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当前位置:首页 > 商业/管理/HR > 信息化管理 > 潮汐流人工湿地低温下NH4N去除模型的比较和优化叶捷
31720117ActaScientiaeCircumstantiaeVol.31No.7Jul.2011No.2008ZX07208-003No.50708101/E080402SupportedbytheNationalKeyScientificandTechnologicalProjectforWaterPollutionControlandManagementNo.2008ZX07208-003andtheNationalNaturalScienceFoundationofChinaNo.50708101/E0804021985—E-maileyejie@126.com*E-mailsongyh@craes.org.cnBiographyYEJie1985—maleE-maileyejie@126.com*CorrespondingauthorE-mailsongyh@craes.org.cn.2011.NH+4-NJ.3171456-1463YeJPengJFGaoHJetal.2011.ComparisonandoptimizationofaNH+4-Nremovalmodelofatidal-flowconstructedwetlandinlowtemperatureseasonsJ.ActaScientiaeCircumstantiae3171456-1463NH+4-N12222*21311.4100822.1000123.1000832010-09-072010-10-212010-11-083NH+4-N、MonodNH+4-N.9~13℃3NH+4-NMonodNH+4-NR2=0.9035.MonodMonodNH+4-NNH+4-NTDO.NH+4-N0253-2468201107-1456-08X703AComparisonandoptimizationofaNH+4-Nremovalmodelofatidal-flowconstructedwetlandinlowtemperatureseasonsYEJie12PENGJianfeng2GAOHongjie2SONGYonghui2*QIUGuanglei2ZHANGPanyue13ZENGGuangming11.CollegeofEnvironmentalScienceandEngineeringHunanUniversityKeyLaboratoryofEnvironmentalBiologyandPollutionControlHunanUniversityMinistryofEducationChangsha4100822.DepartmentofUrbanWaterEnvironmentalResearchChineseResearchAcademyofEnvironmentalSciencesBeijing1000123.CollegeofEnvironmentalScienceandEngineeringBeijingForestryUniversityBeijing100083Received7September2010receivedinrevisedform21October2010accepted8November2010AbstractTosolvetheproblemofthelowefficiencyofnitrogenremovalunderlowtemperaturesinconstructedwetlandswestudiedthetreatmentperformanceofatidal-flowconstructedwetlandwiththreerunningcyclesperdayunderlowtemperatureconditions.WesimulatedtheNH+4-NremovalusingtheapparentkineticmodelmultipleregressionmodelandMonod-mechanismmodel.Theexperimentalresultsshowedthatthetidal-flowconstructedwetlandwiththreerunningcyclesperdayhadahighefficiencyforNH+4-Nremovalat9~13℃anditfittheMonod-mechanismmodelreasonablywellwithacoefficientofdeterminationR2of0.9035.BasedonthisconclusionthelocalsensitivityoftheMonod-mechanismmodelwasanalyzedbymodifiedMorrisscreeningwhichshowedthatintheMonod-mechanismmodelCinwasahighlysensitiveparametertheaveragewatertemperatureTwasasensitiveparameterandDOwasamediumsensitiveparameter.Keywordstidal-flowconstructedwetlandNH+4-NlowtemperaturedynamicmodelMorrisscreeningmethodlocalsensitivityanalysisDOI:10.13671/j.hjkxxb.2011.07.0207NH+4-N1Introduction--Chanetal.2008.、、、Laietal.2009Chungetal.2008Teeetal.2009、1995Grossetal.2007.-.---4.、..2009.NH+4-NNH+4-NNH+4-N3NH+4-N、MonodNH+4-NNH+4-NNH+4-N.2Materialsandmethods2.1130cm、80cm0.042m3.65cm25~50mm15cm8~12mm20cm3~5mm30cm.PLC.1Fig.1Schematicoftheexperimentalequipment2.2CODCr110.00~175.40mg·L-1NH+4-N29.04~44.75mg·L-1PO3-4-P3.36~5.46mg·L-1pH6.0~7.0.2.3COD、NH+4-N、SEPA2002.T、DOYSIDOYSI.2.40.2m3·m-2·d-1.、8.0h4.0h.2009101200911~20104.200911~201029℃20103~2010413℃.2.52.5.12.7541311Table1ParameterswithrespecttoNH+4-NremovalmodelsT℃8~17DOmg·L-10.43~0.72k1h-10.129k0h-13.406CoutNH+4-Nmg·L-116.43~33.45CinNH+4-Nmg·L-129.04~44.75CTh4VL42μmaxmg·L-10.00164Ksmg·L-16.199xmg·L-1771.5θ1.04Kadlec1995Y0.2MetcalfandEddyInc.2003komg·L-10.2MetcalfandEddyInc.2003mgmg.2.5.2Kadlecetal.20002006..Chanetal.20082009Vdcdt=Qin-Qout+Vr1cmg·L-1rNH+4-Nh-1、、.NH+4-NChanetal.2008VdNH+4-Ndt=Vr+Qin-Qout2Qin、Qoutmg·h-1.NH+4-NQin=Qout=0.2VdNH+4-Ndt=Vr3NH+4-Nrr=-kncn4n.n=04r=-k0553k0=-Cout-CinCT6Cout=Cin-k0CT7n=14r=-k1c883k1=lnCin-lnCoutCT9Cout=Cine-k1CT102.5.3y=fx1x2x3x4……11NH+4-NCin、COD、DO、TNH+4-NCoutNH+4-NCout85417NH+4-NChanetal.2008Cout=fCin、COD、DO、T122.5.4MonodNH+4-N、、.VdNH+4-Ndt=V∑mj=1rj+Qin-Qout13rj、、、.NH+4-NQin=Qout=0.VdNH+4-Ndt=V∑mj=1rj14NH+4-NpH6.0~7.0NH+4-NNH+4-N14VdNH+4-Ndt=Vrd15rdNH+4-Nh-1.Cin、DO、TMonodrdChanetal.2008rd=-1YumaxCinKS+CinxDOkO+DOθT-201615、16NH+4-NCout=Cin-CT1YumaxCinKS+CinxDOkO+DOθT-20172.6“”.MorrisFrancos2003Zadoretal.2006.2004S=∑n-1i=0Yi+1-Yi/Y0Pi+1-Pi/n18SYiiYi+1i+1Y0PiiPi+1i+1n.3Results3.1NH+4-N22010Sunetal.1998.NH+4-NNH+4-N.“”、Behrendsetal.2001NH+4-N.200911NH+4-N37.68mg·L-13NH+4-N11.71%NH+4-N20103NH+4-N35.74mg·L-1NH+4-N41.23%.NH+4-N135.25%.3.23.2.1.69NH+4-N1920.954131Cout=Cine-0.4781619Cout=Cin-13.6072202NH+4-N.NH+4-N.3R2=0.7371δ=2.074R2=0.8036δ=1.780..3NH+4-NNH+4-NNH+4-NNH+4-NNH+4-NNH+4-N.2、Fig.2ComparisonofthesimulatedNH+4-NwithobservedNH+4-N3Fig.3Fitsofpredictionsfromtheapparentdynamicmodel3.2.2.SPSSNH+4-NNH+4-NCin、COD、DO、TY=-3.591-0.278X1+0.896X2-10.496X3+0.014X421YNH+4-NCoutmg·L-1X1T℃X2NH+4-NCinmg·L-1X3DOmg·L-1X4CODmg·L-1.4NH+4-N.NH+4-N.5R2=0.8863δ=1.369NH+4-N.4Fig.4ComparisonofthesimulatedNH+4-NwithobservedNH+4-NNH+4-NCoutCin、COD0.8960.014NH+4-NCout、Austin2006.CoutDO、TDO-10.496DODO2006T-0.2782008.06417NH+4-N5Fig.5Fitsofpredictionsfromthemultivariateregressionmodel3.2.3MonodμmaxKsMonodμmaxKsθ、Y、k0Hallingetal.1996Kadlec1995MetcalfandEddyInc.2003NH+4-NMonodCout=Cin-26.22×Cin6.199+CinDO0.2+DOθT-20226MonodFig.6ComparisonofthesimulatedNH+4-NwithobservedNH+4-N6MonodNH+4-N..7R2=0.9035δ=1.232.7y=xθ、Y、k0Coutθ、k0Yθk0TDOTDOHallingetal.1996Kadlec1995MetcalfandEddyInc.2003.NH+4-N22CoutCinTDONH+4-N.7MonodFig.7Fitsofpredictions
本文标题:潮汐流人工湿地低温下NH4N去除模型的比较和优化叶捷
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