保加利亚中北部上侏罗纪-下白垩纪含水层的热势:条件和潜在用途

IF 0.2 Q4 GEOSCIENCES, MULTIDISCIPLINARY
P. Gerginov, N. Stoyanov, S. Valtchev, A. Benderev
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引用次数: 0

摘要

保加利亚北部的区域水文地质条件决定了一个由分层含水层组成的大型自流盆地的存在。地下水温度随深度升高,较深层的条件有利于形成层状热液储层,具有采热潜力。虽然这种绿色能源的利用始于20世纪80年代,但目前仍处于预可行性阶段。上侏罗统—下白垩统含水层产量最高,是保加利亚中北部多层沉积杂岩中最有前景的地热资源。该研究为该层的形成和热采潜力提供了新的认识,该层具有低温热液储层的所有特征。研究内容包括边界圈定、水文地质和热力参数评价以及水力连通性数据。对该流域的流量场和温度场、水热平衡要素以及地下水水质进行了评价。在区域尺度上对热液储层的地下水和热能资源进行了估算,包括回注情景。提出了利用回注井对热能进行潜在利用的不同方案。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Heat potential of the Upper Jurassic–Lower Cretaceous aquifer in Central Northern Bulgaria: conditions and prospective use
The regional hydrogeological conditions in Northern Bulgaria determine the existence of a large artesian basin consisting of layered aquifers. The groundwater temperature increase with depth and the conditions in the deeper layers are favourable for the formation of stratified hydrothermal reservoirs with potential for heat extraction. Although it was initiated in the 1980s, the utilization of this green energy resource is still in a pre-feasibility phase. The Upper Jurassic–Lower Cretaceous aquifer has the highest yield and it is the most prospective geothermal source in the multi-layered sedimentary complex in Central Northern Bulgaria. This study provides new understanding of the formation and potential for extraction of thermal energy from this stratum, which has all characteristics of a low temperature hydrothermal reservoir. The study includes delineation of its boundaries, evaluation of hydrogeological and thermal parameters and data on hydraulic connectivity. The flow and temperature fields, the elements of the water and heat balance, as well as the groundwater quality, have been assessed. The groundwater and thermal energy resources in the hydrothermal reservoir have been estimated on a regional scale, including a scenario with reinjection. Different options for potential utilization of the thermal energy using reinjection wells have been put forward.
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