Identification of Soil Water Migration and Recharge Sources in The Southern Marginal Zone of the Junggar Basin, China

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  • Key Laboratory of Groundwater and Ecology in Arid and Semi-arid Region /Xi‘an Center,China Geological Survey,Xi ‘an,710054 ,Shanxi,China)

Received date: 2016-12-03

  Revised date: 2017-04-27

  Online published: 2017-12-20

Abstract

Abstract:Soil water is the basis of all terrestrial plants in desert area. Investigation on the migration patterns of soil water is necessary for identifying the recharge sources of soil water and for the ecological regeneration in desert area. In this paper, the origin and migration patterns of soil water in a desert area in the southern marginal zone of the Junggar Basin were investigated based on measuring soil moisture content, stable isotopes (δD and δ18O) of soil water and soluble salt ions. The results indicated that the vertical profiles of stable isotopes, water content and soluble salt ions of soil water were in a cyclic variation. The Cl- composition in soil was positively correlated to soil moisture content. The influencing depth of evaporation was 0-1.6 m; soil water in a deep range of 1.6-8.0 m moved downward, and soil water below 8.0 m was influenced by groundwater. The vertical variations of stable isotopes and Cl- composition in soil water indicated that soil water originated from precipitation in desert area. The low values of Cl- composition corresponded to the depleted values of δD and δ18O; δD of soil water varied from -124.10‰ to -97.39‰, which suggested that soil water originated from precipitation or snow melt winter.

Cite this article

SUN Fangqiang,YIN Lihe,MA Hongyun,ZHANG Jun,WANG Xiaoyong,DONG Jiaqiu,HE Shuaijun . Identification of Soil Water Migration and Recharge Sources in The Southern Marginal Zone of the Junggar Basin, China[J]. Arid Zone Research, 2017 , 34(6) : 1271 -1277 . DOI: 10.13866/j.azr.2017.06.08

References

〔1〕 周海,郑新军,唐立松,等.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,2014,34(1):162-169.〔ZHOU Hai,ZHENG Xinjun,TANG Lisong,et al.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,2014,34(1):162-169.〕
〔2〕 吕金岭,张希明,吕朝燕,等.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,2013,33(1), 110-117.〔LU Jingling,ZHANG XiMing,LU Chaoyan, et a1. A preliminary study on the water sources of Haloxylon ammodendron at the southern edge desert of Junggar Basin,  China. Journal of Desert Research,  33,  110-117. (in Chinese with English abstract〕
〔3〕 靳志锋,虎胆·吐马尔白,牟洪臣,等. 土壤冻融温度影响下棉田水盐运移规律〔J〕.干旱区研究,2013,30(4):623-627. 〔JIN Zhifeng, HUDAN Tumarbay, MOU Hongchen, et a1. Soil Water and Salt Migration in Cotton Field under Soil Freezing-Thawing Temperature〔J〕.Arid Zone Research, 2013,30(4):623-627.〕
〔4〕 Jordan M M, Navarro-Pedreno J, Garcia-Sanchez E, et al.Spatial dynamics of soil salinity under arid and semi-Arid conditions:  geological  and  environmental  implications〔J〕.Environmental Geology, 2004, 45(4): 448-456.
〔5〕 苏里坦,阿不都·沙拉木,宋郁东. 膜下滴灌水量对土壤水盐运移及再分布的影响〔J〕.干旱区研究,2011,28(1):79-84.〔 Su Litan, Abudu Shalamu, Song Yudong. E ffects of D rp Irriagation Volume on Soil Water-salt Transfer and Its Redistribution〔J〕.Arid Zone Research,2011,28(1):79-84.〕
〔6〕 任杰,沈振中,杨杰,等. 基于HYDRUS模型低温水入渗下土壤水热运移模拟〔J〕.干旱区研究,2016,33(2):246-252.〔Ren Jie, Shen Zhenzhong, Yang,Jie, et al. Simulation of Water and Heat Transfer in Soil under Low-temperature Water Infiltration based on the HYDRUS Model〔J〕.Arid Zone Research, 2016,33(2):246-252.〕
〔7〕 靳孟贵,张人权,高云福,等.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),1998(5):7- 10.〔JIN Menggui, ZHANG Renquan, GAO Yunfu, et al. Primary Study on Soil Moisture Movement System Application〔J〕. Rural Water Conservancy and Hydropower in China, 1998(5):7- 10.〕
〔8〕  王志明,郭择德,李明香.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,2000,17(2):1-7.〔WANG Zhiming, GUO Zede, LI Mingxiang. Moisture Movement Characteristics in Shallow Unsaturated Loess in Semi-arid Area〔J〕.Arid Area Research, 2000,17(2):1-7. 〕
〔9〕  张光辉,费宇红,申建梅,等.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.〔ZHANG Guanghui, FEI Yuhong, SHEN Jian-mei, et al. Influence of unsaturated zone thickness on precipitation infiltration for recharge of groundwater 〔J〕.Shui Li Xue Bao, 2007,38(5) : 611-617.〕
〔10〕  林丹,靳孟贵,马斌,等.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,2014. 39(6):760-768.〔LIN Dan, JIN Menggui, MA Bin, et al. Characteristics of Infiltration Recharge at Thickening Vadose Zone Using Soil Hydraulic Parameters〔J〕. Earth Science-Journal of China University of Geosciences, 2014. 39(6):760-768.〕
〔11〕 陈建生,王婷,陈茜茜,等. 鄂尔多斯自流盆地地下水来源争议问题讨论〔J〕.地质论评,2013. 59(5):900-908.〔CHEN Jiangsheng, WANG Ting, CHEN Xixi, et al. Discussion on the Origin of Groundwater in the Orods Basin〔J〕. Geological Review, 2013. 59(5):900-908.〕
〔12〕 Zimmermann U, Muinnich K O, Roether W. Downward movement of soil moisture traced by means of hydrogen isotopes〔J〕.Geophysical Monograph Series,1967,11:28-36;
〔13〕 徐学选,张北赢,田均良.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, 2010,21(1):16-22.〔XU Xuexuan, ZHANG Beiying, TIAN Junliang. Experimental Study on the Precipitation-soil Water-groundwater Transformation in Loess Hilly region〔J〕. Advance in Water Science, 2010,21(1):16-22.〕
〔14〕孙芳强,尹立河,马洪云,等.新疆三工河流域土壤水δD和δ18O特征及其补给来源〔J〕干旱区地理,2016,39(6),1298-1304.〔Sun Fangqiang,Yin Lihe,Ma Hongyun, et al. Features of δD andδ18O and Origin of Soil Water in Sangong River Basin,Xinjiang〔J〕.Arid Land Geography,2016,39(6):1298-1304.〕
〔15〕 彭刚,赵成义,李君,等. 新疆塔里木河胡杨根蘖苗水分来源初探〔J〕.干旱区研究, 2014,31(6):1093-1099. 〔PENG Gang, ZHAO Chengyi, LI Jun, et al. Water Source of Root Suckers of Populus euphratica in the Tarim River Basin,Xinjiang〔J〕.Arid Zone Research, 2014,31(6):1093-1099. 〕
〔16〕Zimmermann U,Muinnich K O,Roether W.Downward movement of soil moisture traced by means of hydrogen isotopes〔J〕.Geophysical Monograph Series,1967,11:28-36.
〔17〕 Kwang-Sik Lee,Jun-M Kim,Dong-Rim Lee,et al.Analysis of water movement through an unsaturated zone in Jeju,Korea using stable oxygen and hydrogen isotopes〔J〕.Journal of Hydrology,2007,8:199-211.
〔18〕孙芳强,尹立河,马洪云,等. 新疆三工河流域氢氧同位素特征及其水循环意义〔J〕.人民黄河,2016,38(12),106-109.〔Sun Fangqiang,Yin Lihe,Ma Hongyun, etal. Features of Hydrogen and Oxygen Isotopes and Their Indication of Hydrological Cycle in Sangong River Basin, Xinjiang〔J〕.Yellow River, 2016,38(12),106-109.〕
〔19〕马斌,梁杏,林丹,等.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,2014,33(3):163-174.〔 MA Bin, LIANG Xing, LIN Dan, et al. Tracing Infiltration and Recharge of the Unsaturated Zone Using 2H,18O Isotopes in Shijiazhuang,North China Plain〔J〕. Geological Science and Technology Information, 2014,33(3):163-174.〕
〔20〕田立德,姚檀栋,Tsujimura.M,等.青藏高原中部土壤水中稳定同位素变化〔J〕.土壤学报,2002,39(3):289-295.〔TIAN Lide, YAO Tandong, M.TSUJIN1URA,et al. Stable Isotope in Soil Water in the Middle of Tibetan Plateau〔J〕. Acta Pedolegica Sinica,2002,39(3):289-295.〕
〔21〕A.E.C. Stone, W.M. Edmunds. Unsaturated zone hydrostratigraphies: A novel archive of past climates in dryland continental regions〔J〕. 2016,03(007):1-81.
〔22〕Allison, G. B., Stone, W. J., Hughes, M. W. Recharge in karst and dune elements of a semi-arid landscape as indicated by natural isotopes and chloride〔J〕.Journal of Hydrology,1985. 76, 1-25.
〔23〕Allison G B, Gee G W,Tyler S W. Vadose-zone techniques for estimating groundwater recharge in arid and semiarid regions〔J〕. Soil Science Society of America Journal, 1994,58(1):6-14.
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