泰康和古龙地区粘土矿物对砂岩储层孔隙结构及产能的影响

储油砂岩中,都或多或少地存在粘土矿物胶结物。这些粘土矿物的成分、含量及其产状特征是影响砂岩孔隙结构和油层物性的重要因素。本文主要根据对松辽盆地泰康和古龙地区中部含油组合砂岩的研究,讨论粘土矿物在砂岩孔隙中的分布特征及对孔隙结构和产能的影响。

THE EFFECT OF CLAY MINERAL OCCURRENCE ON PORE STRUCTURES AND PRODUCTION CAPACITY OF SANDSTONES IN TAIKANG AND GULONG AREAS

On the basis of observation by means of scanning electron microscope,the occurrence of clay minerals in pore spaces of sandstone can be divided into threetypes,i.e.1)separated spot type;2)film-like type and 3)bridge-liketype.Sandstones that contains the first type have in the main intergranular porespace.The peak distribution of permeability is consistent with that of theporosity.They show a larger pore radius(6-12μ)and a smaller texture coeffi-cient(Gg<4),good pore connection,high permeability and natural productioncapacity.Sandstones with the second occurrence of clay minerals is generally inconformity with that of the one said above in pore texture feature,porosityand the accordant peak distribution of permeability and porosity,but they havea smaller pore radius(3-9μ),bigger texture coefficient,and show a lower per-meability in samples. Sandstones with the third type occurrence of clay minerals are different tothe other two types.Since clay mineral are formed in a bridge-like way with-in the pore spaces,the primary pore space have been disintegrated into micro-pores among clay minerals.Therefore,the porosity characteristics of these sand-stones are similar to that of claystones,most samples show a small averagepore radius(1μ),a bigger pore texture coefficient(Gg>8).Because mostpores in sandstones turned to be bound pores,their permeability for gas is lessthan 1 md which are devoted merely by a few pore space with radius biggerthan 1μ.The vertical evolution of the above mentioned three types of sandstones canbe seen clearly that,with the increase of the depth,the sandstones with predo-minantly separated spot of kaolinite have gradually changed into sandstoneswith intergranular film-like clay minerals,and finally into sandstones withbridge-like clay minerals represented mainly by flake-like and fibrous illites.Atthe same time,the pore structure and the physical properties of oil reservoirhave been changed accordingly.