Vertical groundwater flux estimation from borehole temperature profiles by a numerical model, RFLUX. Issue 11 (2nd April 2019)

• Record Type: Journal Article
• Authors: Li, Shaoheng; Dong, Linyao; Chen, Jianyao; Li, Rui; Yang, Zhigang; Liang, Zuobing
• Is Part Of: Hydrological processes. Volume 33:Issue 11(2019)
• Page Start: 1542
• Page End: 1552
• Publication Date: 2019-04-02
• Subjects: groundwater -- heat tracer -- Leizhou Peninsula -- nonlinear initial condition -- numerical model -- observed GST and SAT -- surface warming -- velocity estimation; Hydrology -- Periodicals; Hydrology -- Research -- Periodicals; Hydrologic models -- Periodicals; Hydrological forecasting -- Periodicals; 631.432
• DOI: 10.1002/hyp.13420
• Languages: English
• ISSNs: 0885-6087

Abstract

Abstract: We developed a numerical model, RFLUX, which uses the heat tracer method for vertical groundwater flux estimation, and applied it to the Leizhou Peninsula, South China, to provide information to inform local groundwater resource utilization and management. The temperature–depth (TD) profiles of 24 boreholes, along with the observed ground surface temperature (GST) and surface air temperature (SAT) series in recent decades, were collected in this area. Underground TD data demonstrated the capacity to identify groundwater flow patterns, and local GST and SAT data demonstrated a strong correlation with each other over monthly, seasonal, and annual scales. In the RFLUX model, the average GST and SAT series were applied as an upper boundary condition, and a nonlinear initial condition was set using an analytical solution from the literature. The model results of selected TD profiles demonstrated that the annual vertical groundwater flux was about 0.15 m a −1, which tended to be overestimated if a linear initial condition was used. This model can be easily applied with minor modifications, considering its clear purpose and simplicity.