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ENHANCED CONVECTION FOR IN SITU PYROLYSIS OF ORGANIC-RICH ROCK FORMATIONS

机译:对流强化富有机岩层的原位热解

摘要

Method for producing hydrocarbon fluids from an organic-rich rock formation include providing a plurality of in situ heat sources configured to generate heat within the formation so as to pyrolyze solid hydrocarbons into hydrocarbon fluids. Preferably, the organic-rich rock formation is heated to a temperature of at least 270º C. Heating of the organic-rich rock formation continues so that heat moves away from the respective heat sources and through the formation at a first value of effective thermal diffusivity, α1. Heating of the formation further continues in situ so that thermal fractures are caused to be formed in the formation or so that the permeability of the formation is otherwise increased. The method also includes injecting a fluid into the organic-rich rock formation. The purpose for injecting the fluid is to increase the value of thermal diffusivity within the subsurface formation to a second value, α2. The second value α2 is at least 50% greater than the first value α1 and, more preferably, is at least 100% greater than α1.
机译:由富含有机物的岩层生产烃流体的方法包括提供多个原位热源,其被配置为在岩层内产生热量,以便将固体烃热解为烃流体。优选地,将富含有机物的岩层加热至至少270℃的温度。继续对富含有机物的岩层进行加热,使得热量以有效热扩散率的第一值远离各自的热源并通过地层。 ,α1。地层的加热进一步在原位继续,从而导致在地层中形成热裂缝,或者否则地层的渗透性增加。该方法还包括将流体注入到富含有机物的岩层中。注入流体的目的是将地下地层内的热扩散率值增加到第二值α2。第二值α2比第一值α1大至少50%,并且更优选地,比α1大至少100%。

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