华北平原浅层地下水水位动态变化

doi:10.11821/xb200805002

地理学报 ›› 2008, Vol. 63 ›› Issue (5): 462-472.doi: 10.11821/xb200805002

华北平原浅层地下水水位动态变化

王仕琴¹, 宋献方¹, 王勤学², 肖国强³, 刘昌明^1,4

1. 中国科学院地理科学与资源研究所陆地水循环与地表过程重点实验室, 北京100101;
2. 日本国立环境研究所, 筑波305-8506;
3. 天津地质矿产研究所, 天津300170;
4. 北京师范大学水科学研究院水沙科学教育部重点实验室, 北京100875

收稿日期:2007-07-19 修回日期:2008-02-20 出版日期:2008-05-26 发布日期:2008-05-26
通讯作者: 宋献方, 研究员, E-mail:songxf@igsnrr.ac.cn
作者简介:王仕琴(1981-), 博士生, 中国地理学会会员, 主要从事水文水资源、流域水循环研究。 E-mail: wangsq.06b@igsnrr.ac.cn
基金资助:
国家自然科学基金项目(40671034)

Dynamic Features of Shallow Groundwater in North China Plain

WANG Shiqin¹, SONG Xianfang¹, WANG Qinxue², XIAO Guoqiang LIU Changming³

1. Institute of Geographic Sciences and Natural Resources Research, CAS, Beijing 100101, China;
2. National Institute for Environmental Studies, Tsukuba 305-8506, Japan;
3. Tianjin Institute of Geology and Mineral Resources, Tianjin 300170, China;
4. Key Laboratory of Water and Sediment Science, MOE, Water Science College, Beijing Normal University, Beijing 100875, China

Received:2007-07-19 Revised:2008-02-20 Online:2008-05-26 Published:2008-05-26
Supported by:
National Natural Science Foundation of China, No.40671034

摘要/Abstract

摘要：

利用中日合作项目在华北平原设置的自动监测设备KADEC-MIZU II 型地下水水位自计仪, 对2004-2006 年39 处浅层地下水水位监测的结果, 结合区域影响地下水宏观动态类型的主要因素,如地形地貌、地下水埋深、地下水开采程度、地下水漏斗以及河流湖泊等, 叠加各影响因素分区图得到地下水动态影响因素综合分区图, 结合观测孔地下水水位体现的动态特征, 将华北平原地下水观测点分为山前开采型、山前侧向补给- 径流- 开采型、中部河道带补给- 开采型、中部地下水浅埋区降水入渗- 蒸发型动态、黄河影响带侧向补给- 蒸发型动态和滨海平原区入渗- 蒸发型6 大地下水动态类型。在此基础上阐明了大区域范围内不同类型地下水水位年内及多年动态变化的特点, 比较了不同类型区地下水动态所受影响因素的不同。

关键词: 华北平原, 浅层地下水, 地下水动态分区

Abstract:

The groundwater level of 39 unconfined observation wells from 2004 to 2006 in North China Plain (NCP) was monitored using automatic groundwater monitoring data loggers KADEC-MIZU II of Japan. The automatic groundwater sensors were installed for the corporation project between China and Japan. Combined with the monitoring results from 2004 to 2006 with the major factors affecting the dynamic patterns of groundwater, such as relief, depth of groundwater level, discharge extent and rivers, the dynamic regions of NCP groundwater were compiled. According to the dynamic features of groundwater in NCP, six dynamic patterns of groundwater level were identified, including discharge pattern in the piedmont plain, lateral recharge-runoff-discharge pattern in the piedmont plain, rechargedischarge pattern in the middle channel zone, precipitation infiltration-evaporation pattern in the shallow groundwater region of the central plain, lateral recharge-evaporation pattern in the recharge-affected area along the Yellow River, and infiltration-discharge-evaporation pattern in the littoral plain. Based on this, various dynamic patterns features of groundwater were interpreted and different factors of different dynamic patterns were compared.

Key words: North China Plain, shallow groundwater, dynamic region of groundwater

王仕琴, 宋献方, 王勤学, 肖国强, 刘昌明. 华北平原浅层地下水水位动态变化[J]. 地理学报, 2008, 63(5): 462-472.

WANG Shiqin, SONG Xianfang, WANG Qinxue, XIAO Guoqiang LIU Changming. Dynamic Features of Shallow Groundwater in North China Plain[J]. Acta Geographica Sinica, 2008, 63(5): 462-472.

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华北平原浅层地下水水位动态变化

Dynamic Features of Shallow Groundwater in North China Plain

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