Definitions and Laboratory Techniques of Compressional Sound Velocity Parameters and Wet-Water Content, Wet-Bulk Density, and Porosity Parameters by Gravimetric and Gamma Ray Attenuation Techniques
Definitions and Laboratory Techniques of Compressional Sound Velocity Parameters and Wet-Water Content, Wet-Bulk Density, and Porosity Parameters by Gravimetric and Gamma Ray Attenuation Techniques
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压缩声速参数和湿含水量、湿体积密度和孔隙率参数的定义和实验室技术(通过重力和伽马射线衰减技术)
DOI:
10.2973/dsdp.proc.33.app1.1976
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发表时间:
1976
期刊:
影响因子:
--
通讯作者:
R. Boyce
中科院分区:
文献类型:
--
作者:
R. Boyce
On Leg 33 of the Deep Sea Drilling Project the following physical properties were all measured on the same "undisturbed" samples: sound velocity, wet-bulk density (ratio of the weight of wet-saturated sediment to its volume, g/cc), and wet-water content (ratio of the weight of sea water in the sediment to the weight of the wet-saturated sediment, expressed as percent). These parameters allowed calculation of seismic impedance, seismic reflection coefficients, and porosity (ratio of the volume of water in the sediment to the volume of the wet-saturated sediment, expressed as percent). Where possible, velocities were measured parallel and perpendicular to bedding planes, which allowed the acoustic anisotropy to be calculated. In addition to the above individual sampling, the wetbulk density was also determined continuously using the Gamma Ray Attenuation Porosity Evaluator (GRAPE) (Evans, 1965). From this wet-bulk density analog data, porosity can be estimated using the nomogram in the core plots by using assumed or estimated grain density values. The GRAPE device can also be run in a static 2minute counting mode for individual samples (GRAPE Special 2-Minute Count) in addition to the continuous 2-second counting mode. Techniques for sound velocity, wet-water content, and the GRAPE device are discussed in this paper, followed by a discussion of the Leg 33 physical properties presentation.