中国石油大学学报(自然科学版)
中國石油大學學報(自然科學版)
중국석유대학학보(자연과학판)
Journal of China University of Petroleum (Edition of Natural Science)
2015年
5期
7-17
,共11页
操应长%葸克来%朱如凯%张少敏%张响响%郑晓骄
操應長%葸剋來%硃如凱%張少敏%張響響%鄭曉驕
조응장%사극래%주여개%장소민%장향향%정효교
孔喉结构%孔喉参数%致密砂岩%泉四段%松辽盆地南部
孔喉結構%孔喉參數%緻密砂巖%泉四段%鬆遼盆地南部
공후결구%공후삼수%치밀사암%천사단%송료분지남부
pore throat structure%pore throat parameters%tight sandstone%fourth member of Quantou Formation%southern Songliao Basin
综合运用铸体薄片观察、扫描电镜、高压压汞、恒速压汞及图像分析等技术手段,对松辽盆地南部泉四段扶余油层致密砂岩储层储集空间、储集物性、微观孔喉分布及不同尺度孔喉对储层物性的贡献等特征进行精细表征,并分析不同微观孔喉参数与储层物性的相关关系。结果表明,研究区致密砂岩储层物性差、孔喉半径小;储集空间以粒内和粒间溶孔为主,含部分原生孔和黏土矿物晶间孔。储层孔隙半径分布差异不明显,而喉道半径与孔喉比分布差异较大;储层物性越好,喉道半径分布范围越宽,峰值喉道半径越大,并且右偏特征越明显;储层渗透率越高,对渗透率起主要贡献的孔喉半径越大;孔喉比分布与喉道半径分布呈现相反的特征。渗透率主要由岩石中少量的微米级孔喉贡献;纳米级孔喉所占体积很大,却只有较小的渗流能力,并且渗透率越低,纳米级孔喉所占的相对比例越大。微观孔喉结构参数对储层物性的影响主要体现在渗透率上,而对孔隙度的影响较小。
綜閤運用鑄體薄片觀察、掃描電鏡、高壓壓汞、恆速壓汞及圖像分析等技術手段,對鬆遼盆地南部泉四段扶餘油層緻密砂巖儲層儲集空間、儲集物性、微觀孔喉分佈及不同呎度孔喉對儲層物性的貢獻等特徵進行精細錶徵,併分析不同微觀孔喉參數與儲層物性的相關關繫。結果錶明,研究區緻密砂巖儲層物性差、孔喉半徑小;儲集空間以粒內和粒間溶孔為主,含部分原生孔和黏土礦物晶間孔。儲層孔隙半徑分佈差異不明顯,而喉道半徑與孔喉比分佈差異較大;儲層物性越好,喉道半徑分佈範圍越寬,峰值喉道半徑越大,併且右偏特徵越明顯;儲層滲透率越高,對滲透率起主要貢獻的孔喉半徑越大;孔喉比分佈與喉道半徑分佈呈現相反的特徵。滲透率主要由巖石中少量的微米級孔喉貢獻;納米級孔喉所佔體積很大,卻隻有較小的滲流能力,併且滲透率越低,納米級孔喉所佔的相對比例越大。微觀孔喉結構參數對儲層物性的影響主要體現在滲透率上,而對孔隙度的影響較小。
종합운용주체박편관찰、소묘전경、고압압홍、항속압홍급도상분석등기술수단,대송료분지남부천사단부여유층치밀사암저층저집공간、저집물성、미관공후분포급불동척도공후대저층물성적공헌등특정진행정세표정,병분석불동미관공후삼수여저층물성적상관관계。결과표명,연구구치밀사암저층물성차、공후반경소;저집공간이립내화립간용공위주,함부분원생공화점토광물정간공。저층공극반경분포차이불명현,이후도반경여공후비분포차이교대;저층물성월호,후도반경분포범위월관,봉치후도반경월대,병차우편특정월명현;저층삼투솔월고,대삼투솔기주요공헌적공후반경월대;공후비분포여후도반경분포정현상반적특정。삼투솔주요유암석중소량적미미급공후공헌;납미급공후소점체적흔대,각지유교소적삼류능력,병차삼투솔월저,납미급공후소점적상대비례월대。미관공후결구삼수대저층물성적영향주요체현재삼투솔상,이대공극도적영향교소。
The Fuyu Oil layer of the fourth member of Quantou Formation in southern Songliao Basin was studied in detail for the reservoir space, physical property, micro pore throat distribution and contribution of different pore throat scales to reser-voir physical property of tight sandstone reservoirs. A series of techniques were used, including thin section, SEM, high pressure mercury penetration, rate-controlled mercury penetration and image analysis. The correlation of different pore throat parameters and reservoir physical property was analyzed. The results show that, the physical properties of the tight sandstone reservoirs in the study area are poor with small pore throat radius; the reservoir spaces are mainly intra-particles and inter-particles dissolved pores with some primary pores as well as inter-crystal pores in clay minerals. The pore distribution ranges have no significant difference, but the distribution ranges of throat radius and pore throat ratio had apparent difference. In the reservoirs of good physical properties, distribution ranges of throat radius are wider with larger peak values, and more obvious right-skewness. When reservoirs have higher permeability, the pore throat radius that plays major contributions to permeabili-ty are larger. Opposite distribution features exist between pore throat ratio and throat radius. Reservoir permeability is mainly contributed by a small amount of pore throat with micron sizes, although the pore throat with nanoscale sizes accounts for great volume because they hold lower filtration capacity. The lower the reservoir permeability is, the larger proportion is for the pore throat with nanoscale sizes. Micro pore throat parameters have effects mainly on permeability but less on porosity.