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http://www.scirp.org/journal/PaperInformation.aspx?PaperID=53892#.VNsBzSzQrzE
Author(s)
Richard L. Haney1*, Virginia L. Jin2, Mari-Vaughn V. Johnson3, Elizabeth B. Haney4, R. Daren Harmel1, Jeffrey G. Arnold1, Michael J. White1
Affiliation(s)
1United
States Department of Agriculture-Agriculture Research Service,
Grassland, Soil and Water Research Laboratory, Temple, TX, USA.
2United States Department of Agriculture-Agriculture Research Service, Agroecosystem Management Research Laboratory, University of Nebraska, East Campus, Lincoln, NE, USA.
3United States Department of Agriculture-Natural Resource Conservation Service, Temple, TX, USA.
4Texas A&M University, Texas AgriLife Research & Extension Center, Temple, TX, USA.
2United States Department of Agriculture-Agriculture Research Service, Agroecosystem Management Research Laboratory, University of Nebraska, East Campus, Lincoln, NE, USA.
3United States Department of Agriculture-Natural Resource Conservation Service, Temple, TX, USA.
4Texas A&M University, Texas AgriLife Research & Extension Center, Temple, TX, USA.
ABSTRACT
<span
"="">Phosphorus loading and measurement is of concern on lands where
biosolids have been applied. Traditional soil testing for
plant-available P may be inadequate for the accurate assessment of P
loadings in a regulatory environment as the reported levels may not correlate
well with environmental risk. In order to accurately assess potential P
runoff and leaching, as well as plant uptake, we must be able to
measure organic P mineralized by the biotic community in the soil. Soils
with varying rates of biosolid application were evaluated for
mineralized organic P during a 112-day incubation using the difference
between P measured using a rapid-flow analyzer (RFA) and an axial flow
Varian ICP-OES. An increase in the P mineralized from the treated soils
was observed from analysis with the Varian ICP-OES, but not with the
RFA. These results confirm that even though organic P concentrations
have increased due to increasing biosolid application, traditional soil
testing using an RFA for detection, would not accurately portray P
concentration and potential P loading from treated soils.
KEYWORDS
Phosphorus, Anthropogenic Additions, Biosolids, Rapid-Flow Analyzer (RFA), Inductively Coupled Plasma (ICP), Texas Commission of Environmental Quality (TCEQ), Soil Organic C (SOC), Total N (TN), Water-Soluble Organic C (WSOC), Water Soluble Organic N (WSON)
Cite this paper
References
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White, M. (2015) Analysis Methods for the Determination of Anthropogenic
Additions of P to Agricultural Soils. Open Journal of Soil Science, 5, 59-68. doi: 10.4236/ojss.2015.52007.
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