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沸石覆盖原位控制湖泊内源中等活性有机磷迁移转化

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  • 2020-03-10 11:23:18

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中国环境科学2015,35(2):550-557ChinaEnvironmentalScience沸石覆盖原位控制湖泊内源中等活性有机磷迁移转化孙士权,蒋昌波,赵刚,聂小保,谭万春,万俊力,余关龙(长沙理工大学,水沙科学与水灾害防治湖南省重点实验室,湖南长沙410114)摘要:为揭示湖泊内源中等活性有机磷(MLOP)控制与释放发生机制,采用室内模拟试验,研究沸石覆盖原位控制湖泊内源MLOP迁移转化影响因子.结果表明:酸性水体促进内源MLOP迁移,碱性条件下抑制其转化,不同pH值试验水体沉积物中内源MLOP相对浓度~J:[MLOP/TP]p.s>[MLOPFFP]Ptt7>[MLOP/TP]pH6;*~//t度明显提高内源MLOP迁移水平,低温水体相对高温水体沉积物中内源MLOP含量较低,5C条件下内源MLOP迁移表观量最大,其随时间迁移量里幂函数关系,可表示为【MLOP厂rP】=0.282370(为O.9709);好氧或厌氧条件_F,内源MLOP均发生迁移,且迁移特征和影响效能高度一致,迁移平衡后好氧环境内源MLOP和厌氧内源MLOP相对浓度呈线性相关,可表示为[MLOP/TP]~l=l0884[MLOP/TP]~:M一O0271(R为99895);光照因子促使内源MLOP迁移.而避光和沸石粒径因素对内源MLOP迁移影响较小;底栖生物颤蚓通过爬行、摄食、掘穴、栖所建造及分泌排泄等一系列活动影响内源MLOP迁移.沸石原位控制湖泊内源MLOP迁移转化效能较弱.关键词:沸石原位控制:沉积物;中等活性有机磷:迁移转化中图分类号:X703文献标识码:A文章编号:1000—6923(2015)02—0550—08Influencingfactorsofzeolitein—situremediationsystemtocontrolmoderatelylabileorganicphosphorusmigrationandtransformationinshallowwater.SUNShi—quan,JIANGChang—bo。,ZHAOGang,NIEXiao—bao,TANWlan-chun,WANJun—li,YUGuan—long(TheWaterWandScienceandtheWaterDisasterPreventandControlKeyLaboratoryofHunanProvince,ChangshaUniversityofScienceandTechnology,Changsha410114,China).ChinaEnvironmentalScience,2015,35(2):550-557Abstract:Tounravelthemechanismofthecontrolandreleaseoftheendogenousmoderatelylabileorganicphosphorus(MLOP)inthelake,thefactor,whichinfluencedthemigrationandtransformationofendogenousMLOPusingin—situzeolitecappingcontrol,wasstudied.Theresultsofthelaboratorysimulationofin—situzeolitecontrolingendogenouspollutionsinlakesindicatethatacidicwaterbodiespromotedendogenousMLOPmigrationwhilealkalineconditionshinderedit.andtherelativeconcentrationsofendogenousMLOPinsediments,underdiferentpHconditions,were【MLOP/TP]pH8>【MLOP/TP]pH7>[MLOP/TP]pn6;temperaturesignificantlyincreasedthemigrationlevelofendogenousML0D:thecontentofendogenousMLOPinsedimentsinlow.temperaturewaterbodieswaslowerthanthatinhigh—temperatureones.Onconditionof5℃,theendogenousMLOPshowedthehighestapparentmigration,anditalsopresentedapowerfunctionrelationshipwiththemigrationovertime.whichcouldbedescribedas[MLOP/TP]=0.

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