Journal of Jilin University(Earth Science Edition) ›› 2019, Vol. 49 ›› Issue (3): 773-783.doi: 10.13278/j.cnki.jjuese.20170304

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Temperature Tracing Method for Groundwater Flux Under Surface Warming

Dong Linyao1,2, Ren Hongyu1,2, Lei Junshan3, Liu Jigen1,2   

  1. 1. Changjiang River Scientific Research Institute, Changjiang Water Resources Commission, Wuhan 430010, China;
    2. Research Center on Mountain Torrents and Geological Disaster Prevention, Ministry of Water Resources, Wuhan 430010, China;
    3. Changjiang Water Resources Protection Institute, Changjiang Water Resources Commission, Wuhan 430051, China
  • Received:2017-12-15 Online:2019-06-03 Published:2019-06-03
  • Supported by:
    Supported by National Natural Science Foundation of China (41501037) and Technology Demonstration Project of Ministry of Water Resources(SF-201806)

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Abstract: In order to construct the technical system of groundwater velocity calculation using heat Abstract:A least square solver was presented for groundwater flux estimation in one-dimensional conduction advection equation solved numerically with MacCormack scheme. This approach was utilized to estimate the groundwater fluxes of the observed borehole under the effect of ground surface temperature (GST) in both rural and urban areas in Leizhou Peninsula, China. The estimated average groundwater recharge rate is 0.796 m/a, while the average discharge rate is 0.269 m/a. The groundwater recharges occur in the north part of the study area; while the discharges occur near Nansan, Donghai and Luzhou Islands, which fit favorably with the local groundwater flow pattern. Relatively high correlations and low RMSE were detected between the observed and computed borehole temperature-depth profiles, indicating that the estimation is reasonable. The sensitivity analysis of surface temperature and thermal diffusivity of geological bodies and GST indicates that the evaluation of subsurface heat island effects is very important for improving the precision of groundwater flux estimation by using borehole temperatures.

Key words: heat tracer, groundwater flux, surface warming, numerical solution, Leizhou Peninsula

CLC Number: 

  • P641.2
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