Wang Xuan, Zhao Jixia, Li Chunpei, Deng Limei, Cui Rongyang, Zhou Tao, Hussain Zakir, Liu Gangcai
Key Laboratory of Mountain Surface Processes & Ecological Regulation, Institute of Mountain Hazards and Environment, Chinese Academy of Sciences, Chengdu, China.
University of Chinese Academy of Sciences, Beijing, China.
Front Microbiol. 2025 Jan 7;15:1514646. doi: 10.3389/fmicb.2024.1514646. eCollection 2024.
Rock weathering is a fundamental process that shapes Earth's topography, soil formation, and other surface processes. However, the mechanisms underlying the influence of fertilizer application on weathering remain poorly understood, especially with respect to bacterial intervention.
In this study, purple parent rocks from Shaximiao Group (Js) and Penglaizhen Group (Jp) were selected to investigate the effects of fertilizer application on the bacterial community and weathering characteristics of these rock by leaching experiment.
The results revealed that: fertilizer application, especially when at high levels, greatly altered the abundance, diversity and composition of the bacterial community in weathered products. Through redundancy analysis, a decrease in pH and increases in available nutrients (AN and AP) resulting from fertilizer application were identified as the key factors driving changes of bacterial community composition in weathered products. Moreover, fertilizer application promotes the physical and chemical weathering of the parent rocks to some extent. This is especially true for the chemical weathering of Js. Structural equation model indicated that fertilizer application affects weathering through multiple pathways by affecting the chemical properties (pH, C:N and AP), specific bacterial genera (IMCC26256, , and ), and bacterial community composition of weathered products.
Our study links weathering characteristics with chemical properties and bacterial community changes of weathered products after fertilizer application, which plays a key role in controlling and predicting dynamic changes of rock weathering in space and time. It is helpful to further understand the law of human activities affecting the surface processes.
岩石风化是塑造地球地形、土壤形成及其他地表过程的基本过程。然而,施肥对风化影响的潜在机制仍知之甚少,尤其是在细菌干预方面。
本研究选取沙溪庙组(Js)和蓬莱镇组(Jp)的紫色母岩,通过淋溶实验研究施肥对这些岩石细菌群落和风化特征的影响。
结果表明:施肥,尤其是高施用量时,极大地改变了风化产物中细菌群落的丰度、多样性和组成。通过冗余分析,确定施肥导致的pH值下降和有效养分(有效氮和有效磷)增加是风化产物中细菌群落组成变化的关键驱动因素。此外,施肥在一定程度上促进了母岩的物理和化学风化。对于Js的化学风化尤其如此。结构方程模型表明,施肥通过影响风化产物的化学性质(pH值、碳氮比和有效磷)、特定细菌属(IMCC26256等)和细菌群落组成,通过多种途径影响风化。
我们的研究将施肥后风化产物的风化特征与化学性质和细菌群落变化联系起来,这对于控制和预测岩石风化在空间和时间上的动态变化起着关键作用。有助于进一步了解人类活动影响地表过程的规律。