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Three-Dimensional Estimation of Geothermal Potential from Geological Field Data: The Limagne Geothermal Reservoir Case Study (France)

机译:地质现场数据的地热势三维估计:杉龙地热储层案例研究(法国)

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This study presents a methodology for estimating geothermal potential from geological field data in a sedimentary formation. The first step is dedicated to better understand the geometry of geology of the target zone using various data such as field measurements, bore holes and geophysical data. These data are reinterpreted through the construction of a 3D geological model. Inconsistencies are checked and turned into a coherent 3D interpretation by using the 3DGeoModeller software developed by BRGM. The second step consists in investigating the geothermal potential of the area. The geological model is meshed into a 3D unstructured Finite Element mesh using meshing capabilities from GEOWATT AG. Realistic thermal boundary conditions are applied and temperature field is computed using the Finite Element code FRACTure. As a final result, the total amount of geothermal energy available for each aquifer is computed, and the geothermal potential (recoverable energy) is mapped over the entire model. This methodology has been applied to assess the geothermal potential of a clastic reservoir in the Limagne d'Allier basin (Massif Central, France) where the most interesting geothermal target is identified as basal thick-sandstones overlying the crystalline basement. The total amount of recoverable energy in this aquifer is estimated to more than 500 PJ (10~(15) J) in the modelled area. The most energetic zones appear to be located at the north-western edges of the basin, where sediment infill is the thickest.
机译:本研究提出了一种用于估算沉积形成地质场数据的地热势的方法。第一步是使用诸如现场测量,钻孔和地球物理数据的各种数据更好地理解目标区域的几何形状。这些数据通过建造3D地质模型来重新解释。通过使用BRGM开发的3DGeomodeller软件,检查并转换为连贯的3D解释。第二步包括调查该地区的地热潜力。地质模型用来自Geowatt AG的啮合能力啮合到3D非结构化有限元网格中。施加现实的热边界条件,使用有限元码骨折计算温度场。作为最终结果,计算每个含水层可用的地热能总量,并且在整个模型上映射地热势(可恢复能量)。该方法已被应用于评估杉木D'Allier盆地(法国Massif Central,France)中碎屑储层的地热潜力,其中最有趣的地热靶标被鉴定为覆盖晶体地下室的基底厚砂岩。该含水层中可收回能量的总量估计在建模区域中超过500 pj(10〜(15)j)。最精力充沛的区域似乎位于盆地的西北边缘,其中沉积物填充是最厚的。

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