Determination of trace element stability in sediments using redox gel probes: Probe construction and theoretical performance

A simple and inexpensive technique is described that can be used to assess the stability of redox-sensitive compounds in the sediments of wetlands and other shallow water environments. In this method, solid redox-sensitive compounds, such as manganese dioxide (MnO2), are incorporated into agar gels held in rigid plastic holders. One surface of the gel remains exposed along the length of the resulting probe. The probes are pushed vertically into sediments and are left in situ for a period of time (days to weeks), after which they are visually inspected and chemically analyzed. The diffusion of nonreactive solutes (e.g., sulfate) in 2% (wt/vol) agar was unaffected by the presence of immobilized MnO2 particles. The rate of dissolution of particulate MnO2 in agar gels in the presence of an external diffusing reductant (L-ascorbic acid) could be quantified by digital analysis of pixel density on gel images. Redox gel probes incubated in the sediment of a wetland built to remove manganese from circumneutral pH coal mine drainage demonstrated different patterns of depth-dependent MnO2 stability along a 15-m transect. MnO2 gel probe results were consistent with data obtained using sediment cores and porewater diffusion samplers.