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黑河中游典型灌区地下水位的动态变化
引用本文:陈军锋,郜银梁,闫云霞,张成才.黑河中游典型灌区地下水位的动态变化[J].水资源与水工程学报,2012,23(1):59-63.
作者姓名:陈军锋  郜银梁  闫云霞  张成才
作者单位:1. 中国科学院地理科学与资源研究所陆地水循环及地表过程重点实验室,北京,100101
2. 郑州大学水利与环境学院,郑州,450002
基金项目:国家重点基础研究发展计划(973)项目(2009CB421305)资助
摘    要:基于黑河沿岸地下水位观测井近20年实测观测资料,运用Mann-Kendall方法进行年地下水埋深序列的趋势分析,并选取代表观测井分析不同区域在不同时期内的年际与年内变化。结果表明:研究区地下水位埋深整体为增大趋势,区域地下水位下降趋势明显。年内的季节分配表明,从20世纪80年代至今,地下水位变化由水文-灌溉型逐步向开采型转变,其中平川区开采作用最为明显,集中表现在2000年之后,分水是导致这一时期地下水位下降的主要因素。

关 键 词:地下水位  Mann-Kendall趋势分析  季节变化  黑河中游
收稿时间:2011/2/24 0:00:00
修稿时间:2011/5/13 0:00:00

Dynamic change of groundwater level in typical irrigated area of Heihe River middle reach
CHEN Junfeng,GAO Yinliang,YAN Yunxia and ZHANG Chengcai.Dynamic change of groundwater level in typical irrigated area of Heihe River middle reach[J].Journal of water resources and water engineering,2012,23(1):59-63.
Authors:CHEN Junfeng  GAO Yinliang  YAN Yunxia and ZHANG Chengcai
Affiliation:1.Key Laboratory of Water Cycle and Related Land Surface Processes,Institute of Geographic Sciences and Natural Resources Research,CAS,Beijing,100101,China; 2.School of Water Conservancy and Environment,Zhengzhou University,Zhengzhou 450002,China)
Abstract:Based on the observed data of groundwater monitoring wells during the past 20 years,using the method of Mann-Kendall to carry out trend analysis for the groundwater depth series,and selected the typical observed wells to analyze the change in year and years for different area and different periods.The results showed that: the regional groundwater level was evidently declining.From the 1980s to now,the type of dynamic change of groundwater level was gradually transformed from the hydrology-irrigation type to the exploitation type.The exploitation was enhanced.The most obuious area was Pingchuan Zone,especially after 2000.Water delivery to downstream was the main factor leading to the groundwater table decline.
Keywords:groundwater level  Mann-Kendall trend analysis  seasonal change  Heihe River middle reach
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