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ID:39138944
大小:2.01 MB
页数:70页
时间:2019-06-25
《营养盐在胶州湾沉积物——海水界面上的交换速率和通量分析》由会员上传分享,免费在线阅读,更多相关内容在学术论文-天天文库。
1、.重璺望堂查兰堡主堡皇h—●-——__——_——-___—_-———_,——__——-’_—___——___——、●__—_-__—_●_’—_-_—~—_-———-^——————————⋯AbstractAfunctionmethodofcalculatingthenutrientsexchangeratesatthesediment—waterinterfacewithdependenceofexchangeamountontimewasdevelopedbyconsideringtheinfluenceofincub
2、ationtimeandsamplingintervalsIntactsedimentcoresweresampledat16locationsinJiaozhouBayinJuly200IWiththelaboratoryincubationexperiments,benthicexchangeratesofSi03一Si,P04一P’NH4一N,N02一NandN01.Natthesediment—waterinterfaceweremeasuredAtthesametime,therelationshipsweres
3、tudiedbetweenthenutrientsexchangeratesandsedimentwatercontents,thenutrientsconcentrationsinporewategclaycontentsandgrainsizesTheexchangefluxesofdifferentnutrientsatthesediment—waterinterfacewereestimatedbyconsideringtheweightedpercentageofdifferentpatternsofsedime
4、nt.Themainexperimentalresultsareasfollows:1TheexchangeratesofSiOs—Si,P04-P,NH4-N,NOz-NandNOs-Natthesediment—waterinterfaceofJiaozhouBayTheSi03一SieffluxeswereobservedatallstationsandtheexchangeratesweregenerallyrangedfromO8to5lmmol‘m-2.d~.WhiletheeffluxesP04一P’NH4一
5、N,N02一NandN03一Nwereobservedatmostofstationsandtheirexchangeratesrangedfrom438tO395utool·m-2.d—forP04一P'from一0.5to16mmol-m-2.d~forNI-h-N,from一0052toO67mmol·m-2,d~forN02.Nandfrom一2to28mmol·m-2.d~forN03.Nrespectively2Therelationshipsbetweenthenutrientsexchangeratesat
6、thesediment—waterinterfaceinJiaozhouBayandsedimentwatercontents,thenutrientsconcentrationsinporewater,claycontentsandgrainsizeofsediments(1)ItwasshownthattheexchangeFatesofSi03一Siarepositivelyrelatedtothewaterandclaycontentsofthesediments.andtheSi03-Siconcentratio
7、nsinporewater.Furthermore,theexchangerateismainlydependentonthemeandiametersofthesedimentsastheWaterandclaycontentsofthesedimentswerealsodependentontheirdiametersTheexchangeprocessofSiOj—Siatthesediment—waterinterfacewasmainlydominatedbydissolutionofclayanddiffusi
8、onofSiOs·Sifromtheporewatertoseawater.However,thehighercontentoforganicmatterandbioturbationinthesedimentscanpromotetheexchangerategreatlg(2)Theexchange
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