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裂隙岩体渗透率与应力耦合对EGS采热性能的影响

Effects of permeability evolution on EGS hot mining performance

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在增强型地热系统(enhanced geothermal system,EGS)热开采过程中,储层渗透率受应力的影响而动态变化.为揭示裂隙岩体渗透特性和应力之间的耦合作用对系统采热性能的影响,建立双重介质热流固(thermo-hydro-mechanical,THM)耦合模型,分析基质和裂隙渗透率随应力动态变化时储层THM三场变化规律.结果表明:在热应力与水压力共同作用下,基质渗透率逐渐减小,裂隙渗透率呈指数式增加,采热速率主要由裂隙渗透率的动态变化决定,但如果忽略基质渗透率的动态变化,预测的裂隙渗透率比实际提高41.8%,热突破时间提前,会低估近2年的系统运行寿命.因此,同时考虑裂隙和基质渗透率与应力的耦合作用对合理评价EGS系统使用寿命有重要意义.
During the thermal exploitation of enhanced geothermal system(EGS),reservoir permeability varies dynamically under the influence of stress.In order to reveal the coupling mechanism between the permeability of fractured rock matrix and stress field and its influence on the performance of heat mining,a thermo-hydro-mechanical(THM)coupling model of dual mediums including matrix and fracture was established based on the THM coupling theory,and the THM field of the reservoir is analyzed when the matrix and fracture permeability change with the stress.The results show that under the combined action of thermal stress and water pressure,the matrix permeability decreases gradually,and the fracture permeability increases exponentially.Hence,the rate of recovery heat is mainly determined by the dynamic changes of the fracture permeability.However,the predicted fracture permeability is 41.8%higher than the actual permeability if the dynamic changes of the matrix permeability is ignored during the simulation.As a result,the predicted heat breakthrough time is advanced,which would underestimate the system running life of nearly two years.Therefore,it is significant to evaluate the service life of EGS system to consider the coupling effect of fracture and matrix permeability and stress simultaneously.

enhanced geothermal systemthermo-hydro-mechanical couplingpermeabilitystress

何适、李春林、孙可明

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辽宁工程技术大学力学与工程学院,123000阜新

煤炭科学研究总院,100013北京

煤炭科学技术研究院有限公司安全分院,100013北京

青岛理工大学理学院,266033青岛

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增强型地热系统 热流固耦合 渗透率 应力

2024

应用力学学报
西安交通大学

应用力学学报

CSTPCD北大核心
影响因子:0.398
ISSN:1000-4939
年,卷(期):2024.41(4)
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