考虑非线性流动特性的裂隙岩体传热模拟OA
Heat transfer simulation of fractured rock mass considering nonlinear flow behavior
为解决现有模型对非线性流动考虑不足的问题,提出了一种基于有限体积方法的、考虑裂隙非线性流动特性的裂隙岩体热-水耦合数值模拟方法.首先,推导了Forchheimer流动和热传递方程的有限体积离散形式;随后,通过岩石基质与裂隙介质之间的流体质量/热量传递函数,将二者组装成一个非线性方程组,并采用直接迭代法求解;接着,通过相交裂隙模型检验了该方法模拟非线性流动的可靠性;最后,以澳大利亚Habanero地热储层为例,模拟了不同注入压力下的地热开采过程,研究了储层的采热效率.结果表明:高注入压力导致储层的生产寿命缩短,但随着注入压力的进一步增加,生产寿命会缩短至恒定值;Forchheimer流通过非线性惯性效应显著增加了流动阻力,导致高注入压力下实际流量低于线性流预测值,并强化了流体在主要裂隙中的优势通道效应.该研究结果可为干热岩储层注采设计提供参考.
A finite volume method is proposed for the thermo-hydro coupling in fractured rock masses,which accounts for the nonlinear flow behavior in fractures.Firstly,the finite volume discrete formulations of the Forchheimer flow and heat transfer equations were derived.Then,these formulations were assembled into a system of nonlinear algebraic equations via flux/heat transfer functions between the fracture medium and the rock matrix,which was then solved by direct iterative method.The reliability of the proposed method in simulating nonlinear flow was subsequently verified through an intersecting fracture model.Finally,taking the Habanero geothermal reservoir in Australia as an example,the geothermal production process under different injection pressures was simulated to analyze the heat extraction efficiency of the reservoir.The results indicate that high injection pressure reduces the production life of the reservoir,but with further increase of injection pressure,the production life decreases to a constant value.Furthermore,Forchheimer flow significantly increases flow resistance through nonlinear inertial effects,resulting in actual flow rates being lower than linear flow predictions at high injection pressures,and intensifies the preferential channeling effect of fluids in the main fractures.These findings provide references for the injection and production design of dry geothermal reservoirs.
刘加丽;王书钰;陈浩;熊峰;朱淳;张国华
中国电建集团成都勘测设计研究院有限公司,四川 成都 610072中国地质大学(武汉)工程学院,湖北武汉 430074武警警官学院训练基地分队指挥系,广东 广州 510080中国地质大学(武汉)工程学院,湖北武汉 430074河海大学地球科学与工程学院,江苏南京 213022中国地质大学(武汉)工程学院,湖北武汉 430074
资源环境
裂隙岩体非线性流动热-水耦合裂隙介质地热系统
fractured rock massnonlinear flowthermo-hydro couplingfractured mediageothermal system
《安全与环境工程》 2026 (2)
99-107,9
湖北省自然科学基金(三峡创新发展联合基金)重点项目(2024AFD361)中国五矿集团有限公司科技专项计划"揭榜挂帅"项目(WKZB2512BJM500415/011)
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