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Quantifying phosphorus fertilizer distribution and the contribution of fertilizer and soil legacy phosphorus to phosphorus uptake by maize - A P-32-labelling study

文献类型： 外文期刊

作者： Zheng, Dongfang 1 ; Yuan, Huimin 1 ; Yang, Guojiang 2 ; Feng, Gu 1 ; Rengel, Zed 3 ; Shen, Jianbo 1 ;

作者机构： 1.China Agr Univ, Natl Acad Agr Green Dev, Coll Resources & Environm Sci, Key Lab Plant Soil Interact, Beijing, Peoples R China

2.Xinjiang Acad Agr & Reclamat Sci, Res Inst Farmland Water Conservancy & Soil fertili, Shihezi, Xinjiang, Peoples R China

3.Univ Western Australia, UWA Sch Agr & Environm, Soil Sci & Plant Nutr, Perth, WA, Australia

4.Inst Adriat Crops & Karst Reclamat, Split, Croatia

5.China Agr Univ, Natl Acad Agr Green Dev, Coll Resources & Environm Sci, Key Lab Plant Soil Interact,Minist Educ, 2 Yuan Ming Yuan West Rd, Beijing 100193, Peoples R China

关键词： isotopic dilution; P fertilizer partitioning; soil P fractions; soil type; Zea mays L

期刊名称：FOOD AND ENERGY SECURITY （ 影响因子：5.0； 五年影响因子：5.9 ）

ISSN： 2048-3694

年卷期： 2023 年

页码：

收录情况： SCI

摘要： The availability of phosphorus (P) fertilizer applied to soil can diminish rapidly because of the complex soil P immobilization processes. However, the quantitative distribution of fertilizer P in the soil P fractions is not fully understood. Here, two experiments were conducted in a greenhouse using P-32-labelled KH2PO4 to (i) quantify the distribution of P fertilizer in soil fractions, microorganisms and maize shoots grown in contrasting soils; (ii) characterize the effect of planting maize on soil P fractions and (iii) determine the amount of plant P derived from fertilizer vs. soil. Depending on the soil type, 74.1%-84.1% of the labelled P was retained in the soil, 11.4%-14.5% was found in maize shoots and 0.7%-4.5% was present in microorganisms. Distribution of applied P in the soil P fractions was dependent on soil type, with most P present as NaOH-Pi and residual-P in the Red soil, and as HCl-P in the Fluvo-aquic soil. Root-mediated processes were involved in mobilisation of residual-P in all three soils, with significant depletion of NaOH-Pi in the Red soil, NaOH-Pi and HCl-P in the Black soil, and HCl-P in the Fluvo-aquic soil. The plant P derived from fertilizer and soil increased with increasing P addition rates in all three soils. In the soils with low-P availability, fertilizer contributed more P to plants than soil, whereas in the initially high-P soil, the opposite occurred. In conclusion, the partitioning of fertilizer P to various soil P fractions is dependent on the soil type, and the contribution of P derived from fertilizer to maize P uptake was related inversely to the soil legacy P.

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