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Geological CO_2 Storage Supports Geothermal Energy Exploitation: 3D Numerical Models Emphasize Feasibility of Synergetic Use

机译:地质CO_2存储支持地热能开发:3D数值模型强调协同使用的可行性

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Geological storage of CO_2 in deep saline aquifers is considered as option for reducing anthropogenic greenhouse gas emissions into the atmosphere. Most often the same aquifers might allow for provision of geothermal energy potentially resulting in a competitive situation. Within the frame of the present study we evaluated the feasibility of synergetic utilisation of a reservoir suitable for both, CO_2 storage and geothermal heat exploitation, by 3D numerical simulations of simultaneous CO_2 and brine (re-) injection and brine production. Based on structural and petrophysical data from a prospective storage site in the North East German Basin different scenarios were investigated taking into account reservoir permeability anisotropy and varying flow related descriptions of existing faults. Simulation results show that for an isotropic horizontal permeability distribution synergetic use is feasible for at least 30 years. Nevertheless, permeability anisotropy and open faults do have an impact on the CO_2 arrival time at the brine production well and should be taken into account for implementation of a synergetic utilisation in the study area.
机译:深盐含水层中CO_2的地质储存被认为是将人为温室气体排放到大气中的选择性。最常见的含水层可能允许提供地热能可能导致具有竞争力的情况。在本研究的框架内,我们评估了适用于同时CO_2和盐水(RE-)注射和盐水生产的3D数值模拟的CO_2储存和地热剥离的储层协同利用的可行性。基于来自东北德国盆地的潜在储存地点的结构和岩石物理数据不同情景,考虑到储层渗透性各向异性和不同的流量相关的现有故障的相关描述。仿真结果表明,对于各向同性水平渗透性分布,协同用途至少可行至少30年。然而,渗透性各向异性和开放性故障确实对盐水生产的CO_2到达时间产生了影响,并且应考虑到研究区域中的协同利用。

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