...
首页> 外文期刊>Geophysics: Journal of the Society of Exploration Geophysicists >Petrophysical properties of saprolites from the Oak Ridge Integrated Field Research Challenge site, Tennessee
【24h】

Petrophysical properties of saprolites from the Oak Ridge Integrated Field Research Challenge site, Tennessee

机译:田纳西州橡树岭综合田间研究挑战赛站点的腐泥土的岩石物理性质

获取原文
获取原文并翻译 | 示例
           

摘要

At the Oak Ridge Integrated Field Research Challenge site, near Oak Ridge, Tennessee, the shallow saprolitic aquifer is contaminated by nitric acid, uranium, and metals originating from the former S3 settling ponds. To interpret low-frequency geophysical methods used to image contaminant plumes, we have characterized the petrophysical properties of three representative saprolite core samples. Their hydraulic conductivity ranges from 10-~7 to 10-~6 ms-~1 in agreement with field data. Complex conductivity measurements, in the frequency range of 1 mHz to 45 kHz, were performed with NaCl solutions with electrical conductivities in the range 5 × 10-~3 to 2.35 Sm-~1, a range representative of field conditions. The electrical conductivity data were well reproduced with a simple linear conductivity model between the saprolite conductivity and the pore water conductivity. The conductivity plots were used to estimate the formation factor (the cementation exponent was about 2.2 + 0.3) and the surface conductivity (0.007-0.040 Sm-~1). The magnitude of the surface conductivity depended on the degree of weathering and therefore on the amount of smectite and mixed layer (illite-smectite) clays present in the saprolite. The chargeability of the core samples was in the range of 20 to 800 mVV-1 and is strongly dependent on the salinity. We also performed streaming potential measurements with the same pore fluid composition as that used for the complex conductivity measurements. We found an excess of movable electrical charges on the order of 100 to 500 Cm-~3 in agreement with previous investigations connecting the movable excess charge density to permeability. The zeta potential was in the range of-10 to-20mV independent on the salinity. The electrical measurements were consistent with an average cation exchange capacity in the range of 1.4 to 11 cmol kg-~1 and a specific surface area on the order of 4000 to about 30,000 m2 kg-~1.
机译:在田纳西州橡树岭附近的橡树岭综合田间研究挑战赛现场,浅层腐泥土蓄水层被硝酸盐,铀和源自前S3沉淀池的金属污染。为了解释用于对污染物羽流成像的低频地球物理方法,我们表征了三个代表性腐泥土岩心样品的岩石物理性质。与现场数据一致,它们的水力传导率范围从10-〜7到10-〜6 ms-〜1。使用电导率范围为5×10-〜3至2.35 Sm-1的NaCl溶液在1 mHz至45 kHz的频率范围内进行复数电导率测量,该范围代表了现场条件。用腐泥土电导率和孔隙水电导率之间的简单线性电导率模型可以很好地再现电导率数据。电导率图用于估计形成因子(胶结指数约为2.2 + 0.3)和表面电导率(0.007-0.040 Sm-〜1)。表面电导率的大小取决于风化程度,并因此取决于腐泥土中存在的蒙脱石和混合层(伊利石-蒙脱石)粘土的量。核心样品的可充电性在20到800 mVV-1的范围内,并且强烈依赖于盐度。我们还使用与复杂电导率测量相同的孔隙流体成分进行了流电势测量。我们发现与先前将可移动的过量电荷密度与磁导率相关的研究相一致,可移动的电荷过量在100至500 Cm-〜3的数量级。与盐度无关,ζ电势在-10至-20mV的范围内。电学测量与在1.4至11cmol kg-1的范围内的平均阳离子交换容量和在4000至约30,000m2 kg-1的范围内的比表面积一致。

著录项

相似文献

  • 外文文献
  • 中文文献
  • 专利
获取原文

客服邮箱:kefu@zhangqiaokeyan.com

京公网安备:11010802029741号 ICP备案号:京ICP备15016152号-6 六维联合信息科技 (北京) 有限公司©版权所有
  • 客服微信

  • 服务号