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当前位置:首页 > 临时分类 > 底泥和藻体对太湖湖泛的诱发及水体致黑物的供应潜力
J.LakeSci.2015274575-582DOI10.18307/2015.04032015byJournalofLakeSciences*1112**12100372210008、+3、、.+>>.+Fe2+11~9433+2~56.、..ThecontributionofsedimentandalgaltotheformationofblackbloomandtheirpotentialtosupplytheblacksubstanceinwatersinLakeTaihuCAIPing1WUYuchen1LIUXin1&YINHongbin21NanjingForestryUniversityNanjing210037P.R.China2NanjingInstituteofGeographyandLimnologyChineseAcademyofSciencesNanjing210008P.R.ChinaAbstractAlaboratorysimulationsystemwasestablishedtoidentifythecontributionofalgalandsedimentspeciallythetreat-mentsincludingalgalalgal+sedimentandsedimentonlytotheformationofblackbloominLakeTaihu.Blacknessironandsulfurfractionswereanalyzedundervariedanaerobicconditionandthecontributionandpotentialofsedimentfromdifferentalgal-loadedareatoinducetheblackbloomwerededuced.Theresultsindicatedthetreatmentshaveadescendingorderinthecontribu-tiontotheformationofblackbloomasalgaltreatment<sedimenttreatment<algal+sedimenttreatment.Ferrousironinthealgal+sedimenttreatmentwas11to94foldaverage33foldasthatofalgaltreatment.Theconcentrationofreducedsulfideinthealgal+sedimenttreatmentwas2to56foldasthatofothertreatments.Theresultsalsoindicatedthatsedimentinthealgal-load-edareahasgreaterpotentialtoinducetheblackbloomthansedimentinthenonalgal-loadedarea.Whereaslittledifferencewasobservedintheformationofblackbloombetweenanaerobicandnontreatment.AlltheresultsindicatedthatthepotentialtosupplythelowvalencestateofironandsulfideinanaerobicconditionhasadecisiveeffectontheformationofblackbloominLakeTaihu.Thereforeitisnecessarytoenhancethecontrolonalgaldensityinthealgal-loadedarea.KeywordsBlackbloominduceferrousironandsulfidesedimentalgalLakeTaihu.、、.20074km220104***41371479TH2013214.2014-11-282015-01-08.1991~E-mail18362958162@163.com.E-mailhbyin@niglas.ac.cn.576J.LakeSci.20152747236km22012101/2..“”.“”FeS3-6pH、EhFeS“”、、、.7.Fe3+4Fe3+、Fe2+S2-8.S2-Mn2+/Fe2+9-1011“”...、.1.0g/L7~13d12.acidvolatilesulfideAVS13.、+.14、..、+、.11.120149Rigio11cm31°18'26″N119°57'1″E31°20'47″N120°5'5″E63.4h10cm4℃.25#24h.4000/min10min.1.2105℃24h550℃4hTN、TP.Fe2+TFe-15526nmFe3+=TFe-Fe2+.AVS、Pyrite-SES“”16.4g500ml5ml3%.AVS6mol/L15ml1mol/L2ml1min4h650nm.AVS5ml3%15mlCr2+1min48h650nmPyrite-S.5ml3%20ml1min5ml5mlCr2+24h650nmES.、Fe2+、TFe、Fe2+、TFe577FeS550nm.FeS.VcFe2+.0~0.4mmol/L.10mmol/LS2-Na2S·9H2O10mmol/LFe2+FeSO4·7H2O10mmol/LVcFeSVc1∶10.04~0.40mmol/LFeS550nm17.1.31.3.1、、、+3.250ml50g、25g25g+50g100ml.5min.4、6、8、10、13、17d3Fe2+、..1.3.250g、25g100ml250ml35℃TFe、Fe2+、.50g、25g35℃TFe、Fe2+、.22.11Tab.1Thebasicphysico-chemicalcharacteristicsofsediments/%50.753.8/%4.642.91/mV460440TN/mg/kg1.30×1031.25×103TP/mg/kg0.38×1030.37×103AVS/mg/kg1.350.83Pyrite-S/mg/kg7.813.29ES/mg/kg1.230.57Fe2+/mg/kg1.32×1030.55×103TFe/mg/kg8.59×1037.47×103AVS、Pyrite-S、ES、Fe2+21、.TN、TP、TFe.96.83%a34.32g/kg.2.2+、1+.+10d0.82mmol/L..+10dESAVS、Pyrite-S8、40mg/LAVS0.10~0.75mg/L0.43mg/LAVS4.56~6.58mg/L5.57mg/LAVS578J.LakeSci.20152741Fig.1Developmentofblacknessandreducedinorganicsulfurconcentrationindifferenttreatmentsamples+Pyrite-S0.10~0.91mg/L2Fe2+Fig.2DevelopmentofFe2+concentrationindifferenttreatedsamplesPyrite-S15.11~35.36mg/L13d+Pyrite-S15.89mg/L51.49mg/L10d.+Pyrite-S66.7.ES10d+ES0.10mg/L0.75mg/L2.+2~56+.+40%1%、、、.+AVSSO2-4S2-.3Fe2+2.Fe2+5790.37~0.73mg/L+Fe2+4.07mg/L69.19mg/L+Fe2+11~9433+Fe2+Fe2++Fe2+.+FeS.3Fig.3Developmentofreducedinorganicsulfurconcentrationinsedimentsamplesofsynechococcusandnon-synechococcusareas2.3.30.15~0.82mmol/L0.07~0.45mmol/L210d13d.1.33.AVS2.93~5.62mg/LAVS1.65mg/L11.20mg/L1.5Pyrite-S15.89~51.495.86~24.41mg/L2.2ES0.08~0.27mg/LES0.10mg/L0.75mg/L.3580J.LakeSci.20152744Fe2+Fig.4DevelopmentofFe2+concentrationinsedimentsamplesofsynechococcusandnon-synechococcusarea.Fe2+2Fe2+4Fe2+4d4.07mg/L69.19mg/LFe2+4d2.62mg/L59.44mg/L6dFe2+1.2.4.0.16mmol/L0.82mmol/L0.10mmol/L0.61mmol/L10d5.Fe2+56dFe2+Fe2+4.07mg/L69.19mg/LFe2+5.53mg/L59.33mg/L.Fe2+.3-6FeSFe2+S2-.Fe2+S2-.5Fe2+Fig.5DevelopmentofblacknessandFe2+concentrationinsamplesofdifferentlevelsofanaerobic581Pyrite-SAVSESAVS1.65~11.20、2.46~10.90mg/L6.24、6.68mg/LES0.10~0.75mg/L0.09~0.97mg/L0.43、0.53mg/L.、Pyrite-S15.89~51.49、12.54~45.04mg/L6.6Fig.6Developmentofreducedinorganicsulfurconcentrationsinsamplesofdifferentlevelsofanaerobic.--...3、++..、、、18.41DuanHMaRLoiselleSAetal.Opticalcharacterizationofblackwaterbloomsineutrophicwaters.ScienceoftheTotalEnvironment2014482174-183.2.“”.201257121060-1066.3.Fe、Mn、S.201031112652-2660.4.Fe、S、P.20093092520-2526.5..201150-58.6ShenQZhouQShangJetal.BeyondhypoxiaOccurrenceandcharacteristicsofblackbloomsduetothedecompositionofthesubmergedplantPotamogetoncrispusinashallowlake.JournalofEnvironmentalSciences2014262281-288.582J.LakeSci.20152747LiuCShenQZhouQetal.Precontrolofalgae-inducedblackbloomsthroughsedimentdredgingatappropriatedepthinatypicaleutrophicshallowlake.EcologicalEngineering201577139-145.8.-.2009.9HeYTWilsonJTWilkinRT.Transformationofreactiveironmineralsinapermeablereactivebarrierbiowallusedtotreattceingroundwater.EnvironmentalScienceandTechnology200842176690-6696.10LutherLiiGWGlazerBMaSetal.Ironandsulfurch
本文标题:底泥和藻体对太湖湖泛的诱发及水体致黑物的供应潜力
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