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    宁夏输变电塔基扰动区域植被恢复对土壤微生物残体的影响

    Effect of vegetation restoration on soil microbial necromass in disturbed area of power transmission and transformation tower in Ningxia Province

    • 摘要: 输电线路工程的塔基架设会严重破坏周围植被和土壤,造成土壤肥力下降,在该区域进行植被恢复是改善区域生态环境的重要措施。探究土壤微生物残体碳累积情况,可有效评估塔基处植被恢复的生态效益。本研究采用生物标志物法,测定植被恢复区域土壤氨基糖含量,计算微生物残体碳含量对有机碳的贡献,并分析微生物残体碳含量与土壤理化性质和微生物量的关系。结果表明:塔基处植被恢复后,土壤微生物残体碳含量(11.2±0.1 mg/g)显著高于干扰区域土壤(3.9±0.6 mg/g),并恢复到未干扰土壤水平(8.84±1.3 mg/g)。微生物残体碳对土壤有机碳库的贡献从21.9±3.1%恢复到50.8±4.0%,甚至高于未干扰土壤水平30.0±5.2%。土壤微生物残体碳主要由真菌贡献,真菌残体碳对土壤有机碳贡献的范围为18.3%~29.8%,细菌残体碳的贡献范围为13.6%~20.9%。方差分解结果显示,土壤性质和微生物量共同解释了微生物残体碳含量的48.3%,其中,土壤性质解释了35.5%,微生物量解释了变异的27.4%。Mantel分析进一步显示,土壤碳氮含量和微生物量碳与微生物残体碳含量呈显著正相关关系。本研究结果揭示了植被恢复对塔基干扰土壤有机碳含量及其稳定性的重要作用。

       

      Abstract: Abstract: Background The construction of transmission towers in arid regions has impacted their ecological balance, resulting in the degeneration of soil fertility. Vegetation restoration is crucial in these disturbed areas, not only for preventing desertification but also for influencing soil microbial communities, which play a key role in nutrient cycling and soil health. However, the effects of such restoration on soil microbial residues—key indicators of long-term soil quality and ecosystem stability—remain poorly understood. Methods In this study, biomarker was used to determine the soil amino sugar content in vegetation restoration area. We calculated the contribution of microbial residue carbon content to organic carbon, and analyzed the relationship between microbial necromass carbon content and soil properties and microbial biomass. Results The results indicated that the microbial necromass carbon content (11.2±0.1 mg/g) in vegetation restoration soil was significantly higher than that in disturbed soil (3.9±0.6 mg/g), and restored to the level of undisturbed soil (8.84±1.3 mg/g). The contribution of microbial necromass carbon to soil organic carbon recovered from 21.9±3.1% to 50.8±4.0%, even higher than the undisturbed soil level of 30.0±5.2%. Soil microbial necromass carbon was mainly contributed by fungi, and the contribution of fungal residue carbon to soil organic carbon ranged from 18.3% to 29.8%, and that of bacterial residue carbon ranged from 13.6% to 20.9%. The variance decomposition results showed that soil properties and microbial biomass jointly explained 48.3% of the variation in microbial necromass carbon content, in which soil properties explained 35.5% of the variation and microbial biomass explained 27.4% of the variation. Mantel analysis further showed that soil carbon and nitrogen content and microbial biomass carbon were significantly positively correlated with microbial necromass carbon content. Conclusions The results of this study revealed the important role of vegetation restoration on soil organic carbon content and its stability.

       

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