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Record #88932:

Field studies on stress waves in natural snow cover / Robert L. Brown, Andrew Hansen.

Title: Field studies on stress waves in natural snow cover / Robert L. Brown, Andrew Hansen.
Author(s): Brown, Robert L.
Hansen, Andrew.
Date: 1987.
Publisher: Ottawa: National Research Council Canada. Associate Committee on Geotechnical Research
In: National Research Council of Canada. Associate Committee on Geotechnical Research. Technical Memorandum. (1987.), Vol. 140 (1987)
Abstract: Explosives (0.115 to 0.45 kg) were used to generate stress waves. Pressure waves were recorded by array of semiconductor strain-gauge pressure transducers. Results indicate that pore pressures are not negligible and may be responsible for significant part of stress wave attenuation. Stress wave loses high frequency content quickly, but wave impulse, which is time integral of wave pressure, remained nearly constant as it propagated through distance of 5 cm between two large transducers.
Notes:

National Research Council of Canada. Associate Committee on Geotechnical Research. Technical Memorandum. Vol. 140 :89-110 (1987).

Keywords: 551.321.7 -- Snow cover, measurement of properties.
551.578.46 -- Snow cover and snow patches.
534.2 -- Acoustics in ice.
E3 -- Glaciology: instruments and methods.
SPRI record no.: 88932

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100 1# ‡aBrown, Robert L.
245 10 ‡aField studies on stress waves in natural snow cover /‡cRobert L. Brown, Andrew Hansen.
260 ## ‡aOttawa :‡bNational Research Council Canada. Associate Committee on Geotechnical Research,‡c1987.
300 ## ‡ap. 89-110 :‡bdiags.
500 ## ‡aNational Research Council of Canada. Associate Committee on Geotechnical Research. Technical Memorandum. Vol. 140 :89-110 (1987).
520 3# ‡aExplosives (0.115 to 0.45 kg) were used to generate stress waves. Pressure waves were recorded by array of semiconductor strain-gauge pressure transducers. Results indicate that pore pressures are not negligible and may be responsible for significant part of stress wave attenuation. Stress wave loses high frequency content quickly, but wave impulse, which is time integral of wave pressure, remained nearly constant as it propagated through distance of 5 cm between two large transducers.
650 07 ‡a551.321.7 -- Snow cover, measurement of properties.‡2udc
650 07 ‡a551.578.46 -- Snow cover and snow patches.‡2udc
650 07 ‡a534.2 -- Acoustics in ice.‡2udc
650 07 ‡aE3 -- Glaciology: instruments and methods.‡2local
700 1# ‡aHansen, Andrew.
773 0# ‡7nnas ‡tNational Research Council of Canada. Associate Committee on Geotechnical Research. Technical Memorandum. ‡gVol. 140 (1987) ‡wSPRI-41342
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