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Updated: Jan 31, 2026

Utilizing Soil Density Fractionation to Separate Distinct Soil Carbon Pools
Published on: December 16, 2022
Soil phosphorus fractions drove nitrous oxide emissions: Based on nitrification inhibitor and phosphate-solubilizing
Yaohui Liu1, Meng Zhang2, Shengyou Yang3
1College of Forestry and Grassland Science, Jilin Agricultural University, Changchun, 130000, China; College of Forestry, Henan Agricultural University, Zhengzhou, 450046, China; National Forestry and Grassland Administration Key Laboratory for Central Plains Forest Resources Cultivation, Henan Agricultural University, Zhengzhou, 450046, China; Henan Province Engineering Technology Research Center for Idesia, Zhengzhou, 450046, China; Jiangxi Key Laboratory of Subtropical Forest Resources Cultivation, Jiangxi Agricultural University, Nanchang, 330045, China.
Abstract:
Nitrogen and phosphorus are the important factors for improving terrestrial ecosystem productivity, and nitrification inhibitor and phosphate-solubilizing bacterium (PSB) are the sustainable practices to reduce soil nitrous oxide (N2O) emission while enhancing nitrogen and phosphorus availability, resulting in an environmentally friendly terrestrial ecosystem. However, the effects of combined applications of 3, 4-dimethyl pyrazole phosphate (DMPP) and PSB on N2O emission reduction and phosphorus fractions transformation, and their correlations in rhizospheric and non-rhizospheric soils are unclear. In this study, soil chemical properties, N2O emissions and phosphorus fractions, were characterized and analyzed. Although the DMPP inhibited soil N2O emission rate, this inhibitory effect was gradually weakened by the PSB in rhizospheric and non-rhizospheric soils. Compared to the control, DMPP and PSB increased available phosphorus by 10.09 %-33.25 % in rhizospheric soil, and a significant increase (7.33 %) in available phosphorus was only observed as DMPP application in non-rhizospheric soil at the end of incubation. Additionally, contrary results were detected that accumulation but declination of residual-P in rhizospheric and non-rhizospheric soils, respectively, as combined DMPP and PSB on day 28. Soil pH driven soil N2O emission rate, which was also positively affected by available phosphorus, water-soluble inorganic phosphorus (H2O-P), sodium bicarbonate extraction of phosphorus (NaOH-Pi and NaOH-Po). However, positive and negative contributions to the N2O emission rate were generated by residual-P in rhizospheric and non-rhizospheric soils, respectively. In conclusion, the findings suggested that the PSB accelerated soil phosphorus fractions transformation and improved phosphorus availability but weakened the inhibitory capacity of DMPP on N2O emissions.
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