Dynamics of Heat Transport from a Reservoir to the Adjoining Formation in a Thermal Flood

K. Lawal
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Abstract

Heat transfer from a petroleum reservoir to adjoining rocks is detrimental to thermal floods. While such thermal losses are inevitable, understanding the timescales of these heat exchanges would improve the design and management of thermal floods. Employing lumped-parameter system analysis and assuming series flow, this paper presents transfer functions that characterize response times of a reservoir and its surroundings to changes in temperature of the heat source. The reservoir-surrounding system is modelled as individual thermal capacitors and resistors. The transfer functions, solved for a step disturbance, describe the limiting case of negligible interaction between these subsystems. For a step-change in temperature of the heat source, responses of the reservoir and surroundings are simulated for some combinations of their properties. Simulation results explain time-delay between reservoir and surrounding temperatures. The time-delay is controlled by four distinct parameters vis-à-vis surroundings time constant (τr), reservoir time constant (τa), ratio of thermal resistances (R) as well as the ratio of conductive to convective heat flow (βr). These parameters are governed by petrophysical, transport and thermophysical properties of the heating medium, reservoir, and surrounding formation. It is shown that lag-time in thermal responses of reservoir and surroundings can range from few weeks to several years. For practical applications and analyses, these results provide insights into conditions under which a thermal flood may be approximated as adiabatic vs. non-adiabatic.
热驱中储层向相邻地层的热传递动力学
从油藏到相邻岩石的热传递不利于热驱。虽然这种热损失是不可避免的,但了解这些热交换的时间尺度将改善热洪水的设计和管理。本文采用集总参数系统分析方法,假设连续流动,给出了表征热源温度变化对水库及其周围环境的响应时间的传递函数。将储层周围系统建模为单独的热电容器和电阻。对于阶跃扰动的传递函数,描述了这些子系统之间相互作用可忽略的极限情况。对于热源温度的阶跃变化,模拟了储层和周围环境的一些性质组合的响应。模拟结果解释了储层与周围温度之间的时滞。时间延迟由四个不同的参数控制,即-à-vis环境时间常数(τr)、储层时间常数(τa)、热阻比(R)和导热对流热流比(βr)。这些参数受加热介质、储层和周围地层的岩石物理、输运和热物理性质的影响。研究表明,储层和周围环境的热响应滞后时间从几周到几年不等。对于实际应用和分析,这些结果提供了对热驱可以近似为绝热与非绝热的条件的见解。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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