简介:从1999年8至10月,2000年的4至6月,2002年8月至2003年9月,在平均树高为26米的长白山阔叶红松林内,用红外气体分析仪(2250D,LI-CORInc.和LI-COR,820)测定了不同高度的二氧化碳浓度。根据测定的数据,分析了阔叶红松林二氧化碳廓线的日变化和季节变化动态。结果表明:CO2浓度的垂直分布在白天和夜间是不同的,在接近地面处CO2浓度始终最大。从季节CO2廓线看出,在植物生长季节林冠处CO2浓度有明显的成层现象,不同高度(60~2.5m)的CO2浓度3月份变化较小差值为10mmol穖ol-1,而在7月份变化较大,差值为60mmol穖ol-1。7月份林冠处(22,26,32m)CO2浓度梯度较大,浓度差为8mmol穖ol-1。计算位于涡度相关仪器之下的40米高空气柱中CO2贮存状况表明,年际贮存是负值,但对NEE的贡献很小。图4参11。
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:TheimpactsofelevatedtemperatureandCO2onyoungsilverbirch(BetulapendulaRoth)saplingsafter0,25,50or75%artificialdefoliationwereassessedbymeasuringplantheightanddrymassofabovegroundcompartmentsandrootsandvariousmorphologicalandphysiologicalvariables.Defoliationeitherincreasedordecreasedplantgrowthdependingontheseverityofdamageandtheclimatictreatment.At21Cand400mgL-1CO2,defoliatedplantswerenotabletocompensateforthelostfoliage,butgrowthcompensationandadaptationtothechangedconditionsweregreater;growthofyoungdefoliatedsilverbirchsaplingsincreased,whichledtoincreasedheightandatendencytoenhancefinalabovegroundandrootbiomassandleafnitrogenandcarboncontentcomparedtothenondefoliatedcontrols.Nevertheless,theshort-termeffectofthedifferentclimaticconditionsdidnotresultinasignificantovergrowthofdefoliatedplants.AslightincreaseintemperatureandCO2werethemostacceptableconditionsfordefoliatedplants;however,a4CincreasewithcorrespondinglyhigherCO2wasmorestressfulasshownbylessgrowthinheightandbiomassallocationtoleaves,stemsandroots.Thefindingsfromthepilotexperimentaremoreapplicabletoyoungbirchtrees,butstressonyoungtreesmaybereflectedinfuturetreegrowth.
简介:Background:Thispaperexploredthelong-term,ceteris-paribuseffectsofpotentialCO,fertilizationontheglobalforestsector.BasedonthefindingsofNorbyetal.(PNAS2005,102(50))aboutforestresponsetoelevated[CO_2].Methods:ForestproductivitywasincreasedintheGlobalForestProductsModel(GFPM)inproportiontotherising[CO.,]projectedintheIPCCscenarioA1B,A2,andB2.Projectionsoftheforestareaandforeststockandoftheproduction,consumption,prices,andtradeofproductsrangingfromfuelwoodtopaperandpaperboardwereobtainedwiththeGFPMforeachscenario,withandwithoutCO_2fertilizationbeginningin2011andupto2065.Results:C02fertilizationincreasedwoodsupply,leadingtolowerwoodpriceswhichinturninducedmodestlowerpricesofendproductsandhigherglobalconsumption.However,productionandvalueaddedinindustriesdecreasedinsomeregionsduetotherelativecompetitiveadvantagesandtothevaryingregionaleffectsofCO_2fertilization.Conclusion:ThemaineffectofCO,fertilizationwastoraisetheleveloftheworldforeststockin2065by9to10%forscenariosA2andB2andby20%forscenarioA1B.Theriseinforeststockinducedbyfertilizationwasinpartcounteractedbyitsstimulationofthewoodsupplywhichresultedinlowerwoodpricesandincreasedharvests.
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:为研究鸭梨可溶性固形物(SSC)等内在品质对其组织褐变发生的影响,进而为鸭梨组织褐变采前防控技术提供理论依据,利用K—BA100R型无损水果糖度检测仪,按SSC高低对鸭梨进行分级,贮于0℃环境中,分别采用1%02+10%C02浓度的气体进行诱导褐变处理15d和30d,分析鸭梨果实采后品质与其组织褐变的关系。结果表明,诱导处理30d。鸭梨果皮和果肉褐变指数与SSC分别呈极显著(R=0.999,R=0.992)正相关,与果实单果重呈显著(R:0.965,R=0.959)正相关,与可滴定酸(TA)含量呈显著负相关(R=-0.958,R=-0.966)。随着诱导时间的延长,果实组织褐变程度越重,TA和VC含量下降明显,且鸭梨果皮、果肉和果心组织的细胞膜透性增大。同时,在鸭梨果皮组织中,N、Ca和B元素的含量越高,则果皮无褐变或褐变程度较轻;在果肉和果心组织中,无褐变或褐变相对较轻的果实,其K和B元素含量较高:褐变程度较重的果实.其组织中的Ca含量较低。表明鸭梨果实的TA与VC含量及K、B、Ca等元素含量与其组织褐变关系密切,提高鸭梨果实的内在品质可在一定程度上减少褐变的发生.而SSC含量与高CO2伤害型黑心病的发生程度无明显规律。
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:本研究于2013~2014年在内蒙古达茂旗短花针茅荒漠草原设置了氮肥和磷肥的单施和配施样地,以未施肥样地为对照,采用LI-6400土壤碳通量测量系统测定了草地生态系统净碳交换(NEE)、总的生态系统生产力(GEP)和生态系统呼吸(ER)的日、季节变化,并分析了生态系统CO2通量与环境因子之间的关系。研究表明,施肥未改变短花针茅荒漠草原生态系统CO2通量的日、季节变化特征。但NP肥的配施(10gN·m^-2,10gP·m^-2)可显著提高荒漠草原NEE、GEP和ER(P<0.05);三个N肥水平的NEE、GEP和ER大小关系基本表现为N10(10gN·m^-2)≈N5(5gN·m^-2)>N2.5(2.5gN·m^-2),即N5水平是增加荒漠草原生态系统碳汇效应的最佳施氮量。土壤0~10cm含水量是影响短花针茅荒漠草原生态系统净碳交换量和总的生态系统生产力的主要环境因子,温度是影响生态系统呼吸的主要环境因子。