石油实验地质
石油實驗地質
석유실험지질
EXPERIMENTAL PETROLEUM GEOLOGY
2009年
5期
522-527
,共6页
程同锦%王国建%范明%任春%陈伟钧%朱怀平%卢丽%黄欣
程同錦%王國建%範明%任春%陳偉鈞%硃懷平%盧麗%黃訢
정동금%왕국건%범명%임춘%진위균%주부평%로려%황흔
烃类%微渗漏%成因机制%化探异常%实验模拟
烴類%微滲漏%成因機製%化探異常%實驗模擬
경류%미삼루%성인궤제%화탐이상%실험모의
hydrocarbon%micro-seepage%genetic mechanism%geochemical anomalies%experimental simulation
利用自行研制的物理模拟实验装置,对油气聚集成藏以后其中的烃类穿过上覆盖层运移至地表的过程进行了实验室模拟.实验证实,油气藏中的烃类气体由于与外部地层存在压力、浓度的差异而发生渗透和扩散,即微渗漏作用,方向主要是垂向的.垂向微渗漏致使油气藏中的烃类气体可以穿过上覆盖层直至到达地表,现代测试仪器可以在地表检测到来自深部地层的渗漏烃.同时发现,烃类垂向微渗漏具有间歇性、伴有幕式的特点.基于长期观测和实验模拟的结果,提出"气相压驱裂隙渗透"可能是近地表烃类化探异常的主要成因机制.
利用自行研製的物理模擬實驗裝置,對油氣聚集成藏以後其中的烴類穿過上覆蓋層運移至地錶的過程進行瞭實驗室模擬.實驗證實,油氣藏中的烴類氣體由于與外部地層存在壓力、濃度的差異而髮生滲透和擴散,即微滲漏作用,方嚮主要是垂嚮的.垂嚮微滲漏緻使油氣藏中的烴類氣體可以穿過上覆蓋層直至到達地錶,現代測試儀器可以在地錶檢測到來自深部地層的滲漏烴.同時髮現,烴類垂嚮微滲漏具有間歇性、伴有幕式的特點.基于長期觀測和實驗模擬的結果,提齣"氣相壓驅裂隙滲透"可能是近地錶烴類化探異常的主要成因機製.
이용자행연제적물리모의실험장치,대유기취집성장이후기중적경류천과상복개층운이지지표적과정진행료실험실모의.실험증실,유기장중적경류기체유우여외부지층존재압력、농도적차이이발생삼투화확산,즉미삼루작용,방향주요시수향적.수향미삼루치사유기장중적경류기체가이천과상복개층직지도체지표,현대측시의기가이재지표검측도래자심부지층적삼루경.동시발현,경류수향미삼루구유간헐성、반유막식적특점.기우장기관측화실험모의적결과,제출"기상압구렬극삼투"가능시근지표경류화탐이상적주요성인궤제.
A laboratory simulation of the migration process of the hydrocarbons through the overlying cap rock to the surface of the earth has been carried out by means of the self-developed physical simulation device. The results show that the hydrocarbons in the reservoir can permeate and diffuse due to the pressure difference and the concentration difference between the reservoir and its surrounding strata, which is described as micro-seepage, and the direction of this micro-seepage is mainly vertical. It is this vertical micro-seepage that drives the hydrocarbons from the reservoir to migrate through the cap rock and eventually reach the surface of the earth, and the migrated hydrocarbons can be detected by modern apparatus and equipment in the surface. The results also show that the vertical hydrocarbon micro-seepage is characterized by intermittent and episodic migration. A new theory of "gas phase permeation along fracture driven by pressure" has been proposed as the possible main formation mechanism of the near-surface geochemical anomaly based on these simulation results and the long-observed results.