Droughts Legacy Effects on Phosphorus Transformation from Residues and Mineral Fertilizers in Calcareous and Carbonate-Free Soils: A 33P Labeling Study
文献类型： 外文期刊
作者： Farooq, Naila 1 ; Koirala, Manisha 1 ; Loftus, Sara 1 ; Zhang, Xi 2 ; Zamanian, Kazem 3 ; Banfield, Callum C. 4 ; Dippold, Michaela A. 4 ;
作者机构： 1.Univ Gottingen, Biogeochem Agroecosyst, D-37077 Gottingen, Germany
2.Jiangsu Acad Agr Sci, Inst Agr Resources & Environm, Nanjing 210014, Peoples R China
3.Leibniz Univ Hannover, Inst Earth Syst Sci, Sect Soil Sci, Hannover, Germany
4.Univ Tubingen, Dept Geosci, Geobiosphere Interact, D-72076 Tubingen, Germany
关键词： Alternate drying/wetting cycles; Climate change; Legacy effects on microbial traits; Phosphorus; Pre-sowing moisture regime; Sustainable agriculture
期刊名称：JOURNAL OF SOIL SCIENCE AND PLANT NUTRITION （ 影响因子：3.1； 五年影响因子：3.6 ）
ISSN： 0718-9508
年卷期： 2025 年 25 卷 1 期
页码：
收录情况： SCI
摘要： BackgroundWhile well-described for soil properties, we barely know how microbial traits determine the availability of various phosphorus (P) forms to crops.AimsWe traced the dynamics of mineral- versus residue-derived P applied to two contrasting soil types during wheat cultivation.MethodsThe legacy effect of three pre-sowing moisture conditions was investigated: drought (30% water holding capacity, WHC), alternating cycles of drying (30% WHC) and wetting (70% WHC), and well-watered conditions (70% WHC). 33P-labelled cowpea residues (Vigna unguiculate) and KH233PO4 were applied as fertilizers to calcareous and carbonate-free soils.ResultsUnder pre-sowing drought conditions, microbial incorporation of 33P from residue P into polar lipids was four times higher than from mineral P. Calcareous soils showed double the microbial biomass than carbonate-free soils. However, when fertilized with residue P, carbonate-free soils exhibited twice the acid phosphatase activity and a 3- to 6-fold greater 33P uptake into phospholipids normalized per unit microbial biomass C.ConclusionResidue P enhances microbial growth, leading to increased P immobilization, especially in carbonate-free soils. Drought-triggered microorganisms efficiently acquire P from organic sources like residues. This increased microbial P immobilization under pre-sowing drought does not negatively affect plant growth, when a mineralizable organic P pool is consistently available. Regardless of the pre-sowing moisture conditions, residue P fertilization promotes a rapidly cycling microbial biomass-necromass pool, specifically in calcareous soils. This implies that residue P fertilization could be a sustainable, long-term strategy for continuous P supply in P-immobilizing calcareous soils, even under increasing drought conditions due to climate change.
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