储层压力和示踪响应联合诊断方法:估算储层模型准确性的实验和理论研究

IF 1.2 4区 地球科学 Q3 GEOCHEMISTRY & GEOPHYSICS Geofluids Pub Date : 2024-04-13 DOI:10.1155/2024/9329314
Mitsuo Matsumoto, Kazuki Sawayama
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引用次数: 0

摘要

本研究提出了一个新的视角,通过联合诊断常规压力瞬变和示踪测试的响应,提高对地热勘探区渗透结构的认识。压力和示踪响应分别产生表观孔隙度-厚度乘积。它们之间的差异意味着储层模型中存在未知的死角特征。实验室实验和数值模拟验证了这一概念。在假设勘探中的潜在应用表明,根据压力和示踪剂响应确定的孔隙度-厚度乘积的对数比值表明了储层模型的准确性,该模型将随着勘探的进展而不断更新。如果允许假设不同的孔隙厚度乘积分别再现压力和示踪剂响应,则无论渗透结构的精度如何,储层模型都能成功再现合成观测结果。只有当储层模型正确捕捉到渗透结构时,这些孔隙度-厚度乘积才会重合。这一新颖的视角将为成功勘探和开发地热资源以及潜在的一般地球流体资源提供战略指导。
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Joint Diagnostic Approach to Pressure and Tracer Responses from Reservoirs: An Experimental and Theoretical Study to Estimate the Accuracy of Reservoir Models

This study presents a novel perspective for improving the understanding of permeable structures at geothermal prospects by jointly diagnosing the responses of conventional pressure transient and tracer testing. The pressure and tracer responses individually yield apparent porosity–thickness products. The difference between them implies the existence of unknown dead-end features involved in a reservoir model. Laboratory experiments and numerical simulations validate this concept. Potential application to hypothetical exploration demonstrates that the logarithmic ratio of the porosity–thickness products, determined based on pressure and tracer responses, indicates the accuracy of the reservoir model to be successively updated with the progress of the exploration. The reservoir model successfully reproduced the synthetic observations regardless of the accuracy of permeable structure if different porosity–thickness products were allowed to be assumed to individually reproduce pressure and tracer responses. These porosity–thickness products coincided only if the reservoir model correctly captured the permeable structure. This novel perspective will provide strategic guides for successful exploration and development at the prospects of geothermal and, potentially, general geofluid resources.

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来源期刊
Geofluids
Geofluids 地学-地球化学与地球物理
CiteScore
2.80
自引率
17.60%
发文量
835
期刊介绍: Geofluids is a peer-reviewed, Open Access journal that provides a forum for original research and reviews relating to the role of fluids in mineralogical, chemical, and structural evolution of the Earth’s crust. Its explicit aim is to disseminate ideas across the range of sub-disciplines in which Geofluids research is carried out. To this end, authors are encouraged to stress the transdisciplinary relevance and international ramifications of their research. Authors are also encouraged to make their work as accessible as possible to readers from other sub-disciplines. Geofluids emphasizes chemical, microbial, and physical aspects of subsurface fluids throughout the Earth’s crust. Geofluids spans studies of groundwater, terrestrial or submarine geothermal fluids, basinal brines, petroleum, metamorphic waters or magmatic fluids.
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