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重庆温泉及地下热水的分布及成因

拓明明 周训 郭娟 王昕昀 王源 徐中平

水文地质工程地质2018,Vol.45Issue(1):165-172,8.
水文地质工程地质2018,Vol.45Issue(1):165-172,8.DOI:10.16030/j.cnki.issn.1000-3665.2018.01.24

重庆温泉及地下热水的分布及成因

Occurrence and formation of the hot springs and thermal groundwater in Chongqing

拓明明 1周训 1郭娟 2王昕昀 1王源 1徐中平1

作者信息

  • 1. 中国地质大学(北京)水资源与环境学院,北京 100083
  • 2. 中国地质大学(北京)地下水循环与环境演化教育部重点实验室,北京 100083
  • 折叠

摘要

Abstract

Thermal groundwater resources in Chongqing are relatively abundant and the occurrence of the geothermal water is unique.In this paper,the occurrence,hydrochemical features,geothermal reservoir structure,formation conditions and genetic modes of the thermal groundwater in Chongqing are described.The geothermal reservoirs consist of the Lower and Middle Triassic carbonates.The occurrence ofthermal groundwater in Chongqing is controlled by anticlines and is different from that of the common fault-deep circulation controlled by faults.The hot springs mainly exist in the axis,the two flanks and the plunging end of the anticlines.The type of geothermal water occurrence is of the basin-outcropping type.The temperature of the hot water ranges from 32 ℃ to 64 ℃ and the hot springs are of middle-to-low temperature water.Affected by the anticline structures,incongruent dissolution of the carbonates of the Lower Triassic Jialingjiang and Middle Triassic Leikoupo Groups occur.The TDS of the geothermal water are 2-3 g/L and hydrochemical types are mainly of SO4-Ca type.The hot water tends to be fresh owing to the long-term incongruent dissolution of the carbonates,but has not yet reached the freshwater stage.The geothermal water receives heat from the normal heat flow and is of meteoric origin.Groundwater receives recharge from precipitation in the recharge areas (i.e.,the outcropping areas of the carbonates in the cores of the anticlines with elevation of approximately 670-1 500 m),flows along the carbonates in two flanks of the anticlines to the deep parts.After heated,the hot water flows along the anticlines from both north and south to the middle parts of the cores or to the plunging ends of the anticlines and issues in the form of the hot springs.Geothermal wells and tunnels also reveal hot water in the two flanks of the anticlines.

关键词

温泉/地下热水/背斜/水化学/成因

Key words

hot spring/thermal groundwater/anticline/hydrochemistry/formation

分类

天文与地球科学

引用本文复制引用

拓明明,周训,郭娟,王昕昀,王源,徐中平..重庆温泉及地下热水的分布及成因[J].水文地质工程地质,2018,45(1):165-172,8.

基金项目

国家自然科学基金项目(41572223) (41572223)

中央高校基本科研业务费专项资金资助项目(2652016098) (2652016098)

国家重点基础研究发展计划(973)项目(2011CB403005) (973)

水文地质工程地质

OA北大核心CSCDCSTPCD

1000-3665

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