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地下水源热泵定压差取水方式对含水层渗透性的影响

王松庆 张旭

中南大学学报(自然科学版)2011,Vol.42Issue(6):1624-1628,5.
中南大学学报(自然科学版)2011,Vol.42Issue(6):1624-1628,5.

地下水源热泵定压差取水方式对含水层渗透性的影响

Influence of constant pressure difference on aquifer permeability induced by groundwater source heat pump pumping

王松庆 1张旭1

作者信息

  • 1. 同济大学机械工程学院,上海200092
  • 折叠

摘要

Abstract

The mathematic model of aquifer particles migration induced by groundwater source heat pump (GWSHP) pumping was theoretically presented. A case which represents the influence of constant pressure difference on aquifer permeability induced by GWSHP pumping was analysed. The results indicate that the hydraulic conductivity increases by 156,16 and 7 times respectively as aquifer porosity increases 2.57,1.86 and 1.59 times respectively of initial value 20,25 and 30 m in five-year operation of GWSHP for different aquifer thicknesses. Considering particles migration, the permeability of aquifer is affected obviously by GWSHP pumping under constant pressure difference.

关键词

地下水源热泵/定压差/含水层/渗透性

Key words

groundwater source heat pump/ constant pressure difference/ aquifer/ permeability

分类

化学化工

引用本文复制引用

王松庆,张旭..地下水源热泵定压差取水方式对含水层渗透性的影响[J].中南大学学报(自然科学版),2011,42(6):1624-1628,5.

基金项目

国家“十一五”科技支撑计划项目(2006BAJ01B05) (2006BAJ01B05)

中南大学学报(自然科学版)

OA北大核心CSCDCSTPCD

1672-7207

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