exponent, and (<b>d</b>) the multifractal spectrum.</p>
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<p>Segmentation results of the synthesized image: (<b>a</b>) original image; (<b>b</b>) original pixels; (<b>c</b>) local fractal feature values; (<b>d</b>) contour edge state; and (<b>e</b>) segmentation results. Parameters: <math display="inline"><semantics> <mrow> <mrow> <mo>(</mo> <msub> <mi>k</mi> <mn>1</mn> </msub> <mo>,</mo> <msub> <mi>k</mi> <mn>2</mn> </msub> <mo>)</mo> </mrow> <mo>=</mo> <mrow> <mo>[</mo> <mn>8</mn> <mo>,</mo> <mn>60</mn> <mo>]</mo> </mrow> </mrow> </semantics></math>.</p>
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<p><span class="html-italic">q</span> = −10, <span class="html-italic">w</span> = 5. Experimenting with simple images of ice coverage. (<b>a</b>) Original image; (<b>b</b>–<b>d</b>) plots of the segmentation results with <math display="inline"><semantics> <mrow> <mo>(</mo> <msub> <mi>k</mi> <mn>1</mn> </msub> <mo>,</mo> <msub> <mi>k</mi> <mn>2</mn> </msub> <mo>)</mo> </mrow> </semantics></math> parameters of (2,8), (12,23), and (15,30), respectively.</p>
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<p><span class="html-italic">q</span> = −10, <span class="html-italic">w</span> = 5. Experimenting with simple images of ice coverage. (<b>a</b>) Original image; (<b>b</b>–<b>d</b>) plots of the segmentation results with <math display="inline"><semantics> <mrow> <mo>(</mo> <msub> <mi>k</mi> <mn>1</mn> </msub> <mo>,</mo> <msub> <mi>k</mi> <mn>2</mn> </msub> <mo>)</mo> </mrow> </semantics></math> parameters of (2,8), (12,23), and (15,30), respectively.</p>
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<p><span class="html-italic">q</span> = 10, <span class="html-italic">w</span> = 5. Experimenting with complex images of ice cover. (<b>a</b>) Original image; (<b>b</b>–<b>d</b>) plots of the segmentation results with <math display="inline"><semantics> <mrow> <mo>(</mo> <msub> <mi>k</mi> <mn>1</mn> </msub> <mo>,</mo> <msub> <mi>k</mi> <mn>2</mn> </msub> <mo>)</mo> </mrow> </semantics></math> parameters of (25,30), (6,22), and (6,24), respectively.</p>
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<p>(<b>a</b>) The segmented image; (<b>b</b>) a mesh representation of the segmented image; (<b>c</b>) an enlarged view of the mesh in (<b>b</b>); (<b>d</b>) the thickness of the icing area.</p>
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<p>The 20 selected thickness data points.</p>
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<p>(<b>a</b>) The original icing image; (<b>b</b>) a mesh representation of the segmented image; (<b>c</b>) the thickness of the icing area.</p>
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15 pages, 7611 KiB  
Article
Experimental Study on the Impact of High-Frequency Vibration Excitation on Coal Fracturing
by Lei Zhang, Xufeng Wang and Zhijun Niu
Fractal Fract. 2024, 8(9), 546; https://doi.org/10.3390/fractalfract8090546 - 19 Sep 2024
Viewed by 628
Abstract
The ultrasonic vibration rock-breaking method has been successfully applied to hard rock due to its high efficiency and controllable energy, providing a novel approach for the development of a more efficient, intelligent, safe, and environmentally friendly reconstruction method for coal and rock reservoirs. [...] Read more.
The ultrasonic vibration rock-breaking method has been successfully applied to hard rock due to its high efficiency and controllable energy, providing a novel approach for the development of a more efficient, intelligent, safe, and environmentally friendly reconstruction method for coal and rock reservoirs. By subjecting the rock to ultra-high frequency (>15 kHz) vibration load, rapid fatigue damage can be induced within a short period of time, thereby enhancing the extent of cracking in hard rock. In order to investigate the impact of high-frequency vibration excitation on coal cracking, this study conducted exploratory tests using an independently designed ultrasonic vibration excitation system. These tests were combined with nuclear magnetic resonance (NMR) and permeability measurements to compare and analyze the pore fracture structure and permeability changes in coal samples under resonant and non-resonant conditions. Additionally, multifractal characteristics of the coal samples were investigated. The results demonstrate that high-frequency vibration excitation leads to significant expansion of micropores and mesopores in coal samples. Moreover, there is a strong exponential relationship between coal porosity/permeability and excitation time. After 40 s of stimulation, both porosity and permeability increase by 32.4% and over 8400%, respectively; these increases are five times higher for resonance-state compared to non-resonance-state conditions. Furthermore, water-saturated coal samples exhibit multifractal characteristics in their NMR T2 spectrum distribution, and multifractal parameters ΔD(q)and Δα show positive correlations with the proportion of mesoporous/macropores but negative correlations with the proportion of micropores; conversely, Δf shows an opposite trend relative to pore proportions. The pore structure of coal exhibits intricate multi-scale characteristics, and the heterogeneity at various scales is quantified through multifractal analysis. This study confirms the feasibility of utilizing high-frequency vibration excitation for cracking coal rocks while also providing valuable insights for further expanding its application. Full article
(This article belongs to the Special Issue Applications of Fractal Analysis in Underground Engineering)
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<p>Coal samples for mechanical testing.</p>
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<p>Failure characteristics of coal samples.</p>
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<p>Natural frequency testing system.</p>
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<p>Natural frequency test results of coal sample with diameter of 50 mm and height of 100 mm: (<b>a</b>) time–domain signal; (<b>b</b>) frequency–domain signal.</p>
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<p>Coal samples with diameter of 50 mm and height of 100 mm.</p>
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<p>High-frequency vibration testing system.</p>
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<p>Nuclear magnetic resonance system testing system.</p>
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<p>(<b>a</b>) Permeability test device; (<b>b</b>) permeability testing procedure.</p>
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<p>NMR <span class="html-italic">T</span><sub>2</sub> spectra of two coal samples: (<b>a</b>) H1; (<b>b</b>) H2.</p>
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<p>Evolution of <span class="html-italic">T</span><sub>2</sub> spectrum curves of three rock samples: (<b>a</b>) H1; (<b>b</b>) H2.</p>
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<p>Proportion of each peak area of samples under different excitation times: (<b>a</b>) H1; (<b>b</b>) H2.</p>
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<p>Proportion of each peak area of samples under different excitation times: (<b>a</b>) H1; (<b>b</b>) H2.</p>
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<p>Evolution of sample porosity and permeability in resonant and non-resonant states: (<b>a</b>) porosity; (<b>b</b>) permeability.</p>
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<p>(<b>a</b>) Logarithmic curve of partition function and scale; (<b>b</b>) generalized fractal dimension spectrum; (<b>c</b>) mass function spectrum; (<b>d</b>) multifractal spectrum.</p>
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<p>The correlation between pore proportion and multifractal parameters: (<b>a</b>) <span class="html-italic">D<sub>max</sub></span>; (<b>b</b>) Δ<span class="html-italic">D</span>(<span class="html-italic">q</span>); (<b>c</b>) Δ<span class="html-italic">α</span>; (<b>d</b>) Δ<span class="html-italic">f</span>.</p>
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<p>The correlation between pore proportion and multifractal parameters: (<b>a</b>) <span class="html-italic">D<sub>max</sub></span>; (<b>b</b>) Δ<span class="html-italic">D</span>(<span class="html-italic">q</span>); (<b>c</b>) Δ<span class="html-italic">α</span>; (<b>d</b>) Δ<span class="html-italic">f</span>.</p>
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17 pages, 7741 KiB  
Article
Research on Slope Early Warning and Displacement Prediction Based on Multifractal Characterization
by Xiaofei Sun, Ying Su, Chengtao Yang, Junzhe Tan and Dunwen Liu
Fractal Fract. 2024, 8(9), 522; https://doi.org/10.3390/fractalfract8090522 - 4 Sep 2024
Cited by 1 | Viewed by 731
Abstract
The occurrence of landslide hazards significantly induces changes in slope surface displacement. This study conducts an in-depth analysis of the multifractal characteristics and displacement prediction of highway slope surface displacement sequences. Utilizing automated monitoring devices, data are collected to analyze the deformation patterns [...] Read more.
The occurrence of landslide hazards significantly induces changes in slope surface displacement. This study conducts an in-depth analysis of the multifractal characteristics and displacement prediction of highway slope surface displacement sequences. Utilizing automated monitoring devices, data are collected to analyze the deformation patterns of the slope surface layer. Specifically, the multifractal detrended fluctuation analysis (MF-DFA) method is employed to examine the multifractal features of the monitoring data for slope surface displacement. Additionally, the Mann–Kendall (M-K) method is combined to construct the α indicator and f(α) indicator criteria, which provide early warnings for slope stability. Furthermore, the long short-term memory (LSTM) model is optimized using the particle swarm optimization (PSO) algorithm to enhance the prediction of slope surface displacement. The results indicate that the slope displacement monitoring data exhibit a distinct fractal sequence characterized by h(q), with values decreasing as the fluctuation function q decreases. Through this study, the slope landslide warning classification has been determined to be Level III. Moreover, the PSO-LSTM model demonstrates superior prediction accuracy and stability in slope displacement forecasting, achieving a root mean square error (RMSE) of 0.72 and a coefficient of determination (R2) of 91%. Finally, a joint response synthesis of the slope landslide warning levels and slope displacement predictions resulted in conclusions. Subsequent surface displacements of the slope are likely to stabilize, indicating the need for routine monitoring and inspection of the site. Full article
(This article belongs to the Special Issue Fractal and Fractional in Geotechnical Engineering)
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<p>Site plan of the slope: (<b>a</b>) slopes, (<b>b</b>) monitoring devices.</p>
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<p>Displacement–time diagram of the surface layer of the slope.</p>
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<p>Flowchart of MF-DFA calculation.</p>
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<p>Flowchart of PSO algorithm.</p>
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<p><math display="inline"><semantics> <mrow> <mi>q</mi> </mrow> </semantics></math>-order fluctuation function <math display="inline"><semantics> <mrow> <mi>l</mi> <mi>o</mi> <mi>g</mi> <msub> <mrow> <mi>F</mi> </mrow> <mrow> <mi>q</mi> </mrow> </msub> <mfenced separators="|"> <mrow> <mi>s</mi> </mrow> </mfenced> <mo>−</mo> <mi>l</mi> <mi>o</mi> <mi>g</mi> <mi>s</mi> </mrow> </semantics></math> trend plot of double logarithmic fit: (<b>a</b>) Group I, (<b>b</b>) Group II, (<b>c</b>) Group III, (<b>d</b>) Group IV.</p>
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<p><math display="inline"><semantics> <mrow> <mi>q</mi> </mrow> </semantics></math>-order fluctuation function <math display="inline"><semantics> <mrow> <mi>l</mi> <mi>o</mi> <mi>g</mi> <msub> <mrow> <mi>F</mi> </mrow> <mrow> <mi>q</mi> </mrow> </msub> <mfenced separators="|"> <mrow> <mi>s</mi> </mrow> </mfenced> <mo>−</mo> <mi>l</mi> <mi>o</mi> <mi>g</mi> <mi>s</mi> </mrow> </semantics></math> trend plot of double logarithmic fit: (<b>a</b>) Group I, (<b>b</b>) Group II, (<b>c</b>) Group III, (<b>d</b>) Group IV.</p>
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<p>Variation of each index of displacement series: (<b>a</b>) generalized Hurst index, (<b>b</b>) scale function <math display="inline"><semantics> <mrow> <mi>τ</mi> </mrow> </semantics></math>, <math display="inline"><semantics> <mrow> <mi>q</mi> </mrow> </semantics></math>.</p>
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<p>Multiple fractal spectra of surface displacements for each group of side slopes.</p>
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<p>Values of slope landslide warning parameters: (<b>a</b>) <math display="inline"><semantics> <mrow> <mo>Δ</mo> <mi>α</mi> </mrow> </semantics></math> parameter values, (<b>b</b>) <math display="inline"><semantics> <mrow> <mo>Δ</mo> <mi>f</mi> <mo>(</mo> <mi>α</mi> <mo>)</mo> </mrow> </semantics></math> parameter values.</p>
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<p>Predicted results of slope surface displacements.</p>
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<p>Error map of slope displacement prediction.</p>
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<p>Predicted and fitted slope displacements.</p>
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<p>Slope site walk-through map.</p>
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16 pages, 3378 KiB  
Article
Multifractal Analysis of Neuronal Morphology in the Human Dorsal Striatum: Age-Related Changes and Spatial Differences
by Zorana Nedeljković, Bojana Krstonošić, Nebojša Milošević, Olivera Stanojlović, Dragan Hrnčić and Nemanja Rajković
Fractal Fract. 2024, 8(9), 514; https://doi.org/10.3390/fractalfract8090514 - 30 Aug 2024
Viewed by 535
Abstract
Multifractal analysis offers a sophisticated method to examine the complex morphology of neurons, which traditionally have been analyzed using monofractal techniques. This study investigates the multifractal properties of two-dimensional neuron projections from the human dorsal striatum, focusing on potential morphological changes related to [...] Read more.
Multifractal analysis offers a sophisticated method to examine the complex morphology of neurons, which traditionally have been analyzed using monofractal techniques. This study investigates the multifractal properties of two-dimensional neuron projections from the human dorsal striatum, focusing on potential morphological changes related to aging and differences based on spatial origin within the nucleus. Using multifractal spectra, we analyzed various parameters, including generalized dimensions and Hölder exponents, to characterize the neurons’ morphology. Despite the detailed analysis, no significant correlation was found between neuronal morphology and age. However, clear morphological differences were observed between neurons from the caudate nucleus and the putamen. Neurons from the putamen displayed higher morphological complexity and greater local homogeneity, while those from the caudate nucleus exhibited more scaling laws and higher local heterogeneity. These findings suggest that while age may not significantly impact neuronal morphology in the dorsal striatum, the spatial origin within this brain region plays a crucial role in determining neuronal structure. Further studies with larger samples are recommended to confirm these findings and to explore the full potential of multifractal analysis in neuronal morphology research. Full article
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<p>Examples of striatum binary images used in the study: (<b>a</b>) caudate nucleus neuron projection; (<b>b</b>) putamen neuron projection.</p>
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<p>Example images from the three age groups. (<b>a</b>) caudate nucleus neuron projection belonging to the first group; (<b>b</b>) caudate nucleus neuron projection belonging to the second group; (<b>c</b>) putamen neuron projection belonging to the third group.</p>
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<p>Example of area under the spectra (AUS) parameters for one image (caudate nucleus neuron projection). (<b>a</b>) area under the generalized dimension spectra AUS <span class="html-italic">D</span><sub>Q</sub>(<span class="html-italic">Q</span>); (<b>b</b>) area under the Hölder exponent spectra AUS <span class="html-italic">α</span>(<span class="html-italic">Q</span>); (<b>c</b>) area under the singularity spectra AUS <span class="html-italic">f</span>(<span class="html-italic">α</span>) vs. <span class="html-italic">Q</span>.</p>
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<p>Median value multifractal spectra of the three age groups: (<b>a</b>) Generalized dimension spectra <span class="html-italic">D</span><sub>Q</sub>(Q); (<b>b</b>) Hölder exponent spectra <span class="html-italic">α</span>(Q); (<b>c</b>) Singularity spectra <span class="html-italic">f</span>(α) vs. <span class="html-italic">Q</span>; (<b>d</b>) Singularity spectra <span class="html-italic">f</span>(<span class="html-italic">α</span>) vs. <span class="html-italic">α</span>. No statistically significant age-related differences were observed on any part of any spectrum.</p>
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<p>Median value multifractal spectra of the three age groups: (<b>a</b>) Generalized dimension spectra <span class="html-italic">D</span><sub>Q</sub>(Q); (<b>b</b>) Hölder exponent spectra <span class="html-italic">α</span>(Q); (<b>c</b>) Singularity spectra <span class="html-italic">f</span>(α) vs. <span class="html-italic">Q</span>; (<b>d</b>) Singularity spectra <span class="html-italic">f</span>(<span class="html-italic">α</span>) vs. <span class="html-italic">α</span>. No statistically significant age-related differences were observed on any part of any spectrum.</p>
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<p>Median value generalized dimension spectra <span class="html-italic">D</span><sub>Q</sub>(<span class="html-italic">Q</span>) for the two groups. Significant differences were observed for <span class="html-italic">Q</span> value intervals from −10.0 to 1.0 (<span class="html-italic">p</span> &lt; 0.001) and 1.25 to 4.0 (<span class="html-italic">p</span> &lt; 0.05), indicated with green shades. Non-significant differences (<span class="html-italic">p</span> &gt; 0.05) are indicated with red shade.</p>
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<p>Median value Hölder exponent spectra <span class="html-italic">α</span>(<span class="html-italic">Q</span>) for the two groups. Significant differences were observed for <span class="html-italic">Q</span> value intervals from −10.0 to 1.0 (<span class="html-italic">p</span> &lt; 0.001) and 1.25 to 2.0 (<span class="html-italic">p</span> &lt; 0.05), indicated with green shades. Non-significant differences (<span class="html-italic">p</span> &gt; 0.05) are indicated with red shade.</p>
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<p>Median value singularity spectra <span class="html-italic">f</span>(<span class="html-italic">α</span>) vs. <span class="html-italic">Q</span> for the two groups. Significant differences (<span class="html-italic">p</span> &lt; 0.05), indicated with green shades, were observed for <span class="html-italic">Q</span> intervals from −10.0 to −1.5 and −0.5 to 1.5, with the narrow band of <span class="html-italic">p</span> &lt; 0.001 in <span class="html-italic">Q</span> interval of 0 to 1. Non-significant differences (<span class="html-italic">p</span> &gt; 0.05) were observed for <span class="html-italic">Q</span> intervals from −1.25 to −0.75 and 1.75 to 10.0, indicated with the red shade.</p>
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<p>Median value singularity spectra <span class="html-italic">f</span>(<span class="html-italic">α</span>) vs. <span class="html-italic">α</span> for both groups.</p>
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