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粒间孔隙的英文

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"粒间孔隙"怎么读用"粒间孔隙"造句

英文翻译手机手机版

  • intergranular pore-space
  • intergranular space
  • interparticle pore
  • interparticle porosity

例句与用法

  • The preserved average porosity is 10 . 1 % at present . the main reservoir space of chang 4 + 52 ~ chang 62 sandstone in the area is secondary pores , especially the secondary intergranular pores
    研究区储层砂体的储集空间以次生孔隙为主,并以次生粒间孔隙占优势,次为填隙物内溶孔、粒内溶孔。
  • So we can draw a conclusion that the dolostone of c - o stratum in the regions of zhuangxi and chengdao has primarily two genesis types , they are penecontemporaneous dolostone and diagenetic dolostone . the diagenetic dolostone is formed by replacement in intergranular pore water on the course of burial diagenesis
    因此,我们认为桩西、埕岛地区寒武?奥陶系白云岩主要有两种不同的成因类型,即准同生白云岩和成岩白云岩,并且成岩白云岩是在埋藏成岩过程中,在粒间孔隙水中由交代作用形成的。
  • The variations in trace element contents and ratios may hold up a mirror to the lake - level fluctuations and climatic changes , which , in turn , have exerted a direct and important effect on the sequence stratigraphic development . collectively , the reservoir rocks from the yanchang formation consist dominantly of the delta front subfacies subaqueous distributary channel and channel - mouth bar microfacies and delta plain subfacies subaerial distributary channel microfacies fine - grained feldspar sandstones and siltstones . the reservoir rocks have been subjected to three stages of diagenetic and porosity evolution : ( 1 ) the porosity reduction by the mechanical compaction and chemical pressure solution during the early diagenetic stage ; ( 2 ) the porosity increase by the dissolution during the a substage of the late diagenetic stage , and ( 3 ) the porosity reduction by the cementation and filling during the b substage of the late diagenetic stage
    系统的储层特征研究表明,该区延长组储层成因类型主要为三角洲前缘水下分流河道、河口砂坝及三角洲平原水上分流河道微相细粒长石砂岩、粉砂岩;储层岩石经历了压实,胶结,溶蚀等成岩作用,历经早成岩机械压实和化学压溶孔隙缩小期、晚成岩a亚期溶蚀作用孔隙扩大期及晚成岩a亚期( b亚期)胶结充填孔隙缩小期三个成岩-孔隙演化阶段;储层物性总体上具有较低孔渗、低孔渗的特点,孔隙类型主要为粒间溶孔、残余粒间孔隙、粒内溶孔、晶间孔及晶间溶孔,裂缝不发育,储集岩排驱压力和中值压力较高,孔隙结构类型以细小孔-微孔隙,微细喉-微喉型为主。
  • The rehological deformation will result in change of strength of the filling material . during the rapid rehological deformation period , weak filling material was broken and getting finer , the strength decreases at the same time . in the stable deformation period , the fine particles fill up the pores so that the strength increases slowly
    在最初的流变加速期,软弱颗粒逐步破碎细化,强度是衰减的;进入流变稳定变形期后,细化颗粒向粒间孔隙滑移充填,堆石的密实度有所提高,强度又呈缓慢增长趋势。
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