西南石油大学学报(自然科学版)
西南石油大學學報(自然科學版)
서남석유대학학보(자연과학판)
JOURNAL OF SOUTHWEST PETROLEUM UNIVERSITY(SEIENCE & TECHNOLOGY EDITION)
2009年
6期
76-79
,共4页
杨建%康毅力%桑宇%李前贵
楊建%康毅力%桑宇%李前貴
양건%강의력%상우%리전귀
致密砂岩%气藏%克努森数%物理吸附%扩散
緻密砂巖%氣藏%剋努森數%物理吸附%擴散
치밀사암%기장%극노삼수%물리흡부%확산
tight sandstone%gas reservoir%Knudsen number%physical adsorption%diffusion
致密砂岩储层岩性致密,自生粘土矿物类型丰富且含量高,造成致密砂岩储层晶间微孔发育,岩石比表面积巨大,实验测得平均比表面积为2.13 m~2/g.在储层发育的纳微尺度空间内,天然气分子在其中的赋存状态以吸附为主,一旦微孔介质中天然气浓度发生变化,克努森数大于10时,吸附天然气将解吸、扩散、运移.实验室测定致密砂岩天然气扩散系数平均为6.86×10~(-5)m~2/s,通过模拟典型致密砂岩气井生产周期内天然气扩散量,证实扩散是致密砂岩天然气重要产出方式之一.
緻密砂巖儲層巖性緻密,自生粘土礦物類型豐富且含量高,造成緻密砂巖儲層晶間微孔髮育,巖石比錶麵積巨大,實驗測得平均比錶麵積為2.13 m~2/g.在儲層髮育的納微呎度空間內,天然氣分子在其中的賦存狀態以吸附為主,一旦微孔介質中天然氣濃度髮生變化,剋努森數大于10時,吸附天然氣將解吸、擴散、運移.實驗室測定緻密砂巖天然氣擴散繫數平均為6.86×10~(-5)m~2/s,通過模擬典型緻密砂巖氣井生產週期內天然氣擴散量,證實擴散是緻密砂巖天然氣重要產齣方式之一.
치밀사암저층암성치밀,자생점토광물류형봉부차함량고,조성치밀사암저층정간미공발육,암석비표면적거대,실험측득평균비표면적위2.13 m~2/g.재저층발육적납미척도공간내,천연기분자재기중적부존상태이흡부위주,일단미공개질중천연기농도발생변화,극노삼수대우10시,흡부천연기장해흡、확산、운이.실험실측정치밀사암천연기확산계수평균위6.86×10~(-5)m~2/s,통과모의전형치밀사암기정생산주기내천연기확산량,증실확산시치밀사암천연기중요산출방식지일.
In tight sandstone gas reservoir,there is high content of clay mineral,which provides abundant intercrystal pores and surface area compared with conventional reservoir.Experiment reveals that the average specific surface area of tight sandstone is 2.13 m~2/g.Natural gas will be adsorbed in the micro-nano spaces.When Knudsen number is greater than 10,adsorption gas will display desorption,diffusion,migration.Average diffusion coefficient of the gas in tight sandstone is 6.86×10~(-5)m~2/s.Simulation of gas well diffusive flux for typical tight sandstone shows that diffusion is one of the very important ways to tight sandstone gas mass transfer during production.