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29820168ResearchofEnvironmentalSciencesVol.29No.8Aug.2016.29J.20162981187-1194.LUShaoyongWANZhengfenLIFengminetal.Ammonianitrogenadsorptionanddesorptioncharacteristicsoftwenty-ninekindsofconstructedwetlandsubstratesJ.ResearchofEnvironmentalSciences20162981187-1194.2015-12-202016-04-112012ZX07105-0022012-YSKY-14413730271976-lushy2000@163.com.29112221.1000122.266100-29、NH3-N-.、、、、、、、、FreundlichLangmuirNH3-NLangmuirNH3-N51.7000mgg、1.6200mgg、1.3530mgg、1.3500mgg、1.1900mgg.NH3-N.、、、、、NH3-N20%NH3-N24.50%35.51%.、、、NH3-N.、、、NH3-N.X7031001-6929201608-1187-08ADOI10.13198j.issn.1001-6929.2016.08.11AmmoniaNitrogenAdsorptionandDesorptionCharacteristicsofTwenty-NineKindsofConstructedWetlandSubstratesLUShaoyong1WANZhengfen12LIFengmin2ZHANGXueqing21.StateEnvironmentalProtectionScientificObservationandResearchStationforLakeDongtinghuSEPSORSLDStateEnvironmentalProtectionKeyLaboratoryforLakePollutionControlStateKeyLaboratoryofEnvironmentalCriteriaandRiskAssessmentChineseResearchAcademyofEnvironmentalSciencesBeijing100012China2.KeyLaboratoryofMarineEnvironmentalScienceandEcologyMinistryofEducationCollegeofEnvironmentScienceandEngineeringOceanUniversityofChinaQingdao226100ChinaAbstractTheporosityhydraulicconductivityandadsorptionanddesorptioncharacteristicsofammonia-nitrogenNH3-Nintwenty-ninekindsofmaterialswereanalyzedtodeterminemoreeffectiveconstructedwetlandsubstratesforadsorbingNH3-N.Theresultsshowedthattheporosityofsawdustvitroliteeggshellporcelainceramistandvolcanicrockwerelargerwhilethepermeabilityofceramsitespongeironlimestoneshaleceramsiteandgravelwerehigher.FreundlichandLangmuirisothermscouldadequatelypredicttheadsorptionprocess.AccordingtotheestimatesfromtheLangmuirisothermthemaximumtheoreticalsaturatedcapacitiesdecreasedinthefollowingordervolcanicrock1.7000mgg>porcelainceramist1.6200mgg>biochar1.3530mgg>zeolite1.3500mgg>garnet1.1900mgg.IngeneraltherewerethreekindsoftrendsofNH3-Nadsorptionratesinsubstratesonewasfirstincreasethendecreaseandfinallytendedtobalancesecondwasfirstincreasethentendedtobalanceandthirdwasfirstincreasethendecreaseandfinallyincrease.Thevariationofadsorptionratewascloselyrelatedtoeachsubstrate’sadsorptionmechanism.Adsorptionsaturatedsubstratessuchasbiocharcokedaliclaymaifanstoneanthracitezeolitemagnetiteandquartzadsorbed29NH3-Nmainlythroughionexchangewhichismorestablewithsmallerdesorptionrates<20%.ClayceramsiteandvolcanicrockadsorbedNH3-Nthroughcombinedphysicaladsorptionandionexchangewithdesorptionratesof24.5%and35.1%respectively.VolcanicrockporcelainceramistbiocharandzeoliteshowedhigheradsorptionefficiencywhentreatingwastewaterwithhighconcentrationofNH3-N.Consequentlyvolcanicrockporcelainceramistbiocharzeoliteareappropriatesubstratesforconstructedwetlands.Keywordsconstructedwetlandsubstrateammonia-nitrogenadsorptiondesorptionρNH3-N0.2mgL1.、、、2-3NH3-N.NH3-N、、、.NH3-N、4、5、、6-8、8.、、、、9-10NH3-N60%11-13141516-17.NH3-N18.19、18-20..29NH3-N.11.11~2mm、、、、、、、、、、2~4mm、、、、、、、、、、3~5mm、、、1mm、、..ρNH3-N2122.50mm5L5L.1.Φ=V0V×100%1Ф%V0LVL...A、L.s=VW·LA·△h·t2scmsAcm2LcmVWtcm3△hcm.1.2LangmuirFreundlich23-24Q=QmaxKC1+KC3q=kC1n4QNH3-NmggQmaxNH3-NmggCmgLKnk.1.38811829105℃2h1g50mLρ0、5、8、15、25、30、60、80mgLNNH4Cl20mL25℃、175rmin24h5000rmin15minρNH3-N.0.02molLCaCl225℃、175rmin24h5000rmin15minρNH3-N.22.11、229.25..、26.27、、、、、、、..1、2、、、、、、、、50%、、、、、、、、、0.2760cms、、、、、.、、40%40%~50%.28.293%~44%.10d3.530.、、、、.1Table1Porosityandhydraulicconductivityoftenkindsofnon-naturalsubstrates%cms53.980.289343.620.384362.920.561342.160.125863.860.067432.70—51.060.276052.400.008821.260.249050.000.07632Table2Porosityandhydraulicconductivityofnineteenkindsofnaturalsubstrates%cms42.120.179760.840.116645.080.412645.300.155048.460.362537.740.148645.580.129940.960.259663.200.312480.400.090058.300.514843.750.001544.000.218040.000.060046.400.238044.120.106746.420.288545.600.102643.600.36642.2NH3-N110NH3-N>>>>>>>>>、、、、、、NH3-N0.3mgg.20.、、ρNH3-N.ρNH3-N15mgL、、9811293NH3-N.1Fig.1Isothermaladsorptioncurvesoftenkindsofnon-naturalsubstrates18-201mm、、、NH3-NNH3-NρNH3-N.219ρNH3-NρNH3-N60mgL、、、、、、ρNH3-N、、、、、、、、、NH3-N.ρNH3-N0~30mgL、、、ρNH3-N30~60mgLρNH3-N60mgL.、、、ρNH3-N30mgL8.、、、、ρNH3-NNH3-N.、、NH3-N、9.Langmuir31.Freundlich2Fig.2Isothermaladsorptioncurvesofnineteenkindsofsubstrates32-34.LangmuirFreundlich3.3NH3-NQmax462035、、、、、、、.36.、、、、、、、、、、、、、LangmuirFreundlichLangmuir.FreundlichkNH3-NkNH3-N37.FreundlichR2>0.9、、、kNH3-N1n1n138.NH3-NNH3-N.2.3NH3-NNH3-N4、5.NH3-NNH3-N09118293NH3-NTable3NH3-Nadsorptionmodelandrelatedparametersoftwenty-ninekindsofsubstratesmmLangmuirFreundlichQmaxmggKR2knR22~40.68300.02260.89200.03501.7100.86333~50.03670.07280.89270.00682.7900.63862~40.45830.00430.94590.00251.1400.92562~40.23790.00580.95140.00181.1600.85631~20.15320.00770.81310.00161.2000.75391~20.13150.03920.97180.01302.1000.92461~21.35000.01450.93100.03691.4550.88102~40.09800.04150.85100.00942.0600.65901~20.27880.01780.89000.01121.6150.85602~40.08060.03310.89520.00601.8870.74881~20.12230.00920.89800.00171.2640.84802~40.19100.00600.96810.00171
本文标题:29种湿地填料对氨氮的吸附解吸性能比较
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