Recovery of sulfate saturated soils in the Plynlimon catchments, mid-Wales following reductions in atmospheric S inputs from the 1980s to 2011
Hughes, Steven; Reynolds, Brian; Norris, David A.; Brittain, Sarah A.; Dere, Ashlee L.; Woods, Clive; Armstrong, Linda K.; Harman, Sarah A.; Wickham, Heather D.. 2012 Recovery of sulfate saturated soils in the Plynlimon catchments, mid-Wales following reductions in atmospheric S inputs from the 1980s to 2011. Journal of Environmental Monitoring, 14. 1531-1541. 10.1039/C2EM30070BFull text not available from this repository.
Sulfate adsorption capacity of B-horizons of base-poor, predominantly stagnopodzol, soils from the Plynlimon catchments, mid-Wales was determined by combination of laboratory adsorption and desorption isotherms. Results show that sulfate adsorption capacity of a range of stagnopodzol (Histic-stagno-podzol (Leptic), WRB), brown podzolic soil (Histic-umbrisol (Leptic), WRB) and stagnohumic gley (Histic-stagno-gleysol, WRB) B-horizons was positively related to the amounts of extractable (pyrophosphate and oxalate) Fe + Al, with the stagnopodzol and brown podzolic soil Bs horizon having the largest adsorption capacity and stagnohumic gley Bg horizon the smallest adsorption capacity. Results show that dissolved organic carbon (DOC) has a negative but limited effect on sulfate adsorption in these soils. Results obtained from a set of historical soil samples revealed that the grassland brown podzolic soil Bs horizon and afforested stagnopodzol Bs horizon were highly saturated with sulfate in the 1980s, at 63% and 89% respectively, whereas data from some recently sampled soil from two sites revisited in 2010–11 indicates that percentage sulfate adsorption saturation has since fallen substantially, to 41% and 50% respectively. Between 1984 and 2009 the annual rainfall-weighted mean excess SO4-S concentration in bulk precipitation declined linearly from 0.37 mg S l−1 to 0.17 mg S l−1. Over the same period, flow weighted annual mean stream water SO4-S concentrations decreased approximately linearly from 1.47 mg S l−1 to 0.97 mg S l−1 in the plantation afforested Hafren catchment compared to a drop from 1.25 to 0.69 mg S l−1 in the adjacent moorland catchment of the Afon Gwy. In flux terms, the mean decrease in annual stream water SO4-S flux has been approximately 0.4 kg S ha−1 yr−1, whilst the recovery in stream water quality in the Afon Cyff grassland catchment has been partly offset by loss of SO4-S by desorption from the soil sulfur pool of approximately 0.2 kg S ha−1 yr−1.
|Item Type:||Publication - Article|
|Digital Object Identifier (DOI):||10.1039/C2EM30070B|
|Programmes:||CEH Topics & Objectives 2009 onwards > Biogeochemistry
CEH Topics & Objectives 2009 onwards > Biogeochemistry > BGC Topic 1 - Monitoring and Interpretation of Biogeochemical and Climate Changes > BGC - 1.1 - Monitor concentrations, fluxes, physico-chemical forms of current and emerging pollutants ...
|NORA Subject Terms:||Agriculture and Soil Science
Ecology and Environment
|Date made live:||22 Mar 2012 12:08|
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