ISSN 1673-8217 CN 41-1388/TE
主管:中国石油化工集团有限公司 主办:中国石油化工股份有限公司河南油田分公司
符勇, 姜振泉, 马丽, 郭阳, 刘丽娜. 2005: 油气运聚水动力作用中的耗散结构. 石油地质与工程, 19(02): 17-19+6.
引用本文: 符勇, 姜振泉, 马丽, 郭阳, 刘丽娜. 2005: 油气运聚水动力作用中的耗散结构. 石油地质与工程, 19(02): 17-19+6.
2005: Dissipative structure of hydrodynamic hydrocarbon migration and accumulation. Petroleum Geology and Engineering, 19(02): 17-19+6.
Citation: 2005: Dissipative structure of hydrodynamic hydrocarbon migration and accumulation. Petroleum Geology and Engineering, 19(02): 17-19+6.

油气运聚水动力作用中的耗散结构

Dissipative structure of hydrodynamic hydrocarbon migration and accumulation

  • 摘要: 油气运聚是一个不可逆过程,是一个时空有序的耗散结构。沉积水是油气运聚的载体和主要驱动 力,对盆地流体的运动起控制作用,由盆地中心向盆地边缘呈离心流;渗入水由大气降水和地表水的渗入 产生,受重力作用由盆地边缘向盆地中心呈向心流。沉积水与渗入水作用的结果产生一个压力平衡带,油 气就聚集于这个压力平衡带上。油气圈闭要同时具备平衡结构和耗散结构。上部为平衡结构,使油气得 以保存;下部为耗散结构,使油气不断充注,形成大的油气田。泌阳凹陷的油气田呈环带状分布于沉积水 与渗入水锋面位置的压力平衡带上。

     

    Abstract: Hydrocarbon migration and accumulation is an irreversible process and a dissipative structure with order in time and space. Sedimentary water is the carrier and major driving force of hydrocarbon migration and accumulation. It controls fluid motion in basins and flows from basin center to its edge in centrifugal flow. While infiltration water generated from filtration of meteoric water and surface water flows from basin edge to its center in gravity -induced centripetal flow. The interaction of sedimentary water and infiltration water results in a pressure equilibrium zone, where hydrocarbons accumulate. Oil and gas traps should have both an equilibrium structure and a dissipative structure. The upper part of a trap has equilibrium structure which ensure the preservation of oil and gas, while the lower part has dissipative structure which ensure the continuous charging of oil and gas, so as to form large oil and gas fields. Oil and gas reservoirs in Biyang depression distribute in circularity in the pressure equilibrium zone on the frontal surface between sedimentary water and infiltration water.

     

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