首页> 外文会议>International Symposium of the Society of Core Analysts >SCA2003-05: VARIATION OF SPECIAL CORE ANALYSIS PROPERTIES FOR INTERMEDIATE WET SANDSTONE MATERIAL
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SCA2003-05: VARIATION OF SPECIAL CORE ANALYSIS PROPERTIES FOR INTERMEDIATE WET SANDSTONE MATERIAL

机译:SCA2003-05:中间湿砂岩材料的特殊核心分析性能的变化

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Wettability is known to influence fluid flow processes in porous media.Most North Sea sandstone reservoirs fall into the large group of intermediate wet state.However,special core analysis of intermediate wet rock shows a wide variation in properties like;end point saturation,capillary pressure and relative permeability.In this study,we find an improved understanding of the intermediate wet state by dividing the intermediate wet group into three sub-classes.Fractionally-wet(FW),where oil and water wet sites are random with respect to pore size,and mixed wet defined by water and oil wet pores that are sorted by pore size.We assume two classes of mixed wet state,where the oil wet sites are either in the large or the small pores.MWL(mixed-wet large)is defined by oil wet large pores,while MWS(mixed-wet small)refers to the smaller pores are oil wet.The USBM and Amott-Harvey wettability indices are used to group reservoir data into reservoirs with FW,MWS,and MWL behavior.Some of the main results were that the fractional-wet rock has a more robust wettability.Cleaned cores maintain a non-waterwet state,indicating that the wetting sites may be coupled to mineralogy in addition to adsorption/deposition of oil components changing the surface properties of the rock.Also MWS maintains wettability after cleaning,while the mixed wet(MWL)cores become more water wet after solvent cleaning.The average waterflood remaining oil saturation(Sorw)is lowest for MWL cores.The remaining oil saturation for the MWL rocks also show a reduced Sorw with increasing permeability,but the FW and MWS reservoirs indicate a constant Sorw independent of permeability.The type of intermediate wettability has impact on data structure needed to build representative reservoir models.In addition,the type of wettability influences the shape of relative permeability curves and also the capillary pressure relations for different classes of intermediate wettability.
机译:已知润湿性地影响多孔介质中的流体流程。大多数北海砂岩储层落入大群中间湿润状态。然而,中间湿岩的特殊核心分析显示了像这样的性质的宽变化;终点饱和度,毛细管压力并且相对渗透性。在本研究中,通过将中间湿法组分成三个次级,我们发现对中间湿态的了解改善了理解。分枝湿(FW),其中油和水湿位点是随机的孔径并且由水和油湿孔定义的混合湿湿孔由孔径分类。我们假设两类混合湿润状态,其中油湿地位在大或小孔隙上(混合湿大)是由油湿大孔隙定义,而MWS(混合湿法)是指较小的毛孔是油湿润的。USBM和AMOTT-HARVEY润湿性指数用于将储层数据分组为具有FW,MWS和MWL行为的储层。有些主要res ults是分数湿的岩石具有更强大的润湿性。切片的核心保持非水绒纱,表明除了油分的吸附/沉积外,润湿位点也可以偶联到矿物质的吸附/沉积改变岩石的表面性质。清洁后,MWS也保持润湿性,而混合湿润(MWL)芯片在溶剂清洁后变得更加水湿。剩余的油饱和度(SORW)的平均水饱和度最低为MWL核心。MWL岩石的剩余油饱和度也表现出降低索罗因渗透率而增加,但FW和MWS储层表明恒定的索线独立于渗透性。中间润湿性的类型对构建代表性储层模型所需的数据结构影响。此外,润湿性的类型影响相对渗透性曲线的形状以及不同类中间润湿性的毛细管压力关系。

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