GRACE-based monitoring groundwater change in coal mining areas

被引:0
|
作者
Li S. [1 ,2 ]
Shi P. [1 ,3 ]
Gu X. [1 ,2 ]
Fu X. [2 ]
Ni S. [4 ]
Zhang N. [1 ,2 ]
机构
[1] Henan Key Laboratory of Ecological Environment Protection and Restoration of Yellow River Basin, Zhengzhou
[2] Yellow River Institute of Hydraulic Research, Yellow River Conservancy Commission, Zhengzhou
[3] College of Hydrology and Water Resources, Hohai University, Nanjing
[4] Nanjing Hydraulic Research Institute, Nanjing
来源
关键词
Coal mine; GLDAS; GRACE; Groundwater variation; Middle Yellow River;
D O I
10.13243/j.cnki.slxb.20210076
中图分类号
学科分类号
摘要
An extensive coal mining in the middle reaches of the Yellow River, a coal-rich area in China, has produced a relatively severe disruption of the groundwater which is an important water sources for living and production in the region. Therefore, it is fundamental to real time monitor the change of the groundwater. GRACE gravity satellite launched in 2002 has provided a new method for monitoring of a regional scale water storage change. An inverse analysis were carried out on the land water and groundwater storage of the Kuye River Basin, one of major tributaries of the Yellow River, using GRACE and GLDAS in 2009. Having compared precipitation, evaporation and the simulation results of GLDAS and surface-groundwater coupling model, it was found that GRACE can be used to monitor the change of groundwater storage in coal mining region. The land storage and groundwater reduced in 2009 are 15.5mm/m. and 29.4mm/m. respectively, compared with those of the basic period (2004-2009). The fractured water-conducting zones generated by coal mining have opened passages between soil water and groundwater. As a result, the change between them has noticeably related and their correlation coefficient is 0.84. © 2021, China Water Power Press. All right reserved.
引用
收藏
页码:1439 / 1448
页数:9
相关论文
共 45 条
  • [11] WEI F, SHUM C K, MIN Z, Et al., Groundwater storage changes in China from satellite gravity: an overview, International Journal of Remote Sensing
  • [12] WONDWOSEN M S, ADAM M M., Monitoring and comparison of terrestrial water storage changes in the northern high plains using GRACE and in-situ based integrated hydrologic model estimates, Advances in Water Re-sources, 94, pp. 31-44, (2016)
  • [13] NAVEED I, FAISAL H, HYONGKI L, Et al., Satellite gravimetric estimation of groundwater storage variations over Indus Basin in Pakistan, IEEE Journal of Selected Topics in Applied Earth Observations and Remote Sensing, 9, 8, pp. 3524-3534, (2016)
  • [14] OUYANG W, LIN B, WU Y Y., Satellite-based estimation of watershed groundwater storage dynamics in a freeze-thaw area under intensive agricultural developmen, Journal of Hydrology, 537, pp. 96-105, (2016)
  • [15] PASCALL C, RICHARD M, ALFONS R, Et al., Groundwater depletion in Central Mexico: Use of GRACE and InSAR to support water resources managemen, Water Resources Research, 52, 8, pp. 5985-6003, (2015)
  • [16] AHMED M Y, MOHAMED A A, AHMED E H., Assessing groundwater storage changes in the Nubian aquifer us-ing GRACE data, Arabian Journal of Geosciences, 9, 10, pp. 567-576, (2016)
  • [17] 34, (2012)
  • [18] SOUMENDRA N B, ABHIJIT M, DIPANKAR S, Et al., Validation of GRACE based groundwater storage anoma-ly using in-situ groundwater level measurements in India, Journal of Hydrology, 543, pp. 729-738, (2016)
  • [19] LONG D, SCANLON R B, LONGUEVEERGNE L, Et al., GRACE satellite monitoring of large depletion in water storage in response to the 2011 drought in Texas, Geophysical Research Letters, 40, 13, pp. 3395-3401, (2013)
  • [20] JOODAKI G, WAHR J, SWENSON S., Estimating the Human Contribution to groundwater depletion in the Mid-dle East from GRACE data, land surface models, and well observations, Water Resources Research, 50, 3, pp. 2679-2692, (2014)