Journal
SOIL BIOLOGY & BIOCHEMISTRY
Volume 149, Issue -, Pages -Publisher
PERGAMON-ELSEVIER SCIENCE LTD
DOI: 10.1016/j.soilbio.2020.107959
Keywords
Long-term fertilisation; Phosphorus cycling; Soil layers; Substrate sorption; Waste management and recycling
Categories
Funding
- National Key Research and Development Program of China [2016YFD020010X]
- National Natural Science Foundation of China [31872180, 31572194]
- UK-China Virtual Joint Centre for Agricultural Nitrogen (CINAg) - Newton Fund, via UK BBSRC [BB/N013468/1]
- UK-China Virtual Joint Centre for Agricultural Nitrogen (CINAg) - NERC [BB/N013468/1]
- Chinese Ministry of Science and Technology
- UK BBSRC [BBS/E/C/000J0300]
- Lawes Agricultural Trust
- BBSRC [BBS/E/C/000J0300] Funding Source: UKRI
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Maintaining an adequate phosphorus (P) supply for plants and microorganisms is central to agricultural production; however, the long-term effects of organic manure and inorganic fertilizer application on soil P cycling remain unclear. Organic P cycling in a sandy loam soil receiving medium and high rates of farmyard manure (FYM) with and without mineral fertilisers was studied in a long-term field experiment with C-14/P-33 isotope labelling and metagenomic shotgun sequencing. FYM application alone negatively affected soil total P and organic P (P-o) accumulation by enhancing crop offtake, enhancing P-o mineralisation and stimulating P loss from the topsoil by reducing its P sorption potential. The P mineralisation/immobilisation rates detected by the P-33 pool dilution method were significantly correlated with the abundance of microbial P cycling genes. Soil available C and N concentrations were related to gross P mineralisation/immobilisation rates and the abundance of P uptake/scavenging genes. Microbial genes related to P uptake and metabolism were more abundant than P scavenging genes, while P scavenging genes may work efficiently as both of them can sustain similar P mineralisation and immobilisation rates. The addition of FYM also promoted phosphatase activity reflecting the increased supply of P-o in these soils. Our study demonstrates that long-term FYM application alters soil P-o stocks and cycling, and that microbial functional gene abundance was coupled with P cycling rates.
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