Arsenic (As) mobility and transport in the environment are strongly influen
ced by arsenic's associations with solid phases in soil and sediment. We ha
ve tested a sequential extraction procedure intended to differentiate the f
ollowing pools of solid phase arsenic: loosely and strongly adsorbed As; As
coprecipitated with metal oxides or amorphous monosulfides; As coprecipita
ted with crystalline iron (oxyhydr)oxides; As oxides; As coprecipitated wit
h pyrite; and As sulfides. Additions of As-bearing phases to wetland and ri
verbed sediment subsamples were quantitatively recovered by the following e
xtractants of the sequential extraction procedure: As adsorbed on goethite,
1 M NaH2PO4; arsenic trioxide (As2O3), 10 M HF; arsenopyrite (FeAsS), 16 N
HNO3; amorphous As sulfide, 1 N HCl, 50 mM Ti-citrate-EDTA, and 16 N HNO3;
and orpiment (As2S3), hot concentrated HNO3/H2O2 Wet sediment subsamples f
rom both highly contaminated wetland peat and less As-rich sandy riverbed s
ediment were used to test the extraction procedure for intra-method reprodu
cibility. The proportional distribution of As among extractant pools was co
nsistent for subsamples of the wetland and for subsamples of the riverbed s
ediments. In addition, intermethod variability between the sequential extra
ction procedure and a single-step hot concentrated HNO3/H2O2 acid digestion
was investigated. The sum of the As recovered in the different extractant
pools was not significantly different than results for the acid digestion.