4.6 Article

Effect of P fertilizer reduction regime on soil Olsen-P, root Fe-plaque P, and rice P uptake in rice-wheat rotation paddy fields

Journal

PEDOSPHERE
Volume 31, Issue 1, Pages 94-102

Publisher

SCIENCE PRESS
DOI: 10.1016/S1002-0160(20)60052-2

Keywords

crop biomass; crop total P; iron plaque; reduced P input; rice-growth stage; soil-root-aboveground system

Categories

Funding

  1. National Key Research and Development Program of China [2017YFD0800103]
  2. National Natural Science Foundation of China [41671304]
  3. Key Projects in the National 948 Program during the Twelfth Five-Year Plan Period [2011-G30]

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This study found that reducing phosphorus (P) fertilizer application in a rice-wheat rotation system did not significantly impact crop biomass. The PW treatment did not decrease crop total P, root iron (Fe)-plaque P, and soil Olsen-P during the rice growth stages, while the P0 treatment resulted in substantial reductions in these components.
In agricultural systems, it is vital to use limited yet optimal phosphorus (P) resources, because excessive P fertilizer application leads to the accumulation of P in soil, increasing the risk of environmental pollution and causing the waste and exhaustion of P resources. In a rice-wheat rotation system, omitting P fertilizer application in the rice-growing season is a good alternative; however, how this P fertilization reduction influences changes in P in the soil-root-above-ground system is unclear. In this study, after a seven-year rice-wheat rotation at the Yixing (YX) and Changshu (CS) sampling sites, China, compared with P fertilization in rice- and wheat-growing seasons (PR+W), reduced P fertilization (no P fertilizer application in either season, P0; P fertilization only in wheat-growing seasons, PW; and P fertilization only in rice-growing seasons, PR) did not result in substantial variation in crop biomass. The PW treatment did not reduce crop total P, root iron (Fe)-plaque P, and soil Olsen-P at three stages of rice growth (seedling, booting, and harvesting stages) at the YX and CS sites. In contrast, concentrations of soil Olsen-P, aboveground crop total P, and root Fe-plaque P decreased in the P0 treatment by 45.8%-81.0%, 24.6%-30.9%, and 45.6%-73.4%, respectively. In addition, a significant negative correlation was observed between the root Fe-plaque P and crop biomass at the two sites. Significant positive correlations were also observed between root Fe-plaque P and root total P, crop total P, and soil Olsen-P. In addition, the results of a redundancy analysis revealed that soil alkaline phosphatase (ALP) played a major role in the supply of P in soil, and was closely associated with root Fe-plaque P. The results of this study will enhance the understanding of the changes in P in the soil-root-above-ground system, particularly under P fertilizer reduction regimes.

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