Mc. Stordal et al., MERCURY PHASE SPECIATION IN THE SURFACE WATERS OF 3 TEXAS ESTUARIES -IMPORTANCE OF COLLOIDAL FORMS, Limnology and oceanography, 41(1), 1996, pp. 52-61
Surface-water samples were collected from Galveston Bay, Corpus Christ
i Bay, Sabine Lake, and Laguna Madre and analyzed for Hg in the <0.45-
mu m, 0.45-mu m-1-kDa, and <1-kDa fractions. Colloidal material was is
olated with an Amicon cross-flow ultrafiltration system which was rigo
rously tested. Filter-passing Hg concentrations (< 0.45 mu m) ranged f
rom 0.12 to 13.6 pM, with the highest values in Corpus Christi Bay. Wi
thin Galveston and Corpus Christi Bays, filter-passing Hg exhibited no
nconservative estuarine mixing behavior. The colloidal Hg fraction ran
ged from 12 to 93% of the filter-passing pool and averaged 57 +/- 20%,
indicating that a major portion of the operationally defined ''dissol
ved'' Hg is associated with submicron particles and macromolecules >1
kDa. Colloidal Hg covaries with colloidal organic C concentrations in
Galveston Bay waters, suggesting that most of the filter-passing Hg po
ol is associated with large organic macromolecules. The log of the par
ticle-water partition coefficient (K-d) ranged from 4.6 to 5.2, and co
varied with suspended particulate matter concentrations, likely due to
the presence of colloidal Hg.