Using GMS modeling method: calculation of potential exploitation of groundwater in Bac Lieu Province, Vietnam
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https://doi.org/10.15625/1859-3097/22789Keywords:
Potentially exploitable reserves, groundwater, middle-upper Pleistocene aquifer (qp2–3), lower Pleistocene (qp1), GMS model, Bac Lieu ProvinceAbstract
The paper presents the results of research on assessing and determining the potential groundwater exploitation reserves in Bac Lieu Province, the middle-upper Pleistocene aquifer (qp2–3) and the lower Pleistocene aquifer (qp1) using a numerical model. The authors used GMS (Groundwater Modeling System) software to model aquifers, assign calibrated hydrogeological parameter values, input water level and exploitation data up to 2030, and determine groundwater reserves, sources of groundwater reserves, and water level reductions. Model results show that the water level of the qp2–3 aquifer in 2030 at the monitoring borehole Q597030 is -14.5 m, lower than in 2011, 2015, and 2023 by 7.98, 6.07, and 0.502, respectively. Similarly, for the qp1 aquifer, the water level at monitoring borehole Q597040 is -15.994 m, lower than 2011, 2015, and 2023 by 6.93, 5.885, and 1.994, respectively. The potentially exploitable reserves of fresh and saline groundwater of the qp2–3 aquifer in 2023 and 2030 will decrease by 3,120.6 and 527.35 m3/day, respectively. The total potential exploitable reserves of the qp2–3 aquifer in 2023 and 2030 will be 409,937.37 and 406,279.35 m3/day, respectively. The potential exploitable reserves of the qp1 aquifer in the freshwater area in 2023 and 2030 will decrease by 6,077.08 m3/day. The potentially exploitable reserves of the qp1 aquifer in 2023 and 2030 will be 74,603.69 and 68,526.61 m3/day, respectively. Based on the results of the study on potential exploitable groundwater reserves in the study area, this approach is applied to effectively manage and plan groundwater exploitation in Bac Lieu province.
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