• Included in CSCD
  • Chinese Core Journals
  • Included in WJCI Report
  • Included in Scopus, CA, DOAJ, EBSCO, JST
  • The Key Magazine of China Technology
Volume 36 Issue 4
Aug.  2017
Turn off MathJax
Article Contents
YI Lianxing, XIA Riyuan, WANG Zhe, LU Haiping, ZHAO Liangjie. Infiltration coefficient of precipitation in karst peak-cluster depression area:A case study of Zhaidi karst underground river basin[J]. CARSOLOGICA SINICA, 2017, 36(4): 512-517. doi: 10.11932/karst20170412
Citation: YI Lianxing, XIA Riyuan, WANG Zhe, LU Haiping, ZHAO Liangjie. Infiltration coefficient of precipitation in karst peak-cluster depression area:A case study of Zhaidi karst underground river basin[J]. CARSOLOGICA SINICA, 2017, 36(4): 512-517. doi: 10.11932/karst20170412

Infiltration coefficient of precipitation in karst peak-cluster depression area:A case study of Zhaidi karst underground river basin

doi: 10.11932/karst20170412
  • Publish Date: 2017-08-25
  • The precipitation infiltration coefficient α and groundwater runoff modulus M are the most basic hydrogeological parameters.In this paper,based on the high frequency monitoring data of water level, flow, precipitation of Zhaidi karst underground river basin in a hydrological year from March 2013 to February 2014,the precipitation infiltration coefficients for dry season, normal season and rainy season have been computed by means of water balance method,which are 0.352, 0.528, 0.726,respectively, and the average infiltration coefficient is 0.635. The groundwater runoff modulus are 8.32,19.80,61.15 L·s-1·km-2, respectively for the above three seasons, and the average annual runoff modulus is about 33.36 L·s-1·km-2. The calculation method and values of precipitation infiltration coefficient and groundwater runoff modulus have certain reference significance in water resources evaluation for the same karst area.

     

  • loading
  • [1]
    庞莹,张晓红.地下水资源评价中降水入渗系数的分析确定[J].吉林水利,2006,(S1):8-9.
    [2]
    王绍强.对降水入渗系数影响因素的探讨及潜水区域均衡计算法[J].勘察科学技术, 1988,(1):29-34.
    [3]
    李景阳,籍传茂,鄢贵权,等.贵州独山南部岩溶地下水系特征及水资源评价(英文)[J].中国岩溶, 1999,18(3):39-49.
    [4]
    杜毓超,李兆林,韩行瑞,等.沪蓉高速公路乌池坝隧道区岩溶发育特征及其涌水分析[J].中国岩溶,2008,27(1):11-18.
    [5]
    张江华,陈国亮.水均衡法预测岩溶区坑道涌水量的一些见解[J].中国岩溶,1988,7(3):103-108.
    [6]
    陈宏峰,夏日元,梁彬.鄂西齐岳山地区岩溶发育特征及其对隧道涌水的影响[J].中国岩溶, 2003,22(4):33-37.
    [7]
    蒋忠诚,覃小群,曹建华,等.中国岩溶作用产生的大气CO2碳汇的分区计算[J].中国岩溶, 2011,30(4):363-367.
    [8]
    陈引锋,王爱玲.利用钻孔资料确定降雨入渗系数[J].地下水,2008,30(1):37-39.
    [9]
    李庆朝. 用地下水动态资料求降水入渗系数问题的探讨[J]. 聊城师院学报(自然科学版),1996, 9(4):78-80.
    [10]
    丁淑芹. 小流域降水入渗系数的推求方法[J].水土保持科技情报,2000,(1):28.
    [11]
    高殿琪,颜景生. 利用水均衡法求算明水岩溶区降水入渗系数[J]. 山东地质,1991,7(2):107-113.
    [12]
    韩巍,何庚义. 用小流域、泉域水均衡法确定基岩山区降水入渗系数[J]. 长春地质学院学报,1985,(4):79-84.
    [13]
    钟进,董毓,丁坚平. 贵州福泉市双眼井泉小流域流量估算及排洪方案建议[J].中国岩溶,2011, 30(3):291-294.
    [14]
    梁虹,王剑.喀斯特地区流域岩性差异与洪、枯水特征值相关分析:以贵州河流为例[J]. 中国岩溶,1998, 17(1):69-75.
    [15]
    程学丰,刘登宪. 利用矿区灰岩疏(放)水资料计算降水入渗系数[J].淮南矿业学院学报,1994, 14(4):1-5.
    [16]
    王凤生,李桂芬.应用同位素氚计算降水入渗系数的探讨[J].地下水,1990,12(2):70-72.
    [17]
    龚自珍,付利群.辛安村泉域水文地质计算中环境同位素方法的应用[J].中国岩溶,1994,13(3):306-313.
  • 加载中

Catalog

    通讯作者: 陈斌, bchen63@163.com
    • 1. 

      沈阳化工大学材料科学与工程学院 沈阳 110142

    1. 本站搜索
    2. 百度学术搜索
    3. 万方数据库搜索
    4. CNKI搜索

    Article Metrics

    Article views (1496) PDF downloads(910) Cited by()
    Proportional views
    Related

    /

    DownLoad:  Full-Size Img  PowerPoint
    Return
    Return