Measurement of the Biot Structural Factor δ: for Sintered Bronze Spheres

S. R. Bakert, I. Rudnick
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引用次数: 2

Abstract

We have extracted the Biot structural factor 6 [11 for three samples of sintered bronze spheres (nom. dia. 7511, 11011, 50011, porosity 0.4 to 0.5) from measurements of the speed and attenuation of first and second sound in superfluid helium contained in these samples. We find 1 to lie in the range 3.3 to 4.5, about 1+ to 2 times larger than Stoll has estimated for typical marine sediments 121 (we take 6 to be defined by x=6 (awk/vP)', where is the argument of Biot's universal correction function F(K), a is the tortuosity, is the angular frequency, k is the permeability, v is the kinematic viscosity, and P is the porosity). If 6 is the normalfluid viscous p&&ration depth and a is a characteristic pore size, the range of /a covered by these measurements is ximately 0.01 to 1.
烧结青铜球生物结构因子δ:的测定
我们提取了3个烧结青铜球样品的Biot结构因子6[11]。7511,11011,50011,孔隙度0.4至0.5),通过测量这些样品中所含超流氦的第一声和第二声的速度和衰减。我们发现1在3.3到4.5的范围内,大约是Stoll对典型海洋沉积物121的估计的1+到2倍(我们取6定义为x=6 (awk/vP)',其中是Biot通用校正函数F(K)的参数,a是扭曲度,是角频率,K是渗透率,v是运动粘度,P是孔隙度)。如果6是正常流体粘性井深,a是特征孔径,则这些测量所涵盖的/a范围接近0.01至1。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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