简介：Co,Ni,CrandVin25typicalsoilsofChinawerefractionatedintoexchangeable,carbonatebound(calcareoussoils),Mnoxidebound,organicallybound,amorphousFeoxidebound,crystallineFeoxideboundandresidualformsusingaseven-stepsequentialextractionprocedure,soastostudythedistributionofchemicalformsofthesemetalsaswellastheeffectsofsoilproipertiesonthedistribution.TheresultsshowedthatmostofsoilCo,Ni,CrandVwerepresentinresidualforms,andthedistributionratioaveraged48.2%forCo,53.0%forNi,81.5%forCrand68.7%forV.Thespeciationofheavymetalswasgreatlyinfluencedbysoilphysico-chemicalpropertiesandthechemistryofelements.Theresultsalsoindicatedthattherecoveryofmetalelementsbythesequentialextractionprocedurewassatisfactory,withtherelativedifferencebetweenthesumofsevenformsandthetotalcontentinsoilsaveraging9.5%forCo,12.8%forNi,6.6%forCrand7.2%forV.

简介：ForestmanagementisexpectedtoinfluencesoilCO2efflux(FCO2)asaresultofchangesinmicroenvironmentalconditions,soilmicroclimate,androotdynamics.SoilFCO2ratewasmeasuredduringthegrowingseasonof2006inboththinningandnon-thinninglocationswithinstandsrangingfrom0to8yearsafterthemostrecentthinninginChinesefir(Cunninghamialanceolata(Lamb.)Hook)plantationsinHuitongEcosystemResearchStation,Hunan,China.SoiltemperatureandmoisturewerealsomeasuredtoexaminerelationshipsbetweenFCO2andsoilproperties.ForestthinningresultedinhugechangesinFCO2thatvariedwithtimesincecutting.Immediatelyfollowingharvest(year0)FCO2inthinningareaincreasedbyabout30%,declinedto20%–27%belowpre-cuttinglevelsduringyears4–6,andrecoveredtopre-cuttinglevelsat8yearspost-cutting.Asimilartemporalpattern,butwithsmallerchanges,wasfoundinnon-thinninglocations.TheinitialincreaseinFCO2couldbeattributedtoacombinationofrootdecay,soildisturbance,andincreasedsoiltemperatureingaps,whilethesubsequentdecreaseandrecoverytothedeathandgradualregrowthofactiveroots.StrongeffectsofsoiltemperatureandsoilwatercontentonFCO2werefound.ForestthinningmainlyinfluencedFCO2throughchangesintreerootrespiration,andthenetresultwasadecreaseinintegratedFCO2fluxthroughtheentirefellingcycle.

简介：从土壤表面的二氧化碳(CO2)的流动在陆上的生态系统介绍碳(C)周期的一个重要部件并且被很多个关於生命、不能生活的因素控制。以便更好在副热带的森林里理解土壤CO2流动(FCO2)的特征，土壤FCO2率在五种邻近的森林类型被确定(樟脑树森林，马森松森林，混合樟脑树和马森消瘦森林，中国香甜的口香糖森林，并且猛砍松森林)在在长沙的Tianjiling国家公园，湖南省在副热带的中国，从1月到2010年12月。土壤温度(Tsoil)的影响，容量的土壤浇内容(土壤)，玷污pH，玷污器官的碳(SOC)并且玷污土壤FCO2率上的C/nitrogen(N)比率也被调查。年度吝啬的土壤FCO2率与森林类型变化了。土壤FCO2率在樟脑树森林里是最高的(3.53瑮楲畢楴湯?潴琠敨猠楯??中?湡?桴瑡倠?灡汰捩瑡潩?污潳愠捣汥牥瑡摥???牴湡晳牯慭楴湯椠?潳汩猠飼?飼吗？？

简介：Aridsoilswherewaterandnutrientsarescarceoccupyover30%oftheEarth’stotalsurface.However,themicrobialautotrophyintheharshenvironmentsremainslargelyunexplored.Inthisstudy,theabundanceanddiversityofautotrophicbacteriawereinvestigated,byquantifyingandprofilingthelargesubunitgenesofribulose-1,5-bisphosphatecarboxylase/oxygenase(RuBisCO)formI(cbbL)responsibleforCO2fixation,inthearidsoilsunderthreetypicalplanttypes(Haloxylonammodendron,Cleistogeneschinensis,andReaumuriasoongorica)inNorthwestChina.Thebacterialcommunitiesinthesoilswerealsocharacterizedusingthe16SrRNAgene.Abundanceofred-likeautotrophicbacteriarangedfrom3.94×105to1.51×106copiesg-1drysoilandthoseofgreen-likeautotrophicbacteriarangedfrom1.15×106to2.08×106copiesg-1drysoil.Abundanceofbothred-andgreen-likeautotrophicbacteriadidnotsignificantlydifferamongthesoilsunderdifferentplanttypes.TheautotrophicbacteriaidentifiedwiththecbbLgeneprimerweremainlyaffiliatedwithAlphaproteobacteria,Betaproteobacteriaandanunculturedbacterialgroup,whichwerenotdetectedinthe16SrRNAlibrary.Inaddition,25.9%and8.1%ofthe16SrRNAgeneswereaffiliatedwithCyanobacteriainthesoilsunderH.ammodendronandR.soongorica,respectively.However,noCyanobacteria-affiliatedcbbLgenesweredetectedinthesamesoils.TheresultssuggestedthatmicrobialautotrophicCO2fixationmightbesignificantinthecarboncyclingofaridsoils,whichwarrantsfurtherexploration.

简介：Biochar是生物资源热分解获得并且考虑了碳隐遁的一个平均数的一个充满碳的产品。在这研究，从食物与农业科学的学院的农场的沙的石灰质的土壤，绍德国王大学，沙特阿拉伯，与也被修改Conocarpus直立的L的木质的废物。(CW)或biochar(BC)以0的率(控制)从CW生产了，10，30和50gkg−1。土壤pH，溶解的器官的碳(文档)，微生物引起的生物资源碳(MBC)，公司2排放和新陈代谢的商上的修正案的效果(沙的石灰质的土壤的qCO2)在一个60-d孵化实验被学习。结果证明CW的增加与控制和BC的增加相比在土壤pH导致了重要减少。公司2-C排放率比孵化时间什么时候进行在孵化的开始几天内是更高的。特别以更高的率，从与CW修改的土壤的累积公司2-C排放更高(近似到6褶层的3-)与BC从控制和土壤比那修改了。修改BC的土壤证明因为与非修改的土壤，而是累积公司2-C的增加相比排放不在孵化的60d以后是重要的，公司2-C排放的重要增加在孵化的第一天期间评价。在另一方面，CW应用比控制和BC应用导致了更加更高累积的公司2-C排放，MBC和文档。与0白天的异常(在孵化的1h以后)，导致的CW和BC应用程序作为与控制相比降低qCO2的值。力量功能运动模型令人满意地描述了累积公司2-C排放。通常，公司2排放的最低价值与BC在土壤被观察，建议到公司2排放的BC的贡献作为与CW的相比很小。

简介：Anopen-topchamberexperimentwasconductedattheUniversityofMichiganBiologicalStationnearPellston,Michigan,USA,tostudytheeffectsofsoilfertilityandCO2onleaf,stemandrootdarkrespiration(Rd)ofPopulustremuloides.Overall,area-baseddaytimeleafRd(Rda)wassignificantlygreateratelevatedthanatambientCO2inhigh-fertilitysoil,butnotinlow-fertilitysoil.Mass-basedleafRd(Rdm)wasoverallgreaterforhigh-thanforlow-fertilitysoilgrowntreesatelevated,butnotatambientCO2.NighttimeleafRdaandRdmwereunaffectedbysoilfertilityorCO2,norwasstemRda,whichrangedfrom1.0to1.4μmolm-2s-1inthespringand3.5to4.5μmolm-2s-1inthesummer.RootRdawassignificantlyhigherinhigh-thaninlow-fertilitysoil,butwasunaffectedbyCO2.SincebiomassproductionofP.tremuloideswillbesignificantlygreateratelevatedCO2whilespecificRdwilleitherincreaseorremainunchanged,wepredictthatcarbonlosstotheatmospherethroughrespirationfromthisecologicallyimportantspecieswouldincreaseathigherCO2.SoilfertilitywouldalsointeractwithelevatedCO2inaffectingthecarbonflowintheplant-soil-airsystem.

简介：降水在半干旱、干旱的区域是生态系统函数和进程的主要驱动程序。在如此的水有限生态系统，搏动了水输入直接通过弄干的一系列土壤和重新弄湿的周期控制地下的过程。在土壤CO2流出上调查水的分散的增加的效果，一个人工的降水事件(3公里)在亩被用于一个荒芜的灌木生态系统我们在中国的Ordos高原的沙土地。土壤呼吸率在在这块地里增加水以后立即增加了2.84.1次，然后它在48h以内回到了背景水平。在实验期间，土壤CO2生产在2047.0和7383.0mgm之间?2。在灌木陆地，土壤呼吸回答显示出空间变化，有在比在interplant空格的灌木下面的更强壮的脉搏效果。土壤呼吸回答的空间变化仔细与土壤底层可获得性的异质被联系。除了降水，玷污器官的碳和全部的氮水池也在荒芜的生态系统作为土壤CO2损失的决定因素被识别。

简介：Theclosed-jarincubationmethodiswidelyusedtoestimatethemineralizationofsoilorganicC.TherearetwoCpools(i.e.,organicandinorganicC)incalcareoussoil.ToevaluatetheeffectofadditionalcarbonatesonCO2emissionfromcalcareoussoilduringclosed-jarincubation,threeincubationexperimentswereconductedbyaddingdifferenttypes(CaCO3andMgCO3)andamountsofcarbonatetothesoil.TheadditionofcarbonatessignificantlyincreasedCO2emissionfromthesoil;theincreaserangedfrom12.0%intheCaCO3amendedsoilto460%intheMgCO3amendedsoilduringa100-dincubation.CumulativeCO2productionattheendoftheincubationwasthreetimesgreaterintheMgCO3amendedsoilcomparedtotheCaCO3amendedone.TheCO2emissionincreasedwiththeamountofCaCO3addedtothesoil.Incontrast,CO2emissiondecreasedastheamountofMgCO3addedtothesoilincreased.Ourresultsconfirmedthattheclosed-jarincubationmethodcouldleadtoanoverestimateoforganicCmineralizationincalcareoussoils.BecauseofitseffectonsoilpHandthedissolutionofcarbonates,HgCl2shouldnotbeusedtosterilizecalcareoussoiliftheexperimentincludesthemeasurementofsoilCO2production.

简介：Theannualseriesofδ13CweremeasuredintreeringsofthreeCryptomeriafortuneidisks(CF-1,CF-2,andCF-3)collectedfromWestTianmuMountain,ZhejiangProvince,China,accordingtocross-datingtreeringages.Therewasnoobviousdecreasingtrendoftheδ13CannualtimeseriesofCF-2before1835.However,from1835to1982thethreetreeringδ13Cannualseriesexhibitedsimilardecreasingtrendsthatweresignificantly(P≤0.001)correlated.Thedistributioncharacteristicsofascatterdiagrambetweenestimatedδ13CseriesofCF-2frommodelingandtheatmosphericCO2concentrationextractedfromtheLawDomeicecorefrom1840to1978wereanalyzedandacurvilinearregressionequationforreconstructingatmosphericCO2concentrationwasestablishedwithR2=0.98.Also,atestofindependentsamplesindicatedthatbetween1685and1839thereconstructedatmosphericCO2concentrationusingtheδ13CseriesofCF-2hadacloserelationshipwiththeLawDomeandSipleicecores,withastandarddeviationof1.98.ThegeneralincreasingtrendofthereconstructedatmosphericCO2concentrationcloselyreflectedthelong-termvariationofatmosphericCO2concentrationrecordedbothbeforeandaftertheIndustrialRevolution.Between1685and1840theevaluatedatmosphericCO2concentrationwasstable,butafter1840itexhibitedarapidincrease.Givenalongerδ13Cannualtimeseriesoftreerings,itwasfeasibletorebuildarepresentativetimeseriestodescribetheatmosphericCO2concentrationforanearlierperiodandforyearsthatwerenotintheicecorerecord.

简介：钴(公司)在自然地发生在重要数量存在锰(Mn)氧化物并且改变Mn氧化物晶体的生长。四分层的Mn氧化物，Na-buserite(Na公共汽车)并且三共同做从Mn的氧化准备的Na-buserite样品(哦)2与5%，10%，和20%Co/(Mn+公司)臼齿的比率(5Co-Na-bus，10Co-Na-bus，和20Co-Na-bus)，被用来准备todorokite，地球的表面上的普通Mn氧化物，把Mg2+/Co2+离子用作一个模板。结果证明todorokites能被交换Mg2+的非做的Na-buserite的倒流处理获得，三共同做在气压的Na-buserites。然而，todorokites的形成被交换Co2+的Na公共汽车，5Co-Na-bus，和10Co-Na-bus样品的倒流处理禁止。相反，todorokite被交换Co2+的20Co-Na-bus样品的倒流处理在气压下面获得。X光检查光电子光谱学分析证明做的公司在做的Na-buserites的MnO6层作为Co3+存在。在MnO6层的代替的Co3+的数量可以作为一个模板用Co2+离子在buserite的变换起一个关键作用到todorokite。