China Geological Survey Chinese Academy of Geological SciencesHost
科学出版社Publish
Advanced Search
Previous Article Next Article
2017 Vol. 44, No. 5
Article Contents
Article navigation > Geology in China > 2017 > 44(5): 913-923
Next Article Previous Article

SUN Fangqiang, YIN Lihe, WANG Xiaoyong, MA Hongyun, ZHANG Jun, DONG Jiaqiu, HE Shuaijun. 2017. Determination of vertical infiltration recharge of groundwater in the thick unsaturated zone of Sangong River Basin, Xinjiang[J]. Geology in China, 44(5): 913-923. doi: 10.12029/gc20170506
Citation: SUN Fangqiang, YIN Lihe, WANG Xiaoyong, MA Hongyun, ZHANG Jun, DONG Jiaqiu, HE Shuaijun. 2017. Determination of vertical infiltration recharge of groundwater in the thick unsaturated zone of Sangong River Basin, Xinjiang[J]. Geology in China, 44(5): 913-923. doi: 10.12029/gc20170506
shu

Determination of vertical infiltration recharge of groundwater in the thick unsaturated zone of Sangong River Basin, Xinjiang

  • Arid and Semi-arid Region Ground Water and Ecology Key Laboratory, Xi'an 710054, Shaanxi, China; Xi'an Center, China Geological Survey, Xi'an 710054, Shaanxi, China

    • Fund Project: Supported by Ministry of Land and Resources Nonprofit Industry Research (No. 201511047)
More Information
  • Author Bio: SUN Fangqiang, male, born in 1975, doctor, senior engineer, majors in hydrogeology and environmental geology; E-mail: sunfq2003@126.com
  • Corresponding author: WANG Xiaoyong, Wxiaoyong@cgs.cn  
Received Date:  19 September 2017
Revised Date:  09 October 2017
Publish Date:  25 October 2017
    Abstract

  • The authors investigated the origin of soil water and vertical infiltration recharge of groundwater in thick unsaturated zone of arid area based on the characteristics of water content, stable isotopes (δD and δ18O) of soil water and soluble salt ions in soil. The results indicate that the vertical profiles of stable isotopes of soil water depict a cyclic variation as well as water content and chloride of soluble salt ions for the uncultivated regions in desert and cultivated and uncultivated regions in oasis. Each cyclic variation indicates one infiltration event that has involved mixture of newly infiltrated water and existing soil water. The lower value of Cl- content is consistent with the depleted values of δD in each cycle; δD of soil water varies from -124.10‰ to -94.44‰, which suggests that soil water originates from precipitation or snow in winter in desert and in oasis. The vertical infiltration recharge varies in the ranges of 1.29~5.53mm/a, 0.52~1.85mm/a and 0.03~0.08mm/a respectively for the cultivated and uncultivated regions in oasis and the uncultivated regions in desert.

    • FullText(HTML)
  • 加载中
    • References
  • Allison G B, Gee G W, Tyler S W.1994.Vadose-zone Techniques for eestimating groundwater recharge in arid and semiarid regions[J].Soil Science Society of America Journal, 58(1):6-14. doi: 10.2136/sssaj1994.03615995005800010002x

    CrossRef Google Scholar

    Barnes C J, Allison G B.1988.Tracing of Water Movement in the unsaturated zone using stable isotopes of hydrogen and oxygen[J].Journal of Hydrology, 100:143-176. doi: 10.1016/0022-1694(88)90184-9

    CrossRef Google Scholar

    Chen Zhihua, Xu Heng li.1996.Chloride tracer method for estimation natural groundwater recharge in arid and semiarid regions[J].Geological Science and Technology Information, 15(3):87-92(in Chinese with English abstract).

    Google Scholar

    Cai Yuemei, Wang Wenxiang, Zhang Mingjiang, Yin Xiulan, Cai Wutian, Wang Ruijiu, Li Wenpeng.2016.An analysis of the groundwater flow system based on environmental isotopes in Turpan basin[J].Geology in China, 43(4):1439-1445(in Chinese with English abstract).

    Google Scholar

    Chen Jiangsheng, Wang Ting, Chen Xixi, Liu Xiaoyan.2013.Discussion on the origin of groundwater in the Orods Basin[J].Geological Review, 59(5):900-908(in Chinese with English abstract).

    Google Scholar

    Edmunds W M., Ma J Z, Aeschbach-Hertig W.2006.Groundwater recharge history and hydrogeochemical evolution in the Minqin Basin, North West China[J].Applied Geochemistry.21, 2148-2170. doi: 10.1016/j.apgeochem.2006.07.016

    CrossRef Google Scholar

    Gates J B, Edmunds W M, Darling W G.2008.Conceptual model of recharge to southeastern Badain Jaran Desert groundwater and lakes from environmental tracers[J].Applied Geochemistry.23, 3519-3534. doi: 10.1016/j.apgeochem.2008.07.019

    CrossRef Google Scholar

    Jordan M M, Navarro-Pedreno J, Garcia-Sanchez E.2004.Spatial dynamics of soil salinity under arid and semi-Arid conditions geological and environmental implications[J].Environmental Geology, 45(4):448-456. doi: 10.1007/s00254-003-0894-y

    CrossRef Google Scholar

    Jin Menggui, Zhang Renquan, Gao Yunfu, Sun Lianfa.1998.Primary Study on Soil Moisture Movement System Application[J].Rural Water Conservancy and Hydropower in China, (5):7-10(in Chinese with English abstract).

    Google Scholar

    Ji Xibin, Kang Ersi, Chen Rensheng, Zhao Wenzhi, Zhang Zhihui, Jin Bowen.2005.Estimation of ground water budget at the representative irrigated area in the middle stream of Heihe River[J].Hydrogeology & Engineering Geology, (6):25-29(in Chinese with English abstract).

    Google Scholar

    Lu Jingling, Zhang XiMing, Lu Chaoyan, Liu Guojun.A preliminary study on the water sources of Haloxylon ammodendron at the southern edge desert of Junggar Basin, China[J].Journal of Desert Research, 33:110-117(in Chinese with English abstract).

    Google Scholar

    Liu Licai, Chen Honghan, Yang Yi, Wang Jinsheng.2008.Characteristics and genesis of rNa/rCl in shallow groundwater in the Suzhou-Wuxi-Changzhou region[J].Geology in China, 35(1):117-122(in Chinese with English abstract).

    Google Scholar

    Liu Xiaoyan, Chen Jiansheng, Sun Xiaoxu.2010.Application of chloride tracer method to study replenishment ratio of precipitation in desert[J].Transactions of the CSAE, 26(s):146-149(in Chinese with English abstract).

    Google Scholar

    Lin Dan, Jin Menggui, Ma Bin, Wang Bingguo.2014.Characteristics of infiltration recharge at thickening vadose zone using soil hydraulic parameters[J].Earth Science-Journal of China University of Geosciences, 39(6):760-768(in Chinese with English abstract). doi: 10.3799/dqkx.2014.071

    CrossRef Google Scholar

    Ma Jinzhu, Huang Tianming, Ding Zhenyu, Edmunds W, M.2007.Environmental isotopes as the indicators of the groundwater recharge in the South Badain Jaran desert[J].Advances in Earth Science, 22(9):922-930.(in Chinese with English abstract).

    Google Scholar

    Ma Jinzhu, Li Ding, Li Xianghu, Edmunds W, M.2004.Chloride as a tracer and climatic change record from unsaturated zone of Badain Jaran desert[J].Journal of Desert Research, 24(6):674-679.(in Chinese with English abstract).

    Google Scholar

    Ma Bin, Liang Xing, Lin Dan, Liu Shaohua, Xu Min.2014.Tracing infiltration and recharge of the unsaturated zone using 2H, 18O isotopes in Shijiazhuang, North China Plain[J].Geological Science and Technology Information, 33(3):163-174(in Chinese with English abstract).

    Google Scholar

    Radford B J, Silburn D M, Forster B A.2009.Soil chloride and deep drainage responses to land clearing for cropping at seven sites in central Queensland, northern Australia[J].Journal of Hydrology.379:20-29. doi: 10.1016/j.jhydrol.2009.09.040

    CrossRef Google Scholar

    Song Xianfang, Li Fadong, Liu Changming, Tang Changyuan, Zhang Qiuying, Zhang Wangjun.2007.Water cycle in Taihang Mt.and its recharge to groundwater in North China Plain[J].Journal of Natural Resources, 22(3):398-408(in Chinese with English abstract).

    Google Scholar

    Stone A E C, Edmunds M.2016.Unsaturated zone hydrostratigraphies:A novel archive of past climates in dry land continental regions[J].Journal of Hydrology, 03(007):1-81.

    Google Scholar

    Stone W J.1992.Paleohydrologic implications of some deep soil water chloride profiles, Murray Basin, South Australia[J].Journal of Hydrology.132, 201-223. doi: 10.1016/0022-1694(92)90179-Y

    CrossRef Google Scholar

    Scanlon B R, Healy R, Cook P G.2002.Choosing appropriate techniques for quantifying groundwater recharge[J].Hydrogeology Journal, 10(1):18-39. doi: 10.1007/s10040-001-0176-2

    CrossRef Google Scholar

    Tian Lide, Yao Tandong, Tsujimura.M, Sun Weizhen.2002.Stable Isotope in Soil Water in the Middle of Tibetan Plateau[J].Acta Pedolegica Sinica, 39(3):289-295(in Chinese with English abstract).

    Google Scholar

    Wang Bingguo, Jin Menggui, Wang Wenfeng, Yang Lei.2006.Application of Chloride Ion Tracer Method in estimation of vertical infiltration recharge of groundwater in Hebei Plain[J].Water Saving Irrigation, (3):16-20(in Chinese with English abstract).

    Google Scholar

    Wang Zhiming, Guo Zede, Li Mingxiang.2000.Moisture Movement Characteristics in Shallow Unsaturated Loess in Semi-arid Area[J].Arid Area Research, 17(2):1-7(in Chinese with English abstract).

    Google Scholar

    Wang Weixing, Li Gongke, Li Hong, Hou Jiayu, Fang Wanling, Yang Fengtian.2013.Hydrogeochemical characteristics and origin of the geothermal fluid in Tangquan area, Hebei Province[J].Geology in China, 40(6):1935-1941(in Chinese with English abstract).

    Google Scholar

    Wu Zhenhan, Wu Zhonghai, Hu Daogong, Peng Hua, Zhang Yaoling.2009.Carbon and oxygen isotope changes and palaeoclimate cycles recorded by lacustrine deposits of Miocene Wudaoliang Group in northern Tibetan Plateau[J].Geology in China, 36(5):966-975(in Chinese with English abstract).

    Google Scholar

    Xu Xuexuan, Zhang Beiying, Tian Junliang.2010.Experimental study on the precipitation-soil water-groundwater transformation in loess hilly region[J].Advance in Water Science, 21(1):16-22(in Chinese with English abstract).

    Google Scholar

    Yuan Ruiqiang, Long Xiting, Wang Peng, Song Xianfang.2015.Discussion on application of chloride mass balance method[J].Journal of China Hydrology, 35(4):7-13(in Chinese with English abstract).

    Google Scholar

    Yin Lihe.2015.Study on Groundwater Recharge in Ordos Basin[M].Sunshine Press.

    Google Scholar

    Zhang Guanghui, Fei Yuhong, Shen Jianmei, Yang Lizhil.2007.Influence of unsaturated zone thickness on precipitation infiltration for recharge of groundwater[J].38(5):611-617(in Chinese with English abstract).

    Google Scholar

    Zhang Ning, Kang Yingqi, Liu Xiaowen, Bai Liang.1999.Investigation and study on background value of natural dustfall in Gansu[J].Environmental Research and Monitoring in Gansu.12(2):69-73(in Chinese with English abstract).

    Google Scholar

    Zhou Hai, Zheng Xinjun, Tang Lisong, Li Yan.2014.Analysis on seasonal dynamics of δ18O and δD in soil water at a saline desert site in the Southeastern Junggar Basin[J].Journal of Desert Research, 34(1):162-169(in Chinese with English abstract).

    Google Scholar

    蔡月梅, 王文祥, 张明江, 殷秀兰, 蔡五田, 王瑞久, 李文鹏.2016.基于环境同位素分析吐鲁番盆地地下水流系统[J].中国地质, 43(4):1439-1445.

    Google Scholar

    陈建生, 王婷, 陈茜茜, 刘晓艳.2013.鄂尔多斯自流盆地地下水来源争议问题讨论[J].地质论评, 59(5):900-908.

    Google Scholar

    陈植华, 徐恒力.1996.确定干旱-半干旱地区降水入渗补给量的新方法——氯离子示踪法[J].地质科技情报, 15(3):87-92.

    Google Scholar

    吉喜斌, 康尔泗, 陈仁升, 赵文智, 张智慧, 金博文.2005.黑河中游绿洲典型灌区地下水资源总均衡估算[J].水文地质工程地质, (6):25-29.

    Google Scholar

    靳孟贵, 张人权, 高云福, 孙连发.1998.土壤水流动系统及其应用初探[J].中国农村水利水电(农田水利与小水电), (5):7-10.

    Google Scholar

    吕金岭, 张希明, 吕朝燕, 刘国军.201 3.准噶尔盆地南缘荒漠区梭梭维持水源初步研究[J].中国沙漠, 33(1):110-117. doi: 10.7522/j.issn.1000-694X.2013.00016

    CrossRef Google Scholar

    马金珠, 黄天明, 丁贞玉, Edmunds W M.2007.同位素指示的巴丹吉林沙漠南缘地下水补给来源[J].地球科学进展, 22(9):922-930.

    Google Scholar

    马斌, 梁杏, 林丹, 刘绍华, 徐敏.2014.应用2H、18O同位素示踪华北平原石家庄包气带土壤水入渗补给及年补给量确定[J].地质科技情报, 33(3):163-174.

    Google Scholar

    马金珠, 李丁, 李相虎, Edmunds W M.2004.巴丹吉林沙漠包气带Cl-示踪与气候记录研究[J].中国沙漠, 24(6):674-679.

    Google Scholar

    刘晓艳, 陈建生, 孙晓旭.2010.采用氯离子示踪法计算沙漠降雨入渗量[J].农业工程学报, 26(s):146-149.

    Google Scholar

    林丹, 靳孟贵, 马斌, 汪丙国.2014.包气带增厚区土壤水力参数及其对入渗补给的影响[J].地球科学——中国地质大学学报, 39(6):760-768.

    Google Scholar

    刘立才, 陈鸿汉, 杨仪, 王金生.2008.苏锡常地区浅层地下水rNa/rCl特征及其成因初探[J].中国地质, 35(1):117-122.

    Google Scholar

    宋献方, 李发东, 刘昌明, 唐常源, 张秋英, 张万军.2007.太行山区水循环及其对华北平原地下水的补给[J].自然资源学报, 22(3):398-408. doi: 10.11849/zrzyxb.2007.03.009

    CrossRef Google Scholar

    田立德, 姚檀栋, Tsujimura M, 孙维贞.2002.青藏高原中部土壤水中稳定同位素变化[J].土壤学报, 39(3):289-295. doi: 10.11766/trxb200007170301

    CrossRef Google Scholar

    王卫星, 李攻科, 李宏, 侯佳渝, 房万嶺, 杨峰田.2013.河北汤泉地热流体水文地球化学特征及其成因[J].中国地质, 40(6):1935-1941.

    Google Scholar

    王志明, 郭择德, 李明香.2000.半干旱地区包气带浅部黄土中水分运移特征[J].干旱区研究, 17(2):1-7.

    Google Scholar

    汪丙国, 靳孟贵, 王文峰, 杨磊.2006.氯离子示踪法在河北平原地下水垂向入渗补给量评价中的应用[J].节水灌溉, (3):16-20.

    Google Scholar

    吴珍汉, 吴中海, 胡道功, 彭华, 张耀玲.2009.青藏高原北部中新统五道梁群湖相沉积碳氧同位素变化及古气候旋回[J].中国地质, 36(5):966-975.

    Google Scholar

    徐学选, 张北赢, 田均良.2010.黄土丘陵区降水-土壤水-地下水转化实验研究[J].水科学进展, 21(1):16-22.

    Google Scholar

    尹立河.2015.鄂尔多斯盆地地下水补给研究[M].阳光出版社.

    Google Scholar

    袁瑞强, 龙西亭, 王鹏, 宋献方.2015.氯离子质量平衡法应用问题刍议[J].水文, 35(4):7-13.

    Google Scholar

    张光辉, 费宇红, 申建梅, 杨丽芝.2007.降水补给地下水过程中包气带变化对入渗的影响[J]水利学报, 2007, 38(5):611-617.

    Google Scholar

    张宁, 康颖琦, 刘晓文, 白亮.1999.甘肃省大气自然降尘背景值的调查和研究[J].甘肃环境研究与监测, 12(2):69-73.

    Google Scholar

    周海, 郑新军, 唐立松, 李彦.2014.盐生荒漠土壤水稳定氢、氧同位素组成季节动态[J].中国沙漠, 34(1):162-169. doi: 10.7522/j.issn.1000-694X.2013.00295

    CrossRef Google Scholar

    • Relative Articles
  • Cited by
  • Supplements
    • Proportional views
  • 加载中
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

Figures(7)

Tables(3)

Export Citation
PDF
XML

Article Metrics

Article views(2876) PDF downloads(986) Cited by(0)

Access History

Other Articles By Authors

Catalog

    /

    DownLoad:  Full-Size Img  PowerPoint
    Return
    版权所有：中国地质调查局发展研究中心 copyright @2020