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简介:TheMayangCudeposit,westernHunanisamiddle-scalesandstone-typeCudepositpredominantofnativecopper.Fromanangleofgeologicalintegrativefield,fracturegeochemicalfeaturesarestudidedanddiscussedinthispaper.Infracturestructure,variantregularityandtheratiosofelementcouplesparticipatinginmetallogensisthattheirgeochemicalnaturesaresimilarorstronglycorrelative,revealchanginglawsofmetallogenictemperatureandpressurefieldsandmigratingdirectionofmetallogenicelements.Thetheoreticalstudytalliesmuchbetterwithproductivepractice.Theyaremeaningfultoconductprospectingandexployation.
简介:这个工作由进行批实验在沉积调查Cu离子的吸附,包括等温的实验和吸附动力学实验。从等温的实验的数据用Freundlich和Temkin模特儿兰米尔被分析,试验性的运动数据用伪first-order,pseudo-second-order,Elovich,液体电影散开和intra粒子散开模型是合适的。兰米尔模型导致了为平衡数据合适的最好,它显示沉积上的Cu离子的吸附能力是1.0403?mg?有K1>L4.2877的KL价值?L?mg1。也提供的Freundlich和Temkin模型好适合,并且nFnF和A价值是3.8565和66.9964?Lmg1,分别地,显示在Cu离子和沉积之间的更强壮的吸附紧张和吸附精力。与伪first-order和Elovich模型相比,pseudo-second-order模型为描述吸附动力学是更适当的,显示吸附的化学吸着性质。吸附运动过程能被划分成电影散开,毛孔散开和吸附反应。为吸附动力学的控制的步随着吸附过程的发展变化了。全部吸附过程拿了180?min。电影散开是控制步骤为开始的20?min。在期间20~60?min时期,逐渐地增加的毛孔散开和电影散开减少了以便两现象共存了。毛孔散开在60-180期间是控制步骤?min时期。
简介:这篇论文在Guiyang的地表的土壤描述象Cu和Zn那样的重金属污染物质的环境联盟者geochemical特征,GuizhouProvince的首都的城市。在土壤和geochemical标准的重金属的基线集中被建立了在环境上区分自然或人工的影响。用统计上分析方法,我们在Guiyang(18.8mg/kg)建立了Cu的基线,土壤(超过68.4mg/kg)可以承受Cu污染。Zn的数据是46。3mg/kg并且112。0mg/kg。Geoaccumulation指数分析显示有sufferednon污染到的地表的土壤为38%,38%,和22%的Cu帐户为中间污染中间污染,并且仅仅对严重污染中间污染的2%between。承受了Zn的非污染tomid污染的地表的土壤占41%,50%,和7%为中间污染,并且仅仅2%betweenmid污染到严重污染。Cu污染的最大的度在Guiyang的surficials油是5.09。没为53承受Cu污染报道的地表的土壤。2%。Cu的全部的污染度是稍微超过零。Guiyang的地表的土壤因此承受了slightCu污染。Zn污染度的最大的价值是2。85在地表的土壤ofGuiyang。77。8%地表的土壤还没承受了任何Zn污染。Zn的全部的污染度是不到零。在Guiyang的地表的土壤因此从Zn的污染是免费的。
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简介:KelanaJayaMunicipalParkisapopularrecreationparkinPetalingJaya.Thefivelakes,locatedwithinthePark,wereex-miningponds,functioningasfloodretentionpondsandreceivingeffluentsfromnearbyhumanactivitiesmainlyfromresidentsandtransportation.Astudywasconductedtodeterminethedistributionandsourcesofheavymetals(Cd,CuandZn)inthesedimentsofKelanaJayaLakes.ConcentrationsofCd,Cu,andZnforsurfacesedimentweredeterminedbyusingaqua-regiamethodandsequentialextractiontechnique.TotalCdconcentrationsrangedfrom0.48μg/gto2.68μg/gdryweight(dw)foralllakes.TotalCdconcentrationsinsedimentofalllakesexceededCCME(CanadianCouncilofMinistersoftheEnvironment,2001)guidelines.TotalCuconcentrationsrangedfrom7.37μg/gto73.6μg/g(dw).OnlyCuconcentrationinonelakeexceededtheCCMEguidelinesbesideshavingthehighestmeanconcentrationamongall.TotalZnconcentrationsrangedfrom107μg/gto529μg/g(dw).Again,TheZnconcentrationsinthreelakeswerefoundtoexceedCCMEguidelinesforZnconcentrationinfreshwatersediment.GeochemicalstudyonsedimentrevealedthatnonresistantfractionsforCd,CuandZnforotherlakesthereCuandZnindicatedthatlakesinthepark,especiallynearoxidationpondandmonsoondrains,couldhavereceivedanthropogenicmetalsfromdomesticwastes.RehabilitationprogramandregularbiomonitoringatKelanaJayaLakesarethereforerecommended.
简介:ThestrongadaptabilityofBroussonetiapapyrifera(L.)Vent.tolowphosphorus(P)conditionscanbeattributedtothelargeamountofroot-exudedorganicacidsandthehighef?ciencyofPextraction.However,microelementcontentsarein?uencedbylow-Pstress,andtheireffectsonthephotosyntheticcapabilityofB.papyriferaremainunknown.Inthisstudy,weinvestigatedtheeffectsoflow-Ptreatmentonnetphotosyntheticrate(P_N);chlorophylla?uorescence(ChlF)characteristics;andFe,Mn,Cu,andZncontentsofB.papyriferaandMorusalbaL.seedlings.ResultsshowthatB.papyriferaexhibitedbetterphotosyntheticcapabilityundermoderatePde?-ciency(0.125,0.063,and0.031mmol/LPtreatments),whereasthephotosyntheticcapabilityofM.albadecreasedundermoderateandseverePde?ciency(0.016and0mmol/LPtreatments).UndermoderatePde?ciency,thedecreaseinCuandZncontentsinB.papyriferawaslowerthanthatinM.alba.UnderseverePde?ciency,aconsiderabledecreaseofphotosyntheticcapabilityinB.papyriferaandM.albawasassociatedwithlowCuandZncontents.ThePNofthetwoMoraceaespeciesexhibitedabettercorrelationwithCuandZncontentsthanwithFeorMncontent.Pde?ciencycouldnotonlydecreasecyclicphotophorylationandphotosyntheticef?ciency,butcouldalsoaffectthestabilityofthylakoidmembranestructureandelectrontransportef?ciencybyin?uencingthecontentsofCuorZn,therebyaffectingphotosynthesis.
简介:Yinshananticlineistheproductoftectono-dynamicdeformation-metamorphism.Alongtheaxisoftheanticlineexistsabrittle-ductileshearingzonewhichobviouslycontrolstheore-formation.Mineralizationoccursalongtheaxisoftheanticlineinawidthofabout1000m.Intheminingarea,volca-no-subvolcanicrocksofEarlyYanshanperiodaredividedintothreecycles:Iintermediateacidicdacitelavaanddaciteporphyry;Ⅱacidicamphibolelipariteandquartzporphyry;Ⅲintermediateandesiteporphyrite.AmongthemactivitiesofⅠandⅡcyclesaremoreintensiveandareintimatelyrelatedtothemineralization.Yinshanoredepositistheresultofcombinativeprocessesoftectono-dynamicandvolcano—magmatichydrothermalfluids,sothattherearetwocentersofmetallogeniczoning,onebeingtheaxialstrainzoneofYinshananticlinewhichisthecenteroffirstorder,andtheotherbeingporphyrystock,2ndorder.
简介:铂组元素(PGE)的集中从Zhireken,Shakhtama和Aksug斑岩Cu瞬间存款在主要magmatic磁铁矿样品被分析了(西伯利亚,俄国)由激光,决定PGE的范围的脱离诱导地联合的血浆团spectrometry在磁铁矿并且到支票满足从二间主要岩石套房(贫瘠Pluto的套房和使矿物化的斑岩套房)的磁铁矿是否有不同PGE作文。这里介绍的结果显示磁铁矿在PGE被充实相对整个岩石。矿石相关的斑岩和贫瘠Pluto的套房的比较证明磁铁矿在两间套房展出相对类似的PGE分发模式。在Rh和Ru内容的变化被氧易逃逸在岩浆结晶化期间控制。