Ecology and Environment of Tarim River Basin

Estimation of riparian groundwater table depth in the lower reaches of Tarim River under long-term water conveyance

Expand
  • 1. State Key Laboratory of Earth Surface Processes and Resource Ecology, Faculty of Geographical Science, Beijing Normal University, Beijing 100875, China
    2. State Key Laboratory of Numerical Modeling for Atmospheric Sciences and Geophysical Fluid Dynamics (LASG), Institute of Atmospheric Physics, Chinese Academy of Sciences, Beijing 100029, China
    3. State Key Laboratory of Desert and Oasis Ecology, Xinjiang Institute of Ecology and Geography,Chinese Academy of Sciences, Urumqi 830011, Xinjiang, China

Received date: 2021-02-07

  Revised date: 2021-04-20

  Online published: 2021-06-01

Abstract

Accurate estimation of the groundwater table dynamic variation in a riparian zone under ecological water conveyance conditions is of great importance for the sustainable development of water resources management in arid areas. Based on the data of river discharges from ecological water conveyance and the groundwater tables of riparian monitoring wells from 2001 to 2020, this study simulated the dynamic variation of groundwater table at three sections of Yingsu, Alagan, and Yiganbujima in the lower reaches of the Tarim River, Xinjiang, China using a developed quasi-two-dimensional groundwater model, including the groundwater and soil water motion equations. In the calibration period, the observed groundwater table data was used to adjust the critical parameter (i.e., horizontal hydraulic conductivity) of the quasi-two-dimensional model, and the average simulation error of the monitoring wells at each of the three sections was approximately 0.2 m. In the validation period, the groundwater table data from 2011 to 2020 at the monitoring wells of the three sections were compared with the simulated results, and the average error at each of the three sections was approximately 0.5 m. Therefore, the simulated results of the groundwater table were acceptable under the lack of accurate river level data and the model was suitable for simulating the variation of the riparian groundwater table under ecological water conveyance in the lower reaches of the Tarim River. Thus, based on the simulation results from 2001 to 2020, the groundwater table and soil moisture variations were analyzed to demonstrate the response of riparian groundwater and soil moisture to the ecological water conveyance project. The results show that the groundwater table and soil moisture at the three sections evidently increased in 20 years of water conveyance periods. Specifically, the groundwater table increased from approximately 8 m before ecological water conveyance to nearly 4 m, and the corresponding soil moisture rose from 0.20 to 0.35 above. The increasing trend is more significant with the substantial increase of the annual water conveyance amount since 2009. Moreover, the variation of groundwater table presented a certain lag following the change in the water conveyance amount, and a positive correlation between soil moisture and groundwater table makes the soil moisture lags behind the water conveyance amount. Compared with the river discharge, the groundwater hydraulic conductivity plays a more important role in the variation of groundwater table at cross-section; thus, increasing the upswing amplitude of the groundwater table at Yiganbujima sections of the lower segment compared with that of the Alagan section of the middle segment in lower reaches of the Tarim River. Additionally, the inter-annual variations of groundwater and water conveyance amount also indicate that the intermittent ecological water conveyance is essential to achieve a sustainable ecological benefit in the lower reaches of the Tarim River.

Cite this article

DI Zhenhua,XIE Zhenghui,CHEN Yaning . Estimation of riparian groundwater table depth in the lower reaches of Tarim River under long-term water conveyance[J]. Arid Land Geography, 2021 , 44(3) : 659 -669 . DOI: 10.12118/j.issn.1000–6060.2021.03.08

References

[1] 陈亚宁, 张小雷, 祝向民, 等. 新疆塔里木河下游断流河道输水的生态效应分析[J]. 中国科学: D辑, 2004,34(5):475-482.
[1] [ Chen Yaning, Zhang Xiaolei, Zhu Xiangmin, et al. Analysis on the ecological benefits of the stream water conveyance to the dried-up river of the lower reaches of Tarim River, China[J]. Science in China: Series D, 2004,34(5):475-482. ]
[2] Chen Y, Li W, Xu C, et al. Desert riparian vegetation and groundwater in the lower reaches of the Tarim River Basin[J]. Environmental Earth Sciences, 2015,73(2):547-558.
[3] 马跃. 塔里木河下游生态输水对植被和地下水位的影响[J]. 生态环境与保护, 2020,3(4):37.
[3] [ Ma Yue. Effects of ecological water transport on vegetation and groundwater level in the lower reaches of Tarim River[J]. Ecological Environment and Protection, 2020,3(4):37. ]
[4] Ling H, Zhang P, Guo B, et al. Negative feedback adjustment challenges reconstruction study from tree rings: A study case of response of Populus euphratica to river discontinuous flow and ecological water conveyance[J]. Science of the Total Environment, 2017,574:109-119.
[5] Mamat Z, Halik U, Keyimu M, et al. Variation of the floodplain forest ecosystem service value in the lower reaches of Tarim River, China[J]. Land Degradation and Development, 2018,29:47-57.
[6] Zhou H, Chen Y, Hao X, et al. Tree rings: A key ecological indicator for reconstruction of groundwater depth in the lower Tarim River, northwest China[J]. Ecohydrology, 2019,12:e2142, doi: 10.1002/eco.2142.
[7] Liao S, Xue L, Dong Z, et al. Cumulative ecohydrological response to hydrological processes in arid basins[J]. Ecological Indicators, 2020,111:106005, doi: 10.1016/j.ecolind.2019.106005.
[8] 秦景秀, 郝兴明, 张颖, 等. 气候变化和人类活动对干旱区植被生产力的影响[J]. 干旱区地理, 2020,43(1):117-125.
[8] [ Qin Jingxiu, Hao Xingming, Zhang Ying, et al. Effects of climate change and human activities on vegetation productivity in arid areas[J]. Arid Land Geography, 2020,43(1):117-125. ]
[9] 孙天瑶, 李雪梅, 许民, 等. 2000—2018年塔里木河流域植被覆盖时空格局[J]. 干旱区地理, 2020,43(2):415-424.
[9] [ Sun Tianyao, Li Xuemei, Xu Min, et al. Spatial temporal variations of vegetation coverage in the Tarim River Basin from 2000 to 2018[J]. Arid Land Geography, 2020,43(2):415-424. ]
[10] 陈亚宁. 新疆塔里木河流域生态保护与可持续管理[M]. 北京: 科学出版社, 2015.
[10] [ Chen Yaning. Ecological protection and sustainable management of the Tarim River Basin[M]. Beijing: Science Press, 2015. ]
[11] 徐海量, 樊自立, 杨鹏年, 等. 塔里木河近期治理评估及对编制流域综合规划的建议[J]. 干旱区研究, 2016,33(2):223-229.
[11] [ Xu Hailiang, Fan Zili, Yang Pengnian, et al. Evaluation on the management of Tarim River and advices for the future planning of the Tarim River Basin[J]. Arid Zone Research, 2016,33(2):223-229. ]
[12] 陈亚宁, 李卫红, 陈亚鹏, 等. 科技支撑新疆塔里木河流域生态修复及可持续管理[J]. 干旱区地理, 2018,41(5):901-907.
[12] [ Chen Yaning, Li Weihong, Chen Yapeng, et al. Science in supporting the ecological restoration and sustainable development of the Tarim River Basin[J]. Arid Land Geography, 2018,41(5):901-907. ]
[13] 陈亚宁, 李卫红, 陈亚鹏, 等. 新疆塔里木河下游断流河道输水与生态恢复[J]. 生态学报, 2007,27:538-545.
[13] [ Chen Yaning, Li Weihong, Chen Yapeng, et al. Water conveyance in dried-up riverway and ecological restoration in the lower reaches of Tarim River, China[J]. Acta Ecological Sinica, 2007,27(2):538-545. ]
[14] 湾疆辉, 陈亚宁, 李卫红, 等. 塔里木河下游断流河道输水后潜水埋深变化规律研究[J]. 干旱区地理, 2008,31(3):428-435.
[14] [ Wan Jianghui, Chen Yaning, Li Weihong, et al. Variation of groundwater level after ecological water transport in the lower reaches of the Tarim River in recent six years[J]. Arid Land Geography, 2008,31(3):428-435. ]
[15] 刘迁迁, 古力米热?哈那提, 苏里坦, 等. 塔里木河下游河岸带地下水埋深对生态输水的响应过程[J]. 干旱区地理, 2017,40(5):979-986.
[15] [ Liu Qianqian, Gulimire Hanati, Sulitan, et al. Response process of groundwater table to ecological water conveyance in the lower reaches of Tarim River riparian zone[J]. Arid Land Geography, 2017,40(5):979-986. ]
[16] 李丽君, 张小清, 陈长清, 等. 近20 a塔里木河下游输水对生态环境的影响[J]. 干旱区地理, 2018,41(2):238-247.
[16] [ Li Lijun, Zhang Xiaoqing, Chen Changqing, et al. Ecological effects of water conveyance on the lower reaches of Tarim River in recent twenty years[J]. Arid Land Geography, 2018,41(2):238-247. ]
[17] 刘斌, 赵雅莉, 白洁, 等. 塔里木河下游流域输水工程生态效应评价研究[J]. 地理空间信息, 2020,18(3):112-117.
[17] [ Liu Bin, Zhao Yali, Bai Jie, et al. Ecological effect evaluation of water conveyance project in lower reaches of Tarim River[J]. Geospatial Information, 2020,18(3):112-117. ]
[18] 杨鹏年, 邓铭江, 董新光, 等. 间歇输水河道两侧一维地下水非稳定流运动研究——以塔里木河下游为例[J]. 干旱区地理, 2008,31(5):731-736.
[18] [ Yang Pengnian, Deng Mingjiang, Dong Xinguang, et al. 1D groundwater transient movement of intermittent water transmitting[J]. Arid Land Geography, 2008,31(5):731-736. ]
[19] 刘迁迁, 古力米热?哈那提, 王光焰, 等. 间歇性生态输水塔里木河下游断面地下水位变化模拟[J]. 生态学报, 2018,38(15):5519-5528.
[19] [ Liu Qianqian, Gulimire Hanati, Wang Guangyan, et al. Simulation of sectional groundwater level variation in the lower reaches of Tarim River under intermittent ecological water conveyance[J]. Acta Ecologica Sinica, 2018,38(15):5519-5528. ]
[20] 古力米热?哈那提, 张音, 关东海, 等. 生态输水条件下塔里木河下游断面尺度地下水流数值模拟[J]. 水科学进展, 2020,31(1):61-70.
[20] [ Gulimire Hanati, Zhang Yin, Guan Donghai, et al. Numerical simulation of groundwater flow at cross-section scale in the lower reaches of Tarim River under the condition of ecological water conveyance[J]. Advances in Water Science, 2020,31(1):61-70. ]
[21] 狄振华, 谢正辉, 袁星, 等. 输水条件下考虑土壤水和地下水相互作用的河流剖面地下水埋深估计方法[J]. 中国科学: 地球科学, 2010,40(10):1420-1430.
[21] [ Di Zhenhua, Xie Zhenghui, Yuan Xing, et al. Prediction of water table depths under soil water-groundwater interaction and stream water conveyance[J]. Science in China: Series D, 2010,40(10):1420-1430. ]
[22] 谢正辉, 罗振东, 曾庆存, 等. 非饱和土壤水流问题含水量和通量的数值模拟研究[J]. 自然科学进展, 1999,9(12):1280-1286.
[22] [ Xie Zhenghui, Luo Zhendong, Zeng Qingcun, et al. Numerical simulation of water content and flux in unsaturated soil flow problems[J]. Progress in Natural Science, 1999,9(12):1280-1286. ]
[23] 钱亦兵, 周华荣, 赵锐锋, 等. 塔里木河中下游湿地及其周边土壤理化性状的空间异质性[J]. 水土保持学报, 2005,19(6):31-34.
[23] [ Qian Yibing, Zhou Huarong, Zhao Ruifeng, et al. Spatial heterogeneity of soil physical-chemical properties for wetlands and surrounding lands in middle and lower reaches of Tarim River[J]. Journal of Soil and Water Conservation, 2005,19(6):31-34. ]
[24] 汪亮亮, 叶茂, 高生峰, 等. 水热因子对塔里木河下游胡杨年轮指数和植被指数的影响[J]. 南京林业大学学报(自然科学版), 2017,41(5):85-91.
[24] [ Wang Liangliang, Ye Mao, Gao Shengfeng, et al. Effects of hydrothermal factors on vegetation index and tree-ring index of Populus euphratica in the lower reaches of the Tarim River[J]. Journal of Nanjing Forestry University (Natural Science Edition), 2017,41(5):85-91. ]
[25] 马晓东, 李卫红, 朱成刚, 等. 塔里木河下游土壤水分与植被时空变化特征[J]. 生态学报, 2010,30(5):4035-4045.
[25] [ Ma Xiaodong, Li Weihong, Zhu Chenggang, et al. Spatio-temporal variation in soil moisture and vegetation along the lower reaches of Tarim River, China[J]. Acta Ecologica Sinica, 2010,30(5):4035-4045. ]
[26] Dickison R E, Henderson-sellers A, Kennedy P J, et al. Biosphere atmosphere transfer scheme (BATS) for NCAR community climate model[R]. NCAR Technical Note, NCAR/TN 275+STR, 1986.
[27] Clapp R B, Hornberger G M. Empirical equation for some soil hydraulic properties[J]. Water Resources Research, 1978,14:601-604.
[28] Duan Q, Gupta V K, Sorooshian S. Effective and efficient global optimization for conceptual rainfall-runoff model[J]. Water Resources Research, 1992,28:1015-1031.
[29] 白元, 徐海量, 张青青, 等. 基于地下水恢复的塔里木河下游生态需水量估算[J]. 生态学报, 2015,35(3):630-640.
[29] [ Bai Yuan, Xu Hailiang, Zhang Qingqing, et al. Evaluation on ecological water requirement in the lower reaches of Tarim River based on groundwater restoration[J]. Acta Ecologica Sinica, 2015,35(3):630-640. ]
[30] 郭红雨. 塔里木河下游生态输水工程对地下水位变化的影响分析[J]. 西北水电, 2020,185(5):29-32.
[30] [ Guo Hongyu. Analysis of the impact of the ecological water delivery project on the change of groundwater level in the lower reaches of the Tarim River[J]. Northwest Hydropower, 2020,185(5):29-32. ]
Outlines

/