High-rate nitrogen loading accelerates organic phosphorus loss through enzymatic and non-enzymatic processes in a semi-arid grassland

IF 5 2区 农林科学 Q1 SOIL SCIENCE Applied Soil Ecology Pub Date : 2024-11-23 DOI:10.1016/j.apsoil.2024.105755
Nan Jiang , Qi Wang , Dongqi Jiang , Chenran Wu , Jiahui Pu , Wenjing Huang , Zimeng Yao , Zhenhua Chen , Yulan Zhang , Lijun Chen
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Abstract

Semi-arid grasslands suffer from increased nitrogen (N) loading, which affects phosphorus (P) cycling. Phosphorus is essential but limited for all living organisms. Organic P (Po) is crucial for P supply in grasslands response to N loading, but its transformation process remains unclear. To elucidate P cycling, we evaluated P fractions, phosphatase activities, and their coding genes (pho genes phoD, phoX, and phoC) at both DNA and RNA levels in response to a nitrogen loading gradient. The results showed that the total P and Po contents significantly decreased with increasing N loading rates. In contrast, plant and litter biomass P exhibited an opposite trend but were insufficient to offset soil P loss. Unexpectedly, neither the phosphatase activities nor microbial biomass increased with increasing N loading rates, although the DNA abundance of pho genes responded positively to N enrichment. A partial correlation network indicated that N loading rates decreased Po levels through phosphatase activities, which were significantly associated with soil pH and the RNA abundance of pho genes. Moreover, non-enzymatic mineralization may be enhanced in Po cycling in semi-arid grasslands undergoing high N loading, especially following the initial stage of enzymatic mineralization. Although the activity of phosphatases did not continue to rise with increased N loading, the strategy for addressing N-induced P limitation through overconsumption of Po via non-enzymatic processes would accelerate the degradation of the ecosystem in the future.
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在半干旱草地上,高速氮负荷通过酶和非酶过程加速了有机磷的流失
半干旱草原的氮(N)负荷增加,影响了磷(P)的循环。磷对所有生物都是必不可少的,但也是有限的。有机磷(Po)对草原应对氮负荷的磷供应至关重要,但其转化过程仍不清楚。为了阐明磷循环,我们评估了氮负荷梯度下的磷组分、磷酸酶活性及其编码基因(pho 基因 phoD、phoX 和 phoC)的 DNA 和 RNA 水平。结果表明,随着氮负荷率的增加,总磷和总钾含量显著下降。与此相反,植物和枯落物生物量 P 的变化趋势相反,但不足以抵消土壤中 P 的流失。出乎意料的是,随着氮负荷率的增加,磷酸酶活性和微生物生物量都没有增加,尽管 pho 基因的 DNA 丰度对氮富集有积极反应。局部相关网络表明,氮负荷率通过磷酸酶活性降低了磷的含量,而磷酸酶活性与土壤 pH 值和 pho 基因的 RNA 丰度有显著相关。此外,在氮负荷较高的半干旱草地上,非酶矿化可能会促进 Po 循环,尤其是在酶矿化的初始阶段之后。虽然磷酸酶的活性不会随着氮负荷的增加而持续上升,但通过非酶过程过度消耗Po来解决氮引起的P限制的策略将在未来加速生态系统的退化。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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来源期刊
Applied Soil Ecology
Applied Soil Ecology 农林科学-土壤科学
CiteScore
9.70
自引率
4.20%
发文量
363
审稿时长
5.3 months
期刊介绍: Applied Soil Ecology addresses the role of soil organisms and their interactions in relation to: sustainability and productivity, nutrient cycling and other soil processes, the maintenance of soil functions, the impact of human activities on soil ecosystems and bio(techno)logical control of soil-inhabiting pests, diseases and weeds.
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