| 关门咀子水库坝址区域水文地质特征 |
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| 引用本文： | 范旭东,吕宝顺.关门咀子水库坝址区域水文地质特征[J].黑龙江水专学报,2005,32(3):51-52. |
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| 作者姓名： | 范旭东 吕宝顺 |
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| 作者单位： | 1. 鹤岗市水务局,水资源管理办公室,黑龙江,鹤岗,154101
2. 西泉眼水库管理处,黑龙江,阿城,150300 |
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| 摘 要： | 关门咀子水库坝址地层砂砾组，以砂岩为代表的含水层和以泥页岩为主的相对隔水层构成了多层含水层，坝址下部基岩为辉石安山岩和安山质凝灰角砾岩。库区无明显渗漏区。分析并研究坝址区附近水文地质条件，对于工程建设具有重要意义。
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| 关 键 词： | 孔隙潜水 基岩裂隙水 第四系冲积层 水文地质条件 地下水化学特征 关门咀子水库 |
| 文章编号： | 1000-9833(2005)03-0051-02 |
| 收稿时间： | 03 23 2005 12:00AM |
| 修稿时间： | 2005年3月23日 |
The geological hydrology characteristic of dam region at Guanmenzuizi Reservoir |
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| FAN Xu-dong,LU Bao-shun.The geological hydrology characteristic of dam region at Guanmenzuizi Reservoir[J].Journal of Heilongjiang Hydraulic Engineering College,2005,32(3):51-52. |
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| Authors: | FAN Xu-dong LU Bao-shun |
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| Affiliation: | FAN Xu-dong~1,LU Bao-shun~2 |
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| Abstract: | Dam region strutum of Guanmenzuizi Reservoir is formed of sand gravel, water-bearing layer with sandstone as representative and relative aquitard with mud shale as main composition forms unti-layer waterbearing layer. The summer under dam region is augite andesite and andesite tuff breccia. There is no evident leakage in the reservoir region. Analysing and studing hydrology geological condition of dam region nearby is provided with important meaning for the engineering construction. |
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| Keywords: | void water summer cracking water Quaternary alluvium geological hydrology condition chemistry characterisitic of underground water Guanmenzuizi Reservoir |
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