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新疆三工河流域厚层包气带区地下水垂向补给量的厘定

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孙芳强, 尹立河, 王晓勇, 马洪云, 张俊, 董佳秋, 贺帅军. 2017. 新疆三工河流域厚层包气带区地下水垂向补给量的厘定[J]. 中国地质, 44(5): 913-923. doi: 10.12029/gc20170506
引用本文: 孙芳强, 尹立河, 王晓勇, 马洪云, 张俊, 董佳秋, 贺帅军. 2017. 新疆三工河流域厚层包气带区地下水垂向补给量的厘定[J]. 中国地质, 44(5): 913-923. doi: 10.12029/gc20170506
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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
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新疆三工河流域厚层包气带区地下水垂向补给量的厘定

  • 中国地质调查局干旱-半干旱区地下水与生态重点实验室, 陕西 西安 710054;中国地质调查局西安地质调查中心, 陕西 西安 710054

  • 基金项目:
    国土资源部公益性行业科研专项（201511047）资助
详细信息
    作者简介: 孙芳强, 男, 1975, 博士, 高级工程师, 主要从事水文地质与环境地质方面研究; E-mail:sunfq2003@126.com
    通讯作者: 王晓勇, 男, 1977, 硕士, 高级工程师, 主要从事水文水资源研究; E-mail:Wxiaoyong@cgs.cn

  • 中图分类号: P641

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

    摘要

  • 通过对荒漠区荒地、绿洲区耕地及摞荒地厚层包气带剖面土壤水的含水率、易溶盐离子及稳定同位素（δD、δ18O）的测定和分析，对厚层包气带区土壤水的补给来源及地下水的垂向补给量进行了厘定。结果表明：荒漠区荒地、绿洲区耕地与摞荒地土壤含水率、易溶盐中氯离子与土壤水氢氧同位素在垂向上均呈现旋回变化，每个旋回经历了一次新水入渗补给的过程。绿洲区土壤水与荒漠区土壤补给水中的δD值为-124.10‰~-94.44‰，土壤补给水来源于冬季大气降水或降雪的入渗补给。绿洲内耕地区、摞荒地区及荒漠区地下水垂向入渗补给量分别为1.29~5.53 mm/a、0.52~1.85 mm/a及0.03~0.08 mm/a。

    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.

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  • 图 1  各采样剖面分布图

    Figure 1. 

    下载: 全尺寸图片 幻灯片

    图 2  剖面含水量随深度的变化

    Figure 2. 

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    图 3  剖面Cl-随深度的变化

    Figure 3. 

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    图 4  土壤水中δD、δ18O在垂向剖面上的分布

    Figure 4. 

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    图 5  各剖面δD值及Cl-含量旋回特征

    Figure 5. 

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    图 6  各剖面补给水中δD与δ18O同位素关系

    Figure 6. 

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    图 7  新疆乌鲁木齐地区氢氧同位素年内变化

    Figure 7. 

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    表 1  各采样点土地利用及剖面采样特征

    Table 1.  Land use practices and distribution of samples in different profiles

    下载: 导出CSV

    表 2  各剖面旋回段中补给水δD值及Cl-含量统计

    Table 2.  Statistic characteristics of δD and Cl- for recharge water in different profiles

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    表 3  各剖面旋回段的垂向入渗补给量

    Table 3.  Vertical infiltration recharge in different profiles

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    • 参考文献(57)

  • 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

    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

    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).

    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). http://geochina.cgs.gov.cn/ch/reader/view_abstract.aspx?file_no=20160427&flag=1

    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).

    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

    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

    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

    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). http://agris.fao.org/agris-search/export!exportTopEndNoteXML.action?agro...

    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).

    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). http://d.wanfangdata.com.cn/Periodical_zgsm201301016.aspx

    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). http://geochina.cgs.gov.cn/ch/reader/view_abstract.aspx?file_no=20080112&flag=1

    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). https://www.researchgate.net/publication/287865003_Application_of...

    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

    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). http://www.adearth.ac.cn/EN/abstract/abstract3750.shtml

    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).

    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).

    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

    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).

    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. https://www.sciencedirect.com/science/article/pii/S0012825216300526

    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

    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

    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).

    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). http://en.cnki.com.cn/Article_en/CJFDTOTAL-JSGU200603005.htm

    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).

    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). http://geochina.cgs.gov.cn/ch/reader/view_abstract.aspx?file_no=20130622&flag=1

    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). http://geochina.cgs.gov.cn/ch/reader/view_abstract.aspx?file_no=20090502&flag=1

    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). http://sourcedb.iswc.cas.cn/zw/lw/201601/t20160125_4523318.html

    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). http://vzj.geoscienceworld.org/content/4/1/72

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

    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).

    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).

    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).

    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. http://geochina.cgs.gov.cn/ch/reader/view_abstract.aspx?file_no=20160427&flag=1

    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. https://www.wenkuxiazai.com/doc/3864793f561252d380eb6ee6...

    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. http://www.cqvip.com/QK/93477A/199603/5182872.html

    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. http://www.cqvip.com/QK/90596X/200506/20567928.html

    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. http://www.wenkuxiazai.com/doc/9318e5b2eefdc8d376ee32c1.html

    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

    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. http://new.wanfangdata.com.cn/details/detail.do?_type=perio&id=dqkxjz200709006

    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.

    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. http://www.doc88.com/p-0788912092991.html

    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. http://www.wenkuxiazai.com/doc/99c3cb617e21af45b307a88b-2.html

    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. http://www.cqvip.com/QK/94035X/201406/50075869.html

    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. http://geochina.cgs.gov.cn/ch/reader/view_abstract.aspx?file_no=20080112&flag=1

    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

    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

    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. http://geochina.cgs.gov.cn/ch/reader/view_abstract.aspx?file_no=20130622&flag=1

    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.

    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. http://www.wenkuxiazai.com/doc/67954c61a98271fe910ef9ac-2.html

    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. http://geochina.cgs.gov.cn/ch/reader/view_abstract.aspx?file_no=20090502&flag=1

    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. http://www.doc88.com/p-059298476463.html

    尹立河.2015.鄂尔多斯盆地地下水补给研究[M].阳光出版社.

    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. http://or.nsfc.gov.cn/handle/00001903-5/266794

    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. http://jhe.ches.org.cn/jhe/ch/reader/view_abstract.aspx?file_no=200705611&flag=1

    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.

    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

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收稿日期:  2017-09-19
修回日期:  2017-10-09
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