Analysis on the hydrogeology characteristics and exploitation potential of the emergency karst water source field in Xishan region, Beijing
-
摘要: 应急水源地位于北京西山四季青地区,取水层位为奥陶系含水层,属覆盖型水源地。奥陶系岩溶地下水水量大、水质优良,是保障北京供水安全的后备水源。本文在综合分析奥陶系岩溶地下水水文地质特征基础上,以群孔抽水试验为基础,采用相关分析法预测水位,从岩溶地下水的富水性、地下水流场、地下水资源方面分析岩溶水的开采潜力,确保在出现水源危机时,岩溶地下水能够作为后备水源地为城市供水。结果表明,岩溶地下水应急水源地岩溶裂隙发育,补给条件好,地下水径流强度大,水质优良,具有6万m3/d的开采潜力,即当水源地增加每日6万m3应急开采时,水位埋深预测值为52.94m,能够满足现有取水设备条件,且不会影响其它水源井的运行。Abstract: Emergency groundwater source field locates in Sijiqing region, which is a covered karst water source field; the water intaking horizon is the Ordovician aquifer. Ordovician karst water is back-up water resource of Beijing city for safe water supply with good water yield property and excellent water quality. Based on comprehensive analysis on the Ordovician karst groundwater hydrogeologic characteristics and pumping test data, groundwater table is predicted with correlation analysis method in this paper. Exploitation potential of karst groundwater is analyzed in view of water-bearing capacity and groundwater flow field as well as groundwater resources to ensure the groundwater can be used as back-up water source for city water supply in the event of water crisis. The results indicate that, karst groundwater system is characterized by developed karst fissure, good recharge condition and good water quality, great groundwater flow intensity. The emergency karst groundwater source field has a 60 000 m3/d of the exploitation potentiality. When water source field increase emergency extraction of 60 000 m3/d, the predicted groundwater depth is 52.94m, which can met the demand of existing water facilities and does not affect the other wells’ normal running.
-
Key words:
- karst water /
- emergency water source /
- correlation analysis /
- pumping test /
- exploitation potential /
- Xishan in Beijing
-
[1] 中国科学院地质研究所岩溶研究组.中国岩溶研究[M].北京:科学出版社,1979:1-3. [2] 刘启仁,张凤岐,秦毅苏,等.中国北方岩溶水资源的形成、分布与合理开发利用[J].水文地质工程地质,1992,(4):41-44. [3] 北京市地质矿产局.北京市区域地质志[M].北京:地质出版社,1991:51-90. [4] 鲍亦冈,刘振锋,王世发,等.北京市岩石地层[M].北京:中国地质大学出版社,1996:37-97. [5] 张吉顺,善文琅.北京西山地质研究[M]武汉:中国地质大学出版社1990:78-125. [6] 张大纯,张人权,史毅虹,等.水文地质学基础[M].北京:地质出版社,1995:70-88. [7] 杨成田.专门水文地质学[M].北京:地质出版社,1981:195-241. [8] 钱家忠,吴建中,朱学愚,等.徐州市张集水源地裂隙岩溶水群孔抽水试验研究[J].水科学进展,2003,14(05):598-601. [9] 殷昌平,孙庭芳,金良玉,等.地下水水源地勘查与评价[M].北京:地质出版社,1993:202-234. [10] 赵广利,赵正明.渭北中部岩溶水赋存规律及开发潜力研究[C]煤田地质与可持续发展研究论文集,2003:78-82. [11] 第一机械工业部勘测公司,第二机械工业部第四设计研究院勘察大队,第二机械工业部地质四队,等.供水水文地质手册(第三册)[M].北京:地质出版社,1990:37-145. -

计量
- 文章访问数: 5111
- HTML浏览量: 738
- PDF下载量: 2612
- 被引次数: 0