新疆喀什三角洲地下水流系统的水化学和同位素标记

魏兴; 周金龙; 梁杏; 乃尉华; 曾妍妍; 范薇; 李斌

doi:10.3799/dqkx.2019.177

Volume 45 Issue 5

May 2020

Turn off MathJax

Article Contents

Article Navigation > Earth Science > 2020 > 45(5): 1807-1817

Wei Xing, Zhou Jinlong, Liang Xing, Nai Weihua, Zeng Yanyan, Fan Wei, Li Bin, 2020. Hydrochemical and Isotopic Markers of Groundwater Flow Systems in the Kashgar Delta Area in Xinjiang. Earth Science, 45(5): 1807-1817. doi: 10.3799/dqkx.2019.177

Citation:

Wei Xing, Zhou Jinlong, Liang Xing, Nai Weihua, Zeng Yanyan, Fan Wei, Li Bin, 2020. Hydrochemical and Isotopic Markers of Groundwater Flow Systems in the Kashgar Delta Area in Xinjiang. Earth Science, 45(5): 1807-1817. doi: 10.3799/dqkx.2019.177

Citation:

Wei Xing, Zhou Jinlong, Liang Xing, Nai Weihua, Zeng Yanyan, Fan Wei, Li Bin, 2020. Hydrochemical and Isotopic Markers of Groundwater Flow Systems in the Kashgar Delta Area in Xinjiang. Earth Science, 45(5): 1807-1817. doi: 10.3799/dqkx.2019.177

PDF( 2020 KB)

Hydrochemical and Isotopic Markers of Groundwater Flow Systems in the Kashgar Delta Area in Xinjiang

doi: 10.3799/dqkx.2019.177

Wei Xing^{1, 2
,
,},
Zhou Jinlong^{1, 2
,
,
,},
Liang Xing³,
Nai Weihua⁴,
Zeng Yanyan^{1, 2},
Fan Wei^{1, 2},
Li Bin⁴

1.
College of Water Conservancy and Civil Engineering, Xinjiang Agricultural University, Urumqi 830052, China
2.
Xinjiang Hydrology and Water Resources Engineering Research Center, Urumqi 830052, China
3.
School of Environment Studies, China University of Geosciences, Wuhan 430074, China
4.
No.2 Hydrogeological and Engineering Geological Team of Xinjiang Bureau of Geology and Mineral Resources Exploration and Development, Changji 831100, China

Received Date: 2019-07-17
Publish Date: 2020-05-15

Abstract

Abstract

The shortage of groundwater caused by poor water quality is more prominent in the Kashgar delta of Xinjiang, so it is practical significance to study groundwater flow system. Based on the divisions of groundwater aquifer system in Kashgar delta, the characteristics of the groundwater hydrochemistry and cycle regeneration were analyzed using hydrogeochemistry and environmental isotope age test methods. The research results show that the delta aquifer system consists of unconfined groundwater in piedmont sloping alluvial-diluvial plain, unconfined groundwater in river alluvial plain and confined groundwater in river alluvial plain. The evolution of groundwater hydrochemistry types is HCO₃·SO₄-Ca→SO₄-Ca→SO₄·Cl-Mg·Na→SO₄·Cl-Na along the groundwater flow direction. With the increased TDS, the groundwater quality tends towards salinization. Piedmont sloping alluvial-diluvial plain is the main dissolution-runoff zone and the river alluvial plain is main runoff-accumulation salt zone. The groundwater renewal rate in the study area is 0.03%~16.35%·a^-1, which is characterized by unconfined groundwater in piedmont sloping alluvial-diluvial plain > unconfined groundwater in river alluvial plain > confined groundwater in river alluvial plain. Estimated by ³H, the age of unconfined groundwater in piedmont sloping alluvial-diluvial plain is 8~49 a, with an average of 29 a.The age of unconfined groundwater in river alluvial plain is 14~ > 50 a, in which the average age of upper unconfined groundwater is 24 a, and the average age of lower unconfined groundwater is > 50 a. Estimated by ¹⁴C, the age of unconfined groundwater in river alluvial plain is 476~33 623 a, with an average of 8 106 a. The age of confined groundwater in river alluvial plain is 5 186~34 578 a, with an average of 30 043 a, being "older" than unconfined groundwater. Based on the above characteristics, the groundwater aquifer systems in Kashgar delta are divided into two local flow systems (Ⅰ₁ and Ⅰ₂) with faster renewal rate and a regional flow system (Ⅱ) with slow circulation.
- Kashgar delta in Xinjiang,
- hydrogeochemistry,
- isotope age,
- renewal rate,
- groundwater flow system,
- hydrogeology

FullText(HTML)

References(49)

References

Abdou Babaye, M. S., Orban, P., Ousmane, B., et al., 2019. Characterization of Recharge Mechanisms in a Precambrian Basement Aquifer in Semi-Arid South-West Niger. Hydrogeology Journal, 27(2):475-491. https://doi.org/10.1007/s10040-018-1799-x

Atkinson, A.P., Cartwright, I., Gilfedder, B.S., et al., 2014. Using ¹⁴C and ³H to Understand Groundwater Flow and Recharge in an Aquifer Window. Hydrology and Earth System Sciences, 18(12):4951-4964. https://doi.org/10.5194/hess-18-4951-2014

Ba, W.L., Zhou, H.R., Liang, X.Q., et al., 2013. Ecological Footprint and Its Application in Ecological Planning in Kashgar Prefecture.Arid Zone Research, 30(5):905-912 (in Chinese with English abstract). http://d.old.wanfangdata.com.cn/Periodical/ghqyj201305024

Chen, Y. X., Yang, F. T., Su, X. S., et al., 2016. Estimation of Groundwater Renewal Rate Using Environmental Isotopes in the Arid Upper Peacock River, NW China.Journal of Radioanalytical and Nuclear Chemistry, 310(2):911-917. https://doi.org/10.1007/s10967-016-4979-y

Chen, Z.Y., Liu, J., Yang, X.K., et al., 2010. The Environmental Isotope Markers of Groundwater Flow Patterns of the Song-Nen Plain.Earth Science Frontiers, 17(6):94-101 (in Chinese with English abstract). http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=dxqy201006013

Cui, Y.L., Liu, F., Hao, Q.C., et al., 2015. Characteristics of Hydrogen and Oxygen Isotopes and Renewability of Groundwater in the Nuomuhong Alluvial Fan. Hydrogeology & Engineering Geology, 42(6):1-7 (in Chinese with English abstract). http://d.old.wanfangdata.com.cn/Periodical/swdzgcdz201506001

Edmunds, W. M., 2009. Geochemistry's Vital Contribution to Solving Water Resource Problems.Applied Geochemistry, 24(6):1058-1073. https://doi.org/10.1016/j.apgeochem.2009.02.021

Gabrielli, C. P., Morgenstern, U., Stewart, M. K., et al., 2018. Contrasting Groundwater and Streamflow Ages at the Maimai Watershed. Water Resources Research, 54(6):3937-3957. https://doi.org/10.1029/2017wr021825

Gonfiantini, R., Roche, M. A., Olivry, J. C., et al., 2001. The Altitude Effect on the Isotopic Composition of Tropical Rains.Chemical Geology, 181(1-4):147-167. https://doi.org/10.1016/s0009-2541(01)00279-0

Huang, X.Q., Liu, Q., Xue, Z.Q., et al., 2014. The Characteristics of Groundwater Isotopes in Upper Reach Plain of Qingshui River, Ningxia. Journal of Arid Land Resources and Environment, 28(2):143-148 (in Chinese with English abstract). http://d.old.wanfangdata.com.cn/Periodical/ghqzyyhj201402025

Le Gal la Salle, C., Marlin, C., Leduc, C., et al., 2001. Renewal Rate Estimation of Groundwater Based on Radioactive Tracers (³H, ¹⁴C) in an Unconfined Aquifer in a Semi-Arid Area, Iullemeden Basin, Niger. Journal of Hydrology, 254(1/2/3/4):145-156. https://doi.org/10.1016/s0022-1694(01)00491-7

Li, H., Wen, Z., Xie, X.J., et al., 2017. Hydrochemical Characteristics and Evolution of Karst Groundwater in Sanqiao District of Guiyang City.Earth Science, 42(5):804-812 (in Chinese with English abstract). http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=dqkx201705016

Li, L.Q., Wang, Z.Z., He, H.X., et al., 2019. Research of Water Resources Multi-Dimensional Equilibrium Allocation Based on Eco-Hydrological Threshold Regulation in Inland Arid Region. Journal of Hydraulic Engineering, 50(3):377-387 (in Chinese with English abstract). http://d.old.wanfangdata.com.cn/Periodical/slxb201903011

Liu, F., Cui, Y.L., Zhang, G., et al., 2014. Using the ³H and ¹⁴C Dating Methods to Calculate the Groundwater Age in Nuomuhong, Qaidam Basin.Geoscience, 28(6):1322-1328 (in Chinese with English abstract). http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=xddz201406026

Ma, B., Jin, M. G., Liang, X., et al., 2018. Groundwater Mixing and Mineralization Processes in a Mountain-Oasis-Desert Basin, Northwest China:Hydrogeochemistry and Environmental Tracer Indicators. Hydrogeology Journal, 26(1):233-250. https://doi.org/10.1007/s10040-017-1659-0

Mao, X.M., Liang, X., Wang, F.L., et al., 2010. Calibrating Deep Groundwater ¹⁴C Ages of North China Plain with TDIC and a Comparative Study.Earth Science Frontiers, 17(6):102-110 (in Chinese with English abstract). http://d.old.wanfangdata.com.cn/Periodical/dxqy201006014

Mao, X. M., Wang, H., Feng, L., 2018.¹⁴C Age Reassessment of Groundwater from the Discharge Zone due to Cross-Flow Mixing in the Deep Confined Aquifer. Journal of Hydrology, 560:572-581. https://doi.org/10.1016/j.jhydrol.2018.03.052

Nai, W.H., Shi, J., Wang, W.K., et al., 2018. Isotopic Age Characteristics and Renewal Rate of Groundwater in Kashgar Plain. Xinjiang Geology, 36(3):406-409 (in Chinese with English abstract). http://d.old.wanfangdata.com.cn/Periodical/xjdz201803021

Pearson Jr, F. J. White, D.E., 1967. Carbon 14 Ages and Flow Rates of Water in Carrizo Sand, Atascosa County, Texas. Water Resources Research, 3(1):251-261. https://doi.org/10.1029/wr003i001p00251

Ruan, Y.F., Zhao, L.J., Xiao, H.L., et al., 2015. The Groundwater in the Heihe River Basin:Isotope Age and Renewability. Journal of Glaciology and Geocryology, 37(3):767-782 (in Chinese with English abstract). http://d.old.wanfangdata.com.cn/Periodical/bcdt201503024

Su, X.S., Lin, X.Y., Dong, W.H., et al., 2006.¹⁴C Age Correction of Deep Groundwater in Yinchuan Plain. Journal of Jilin University (Earth Science Edition), 36(5):830-836 (in Chinese with English abstract). http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=cckjdxxb200605020

Tamers, M. A., 1975. Validity of Radiocarbon Dates on Ground Water.Geophysical Surveys, 2(2):217-239. https://doi.org/10.1007/bf01447909

Vogel, J.C., 1970. Carbon-14 Dating of Groundwater.In: Isotope Hydrology.IAEA, Vienna, 225-239.

Wei, W., Chen, Z.Y., Zhao, H.M., et al., 2011. Comparison of ⁴He and ¹⁴C Dating of Groundwater from Quaternary Confined Aquifers in Hebei Plain. Journal of Jilin University (Earth Science Edition), 41(4):1144-1150 (in Chinese with English abstract). http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=cckjdxxb201104026

Wei, X., Zhou, J.L., Nai, W.H., et al., 2019. Hydrochemical Characteristics and Evolution of Groundwater in the Kashgar Delta Area in Xinjiang. Environmental Science, 40(9):4042-4051 (in Chinese with English abstract). http://d.old.wanfangdata.com.cn/Periodical/hjkx201909023

Xiao, Y., Shao, J. L., Cui, Y. L., et al., 2017. Groundwater Circulation and Hydrogeochemical Evolution in Nomhon of Qaidam Basin, Northwest China. Journal of Earth System Science, 126(2):26. https://doi.org/10.1007/s12040-017-0800-8

Xie, Q.M., Wang, Z.L., Yin, C.M., et al., 2019. Tectonic Evolution Characteristics of Yingjisha and Pishan Areas and the Influence on Petroleum Accumulation in the Southwest Depression, Tarim Basin.Petroleum Geology & Experiment, 41(2):165-175 (in Chinese with English abstract). http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=sysydz201902003

Yang, L.Z., Zhang, G.H., Liu, Z.Y., et al., 2009. Isotope Age of Groundwater in Lubei Plain and an Evaluation of Its Renewable Capacity. Acta Geoscientica Sinica, 30(2):235-242 (in Chinese with English abstract). http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=dqxb200902012

Yu, H.T., Ma, T., Deng, Y.M., et al., 2017. Hydrochemical Characteristics of Shallow Groundwater in Eastern Jianghan Plain. Earth Science, 42(5):685-692 (in Chinese with English abstract). http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=dqkx201705004

Yuan, R.Q., Long, X.T., Wang, P., et al., 2015. Renewal Rate of Groundwater in the Baiyangdian Lake Basin.Progress in Geography, 34(3):381-388 (in Chinese with English abstract). http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=dlkxjz201503013

Zhai, Y.Z., Wang, J.S., Zhou, J., 2013. Hydrochemical and Isotopic Markers of Flow Patterns and Renewal Mode of Groundwater in Chaobai River Alluvial Fan in Beijing.Journal of Basic Science and Engineering, 21(1):32-44 (in Chinese with English abstract). http://cn.bing.com/academic/profile?id=391aae91bf7bc13d9a01335463104b65&encoded=0&v=paper_preview&mkt=zh-cn

巴乌龙, 周华荣, 梁雪琼, 等, 2013.喀什地区生态足迹分析及其在生态规划中的应用.干旱区研究, 30(5):905-912. http://d.old.wanfangdata.com.cn/Periodical/ghqyj201305024

陈宗宇, 刘君, 杨湘奎, 等, 2010.松嫩平原地下水流动模式的环境同位素标记.地学前缘, 17(6):94-101. http://d.old.wanfangdata.com.cn/Periodical/dxqy201006013

崔亚莉, 刘峰, 郝奇琛, 等, 2015.诺木洪冲洪积扇地下水氢氧同位素特征及更新能力研究.水文地质工程地质, 42(6):1-7. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=swdzgcdz201506001

黄小琴, 柳青, 薛忠岐, 等, 2014.宁夏固原地区地下水同位素特征研究.干旱区资源与环境, 28(2):143-148. http://d.old.wanfangdata.com.cn/Periodical/ghqzyyhj201402025

李华, 文章, 谢先军, 等, 2017.贵阳市三桥地区岩溶地下水水化学特征及其演化规律.地球科学, 42(5):804-812. doi: 10.3799/dqkx.2017.068

李丽琴, 王志璋, 贺华翔, 等, 2019.基于生态水文阈值调控的内陆干旱区水资源多维均衡配置研究.水利学报, 50(3):377-387. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=slxb201903011

刘峰, 崔亚莉, 张戈, 等, 2014.应用氚和¹⁴C方法确定柴达木盆地诺木洪地区地下水年龄.现代地质, 28(6):1322-1328. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=xddz201406026

毛绪美, 梁杏, 王凤林, 等, 2010.华北平原深层地下水¹⁴C年龄的TDIC校正与对比.地学前缘, 17(6):102-110. http://d.old.wanfangdata.com.cn/Periodical/dxqy201006014

乃尉华, 史杰, 王文科, 等, 2018.喀什平原区地下水同位素年龄特征及更新速率分析.新疆地质, 36(3):406-409. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=xjdz201803021

阮云峰, 赵良菊, 肖洪浪, 等, 2015.黑河流域地下水同位素年龄及可更新能力研究.冰川冻土, 37(3):767-782. http://d.old.wanfangdata.com.cn/Periodical/bcdt201503024

苏小四, 林学钰, 董维红, 等, 2006.银川平原深层地下水¹⁴C年龄校正.吉林大学学报(地球科学版), 36(5):830-836. http://d.old.wanfangdata.com.cn/Periodical/cckjdxxb200605020

卫文, 陈宗宇, 赵红梅, 等, 2011.河北平原第四系承压水⁴He与¹⁴C测年对比.吉林大学学报(地球科学版), 41(4):1144-1150. http://d.old.wanfangdata.com.cn/Periodical/cckjdxxb201104026

魏兴, 周金龙, 乃尉华, 等, 2019.新疆喀什三角洲地下水化学特征及演化规律.环境科学, 40(9):4042-4051. http://d.old.wanfangdata.com.cn/Periodical/hjkx201909023

解巧明, 王震亮, 尹成明, 等, 2019.塔里木盆地西南坳陷英吉沙与皮山地区构造演化特征及对油气成藏的影响.石油实验地质, 41(2):165-175. http://d.old.wanfangdata.com.cn/Periodical/sysydz201902003

杨丽芝, 张光辉, 刘中业, 等, 2009.鲁北平原地下水同位素年龄及可更新能力评价.地球学报, 30(2):235-242. http://d.old.wanfangdata.com.cn/Periodical/dqxb200902012

於昊天, 马腾, 邓娅敏, 等, 2017.江汉平原东部地区浅层地下水水化学特征.地球科学, 42(5):685-692. doi: 10.3799/dqkx.2017.056

袁瑞强, 龙西亭, 王鹏, 等, 2015.白洋淀流域地下水更新速率.地理科学进展, 34(3):381-388. http://d.old.wanfangdata.com.cn/Periodical/dlkxjz201503013

翟远征, 王金生, 周俊, 2013.北京市潮白河冲洪积扇地下水流动和更新模式的水化学和同位素标记.应用基础与工程科学学报, 21(1):32-44. http://d.old.wanfangdata.com.cn/Periodical/yyjcygckxxb201301004

Relative Articles

Supplements(0)

Cited By

Proportional views

Proportional views

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

Figures(4) / Tables(5)

Get Citation

PDF

XML

Article views (981) PDF downloads(66)

Hydrochemical and Isotopic Markers of Groundwater Flow Systems in the Kashgar Delta Area in Xinjiang

doi: 10.3799/dqkx.2019.177

Abstract

References

Proportional views

Catalog

通讯作者: 陈斌, bchen63@163.com

Proportional views

Export File

Citation

Format

Content