[1]申豪勇,梁永平,唐春雷,等.应用氯量平衡法估算娘子关泉域典型岩溶区的降水入渗系数[J].水文地质工程地质,2018,45(06):31.[doi:10.16030/j.cnki.issn.1000-3665.2018.06.05]
 SHEN Haoyong,LIANG Yongping,TANG Chunlei,et al.Estimation of the infiltration coefficient based on chloride mass balance in a typical karst region of the Niangziguan spring area[J].Hydrogeology & Engineering Geology,2018,45(06):31.[doi:10.16030/j.cnki.issn.1000-3665.2018.06.05]
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应用氯量平衡法估算娘子关泉域典型岩溶区的降水入渗系数()
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《水文地质工程地质》[ISSN:1000-3665/CN:11-2202/P]

卷:
45卷
期数:
2018年06期
页码:
31
栏目:
出版日期:
2018-11-15

文章信息/Info

Title:
Estimation of the infiltration coefficient based on chloride mass balance in a typical karst region of the Niangziguan spring area
文章编号:
1000-3665(2018)06-0031-05
作者:
申豪勇梁永平唐春雷赵春红王志恒
中国地质科学院岩溶地质研究所/自然资源部广西壮族自治区岩溶动力学重点实验室,广西 桂林541004
Author(s):
SHEN Haoyong LIANG Yongping TANG Chunlei ZHAO Chunhong WANG Zhiheng
Institute of Karst Geology, CAGS/Karst Dynamics Laboratory, MNR&GZAR, Guilin, Guangxi541004, China
关键词:
地下水补给氯量平衡法降水入渗系数娘子关泉域
Keywords:
groundwater recharge chloride mass balance infiltration coefficient of precipitation Niangziguan Spring
分类号:
P641.134
DOI:
10.16030/j.cnki.issn.1000-3665.2018.06.05
文献标志码:
A
摘要:
娘子关泉作为北方著名的岩溶大泉,研究程度较高,降水入渗补给作为泉域内岩溶地下水的主要补给来源,开展降水入渗系数的研究对于评价岩溶地下水资源量、分析娘子关泉水流量的变化具有重要意义。氯量平衡法利用氯离子质量守恒的原理直接估算降水入渗系数,该方法简便、有效,在国内外很多地区都进行了应用。通过在娘子关泉域内碳酸盐岩裸露区和覆盖区分别选择典型区,运用该方法分别估算了裸露区中等岩溶发育区和覆盖区的降水入渗系数,得到的结果分别为0.21和0.11,取得的结果与该地区已有的成果基本吻合,为该地区降水入渗系数的准确估算提供了新的方法,同时也为氯量平衡法在同类型地区的应用提供了借鉴。
Abstract:
As one of the famous karst springs in northern China, the Niangziguan Spring was much examined. Infiltration of precipitation is the main recharge source of the karst groundwater. Research on the infiltration coefficient of precipitation is of important significance for the karst groundwater resource evaluation and spring flow analyses. The major achievements of the infiltration coefficient of precipitation are based on the water balance method in the karst groundwater system. The precipitation recharge is given through the water-budget equation, and the results will decrease with the increasing karst groundwater system. This method can cause errors because of the uncertainty of the karst groundwater system. Chloride mass balance (CMB) is a simple and valid estimation method of recharge from precipitation, and it has widely been used at home and abroad. In the Niangziguan karst spring area, two typical karst regions were separately selected in the outcropping areas of the carbonates and the covered carbonate areas. The CMB were adopted to estimate the vertical infiltration coefficient at these two regions, and the results are 0.21 at outcropping carbonate area and 0.11 at covered carbonate area. The results are in a good agreement with the data from the predecessors. This paper contributes to promote the applications and developments of the CMB method in karst areas in northern China.

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备注/Memo

备注/Memo:
收稿日期: 2018-05-09; 修订日期: 2018-07-01
基金项目: 国家重点研发计划(2017YFC0406104);国家自然科学基金项目(41672253);中国地质调查局调查项目(DD20189807;DD20160242)
第一作者: 申豪勇(1988-),男,研究实习员,主要从事岩溶水文地质研究。E-mail: shenhaoyong@karst.ac.cn
通讯作者: 梁永平(1962-),男,研究员,硕士生导师,主要从事中国北方岩溶地下水的调查与研究工作。E-mail:lyp0261@karst.ac.cn
更新日期/Last Update: 2018-11-15