Nitrogen and carbon inputs regulate soil phosphorus transformation through abiotic and biotic mechanisms in a semi-arid grassland

IF 3.9 2区 农林科学 Q1 AGRONOMY Plant and Soil Pub Date : 2025-01-21 DOI:10.1007/s11104-025-07225-9
Muyu Tian, Nan Jiang, Yulan Zhang, Dongqi Jiang, Chenran Wu, Guohui Wu, Weiwen Qiu, Lijun Chen, Jingkuan Wang, Zhenhua Chen
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Abstract

Aims

The aim of this study was to investigate the effects of varying nitrogen (N) and carbon (C) levels on soil phosphorus (P) compositions, abiotic factors (pH and moisture content), and biotic factors (dehydrogenase (DHA) and phosphatases).

Methods

A field experiment was conducted at the Inner Mongolia prairie, where different levels of N (0, 25, 50, 100, 200 kg N ha−1 yr−1) and C (0, 250, 500 kg C ha−1 yr−1) were applied to study their effects on soil P transformations.

Results

High N levels significantly decreased soil pH, concentrations of diesters, activities of DHA and acid phosphomonoesterase (AcP), phosphodiesterase, and inorganic pyrophosphatase (IPP); whereas, increased concentrations of phosphonate, polyphosphate, and myo-IHP; which could potentially affect nutrient availability, microbial processes and soil fertility. Additionally, C supplementation significantly increased concentrations of diesters and myo-IHP, and activities of DHA and IPP, suggesting C supplementation may improve P stability in contexts of excessive natural and anthropogenic N enrichment. SEM revealed two discrepant nutrition-driven modes in P transformation: i) the N-driven mode, where N addition directly affected phosphonate concentrations and indirectly affected P transformation through both abiotic (pH and moisture content) and biotic (AcP and IPP) factors; ii) the C-driven mode, where C addition directly affected concentrations of monoesters and indirectly affected pyrophosphate concentrations through a biotic (IPP) factor.

Conclusion

Our findings reveal how biotic and abiotic factors regulate P transformation through C management under N enrichment, enhancing our understanding of environmental influences on P cycling via phosphatase and benefiting sustainable grassland practices.

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半干旱草原氮素和碳输入通过生物和非生物机制调控土壤磷转化
目的研究不同氮(N)和碳(C)水平对土壤磷(P)组成、非生物因子(pH和含水量)和生物因子(脱氢酶(DHA)和磷酸酶)的影响。方法在内蒙古草原进行田间试验,分别施用不同水平N(0、25、50、100、200 kg N ha−1 yr−1)和C(0、250、500 kg C ha−1 yr−1),研究其对土壤磷转化的影响。结果高氮水平显著降低了土壤pH、酯类物质浓度、DHA、酸性磷酸单酯酶(AcP)、磷酸二酯酶和无机焦磷酸酶(IPP)活性;然而,磷酸盐、多磷酸盐和myo-IHP浓度增加;这可能会影响养分有效性、微生物过程和土壤肥力。此外,补充C显著提高了di酯和myo-IHP的浓度,以及DHA和IPP的活性,这表明补充C可能改善了自然和人为氮富集情况下磷的稳定性。SEM揭示了磷转化的两种不同的营养驱动模式:1)N驱动模式,其中N添加直接影响磷酸盐浓度,并通过非生物(pH和水分含量)和生物(AcP和IPP)因素间接影响磷转化;ii) C驱动模式,其中C的加入直接影响单酯的浓度,并通过生物(IPP)因素间接影响焦磷酸盐的浓度。结论本研究揭示了生物和非生物因子在富氮条件下通过C管理调控磷转化的机制,增强了我们对环境对磷通过磷酸酶循环的影响的认识,有利于草地可持续发展。
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来源期刊
Plant and Soil
Plant and Soil 农林科学-农艺学
CiteScore
8.20
自引率
8.20%
发文量
543
审稿时长
2.5 months
期刊介绍: Plant and Soil publishes original papers and review articles exploring the interface of plant biology and soil sciences, and that enhance our mechanistic understanding of plant-soil interactions. We focus on the interface of plant biology and soil sciences, and seek those manuscripts with a strong mechanistic component which develop and test hypotheses aimed at understanding underlying mechanisms of plant-soil interactions. Manuscripts can include both fundamental and applied aspects of mineral nutrition, plant water relations, symbiotic and pathogenic plant-microbe interactions, root anatomy and morphology, soil biology, ecology, agrochemistry and agrophysics, as long as they are hypothesis-driven and enhance our mechanistic understanding. Articles including a major molecular or modelling component also fall within the scope of the journal. All contributions appear in the English language, with consistent spelling, using either American or British English.
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