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基于多孔非稳定抽水试验的缓倾层状含水层各向异性渗透参数计算

江冰 唐一格 夏强 许模

成都理工大学学报(自然科学版)2017,Vol.44Issue(6):756-761,6.
成都理工大学学报(自然科学版)2017,Vol.44Issue(6):756-761,6.DOI:10.3969/j.issn.1671-9727.2017.06.13

基于多孔非稳定抽水试验的缓倾层状含水层各向异性渗透参数计算

Calculation of anisotropic permeability parameters of flat pitch aquifer based on multiple-well unsteady pumping test

江冰 1唐一格 2夏强 1许模1

作者信息

  • 1. 地质灾害防治与地质环境保护国家重点实验室(成都理工大学),成都610059
  • 2. 重庆诚德岩土工程勘察有限公司,重庆401147
  • 折叠

摘要

Abstract

The parameters of anisotropy of hydrogeology can be obtained through drawdown-time relationship of multiple-well pumping test.In this paper,the multiple-well unsteady pumping test data are used to calculate the main direction and specific value of permeability tensor by Matlab incorporating with non-axial anisotropic permeability tensor theory.The final result which is consistent with the actual drawdown condition is obtained after contrastive analysis from two separate test results,with the main direction range of [8°,18°],and the Ky/Kx range of [7.5,13].The calculation method proves to be feasible and rational for the non-axial anisotropic permeability tensor theory.It points out that the key parameter to calculate anisotropic permeability parameters is the intercept of s-lnt curve.

关键词

抽水试验/层状含水层/各向异性/渗透系数张量

Key words

pumping test/layered aquifer/anisotropy/permeability tensor

分类

天文与地球科学

引用本文复制引用

江冰,唐一格,夏强,许模..基于多孔非稳定抽水试验的缓倾层状含水层各向异性渗透参数计算[J].成都理工大学学报(自然科学版),2017,44(6):756-761,6.

基金项目

国家自然科学基金青年基金项目(41502237). (41502237)

成都理工大学学报(自然科学版)

OA北大核心CSCDCSTPCD

1671-9727

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