简介：Cultivationisoneofthemostimportanthumanactivitiesaffectingthegrasslandecosystembesidesgrazing,butitsimpactsonsoiltotalorganiccarbon(C),especiallyontheliableorganicCfractionshavenotbeenfullyunderstoodyet.Inthispaper,theroleofcroppinginsoilorganicCpoolofdifferentfractionswasinvestigatedinameadowstepperegioninInnerMongoliaofChina,andtherelationshipsbetweendifferentCfractionswerealsodiscussed.TheresultsindicatedthattheconcentrationsofdifferentCfractionsatsteppeandcultivatedlandalldecreasedprogressivelywithsoildepth.Aftertheconversionfromsteppetospringwheatfieldfor36years,totalorganiccarbon(TOC)concentrationatthe0to100cmsoildepthhasdecreasedby12.3%to28.2%,andTOCofthesurfacesoilhorizon,especiallythoseof0-30cmdecreasedmoresignificantly(p<0.01).Thedissolvedorganiccarbon(DOC)andmicrobialbiomasscarbon(MBC)atthedepthof0-40cmwerefoundtohavedecreasedby66.7%to77.1%and36.5%to42.4%,respectively.IntheS.baicalensissteppe,theratiosofsoilDOCtoTOCvariedbetween0.52%and0.60%,andthoseinthespringwheatfieldwereonlyintherangeof0.18%-0.20%.Themicrobialquotients(qMBs)inthespringwheatfield,varyingfrom1.11%to1.40%,werealsolowerthanthoseintheS.baicalensissteppe,whichwereintherangeof1.50%-1.63%.ThechangeofDOCwasmuchmoresensitivetocultivationdisturbance.SoilTOC,DOC,andMBCweresignificantlypositivecorrelatedwitheachotherintheS.baicalensissteppe,butinthespringwheatfield,thecorrelativitybetweenDOCandTOCandthatbetweenDOCandMBCdidnotreachthesignificancelevelof0.05.更多还原

简介：为了研究中国东南沿海滨海湿地生态系统植物的养分循环机制,于2010年1月、4月、7月和10月,对广西茅尾海茳芏（Cyperusmalaccensis）种群中的茳芏进行采样,并测定其有机碳含量、全氮含量、全磷含量和生物量。结果表明,茳芏种群地上部分的有机碳含量、全氮含量和全磷含量都高于地下部分的有机碳含量、全氮含量和全磷含量;其有机碳含量的季节变化规律为春季和冬季低、夏季和秋季高,全氮含量和全磷含量的季节变化规律表现为春季和冬季高、夏季和秋季低;茅尾海茳芏生产力主要受氮元素限制,但磷元素的作用不可忽视。

简介：2010年11月采集了黄河口潮滩湿地两种典型生态系统[碱蓬（Suaedasalsa）盐沼和光滩]表层土壤样品,进行了7d的室内厌氧培养,并测定分析CH4产生潜力及其对有机物和氮输入的响应。研究结果表明,在培养周期内,碱蓬盐沼和光滩表层土壤CH4的产生潜力都在培养的第7天后达到最大,平均值分别为0.0357μg/（g·d）和0.0013μg/（g·d）,前者表层土壤的CH4产生潜力高于后者;有机物输入在一定程度上促进了CH4产生潜力,且其对碱蓬盐沼的CH4产生潜力较光滩具有更大的促进作用。尽管葡萄糖对于潮滩湿地CH4产生潜力的促进程度高于乙酸钠,但二者的差异性并不显著（p〉0.05）;氮输入对潮滩湿地土壤CH4产生潜力的影响与氮输入的形态和土壤理化性质等多种因素有关;NH4＋的添加促进了碱蓬盐沼和光滩土壤CH4产生潜力的增加,尽管其对于碱蓬盐沼的促进程度要高于光滩,但二者的差异性并不显著（p〉0.05）;NO3-的添加对碱蓬盐沼土壤的CH4产生潜力表现为抑制作用,而对光滩土壤的CH4产生潜力表现为促进作用。在当前外源有机物和氮（NH4＋—N为主）为黄河入海主要污染物的情况下,黄河口潮滩湿地土壤作为CH4源,在估算潮间带土壤温室气体排放清单时应给予特别关注。