| 松嫩平原地下水系统循环特征 |
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| 引用本文： | 张玉珊,崔世平,张敏.松嫩平原地下水系统循环特征[J].吉林地质,2014(3):102-104. |
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| 作者姓名： | 张玉珊 崔世平 张敏 |
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| 作者单位： | 吉林省地质调查院,吉林长春,130061 |
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| 摘 要： | 松嫩平原是松辽地下水系统区的一部分,是一个多层叠置的地下水盆地,西部以大兴安岭山地为界,西南部以松辽分水岭为界,东南部以长白山山地为界,北部、东部以吉黑省界为界,是一个相对完整的一级地下水系统。本文主要叙述潜水地下水系统的补给、径流、排泄特征。
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| 关 键 词： | 松嫩平原 地下水系统 循环特征 |
Circulation features of groundwater system in Songnen Plain |
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| ZHANG Yu-shan,CUI Shi-ping,ZHANG Min.Circulation features of groundwater system in Songnen Plain[J].Jilin Geology,2014(3):102-104. |
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| Authors: | ZHANG Yu-shan CUI Shi-ping ZHANG Min |
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| Institution: | ( Institute of Geological Survey of Jilin Province, Changchun 130061, Jilin, China) |
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| Abstract: | Songnen Plain is a part of the Songliao groundwater system district, is a multi-layer overlapping groundwater basin. Greater Khingan Range mountain as the west boundary, Songliao watershed as southwest boundary, southeast boundary is Changbai Mountain land, the north and east bounded by Jilin-Heilongjiang provincial boundaries, which is a relatively complete Class A groundwater system. In this paper, the authors mainly describe the recharge, runoff, discharge features of phreatic groundwater system. |
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| Keywords: | Songnen Plain groundwater system circulation features |
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