Arbuscular mycorrhizal hyphal networks and glomalin-related soil protein jointly promote soil aggregation and alter aggregate hierarchy in Calcaric Regosol
Lingling Ji , Xiuhua Chen , Chuanqin Huang , Wenfeng Tan
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引用次数: 0
Abstract
The Loess Plateau of China (LPC) is one of the most severely eroded areas in the arid and semi-arid regions of northern China. Improving soil aggregate stability and hierarchy in Calcaric Regosol is vital for mitigating soil erosion. However, Calcaric Regosol exhibits weak aggregate hierarchy, and there is limited correlation between its aggregate stability and soil organic matter (SOM). Arbuscular mycorrhizal (AM) fungi, known for their soil-structuring capabilities, may hold potential for improving aggregate stability, yet their specific impact on calcareous soil remains unclear. In this study, a three-compartment growth system was used to separate the root and AM fungi, and the impact of AM fungi on soil aggregate stability and hierarchy was quantified. The AM fungi, Rhizophagus intraradices and Funneliformis mosseae, were separately inoculated into mycorrhizal compartments under well-watered and drought stress conditions. Aggregate stability was measured through the wet sieving method and ultrasonic dispersive technology, while aggregate hierarchy was assessed by characteristic disruption and dispersion curves. The results revealed that AM fungi significantly increased the water-stable aggregate stability, and the inoculation reduced the rate of macroaggregate disruption and microaggregate dispersion rate mediated by hyphal network and glomalin. Despite these improvements, the characteristic curves indicated no strong aggregate hierarchy. A permutation test identified hyphal length and glomalin-related soil protein (GRSP) as critical factors contributing to soil aggregate stability. These results suggest that increases in hyphae and GRSP, which are important components of SOM, promote soil aggregation and modify aggregate hierarchy in calcareous soils. This study introduces an energy-based approach to investigate the soil aggregate hierarchy, proposing AM fungi as an effective ecological strategy to restore aggregate stability and mitigate soil erosion on the LPC.
中国黄土高原(LPC)是中国北方干旱和半干旱地区水土流失最严重的地区之一。提高钙质团粒结构的稳定性和层次性对减轻水土流失至关重要。然而,钙质团粒结构薄弱,团粒稳定性与土壤有机质(SOM)之间的相关性有限。丛枝菌根(AM)真菌以其土壤结构能力而著称,可能具有改善团聚稳定性的潜力,但其对石灰性土壤的具体影响仍不清楚。本研究采用三室生长系统将根和 AM 真菌分开,并量化了 AM 真菌对土壤团聚体稳定性和层次结构的影响。在水分充足和干旱胁迫条件下,将 AM 真菌(Rhizophagus intraradices 和 Funneliformis mosseae)分别接种到菌根分区中。聚合体稳定性通过湿筛法和超声波分散技术进行测量,聚合体层次结构则通过特征破坏和分散曲线进行评估。结果表明,AM 真菌显著提高了水稳聚合稳定性,接种降低了由菌丝网络和胶霉素介导的大聚合体破坏率和微聚合体分散率。尽管有这些改善,但特征曲线表明聚集体并没有很强的层次性。通过置换检验,确定菌丝长度和胶霉素相关土壤蛋白质(GRSP)是影响土壤团聚稳定性的关键因素。这些结果表明,作为 SOM 重要组成部分的菌丝和 GRSP 的增加会促进土壤团聚,并改变石灰性土壤中的团聚层次结构。这项研究引入了一种基于能量的方法来研究土壤团聚体的层次结构,并提出了一种有效的生态策略,即利用 AM 真菌来恢复团聚体的稳定性并减轻 LPC 上的土壤侵蚀。
期刊介绍:
Geoderma - the global journal of soil science - welcomes authors, readers and soil research from all parts of the world, encourages worldwide soil studies, and embraces all aspects of soil science and its associated pedagogy. The journal particularly welcomes interdisciplinary work focusing on dynamic soil processes and functions across space and time.