复杂油气藏
複雜油氣藏
복잡유기장
COMPLEX HYDROCARBON RESERVOIRS
2012年
2期
20-24
,共5页
火山岩%核磁共振%T2截止值%可动流体
火山巖%覈磁共振%T2截止值%可動流體
화산암%핵자공진%T2절지치%가동류체
volcanic rocks%NMR%T2 cut - off value%movable fluid
在松辽盆地火山岩中选取全直径岩样利用饱和水多次离心法进行火山岩岩心核磁共振实验分析,解决了核磁共振测井方法的关键参数T2截止值的确定问题,打破了认为火山岩T2截止值为同一T2截止值(90ms)的传统认识。把实验结果同其它实验方法获得的结果进行横向对比分析发现,利用新的T2截止值可以准确计算可动流体孔隙度、束缚水孔隙度等参数,并确定了T2图谱的分布与岩心孔隙结构之间的关系。将实验成果应用到核磁共振测井在单井储层评价中取得了良好的成果。
在鬆遼盆地火山巖中選取全直徑巖樣利用飽和水多次離心法進行火山巖巖心覈磁共振實驗分析,解決瞭覈磁共振測井方法的關鍵參數T2截止值的確定問題,打破瞭認為火山巖T2截止值為同一T2截止值(90ms)的傳統認識。把實驗結果同其它實驗方法穫得的結果進行橫嚮對比分析髮現,利用新的T2截止值可以準確計算可動流體孔隙度、束縳水孔隙度等參數,併確定瞭T2圖譜的分佈與巖心孔隙結構之間的關繫。將實驗成果應用到覈磁共振測井在單井儲層評價中取得瞭良好的成果。
재송료분지화산암중선취전직경암양이용포화수다차리심법진행화산암암심핵자공진실험분석,해결료핵자공진측정방법적관건삼수T2절지치적학정문제,타파료인위화산암T2절지치위동일T2절지치(90ms)적전통인식。파실험결과동기타실험방법획득적결과진행횡향대비분석발현,이용신적T2절지치가이준학계산가동류체공극도、속박수공극도등삼수,병학정료T2도보적분포여암심공극결구지간적관계。장실험성과응용도핵자공진측정재단정저층평개중취득료량호적성과。
Using whole diameter volcanic cores, which were saturated by water after repeatedly centrifugation, the nu- clear magnetic resonance (NMR) experiments were carried out to determine the key parameter - T2 cut - off value of NMR well logging method. The traditional understanding that the volcanic T2 cut - off value is the same one for 90ms was broken out by the new value. By comparing with other experimental results, it is found that the new value can be used to calculate accurately the porosities of movable fluid and bound water and determinate the relationship between the distribution of core T2 map and pore structure. The experimental results were applied in NMR logging for reservoir evaluation of single well and good results were obtained.