| 三江平原建三江地下水激发补给初步分析 |
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| 引用本文： | 姚章村,安瑞强,董经财,马艳. 三江平原建三江地下水激发补给初步分析[J]. 黑龙江水专学报, 2001, 28(3): 20-23 |
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| 作者姓名： | 姚章村 安瑞强 董经财 马艳 |
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| 作者单位： | 1. 黑龙江农垦勘测设计研究院
2. 建三江农垦分局水利局 |
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| 基金项目： | 三江平原“九五”期间国家重点科技攻关项目（96－004－02－03－01）。 |
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| 摘 要： | 三江平原建三江地区有巨厚的地下水含水层。地表大部分覆盖着平均约10m厚的亚粘土，且地势平缓。形成本地区垂直补给困难，侧向补给缓慢，但是具有优越激发补给的自然社会条件，开采降深15m，每年可获得大量激发补给（江河为主），占开采资源量的80％。
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| 关 键 词： | 亚粘土层 含水层 开采降深 激发补给 地下水 建三江地区 三江平原 |
| 文章编号： | 1000-9833(2001)03-0020-04 |
| 修稿时间： | 2001-04-25 |
Preliminary studies on underground water resources stimulated supplement in Jiansanjiang Region of Sanjiang Plain |
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| YAO Zhang-cun,AN Rui-qiang,DONG Jing-cai,MA Yan. Preliminary studies on underground water resources stimulated supplement in Jiansanjiang Region of Sanjiang Plain[J]. Journal of Heilongjiang Hydraulic Engineering College, 2001, 28(3): 20-23 |
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| Authors: | YAO Zhang-cun AN Rui-qiang DONG Jing-cai MA Yan |
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| Abstract: | The Jiansangjiang Region of Sanjiang Plain owns huge and thick containing underground water layer. Although most of the earth surface, on an average, holds about 10 meters thickness sub-clay layer, and the topography is gentle, which makes it difficult for this region undergroud water to compensate vertically and slow for it to do from side, this region owns favorable natural conditions, when the underground water drops 15 meters depth, which can attain an average several billions cubic meters water resources compensation by stimulated rivers year after year, the stimulated compensation occupies 80% of the extracted undergroud water resources. |
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| Keywords: | sub-clay layer containing water layer dropping depth to extract stimulated rivers' compensating extraction and compensation balance |
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