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Major Ion and Trace Metal Geochemistry of an Acidic Septic‐System Plume in Silt
Author(s) -
Robertson W. D.,
Blowes D. W.
Publication year - 1995
Publication title -
groundwater
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 0.84
H-Index - 94
eISSN - 1745-6584
pISSN - 0017-467X
DOI - 10.1111/j.1745-6584.1995.tb00282.x
Subject(s) - trace metal , trace (psycholinguistics) , geology , plume , silt , geochemistry , metal , environmental chemistry , earth science , chemistry , metallurgy , materials science , geomorphology , geography , linguistics , philosophy , meteorology
Four years of detailed ground‐water monitoring at a newly installed, seasonal‐use, domestic septic system located on poorly buffered (CaCO 3 equivalent content ≤ 1.6 wt.%) lacustrine silt, has revealed the development of an acidic ground‐water plume. Acid, generated by the partial oxidation of effluent NH 4 + dissolved organic carbon (DOC), and possibly sulfide minerals present in the sediment, has resulted in a distal plume core zone with pH values in the range of 4.4 to 5.0. The acidic zone, where NH 4 + does, however, persist (> 2 mg/1, as N) and where DOC remains elevated (6–13 mg/1), is associated with high average concentrations of the trace metals Fe (4.7 mg/1), Al (1.9 mg/1), and Mn (3.6 mg/1). Attenuation of nitrogen along the plume core flowpath is indicated by a decrease in the N/ Cl − ratio from an effluent value of 1.7, to a plume value of only 0.5 after 4 m of subsurface flow. Increased SO 4 2− levels observed in the zone of N depletion suggest that attenuation can be at least partly attributed to reduction of plume NO 3 − by oxidation of reduced S present in the sediment. PO 4 3− has not migrated significantly beyond the infiltration bed gravel layer, demonstrating that PO 4 3− mobility is limited in these sediments (retardation factor > 10).