长期施用矿物肥料会降低土壤微生物多样性,从而削弱微生物转化氮功能的稳定性

Zhou Zhang, Ruirui Chen, Evgenia Blagodatskaya, Sergey Blagodatsky, Deyan Liu, Yongjie Yu, Xiaolin Zhu, Youzhi Feng
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引用次数: 0

摘要

引言 在气候变化不断加剧的情况下,确保功能稳定性对于农业生态系统的可持续发展和土壤健康至关重要。众所周知,矿物肥料能增强土壤氮转化功能的强度,但其对功能稳定性的影响仍不明确。 材料与amp; 方法 本研究评估了干旱-润湿过程中土壤微生物氮转化功能的三个稳定性组成部分(抵抗力、恢复力和复原力)以及其维度。我们调查了在矿物肥(NPK)、矿物肥加有机添加剂(OMN)和不施肥(CK)三种施肥策略下施肥 10 年后的酶活性和功能基因丰度。 结果 在 CK、NPK 和 OMN 处理中,抗性分别为 0.60、0.66 和 0.56;复原力分别为 0.46、0.28 和 0.46;恢复力分别为 0.83、0.73 和 0.82。长期施用矿质肥料的土壤在干旱-润湿过程中表现出最高的抗性,但复原力和恢复力最低。此外,施用矿物肥料的土壤稳定性维度最低,椭球体积最小,负相关最大。土壤微生物α多样性被认为是功能稳定性的关键预测因子,与各种施肥策略的稳定性呈正相关。 结论 矿物施肥会降低阿尔法多样性,对干旱条件下农业生态系统的可持续发展构成挑战。矿质肥料加有机添加剂具有较强的氮转化功能和适度的稳定性,因此是一种最佳施肥策略。这些结果为优化农业生态系统管理和促进土壤可持续发展提供了宝贵的启示。
本文章由计算机程序翻译,如有差异,请以英文原文为准。

Long-term application of mineral fertilizer weakens the stability of microbial N-transforming functions via the decrease of soil microbial diversity

Long-term application of mineral fertilizer weakens the stability of microbial N-transforming functions via the decrease of soil microbial diversity

Introduction

Ensuring functional stability is crucial for the sustainable development and soil health of agroecosystems amidst escalating climate changes. Although mineral fertilization is known to enhance the strength of soil N-transforming functions, its effects on functional stability remain unclear.

Materials & Methods

This study evaluated three stability components (resistance, resilience, and recovery), along with the dimensionality of soil microbial N-transforming functions during drought-rewetting process. We investigated enzymatic activity and functional gene abundances after 10 years of fertilization under three strategies, mineral fertilization (NPK), mineral fertilization plus organic amendments (OMN), and no fertilization (CK).

Results

The resistance was 0.60, 0.66 and 0.56; the resilience was 0.46, 0.28 and 0.46; and the recovery was 0.83, 0.73 and 0.82, respectively in the CK, NPK and OMN treatments. Soils with long-term mineral fertilization exhibited the highest resistance but the lowest resilience and recovery during drought-rewetting. Furthermore, mineral fertilization demonstrated the lowest dimensionality of stability, with smallest ellipsoid volume and most negative correlations. Soil microbial alpha diversity was identified as a key predictor of functional stability, positively correlating with stability across fertilization strategies.

Conclusion

Mineral fertilization, which decreased alpha diversity, posed challenges for sustainable development of agroecosystems under drought conditions. Mineral fertilization plus organic amendments provided strong N-transforming functions and moderate stability, making it as an optimal fertilization strategy. These results offer valuable insights for optimizing agroecosystem management and advancing soil sustainability.

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