简介:Sulfurtransformationin3soilsmaintainedinaclosedincubationsystemanditsavailabilitytoplantswereinvestigatedusingcarrier-free^35S-SO4^2-and^35S-labeledryegrassstraw.Forcarrier-freeNa2^35SO4treatment,78%,70%and64%of^35SappliedwerefoundinCa(H2PO4)2-extractaleSfraction,4%,5%and7%inslowlysolubleinorganicS,11%,15%and18%inC-O-S,5%,7%,and6%inC-bondedS,and5%,7%and6%inunidentifiedorganicS120daysafterincubationinblacksoil,cinnamonsoilandchestnutsoil,respectively.Mostof35Suptakebyplantscamefromextractable35SO4^2-,andlittlefromC-O-^35SandC-bonded^35S,Inthetreatmentwith35S-labeledstraw,51%,46%and36%of35SincorporatedwerefoundinCa(H2PO4)2-extractableSfraction,7%,6%and7%inslowlysolubleinorganicS,13%,15%and18%inC-O-S,8%,8%and6%inC-bondedS,and18%,25%and35%inunidentifiedorganicSattheendofincubationinabove-mentonedthreesoils,respectively.HigheravailabilityofC-O-35S,C-bonded35Sandunidentifiedorganic35Sfrom35S-labeledstrawwasobservedin35S-labeledstrawtreatmentcomparedtocarrier-freeNa2^35SO4treatment.
简介:金沙江上游地质灾害频发,地质环境演化相对复杂。为研究堰塞湖溃坝后堆积物的来源与坝体物质、沉积环境的关系,以金沙江上游雪隆囊古滑坡堰塞湖溃坝堆积物为主要研究对象,通过野外实地调查取样和室内粒度筛分试验,对雪隆囊滑坡堰塞湖溃坝堆积物的粒度进行测试,并分别对滑坡堰塞湖溃坝堆积物的上、中、下游3段的粒度特征进行研究。结果表明:从溃坝堆积体的上游到下游,粒度分布曲线分别为单峰、多峰、双峰;上游粒度组成主要以砾石为主,中游和下游主要以细砂和极细砂为主,粒度从上游到下游依次有明显的细化趋势,平均粒度由粗变细,分选性整体上较差和差。以上这些特点综合反映出溃坝堆积体的上游段到下游段的水动力条件在逐渐减弱,其中堆积体上游段砾石部分来自坝体物质,而中、下游段细粒部分既可能来自坝体,又可能来自堰塞湖溃坝前的上游湖相沉积层。
简介:EctomycorrhizalfungusLaccariabicolorS238N,isolatedfromaforestsoilincentralFrancein1990s,hasdemonstratedunequivocallyandabilitytopromotepinegrowth.Inthepresentnurserybedexperiment,theabilityofthisectomycorrhizalfungustoincreasegrowthandPandKuptakeofDouglasFirseedlings(Zone22)wasexamined.Growthofinoculatedseedlingswasovertwice(plantheight)andthreetimes(biomass)thatofnon-inoculatedones.Similarly,boththeconcentrationsandtheamountsofPandKuptakebyseedlingsweresignificantlyincreasedbyfungalinoculation,indicatingtheimprovementofPandKnutritioninmycorrhizalseedlings.Incontrast,Al-Pinthesoilswasdecreasedobviouslybyplants,especiallybymycorrhizas,suggestingutilizationofthissoilPpoolbyplantsandmoreefficientAl-Pmobilizationbymycorrhizasthanbynomycorrhizas.Moreover,Kextractedby1mol/LHClfollowingconsecutiveextractionofH2OandCH3COONH4,whichmaynotbeplantavailable,couldbeutilizedbyfunguscoloniedroots.ThiscouldbeexplainedbythereleaseofprotonsandoxalatebyhypaewhichleadstoreplacementofinterlayerKinnonexpanded2:1claymineralsandbio-weatheringofphyllosilicates.
简介:岩溶石漠化是广西脆弱生态恢复建设中面临的突出生态环境问题.以1988、1998和2008年3个时相的TM/ETM卫星数据为主要信息源,综合碳酸盐空间分布图、石漠化状况实地调查结果和历史资料,基于3S技术,构建岩溶石漠化遥感监测和分级评价模型,研究广西平果县岩溶区石漠化空间分布特征及演变规律.结果表明:1)岩溶石漠化遥感监测和分级评价模型能够反映平果县石漠化状况,基本符合实地调查结果;2)平果县岩溶石漠化主要分布在该县西南部和中部,1988-2008年,平果县总体石漠化程度经历了稍加重然后逐渐变轻的变化趋势,石漠化呈现动态、缓慢、反复、可治理等特点.建议采取先易后难、逐步改善的治理策略.研究结果可为中国西南岩溶石漠化治理和区域生态建设的宏观决策提供参考.