石油实验地质
石油實驗地質
석유실험지질
EXPERIMENTAL PETROLEUM GEOLOGY
2014年
3期
370-375
,共6页
林晓英%郭春阳%曾溅辉%高宇
林曉英%郭春暘%曾濺輝%高宇
림효영%곽춘양%증천휘%고우
低渗透砂岩%天然气运聚%非达西流%储层物性%充注动力
低滲透砂巖%天然氣運聚%非達西流%儲層物性%充註動力
저삼투사암%천연기운취%비체서류%저층물성%충주동력
low-permeability sandstone%natural gas migration and accumulation%non-Darcy flow%reservoir physical property%driving force
低渗透砂岩气藏勘探表明,其形成与分布具有独特的特征,很难用常规天然气成藏理论进行解释与描述。在低渗透砂岩天然气岩心充注模拟实验的基础上,对低渗透砂岩天然气藏的运移和聚集特征进行了研究。研究结果表明:气体在低渗透砂岩中的运移需要克服储层的最小阻力和最大阻力,当运移动力位于二者之间时,气体的主要运移方式表现为非达西流;运移动力小于最小阻力时,气体的运移方式为扩散;运移动力大于最大阻力时,气体的运移方式为达西流。正是这种复杂的气体运移方式,导致了低渗透砂岩中复杂的气水分布关系。天然气的聚集成藏过程主要受运聚动力、储层物性和束缚水饱和度控制。随运聚动力的增加,含气饱和度逐渐增加,并在束缚水的影响下最终趋于稳定,含气饱和度一般小于60%。在相同的动力下,渗透率越大的储层含气饱和度越大,这也是“甜点”成藏的主要原因。
低滲透砂巖氣藏勘探錶明,其形成與分佈具有獨特的特徵,很難用常規天然氣成藏理論進行解釋與描述。在低滲透砂巖天然氣巖心充註模擬實驗的基礎上,對低滲透砂巖天然氣藏的運移和聚集特徵進行瞭研究。研究結果錶明:氣體在低滲透砂巖中的運移需要剋服儲層的最小阻力和最大阻力,噹運移動力位于二者之間時,氣體的主要運移方式錶現為非達西流;運移動力小于最小阻力時,氣體的運移方式為擴散;運移動力大于最大阻力時,氣體的運移方式為達西流。正是這種複雜的氣體運移方式,導緻瞭低滲透砂巖中複雜的氣水分佈關繫。天然氣的聚集成藏過程主要受運聚動力、儲層物性和束縳水飽和度控製。隨運聚動力的增加,含氣飽和度逐漸增加,併在束縳水的影響下最終趨于穩定,含氣飽和度一般小于60%。在相同的動力下,滲透率越大的儲層含氣飽和度越大,這也是“甜點”成藏的主要原因。
저삼투사암기장감탐표명,기형성여분포구유독특적특정,흔난용상규천연기성장이론진행해석여묘술。재저삼투사암천연기암심충주모의실험적기출상,대저삼투사암천연기장적운이화취집특정진행료연구。연구결과표명:기체재저삼투사암중적운이수요극복저층적최소조력화최대조력,당운이동력위우이자지간시,기체적주요운이방식표현위비체서류;운이동력소우최소조력시,기체적운이방식위확산;운이동력대우최대조력시,기체적운이방식위체서류。정시저충복잡적기체운이방식,도치료저삼투사암중복잡적기수분포관계。천연기적취집성장과정주요수운취동력、저층물성화속박수포화도공제。수운취동력적증가,함기포화도축점증가,병재속박수적영향하최종추우은정,함기포화도일반소우60%。재상동적동력하,삼투솔월대적저층함기포화도월대,저야시“첨점”성장적주요원인。
The explorations of gas reservoirs in low-permeability sandstones have indicated that they have unique characteristics, hence are difficult to interpret and describe with conventional natural gas accumulation theories. Based on the experiments of natural gas charging of cores, the migration and accumulation characteristics of natu-ral gas in low-permeability sandstone reservoirs were studied. It has been concluded that the main gas migration way is diffusion when the driving force is less than the minimum reservoir resistance;the main migration way is non-Darcy flow when the driving force is between the minimum and maximum reservoir resistance;the main mi-gration way is Darcy flow when the driving force is more than the maximum reservoir resistance. It is this complex gas migration and accumulation way that leads to complicated gas water distribution relationship in low-permeabi-lity sandstones. The process of gas migration and accumulation is controlled by the driving force of gas migration and accumulation, sandstone physical properties and bound water saturation. With the increase of driving force, gas saturation gradually improves and finally becomes stable ( usually less than 60%) due to the influence of bound water in sandstone reservoirs. With the same driving force, gas saturation increases with the improvement of permeability, which explains the accumulation of “desserts”.