简介:CO2充注驱油是一种普遍的地质现象,对揭示油气藏中油气的动态成藏规律具有重要的指示意义。海拉尔盆地乌尔逊凹陷含片钠铝石砂岩既示踪了CO2充注,又记录了油气充注,是进行CO2充注驱油研究的理想岩石类型。通过岩石学和流体包裹体地球化学研究,确定了含片钠铝石砂岩的成岩共生序列、油气充注历史和CO2充注驱油的微观证据。研究表明,该区油气充注是一个连续的过程,开始于石英次生加大早期(120Ma),在片钠铝石沉淀前(105-95Ma)达到充注高峰。CO2充注晚于大规模油气充注,充注之后形成的自生矿物组合为片钠铝石与铁白云石。片钠铝石中首次发现一定数量的原生油气包裹体,为CO2充注驱油提供了重要的微观证据。
简介:摘要:CO2气体溶于水中形成碳酸后引起电化学腐蚀,如不及时采取有效措施,将导致油套管的严重破坏甚至油井报废。CO2对油、套管的腐蚀是油田开发的一个亟待解决的重要课题。
简介:CarboncycleisconnectedwiththemostimportantenvironmentalissueofGlobalChange.Asoneofthemajorcarbonreservoirs,oceansplayanimportantpartinthecarboncycle.Inrecentyears,ironseemstogiveusagoodnewsthatoceanicironfertilizationcouldstimulatebiologicalproduc-tivityasCO2sinkofhuman-producedCO2.Oceanicironfertilizationexperimentshaveverifiedthataddingironintohighnutrientlowchlorophyll(HNLC)seawaterscanincreasephytoplanktonproductionandexportorganiccarbon,andhenceincreasecarbonsinkofanthropogenicCO2,toreduceglobalwarming.Insixtydays,theexportorganiccarboncouldreach10000timesforaddingironbymodelpredictionandinsituexperiment,I.e.TheatmosphericCO2uptakeandinorganiccarbondrawdowninupperseawatersalsohavethesamemagnitude.Therefore,oceanicironfertilizationisoneofthestrate-giesforincreasingcarbonsinkofanthropogenicCO2.Thepaperisfocusedontheironfertilization,es-peciallyinsituoceanironexperimentsinorderthatthefutureresearchismoreefficient.
简介:Shallowfreshwaterbodiesinpeatareascouldbeanimportantcontributortogreenhousegasesintheatmosphere.Inthisstudy,thepartialpressureofCO2inthesurfacewateroftheDianshanLakewasinvestigatedinsituinAugust2011.TheaveragepCO2inthestudyareawas2300μatmandfluctuatedwithintherangeof989–5000μatm.pCO2showedareversetrendtothevariationsofpHandDOinthesurfacewateroftheDianshanLake.ThewatertoairdiffusionfluxofCO2oftheupstream,middlelakeanddownstreamwererespectively63,33and14mmol/m2/d.Onaverage,thediffusionfluxofCO2ofthewholelakewas31mmol/m2/d.Consequently,ourresultsshowthatduringthesamplingseason,theDianshanLakeappearstobeagreatsourceofCO2.ItisalsodemonstratedthatrespirationcouldbethedominantbiochemicalreactionintheDianshanLakeinsummer.