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鄂尔多斯盆地苏里格气田异常低压成因机制研究
引用本文:马德文,邱楠生,许威.鄂尔多斯盆地苏里格气田异常低压成因机制研究[J].地质科学,2011,46(4):1055-1067.
作者姓名:马德文  邱楠生  许威
作者单位:中国石油大学(北京)油气资源与探测国家重点实验室 北京 102249
摘    要:利用SRK状态方程定量研究了温度下降和天然气散失对地层压力的影响.研究表明:利用真实气体状态方程不仅可以定量分析温度降低对地层压力的影响,而且可以定量研究气藏的散失量及其对地层压力的影响.早白垩世末( 100 Ma)至今,地层温度下降了约60℃,导致地层压力下降约22%;天然气散失约17%~24%,导致地层压力下降约2...

关 键 词:鄂尔多斯盆地  苏里格气田  异常低压  温度下降  气体散失  压力演化
收稿时间:2011-01-06

Analysis on mechanism of abnormal low pressure in Sulige gas field,Ordos Basin
Ma Dewen,Qiu Nansheng,Xu Wei.Analysis on mechanism of abnormal low pressure in Sulige gas field,Ordos Basin[J].Chinese Journal of Geology,2011,46(4):1055-1067.
Authors:Ma Dewen  Qiu Nansheng  Xu Wei
Institution:State Key Laboratory of Petroleum Resource and Prospecting,China University of Petroleum,Eeijing 102249
Abstract:The effects of temperature decrease and gas dissipation on pore pressure was studied by using the SRK state equation.It was found that temperature decrease and gas dissipation were main mechanism of abnormal low formation pressure in the Sulige gas field,which resulting in the decrease of formation pressure and pressure coefficient.The temperature decrease of 60 ℃ results in formation pressure decrease by about 22% while gas dissipation about 17% ~24%,resulting in formation pressure decrease by about 23% ~32% after Early Cretaceous(100 Ma).It showed that the higher paleotemperature of the reservoirs the greater pressure decrease due to gas dissipation and the more gas diffusion of the gas field the smaller pressure drop causing by temperature decrease.The burial depth of water table and density difference between gas and water has so little contribution to the abnormal low formation pressure that they were not the mechanism of abnormal low formation pressure in Sulige gas field.The pressure evolution history of main reservoir was resumed using coupled fluid flow compaction model,combined with the main mechanism of abnormal formation pressure,constrained in measured formation pressure and paleopressure determined by means of fluid inclusion.The evolution of formation pressure can be divided into three stages: 1)normal pressure before 200 Ma; 2)pressure increase and accumulation of abnormal high formation pressure from 200 Ma to 100 Ma.The formation pressure and pressure coefficient gradually increased and reached maximum at 100 Ma; 3)pressure release after 100 Ma.Temperature decrease and gas dissipation caused by tectonic uplift and denudation resulted in formation pressure decrease and finally evolved to the current state of abnormal low formation pressure.With the characteristics of low permeability and low porosity,the development of abnormal high formation pressure has great significance to the hydrocarbon migration and accumulation in this area.The decrease of formation pressure at later period was beneficial to gas preservation.
Keywords:Ordos Basin  Sulige gea field  Abnormal low formation pressure  Gas dissipation  Temperatute decresae  Pressure evolution
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