Phosphorus transformation response to soil properties changes induced by manure application in a calcareous soil

Yan, Zhengjuan; Chen, Shuo; Dari, Biswanath; Sihi, Debjani; Chen, Qing

doi:10.1016/j.geoderma.2018.02.035

Title: Phosphorus transformation response to soil properties changes induced by manure application in a calcareous soil

Journal Article · 28 February 2018 · Geoderma

DOI: https://doi.org/10.1016/j.geoderma.2018.02.035 · OSTI ID:1463987

Yan, Zhengjuan ^[1]; Chen, Shuo ^[1];

^[2];

^[3]; Chen, Qing ^[1]

China Agricultural Univ., Beijing (China). College of Resources and Environmental Sciences
Univ. of Idaho, Aberdeen, ID (United States). Aberdeen Research and Extension Center
Univ. of Maryland Center for Environmental Science, Frostburg, MD (United States). Appalachian Lab.; Oak Ridge National Lab. (ORNL), Oak Ridge, TN (United States). Climate Change Science Inst. Environmental Sciences Division

Management of phosphorus (P) loss in soils with heavy manure application requires improved understanding of the transformation characteristics of soil P. Influences of manure application on the forms and sorption-desorption characteristics of P in surface (0–30 cm) and subsurface (30–60 cm) layer of a calcareous soil were investigated in this paper in a six-year field trial in comparison to chemical fertilizer application. Hedley fractionation and P K-edge X-ray absorption near-edge structure spectroscopy were used to determine the soil P forms. Manure (M) and chemical fertilizer (F) treatments resulted in P accumulation in two soil depths, but the total P accumulation in surface soil with M treatment was significantly lower than F treatment with similar P surplus. Compared to control, M and F treatments were significantly increased the proportion of labile P at both depths. In surface soil, M treatment significantly decreased stable Ca-associated P proportion and increased Fe-associated P and inositol hexakisphosphate proportions. The accumulation and transformation of P in M treatment distinctly decreased P sorption maximun, sorption coefficient and buffer capacity, and increased the degree of P saturation and P desorption relative to F treatment. The soil properties of pH, organic carbon (OC), total nitrogen (TN), Mehlich-3 extractable Ca and Fe, and phytase in surface soil and pH, OC, TN, Mehlich-3 extractable Ca and dehydrogenase in subsurface soil had significant effects on the compositions of soil P (P < 0.05), respectively. Finally, lowered pH due to manure application mainly contributed to P transformation and release in the calcareous soil.

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Research Organization:: Oak Ridge National Laboratory (ORNL), Oak Ridge, TN (United States)

Sponsoring Organization:: USDOE; National Natural Science Foundation of China (NSFC); National Key Research and Development Program of China

Grant/Contract Number:: AC05-00OR22725; 41571281; 41601302; 2016YFD0801006

OSTI ID:: 1463987

Journal Information:: Geoderma, Vol. 322; ISSN 0016-7061

Publisher:: ElsevierCopyright Statement

Country of Publication:: United States

Language:: English

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Cited by: 85 works

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