简介:<正>ThebrineshrimpArtemiaisoftenabundantlyfoundinhypersalineenvironments.Thelarvae(‘nauplii’)hatchingfromitsdormantembryos(‘cysts’)areacruciallivefooditemforthelarvalstagesoffishandshrimpinaquaculture
简介:DNAbarcodingisapowerfulapproachforcharacterizingspeciesoforganisms,especiallythosewithalmostidenticalmorphologicalfeatures,therebyhelpingtotoestablishphylogeneticrelationshipsandrevealevolutionaryhistories.Inthisstudy,wechosea648-bpsegmentofthemitochondrialgene,cytochromecoxidasesubunit1(COI),asastandardbarcoderegiontoestablishphylogeneticrelation-shipsamongbrineshrimp(Artemia)speciesfrommajorhabitatsaroundtheworldandfurtherfocusedonthebiodiversityofArtemiaspeciesinChina,especiallyintheTibetanPlateau.SamplesfromfivemajorsaltlakesoftheTibetanPlateaulocatedataltitudesover4,000mshowedcleardifferencesfromotherArtemiapop-ulationsinChina.Wealsoobservedtwoconsistentaminoacidchanges,153A/Vand183L/F,intheCOIgenebetweenthehighandlowaltitudespeciesinChina.Moreover,indelsintheCOIsequencewereidentifiedincystandadultsamplesuniquetotheCoQenpopulationfromtheTibetanPlateau,demonstratingtheneedforadditionalinvestigationsofthemitochondrialgenomeamongTibetanArtemiapopulations.
简介:<正>BrineresourceisrichinChina,butitsexploitationhasbeenaproblem.Hypersalinebrinewillcorrodeequipmentandmaterialsseriouslyduringthebrineexploitationandtransportation.Thecorrosionproblemcancausegreat
简介:<正>1IntroductionThemainproductionofYabulaisaltlakewasoriginalsaltandrecycledsaltmanyyearsago.Afterdecade’sproduction,thesalelakeresourceismoreandmoredeficient.Glauber’ssaltandmagnesiumsaltareconcentratedinbrinenow.Itcouldaffectthequalityofthesalt.Inrecentyears,researchhaddonemuchworkto
简介:<正>1IntroductionThereexistcalciumandsulfateionsoutsidesodiumchlorideinsolutionminingforcalciumsulfatebrine.Thecalciumandsulfateionsnotonlyaffectthepurityofthevacuumsaltproducts,butalsoincreasethescalingofvacuumevaporationtanksandbrinereusingpipes.Additiveshavecertainimpactsonthecrystallizationdynamics(Randolphetal.,1971).Thecrystallization
简介:Theadsorptionpropertytheoperatinglife,theoperatingexchangecapacityandregenerationofD412macroporousphosphonomethylaminachelatingresinforremovingCa2+,Mg2+andFe2+fromhighpHbrineofalkaliproductionbyionicmembranewereinvestigatedTheresinshowedgoodphysical-chemicalandkineticproperty,highexchangecapacity,excellentdurability.
简介:在从Libixia节的Jialingjiang形成的破裂的大多数静脉mineralsdeposited,Hechan区域包括大量僵绳白云石和伴随的天青石,方解石和荧石。这研究分析了性质,来源,由飞机光岩相学的液体的进化,液体包括方法,阴极射线发光图象,和稳定的同位素的作文。在白云石的二阶段的水的液体包括的homogenization温度在100和270°C之间变化。与δ18O数据,为破裂屑的降水负责的液体有δ18在10‰之间的O值并且18‰(相对降雪)。僵绳白云石和伴随的矿物质是在提高的温度的稠密的盐水的活动的结果。而且,液体从导出水兵的盐水的混合物被导出并且更深传播的分析表演流动。这液体在成岩作用期间在Sr被充实并且在骨折并且为地区性的矿化作用形成了天青石。僵绳白云石的溶解被归因于冷却Mg/Ca-decreased液体,它可以联系到一在包围碳酸盐石膏沥滤到天青石。
简介:第一,在在Qarhan盐湖的intercrystal盐水和它的媒介盐层(盐存款)之间的一系列化学反应的宏观的化学平衡状态被使用Pitzer理论学习。有溶解比率的积累的矿石的宏观的溶解度产品和它的关系的概念被介绍,它在在Qarhan盐湖溶解并且开车钾盐的利用的数字模型被使用。并且第二,在多部件为反应溶质与形成运输的想法的一个模型一起当模特儿在多孔的媒介的新鲜地下水系统是一本参考书,一个二维的运输模型在多部件盐水结合了一系列化学反应多孔的系统(盐存款)被使用Pitzer理论开发。同时,模型被使用在Qarhan盐湖为钾/镁运输建模以便在溶解并且开车的过程并且到为在盐的采矿溶解并且捕获最大的钾/镁的最佳的注射/抽象策略在Qarhan盐湖扔的设计学习固体和液体阶段的转移法律。