{"refrec":{"BRefID":134126,"RR":"<b>Morris, A.W.</b> (1986). Removal of trace metals in the very low salinity region of the Tamar Estuary, England. <i>Sci. Total Environ. 49</i>: 297-304. <a href=\"https://dx.doi.org/10.1016/0048-9697(86)90245-7\" target=\"_blank\">https://dx.doi.org/10.1016/0048-9697(86)90245-7</a>","BEntID":128055,"PublicFlag":1,"CheckedFlag":0,"wosflag":1,"vabbflag":1,"RefStringPartII":". <i>Sci. Total Environ. 49</i>: 297-304. <a href=\"https://dx.doi.org/10.1016/0048-9697(86)90245-7\" target=\"_blank\">https://dx.doi.org/10.1016/0048-9697(86)90245-7</a>","DocTypID":8,"DocType":"Journal article","MarineFlag":1,"FreshFlag":0,"BrackishFlag":0,"TerrestrialFlag":0,"Authorstring":"Morris, A.W.","OrigTitleTranslFlag":0,"Authorstringtrunc":"Morris, A.W.","Englishabstract":"Field observations have shown that the removal of a substantial proportion of the riverine influx of dissolved trace metals is a consistent feature of the very low salinity, high turbidity zone of the Tamar Estuary. Comparison of field data with the predictions of a simple sorptive equilibrium model indicates that the removal occurs through rapid uptake onto suspended particles comprising the estuarine turbidity maximum. 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