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安徽淮河流域平原区地下水水温分布特征

杨佩明 杨则东 焦团理

安徽地质Issue(2):136-138,3.
安徽地质Issue(2):136-138,3.

安徽淮河流域平原区地下水水温分布特征

Groundwater temperature distribution features for the plains in the Huai River basin, Anhui

杨佩明 1杨则东 1焦团理1

作者信息

  • 1. 安徽省地质调查院, 安徽 合肥 230001
  • 折叠

摘要

Abstract

  This paper introduced the Quaternary geology and hydrogeology of the plains in the Huai River basin, Anhui. Based on analysis of spatial distribution features of sampled 1362 sets of groundwater temperature data, it is suggested that the groundwater temperature is higher in west and lower in east, and the potential surface source geothermal re-sources lie in the areas as Mengcheng, Fengtai-Shouxian-Changfeng, Jieshou-Bozhou and Dandangshan.

关键词

淮河流域/平原/地下水/水温/地热/安徽

Key words

plain/groundwater/water temperature/geotherm/the Huai River basin/Anhui

分类

天文与地球科学

引用本文复制引用

杨佩明,杨则东,焦团理..安徽淮河流域平原区地下水水温分布特征[J].安徽地质,2012,(2):136-138,3.

安徽地质

1005-6157

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