The role of colloidal material in the fate and cycling of trace metals in estuarine and coastal waters

摘要

Trace metals in natural colloidal material (l-400nm) were investigated in the River Beaulieu, the Trent-Humber system and the Celtic Sea. Colloidal and truly dissolved (10,000molecular weight) fractionswere separated by cross-flow filtration (CFF). Filtration artefacts (conventional and CFF) involving filterblockage and colloid aggregation/disaggregation transformations were minimised through appropriateprotocols.65Zn equilibration experiments were carried out with Beaulieu River colloids (0A^m). The initialuptake of 65Zn onto colloidal material (10 to 15 %) was very rapid (seconds to minutes) but a largefraction of the tracer remained in the truly dissolved phase. Preliminary modelling to estimate the fractionof colloidal zinc under variable SPM concentrations and Kc sensitivities was completed using differentpartition coefficients (Kc and Kf) derived during the equilibration experiments. Initial 65Zn-colloidpartitioning was related to the mass concentrations (and theoretical surface area) of colloids and colloidalaggregates. The 65Zn radiotracer/colloid association was exchangeable but overall equilibriumpartitioning of colloidal/truly dissolved 65Zn did not change with increased total zinc concentration. Loosehydrophobic colloidal aggregates (filaments) with Mn hydroxide coatings formed during sample storageand were capable of removing ~60% of the 65Zn. Field flow fractionation (FFF) of colloidal BeaulieuRiver water highlighted the significance of the smaller colloidal fractions (0.08^m and 0.08 to 0.134m)which contained the highest concentration of Fe, Mn and Zn when normalised to an assumed geometricsurface area.A spatial and seasonal investigation of colloidal trace metals in the Trent/Humber system identifiedgroups of metals with varying colloidal associations in the order (high to low); Fe Pb, Mn Cu, Zn, Ni Cd. Colloidal Fe, Pb and Mn all illustrated removal in the low salinity region of the estuary. Ni (mainlytruly dissolved) showed somewhat conservative behaviour. Total dissolved Cd (and Zn) consistentlyshowed a mid-estuarine maximum (truly dissolved), which was attributed to chloro-complex formation orionic exchange with major seawater ions. For most metals, the positioning and intensity of the turbiditymaximum zone (TMZ) appeared to have greatest control on their removal. Cu is controlled seasonally byinput of organic ligands (truly dissolved/microcolloidal). The existence of separate organic and inorganiccolloidal pools was proposed, which may have seasonally variable signatures. The presence of lowermolecular weight (10,000Da) colloids is significant for Pb and Cu.Investigations of colloidal Al in the Celtic Sea highlighted problems with colloid disruption within thecross-flow system, and detection of Al colloids using a surface active fluorometric technique. Watercolumn profiles of reactive and dissolved (0.4/u.m) Al gave insights into processes controlling Aldistribution and concentration. Resuspension of Celtic Sea sediment led to an instantaneous release oftruly dissolved Al derived from authigenic mineral dissolution. FFF analysis of samples from theresuspension experiments showed that colloidal Al was not a significant fraction (20% of total dissolvedAl). On the basis of these experiments it was possible to estimate that, in the absence of scavenging, theinput of truly dissolved Al from typical resuspension events could be sufficient to account for the 5-8nMincrease in dissolved Al concentrations observed close to the bed.This research has contributed towards a new approach to interpretation of trace metal speciation andprocesses in a variety of natural waters. Assessment of the role of colloidal and truly dissolved phaseswithin the 'dissolved' fraction has enabled better understanding of particle/water/metal interactions. Thedescription of trace metal/colloid partitioning and associations within these multicomponent systems hasthe potential to enhance their modelling in the future.