石油与天然气地质
石油與天然氣地質
석유여천연기지질
OIL & GAS GEOLOGY
2014年
2期
266-271
,共6页
李军%路菁%李争%武清钊%南泽宇
李軍%路菁%李爭%武清釗%南澤宇
리군%로정%리쟁%무청쇠%남택우
四孔隙模型%测井%定量评价%页岩气%储层评价
四孔隙模型%測井%定量評價%頁巖氣%儲層評價
사공극모형%측정%정량평개%혈암기%저층평개
‘four-pore’ model%wireline log%quantitative evaluation%shale gas%reservoir evaluation
页岩气储层微观孔隙组分复杂,分为有机孔隙、碎屑孔隙、粘土孔隙和微裂缝。在岩心和测井响应特征分析基础上,提出利用测井资料定量评价页岩储层总孔隙及其微观孔隙组分的方法:①基于体积模型,利用密度测井资料或声波测井资料确定页岩储层总孔隙度;②综合利用常规测井资料和自然伽马能谱测井资料确定有机质体积含量,依据扫描电镜( SEM)技术确定刻度系数,得到有机孔隙度计算方法;③粘土孔隙是束缚水主要赋存空间,利用测井资料逐点确定粘土含量,并与邻近泥岩相关联,得到粘土孔隙度计算方法;④基于微裂缝的双侧向测井响应特征,通过正反演数值模拟计算,得到微裂缝计算方法;⑤总孔隙度与有机孔隙、粘土孔隙和微裂缝之差即为碎屑孔隙度。岩心结果表明,采用上述方法计算各微观孔隙组分与岩心测试结果吻合,表明方法的正确性。
頁巖氣儲層微觀孔隙組分複雜,分為有機孔隙、碎屑孔隙、粘土孔隙和微裂縫。在巖心和測井響應特徵分析基礎上,提齣利用測井資料定量評價頁巖儲層總孔隙及其微觀孔隙組分的方法:①基于體積模型,利用密度測井資料或聲波測井資料確定頁巖儲層總孔隙度;②綜閤利用常規測井資料和自然伽馬能譜測井資料確定有機質體積含量,依據掃描電鏡( SEM)技術確定刻度繫數,得到有機孔隙度計算方法;③粘土孔隙是束縳水主要賦存空間,利用測井資料逐點確定粘土含量,併與鄰近泥巖相關聯,得到粘土孔隙度計算方法;④基于微裂縫的雙側嚮測井響應特徵,通過正反縯數值模擬計算,得到微裂縫計算方法;⑤總孔隙度與有機孔隙、粘土孔隙和微裂縫之差即為碎屑孔隙度。巖心結果錶明,採用上述方法計算各微觀孔隙組分與巖心測試結果吻閤,錶明方法的正確性。
혈암기저층미관공극조분복잡,분위유궤공극、쇄설공극、점토공극화미렬봉。재암심화측정향응특정분석기출상,제출이용측정자료정량평개혈암저층총공극급기미관공극조분적방법:①기우체적모형,이용밀도측정자료혹성파측정자료학정혈암저층총공극도;②종합이용상규측정자료화자연가마능보측정자료학정유궤질체적함량,의거소묘전경( SEM)기술학정각도계수,득도유궤공극도계산방법;③점토공극시속박수주요부존공간,이용측정자료축점학정점토함량,병여린근니암상관련,득도점토공극도계산방법;④기우미렬봉적쌍측향측정향응특정,통과정반연수치모의계산,득도미렬봉계산방법;⑤총공극도여유궤공극、점토공극화미렬봉지차즉위쇄설공극도。암심결과표명,채용상술방법계산각미관공극조분여암심측시결과문합,표명방법적정학성。
The micropores of the shale gas reservoir consist of organic pore ,clastic pore ,clay pore and micro-fracture .After a comprehensive analysis of core properties and the logging response characteristics ,several new methods are proposed to evaluate total porosity and porosity of each micropore type of shale gas reservoir quantitatively .1) Based on the volume model,the DEN or DT is used to determine the total porosity of shale gas reservoir .2)Conventional logs and SGR (Natural Gamma Ray Spectroscopy ) logs are utilized to determine the volume-percent of organic matter content of shale gas reservoir , a scale parameter is determined by SEM technique ,and finally a method for calculating the organic porosity is set up .3) Considering the clay pore is the main storage space for bound water ,clay content is obtained from logs and correlated with the adjoining shale to get the evaluation method of clay porosity .4) Based on the response characteristics of dual laterolog for micro-fracture,an evaluation method of micro-fracture porosity is proposed by forward and inverse numerical simulation computations.5)The clastic porosity can be determined by subtracting organic porosity ,clay porosity and micro-fracture po-rosity from the total porosity .A good agreement is found between the core analysis and the micropore porosity computed by using the above methods ,which indicates the validity of the methods proposed in this paper .