Development of relationship between specific storage and depth of sandy and clay formations
Development of relationship between specific storage and depth of sandy and clay formations
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DOI：
10.1007/s00254-001-0481-z
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发表时间：
2002-03
期刊：
影响因子：
--
通讯作者：
V. Shestakov
中科院分区：
文献类型：
--
作者：
V. Shestakov
本研究总结了已发表的数据和现场实验，以验证一个半经验关系的粒状含水岩石的比存储和压缩性参数，其位置深度在数百米的范围内。利用太沙基压缩方程和地应力分布的一个前提条件，得到了比蓄水层与距地表深度的双曲线方程。用该公式计算的比贮量与实测资料比较表明，该公式对砂体的比贮量计算值为6×10- 4 ~ 3×10- 3，典型值为10 - 3，与实测值吻合较好。本研究是与水文地质学的一个分支--水文地质力学相联系的。米罗年科在密切合作中制定和发展。
This study summarizes published data and field experiments to validate a semi-empirical relation of specific storage and compressibility parameters of granular water-bearing rocks to their location depth within the hundreds of meters' range. Using the Terzaghi compression equation and a precondition of geostatic stress distribution a hyperbolic equation relating specific storage aquifer with depth from ground surface is obtained in the form. Comparison of specific storage calculated by the obtained equation with field data shows it to be in good agreement for sands, with the parameterAranging from 6×10–4to 3×10–3and with a typical value of 10–3. This study is associated with hydrogeomechanics, a branch of hydrogeology that the author and V.A. Mironenko have formulated and developed in close collaboration.