Sr. Hoffmann et al., A critical evaluation of tangential flow ultrafiltration for trace metal studies in freshwater systems. 1. Organic carbon, ENV SCI TEC, 34(16), 2000, pp. 3420-3427
Citations number
30
Categorie Soggetti
Environment/Ecology,"Environmental Engineering & Energy
The utility of tangential flow ultrafiltration (TFUF) for size fractionatio
n of natural organic matter(NOM) in freshwater streams was investigated, fo
cusing on characterization or elimination of potential artifacts. Spiral-wo
und polyethersulfone (PES) and regenerated cellulose (RCL) membranes with n
ominal molecular weight limits of 10 kilodalton (kDa) and 100 kDa were comp
ared as part of a large project assessing the utility of large volume (>5 L
) ultrafiltration for determining trace metal speciation in freshwaters. Wi
th careful cleaning, reliable fractionations of carbon and trace metals in
freshwater can be obtained, and a detailed protocol necessary to avoid pote
ntially significant biases is presented. Both PES and RCL membranes can be
cleaned efficiently to provide low carbon blanks (<0.03 mg C L-1) and recle
aned at least 10 times without compromising membrane integrity. For RCL, re
sidual acid from the cleaning procedure can lower the permeate pH to below
4 in low-alkalinity river samples, but this acid can be removed prior to sa
mple filtration with a simple treatment. Mass balance experiments with stre
am NOM show good recovery (99.7% +/- 9.5%, n = 67). Sorption losses are ver
y low ton average, <2%) to RCL membranes hut are higher for PES. Replicate
precision is typically better than +/-5% for carbon. There are significant
differences between PES and RCL membranes: permeate carbon levels are simil
ar, but RCL predicts a larger >10 kDa fraction and carbon sorption is more
significant on PES. These findings could be explained by greater hydrophobi
c interactions of dissolved organic carbon with PES and charge interactions
with RCL. A strong negative correlation is observed between the percent of
colloidal carbon (10 kDa - 0.4 mu m) and the log specific conductance of s
treamwaters (R-2 = 0.71).