Slowness is the seventh studio album by Hong Kong recording-artist Kay Tse. It was released on December 21, 2009 by Cinepoly Records. The theme of the album is slowness, pointing out how life in urban cities has becoming increasingly restless and fast paced. Tse worked with several producers in this album, most notably her frequent collaborator, the songwriter Adrain Chow. He is also the executive producer for the album. Musically, the album consists of slow-tempo cantopop while incorporating jazz elements.

The first single from Slowness, "Living" <<活著>> was a critical success, which reached number one in three of the four major charts of Hong Kong. Three more singles were released which received moderate success. Tse promoted the album by promoting the songs in a number of live appearances, including a mini concert series.

Singles

^ Single was unable to chart due to disagreement between Universal Music Group and TVB

Track listing

! is an album by The Dismemberment Plan. It was released on October 2, 1995, on DeSoto Records. The band's original drummer, Steve Cummings, played on this album but left shortly after its release.

Track listing

Personnel

The following people were involved in the making of !:

References

"@" is a studio album by John Zorn and Thurston Moore. It is the first collaborative album by the duo and was recorded in New York City in February, 2013 and released by Tzadik Records in September 2013. The album consists of improvised music by Zorn and Moore that was recorded in the studio in real time with no edits or overdubs.

Reception

Allmusic said "@ finds two of New York City's longest-running fringe dwellers churning out sheets of collaborative sounds that conjoin their respective and distinct states of constant freak-out... These seven improvisations sound inspired without feeling at all heavy-handed or urgent. More so, @ succeeds with the type of conversational playing that could only be achieved by two masters so deep into their craft that it probably feels a lot like breathing to them by now".

Track listing

All compositions by John Zorn and Thurston Moore

Albums of recorded music were developed in the early 20th century, first as books of individual 78rpm records, then from 1948 as vinyl LP records played at 33 ¹⁄₃ rpm. Vinyl LPs are still issued, though in the 21st century albums sales have mostly focused on compact disc (CD) and MP3 formats. The audio cassette was a format used in the late 1970s through to the 1990s alongside vinyl.

An album may be recorded in a recording studio (fixed or mobile), in a concert venue, at home, in the field, or a mix of places. Recording may take a few hours to several years to complete, usually in several takes with different parts recorded separately, and then brought or "mixed" together. Recordings that are done in one take without overdubbing are termed "live", even when done in a studio. Studios are built to absorb sound, eliminating reverberation, so as to assist in mixing different takes; other locations, such as concert venues and some "live rooms", allow for reverberation, which creates a "live" sound. The majority of studio recordings contain an abundance of editing, sound effects, voice adjustments, etc. With modern recording technology, musicians can be recorded in separate rooms or at separate times while listening to the other parts using headphones; with each part recorded as a separate track.

Slowness (s) is a quantity introduced in Seismology which is the reciprocal of velocity. Thus travel time of a wave is the distance that the wave travels times the slowness of the medium ( in seismology, it refers to different layers of Earth exhibiting different densities) Thus,

Slowness = 1/Velocity

If we divide the path followed by the ray into N segments numbered i = 1, 2 .. N the total travel time of the wave is

Therefore, the residual travel time is due to departures in slowness experienced by the wave along the raypath.

Sonic well logs

Measurements of interval transit time, designated , made during wireline logging are used to determine sonic velocities of the wallrock in boreholes. The tool used has sources and receivers that are in contact with the wellbore and it measures the delay between the source being triggered and the signal being received. The measurements are normally in the units of microseconds per foot and are recorded on the well log.

References

External links