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2020 , Vol. 37 >Issue 6: 775 - 783

DOI: https://doi.org/10.7523/j.issn.2095-6134.2020.06.008

地球科学

南水北调工程对华北平原水储量变化的影响

  • 李嘉 ,
  • 唐河 ,
  • 饶维龙 ,
  • 张岚 ,
  • 孙文科
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  • 中国科学院大学地球与行星科学学院 中国科学院计算地球动力学重点实验室, 北京 100049

收稿日期: 2019-12-27

  修回日期: 2020-03-17

  网络出版日期: 2020-11-15

基金资助

中国科学院前沿科学重点项目（QYZDY-SSWSYS003）和国家自然科学基金（41974093，41774088）资助

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Influence of South-to-North Water Transfer Project on the changes of terrestrial water storage in North China Plain

  • LI Jia ,
  • TANG He ,
  • RAO Weilong ,
  • ZHANG Lan ,
  • SUN Wenke
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  • Key Laboratory of Computational Geodynamics of CAS, College of Earth and Planetary Sciences, University of Chinese Academy of Sciences, Beijing 100049, China

Received date: 2019-12-27

  Revised date: 2020-03-17

  Online published: 2020-11-15

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摘要

南水北调工程自2014年底正式通水后对华北平原水储量亏损趋势的影响程度是一个尚未评估的科学问题。基于GRACE及GRACE Follow-on重力卫星观测数据计算华北平原水储量变化，并与南水北调输水量（3.08 Gt/a）进行对比，发现2004—2015年华北平原陆地水储量变化速率为（-5.92±0.53）Gt/a，2015—2019年变化速率有所抬升，变为（-2.96±2.79）Gt/a，表明华北平原陆地水储量亏损速率降低50%，长期亏损趋势得以明显缓解。同时，北京市和天津市的水量亏损趋势也明显改观。因此，南水北调工程显著改善了华北地区水资源紧张的局面，发挥了积极有效的重要作用。

关键词： 华北平原; 南水北调; 水储量; GRACE

本文引用格式

李嘉 , 唐河 , 饶维龙 , 张岚 , 孙文科 . 南水北调工程对华北平原水储量变化的影响[J]. 中国科学院大学学报, 2020 , 37(6) : 775 -783 . DOI: 10.7523/j.issn.2095-6134.2020.06.008

Abstract

The impact of the South-to-North Water Transfer Project on the terrestrial water storage (TWS) depletion in the North China Plain since the formal water supply at the end of 2014 has not been evaluated. Based on the data of GRACE and GRACE Follow-on gravity satellites, this paper calculates the changes of water storage in the North China Plain, and compares it with the water amount (3.08 Gt/a) supplied by the South-to-North Water Transfer Project. It is found that the change rate of TWS in the North China Plain from 2004 to 2015 is (-5.92±0.53) Gt/a, and the change rate in 2015-2019 is (-2.96±2.79) Gt/a. The results show that the change rate of TWS was decreased by 50%, and the trend of long-term depletion was alleviated obviously. At the same time, the trend of TWS in Beijing and Tianjin has also changed significantly. Therefore, the South-to-North Water Transfer Project had significantly improved the situation of TWS in North China, and played an active and effective role.

Key words： North China Plain; South-to-North Water Transfer Project; terrestrial water storage; GRACE

参考文献

[1] Liu C M, Y J J, Kendy E. Groundwater exploitation and its impact on the environment in the North China Plain[J]. Water International, 2001, 26(2):265-272.
[2] 张兆吉, 雒国中, 王昭, 等. 华北平原地下水资源可持续利用研究[J]. 资源科学, 2009, 31(3):355-360.
[3] Long D, Pan Y, Zhou J, et al. Global analysis of spatiotemporal variability in merged total water storage changes using multiple GRACE products and global hydrological models[J]. Remote Sensing of Environment, 2017(192):198-216.
[4] 常乐, 钱安, 易爽, 等. 基于卫星重力、卫星测高和温盐度综合数据的中国近海各区域海平面变化[J]. 中国科学院大学学报, 2017, 34(3):371-379.
[5] 许厚泽. 卫星重力研究:21世纪大地测量研究的新热点[J]. 测绘科学, 2001, 26(3):1-3.
[6] 孙文科. 低轨道人造卫星(CHAMP、GRACE、GOCE)与高精度地球重力场:卫星重力大地测量的最新发展及其对地球科学的重大影响[J]. 大地测量与地球动力学, 2002, 22(1):92-100.
[7] Tapley B D, Bettadpur S, Ries J C, et al. GRACE measurements of mass variability in the Earth system[J]. Science, 2004, 305(5683):503-505.
[8] Famiglietti J S, Lo M, Ho S L, et al. Satellites measure recent rates of groundwater depletion in California's Central Valley[J]. Geophysical Research Letters, 2011, 38(3):403-406.
[9] 钟敏, 段建宾, 许厚泽, 等. 利用卫星重力观测研究近5年中国陆地水量中长空间尺度的变化趋势[J]. 科学通报, 2009, 54(9):1290-1294.
[10] Feng W, Zhong M, Lemoine J M, et al. Evaluation of groundwater depletion in North China using the gravity recovery and climate experiment (GRACE) data and ground-based measurements[J]. Water Resources Research, 2013, 49(4):2110-2118.
[11] Huang Z, Pan Y, Gong H, et al. Subregional-scale groundwater depletion detected by GRACE for both shallow and deep aquifers in North China Plain[J]. Geophysical Research Letters, 2015, 42(6):1791-1799.
[12] Gong H, Pan Y, Zheng L, et al. Long-term groundwater storage changes and land subsidence development in the North China Plain (1971-2015)[J]. Hydrogeology Journal, 2018, 26(5):1417-1427.
[13] Zhao Q, Zhang B, Yao Y B, et al. Geodetic and hydrological measurements reveal the recent acceleration of groundwater depletion in North China Plain[J]. Journal of Hydrology, 2019(575):1065-1072.
[14] 王建华, 赵建世, 李海红, 等. 南水北调水资源综合配置研究[M]. 北京:科学出版社,2013:183-188.
[15] 北京市水务局. 北京市水资源公报(2018年度)[EB/OL]. 北京:北京市水务局, 2018.[2020-03-06]. http://swj.beijing.gov.cn/zwgk/szygb/.
[16] 天津市水务局. 2018年天津市水资源公报[EB/OL]. 天津:天津市水务局, 2018.[2020-03-06]. http://swj.tj.gov.cn/swj/.
[17] 水利部海河水利委员会. 2018年海河流域水资源公报[EB/OL]. 北京:水利部海河水利委员会, 2019.[2020-03-06]. http://www.hwcc.gov.cn/.
[18] Cheng M K, Tapley B D. Variations in the Earth's oblateness during the past 26 years[J]. Journal of Geophysical Research:Solid Earth, 2004, 109(B9):402-410.
[19] Swenson S, Chambers D, Wahr J. Estimating geocenter variations from a combination of GRACE and ocean model output[J]. Journal of Geophysical Research:Solid Earth, 2008, 113(B8):410-421.
[20] Wahr J, Molenaar M, Bryan F. Time variability of the Earth's gravity field:hydrological and oceanic effects and their possible detection using GRACE[J]. Journal of Geophysical Research:Solid Earth, 1998, 103(B12):30205-30230.
[21] 冯伟, 王长青, 穆大鹏, 等. 基于GRACE的空间约束方法监测华北平原地下水储量变化[J]. 地球物理学报, 2017, 60(5):1630-1642.
[22] Foster S, Garduno H, Evans R, et al. Quaternary aquifer of the North China Plain:assessing and achieving groundwater resource sustainability[J]. Hydrogeology Journal, 2004, 12(1):81-93.
[23] 钱永, 张兆吉, 费宇红, 等. 华北平原浅层地下水可持续利用潜力分析[J]. 中国生态农业学报, 2014, 22(8):890-897.
[24] Swenson S, Wahr J. Methods for inferring regional surface-mass anomalies from gravity recovery and climate experiment (GRACE) measurements of time-variable gravity[J]. Journal of Geophysical Research, 2002, 107(B9):2193-2205.
[25] Klees R, Zapreeva E A, Winsemius H C, et al. The bias in GRACE estimates of continental water storage[J]. Hydrology and Earth System Sciences, 2007(11):1227-1241.
[26] Landerer F W, Swenson S C. Accuracy of scaled GRACE terrestrial water storage estimates[J]. Water Resources Research, 2012, 48(4):531-541.
[27] Rodell M, Velicogna I, Famiglietti J S. Satellite-based estimates of groundwater depletion in India[J]. Nature, 2009, 460(7258):999-1002.
[28] Su X L, Ping J S, Ye Q X. Terrestrial water variations in the North China Plain revealed by the GRACE mission[J]. Science China Earth Sciences, 2011, 54(12):1965-1970.
[29] Moiwo J P, Tao F, Lu W. Analysis of satellite-based and in situ hydro-climatic data depicts water storage depletion in North China Region[J]. Hydrological Processes, 2013, 27(7):1011-1020.
[30] Feng W, Shum C, Zhong M, et al. Groundwater storage changes in China from satellite gravity:an overview[J], Remote Sensing, 2018, 10(5):674:698.
[31] Yi S, Wang Q, Sun W. Basin mass dynamic changes in China from GRACE based on a multi-basin inversion method[J]. Journal of Geophysical Research:Solid Earth, 2016, 121(5):3782-3803.
[32] Zhang L, Yi S, Wang Q Y, et al. Evaluation of GRACE mascon solutions for small spatial scales and localized mass sources[J]. Geophysical Journal Internal, 2019, 218(2):1307-1321.
[33] Rodell M, Houser P R, Jambor U, et al. The global land data assimilation system[J]. Bulletin of the American Meteorological Society, 2004, 85(3):381-394.
[34] Han Z S. Groundwater resources protection and aquifer recovery in China[J]. Environmental Geology, 2003, 44(1):106-111.
[35] 崔亚莉, 王亚斌, 邵景力, 等. 南水北调实施后华北平原地下水调控研究[J]. 资源科学, 2009, 31(3):382-387.
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