| 三江平原典型地下水动态曲线诠释 |
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| 引用本文： | 姚丽娟. 三江平原典型地下水动态曲线诠释[J]. 水利科技与经济, 2008, 14(5): 379-381 |
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| 作者姓名： | 姚丽娟 |
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| 作者单位： | 黑龙江农垦勘测设计研究院,黑龙江,佳木斯,154002 |
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| 摘 要： | 一个农场（地区）只要通过一条或几条地下水动态曲线分析，就可以掌握农场地下水开发是否合理，水资源开发是否可持续及开发利用中应该注意的事项，说明对地下水位长期观测及资料积累与整理分析的重要性与必要性。
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| 关 键 词： | 地下水位 地下水埋深 采补平衡 开采下降 补给上升 排泄下降 可持续利用 |
| 文章编号： | 1006-7175(2008)05-0379-03 |
| 修稿时间： | 2007-09-26 |
Explanation about the Typical Groundwater Dynamic Curve of Sanjiang Plain |
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| YAO Li-juan. Explanation about the Typical Groundwater Dynamic Curve of Sanjiang Plain[J]. Water Conservancy Science and Technology and Economy, 2008, 14(5): 379-381 |
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| Authors: | YAO Li-juan |
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| Affiliation: | YAO Li - juan (Heilongjiang Reclamation Investigation Design and Research Institute, Jiamusi 154002, Heilongjiang, China) |
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| Abstract: | For a farm, whether the development of groundwater is reasonable or not, whether the development of water resource is sustainable or not and the items that should be taken notice of during developing process can be mastered only by analyzing one or several groundwater dynamic curves, which expresses the importance and necessity of the long - term watching and data＇ s accumtdation, sorting and analysis. |
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| Keywords: | groundwater table buried depth balance of mining and recharging falling caused by mining rising caused by recharging falling caused by drainage sustainable utilization |
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