Lead sequestration and species redistribution during soil organic matter decomposition.
The turnover of soil organic matter (SOM) maintains a dynamic chemical environment in the forest floor that can impact metal speciation on relatively short timescales. Here we measure the speciation of Pb in controlled and natural organic (O) soil horizons to quantify changes in metal partitioning during SOM decomposition in different forest litters. We provide a link between the sequestration of pollutant Pb in O-horizons, estimated by forest floor Pb inventories, and speciation using synchrotron-based X-rayfluorescence and X-ray absorption spectroscopy. When Pb was introduced to fresh forest O(i) samples, it adsorbed primarily to SOM surfaces, but as decomposition progressed over two years in controlled experiments, up to 60% of the Pb was redistributed to pedogenic birnessite and ferrihydrite surfaces. In addition, a significant fraction of pollutant Pb in natural soil profiles was associated with similar mineral phases (approximately 20-35%) and SOM (-65-80%). Conifer forests have at least 2-fold higher Pb burdens in the forest floor relative to deciduous forests due to more efficient atmospheric scavenging and slower organic matter turnover. We demonstrate that pedogenic minerals play an important role in surface soil Pb sequestration, particularly in deciduous forests, and should be considered in any assessment of pollutant Pb mobility.
Department of Earth Sciences, Dartmouth College, Hanover, New Hampshire 03755, USA. aschroth@usgs.gov
Andrew W
AW
Schroth
Benjamin C
BC
Bostick
James M
JM
Kaste
Andrew J
AJ
Friedland
D007854:Lead / Q000737:chemistry / Q000302:isolation & purification*; D009930:Organic Chemicals / Q000737:chemistry*; D012987:Soil / Q000032:analysis*; D013057:Spectrum Analysis / Q000379:methods; D014965:X-Rays
D009930:Organic Chemicals; D012987:Soil; D007854:Lead