首页|致密砂岩储层孔隙结构分形与分级评价——以莺歌海盆地乐东区黄流组为例

致密砂岩储层孔隙结构分形与分级评价——以莺歌海盆地乐东区黄流组为例

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[目的]明确致密砂岩储层孔喉微观形态,划分储层孔隙结构级次,多角度半定量评价储层的储集特征和渗流能力,有助于明确具有高效产能潜力的储层类型.[方法]以莺歌海盆乐东区黄流组致密砂岩为例,利用铸体薄片、扫描电镜、高压压汞等实验手段,开展储层孔隙结构分形维数计算与分级评价的研究.[结果]致密砂岩储层质量的影响因素之一是大孔喉孔隙结构;分形维数越接近3,孔隙结构越复杂,连通的大孔喉越少.依据孔喉分级特征、成岩相、孔隙结构复杂程度,建立了孔隙结构分级评价的四类模型:类型Ⅰ为小孔喉优势型储层,强胶结成岩相,大孔喉孔隙度占比小于45%,Dmax值为2.75~2.90,致密储层;类型Ⅱ为大—小孔喉连续型储层,弱胶结—弱溶蚀成岩相,大孔喉孔隙度占比45%~70%,Dmax值为2.70~2.85,低渗储层;类型Ⅲ为大孔喉优势型储层,强溶蚀成岩相,大孔喉孔隙度占比大于70%,Dmax值为2.55~2.65,优质储层;类型Ⅳ为大孔喉单峰型储层,强压实成岩相,大孔喉孔隙度占比50%~60%,Dmax值为2.65~2.75,低渗储层.通过Fisher判别方法,建立储层类型测井预测模型,对比储层类型与气测响应和储层含气饱和度,发现Ⅲ类储层的产气效能高,具有勘探价值.[结论]研究成果为致密砂岩储层评价与分类提供了新思路,明确了储层孔隙结构对气水分布存在控制作用.
Pore Structure Fractal and Graded Evaluation in Tight Sandstone Reservoirs:A case study of the Huangliu Formation in the Ledong area,Yinggehai Basin
[Objective]Tight sandstone reservoirs have small pore throats,various pore throat types,and strong het-erogeneity.Clarifying the micro morphology of pore throat in tight sandstone reservoirs and dividing the grading of res-ervoir pore structure are important for evaluating the reservoir quality.Multi angle and semi quantitative evaluation of reservoir capacity and flow characteristics is helpful for clarifying the types of reservoirs with high productivity poten-tial.[Methods]Taking the tight sandstones of the Huangliu Formation in the Ledong area of Yinggehai Basin as an example,this study uses the experimental methods of casting thin section,scanning electron microscope(SEM),and high-pressure mercury injection(HPMI).By analyzing the reservoir diagenesis,dividing the reservoir pore throat types,and calculating fractal dimension parameters,the pore structure characteristics are clarified.To analyze the influence of reservoir microstructure parameters on macro physical properties,the pore throat radius scale and the tight sandstone reservoir types are divided,and research on fractal dimension calculation and grading evaluation of reservoir pore structure is performed.[Results]The HPMI experimental results show that the pore-throat radius of tight sandstone reservoirs in the Huangliu Formation has a bimodal distribution,the displacement pressure is be-tween 0.14-2.75 MPa,and the average pore throat radius is between 0.08-1.10 µm.For a better reservoir type,the proportion of the large pore-throat is higher.Using the HPMI fractal dimension(D)to evaluate the pore-throat struc-ture characteristics of the Huangliu Formation reservoirs,when the fractal dimension is closer to 3,the pore throat ra-dius is smaller,the throat is more complex,and the reservoir quality worsens.Owing to the double peak distribution of the pore-throat radius in the Huangliu Formation tight reservoirs,the mercury inlet curves display segmentation.Therefore,the fractal dimensions of large pore throat(Dmax)and small pore throat(Dmin)are calculated in this study.The Dmax value has the strongest correlation with porosity and permeability.The pore structure characteristics of large pore-throat are one of the important factors affecting the reservoir quality.Based on the intersection of the two linear fitting curves in the lg SHg-lgPc diagram and whether mercury is injected into the pore space,the tight sandstone is di-vided into three levels:large,small,and isolated pore-throats.The closer the fractal dimension is to 2,the more con-nected the large pore-throat spaces are in the reservoirs,and the correlation between large pore-throat porosity and permeability is higher.Therefore,the large pore-throat can more effectively characterize the reservoir quality and pore throat structure.Based on the grading characteristics of pore throats,diagenetic facies,and the complexity of pore structure,four types of models for grading evaluation of pore structure are established.Type Ⅰ is the small pore-throat dominant reservoirs with strongly cemented diagenetic facies,and the proportion of large pore-throat porosity is less than 45%.The D value ranges from 2.70-2.80,and the Dmax value is 2.75-2.90,with an isolated point-single point connecting bundle throat and tight reservoir.Type Ⅱ is the large to small pore-throat continuous reservoirs,with weakly cemented and dissolved diagenetic facies.Large pore-throat porosity accounts for 45%-70%.The D value is 2.60-2.80,and the Dmax value is 2.70-2.85,in a single-point and multi-point connecting curved sheet throat,low permeability reservoir.Type Ⅲ is the large pore-throat dominant reservoirs,with strong dissolution diagenetic facies.Large pore-throat porosity accounts for more than 70%.The D value distribution is 2.55-2.60,and the Dmax value is 2.55-2.65,in a network connection thick throat,high-quality reservoir.Type Ⅳ is the single peak reservoir with large pore-throat and strongly compacted diagenetic facies.Large pore-throat porosity accounts for 50%-60%.The D value distribution is 2.70-2.80,and the Dmax value is 2.65-2.75,in a multi-point connection of tube bundle throat,low permeability reservoir.Using the reservoir permeability,porosity,and Dmax parameters,through Fisher's discrim-inant method,new parameters F1 and F2 are obtained,and the reservoir type discrimination criteria were estab-lished.Finally,the logging prediction model of reservoir type is established.Comparing the reservoir type with gas logging response and gas saturation,under the same geological background,the gas logging response in type Ⅲ,type Ⅱ,and type Ⅰ reservoirs is shown to gradually decrease.Type Ⅲ reservoir has strong reservoir and seepage ca-pacity,high gas production efficiency,and good exploration value.Type Ⅳ reservoirs can be used as a barrier in sand bodies,and type Ⅰ reservoirs have poor reservoir capacity.[Conclusion]Using reservoir diagenesis,pore structure characteristics,and fractal dimension parameters,the tight sandstone reservoir quality can be semi-quanti-tatively classified,providing a new idea for tight sandstone reservoir evaluation and classification,and clarifying the control effect of reservoir pore structure on gas-water distribution.

Yinggehai Basintight sandstone reservoirshigh-pressure mercury injectionpore structure fractal

赵静、黄志龙、张景缘、邓广君、许马光

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中国石油大学(北京)油气资源与探测国家重点实验室,北京 102249

中国石油大学(北京)地球科学学院,北京 102249

中海石油(中国)有限公司海南分公司,海口 570100

中海石油(中国)有限公司湛江分公司,广东湛江 524057

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莺歌海盆地 致密砂岩储层 高压压汞 孔隙结构分形

中海石油(中国)有限公司科技重点项目子课题

CNOOC-KJ 135 ZDXM 38 ZJ 02 ZJ

2024

沉积学报
中国矿物岩石地球化学学会沉积学专业委员会 中国地质学会沉积地质专业委员会 中国科学院地质与地球物理研究所兰州油气资源研究中心

沉积学报

CSTPCD北大核心
影响因子:1.54
ISSN:1000-0550
年,卷(期):2024.42(1)
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