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    坡向对公路边坡土壤有机碳恢复的短期影响

    Short-term effects of slope aspect on the soil organic carbon recovery of highway slopes

    • 摘要: 明确不同坡向对边坡土壤碳恢复的差异,分析主要的影响因素,并通过人工措施作用于这些因素,可为生态边坡碳汇功能的恢复奠定基础。以广连高速公路上恢复1 a的人工边坡为研究对象,对不同坡向边坡的植被恢复情况、土壤有机碳质量分数、土壤理化性质,及土壤细菌群落特征和酶活性进行对比分析,并通过偏最小二乘回归法探究边坡短期土壤有机碳变化的主要驱动因子。结果表明:阴坡的植被恢复情况显著优于其他坡向的边坡,且土壤有机碳质量分数也表现为阴坡 > 阳坡(半阳坡)。阴坡的土壤含水率、有效养分质量分数显著大于其他坡向,土壤细菌群落结构和酶活性在不同坡向间也存在显著差异。除土壤水分和养分质量分数,放线菌门相对丰度也是影响短期土壤有机碳变化的主要因素。综上,不同坡向间的水热条件差异,通过改变边坡土壤水分、养分质量分数和细菌群落组成,对边坡短期土壤有机碳恢复产生影响。通过微生物菌剂改变土壤细菌群落组成,可作用于边坡短期内土壤有机碳的累积过程。本研究结果可为人工边坡碳汇功能恢复技术的改进提供依据。

       

      Abstract:
      Background Clarifying the impact of slope aspect on the short-term soil carbon recovery of slopes, and analyzing the main influencing factors may provide scientific basis for the improvement of carbon sink recovery technology of artificial slope.
      Methods This study focuses on the artificial slopes on the Guanglian Expressway, which have been restored for one year. The vegetation restoration, soil organic carbon content, soil physicochemical properties, soil bacterial community characteristics, and enzyme activity of slopes were compared and analyzed with different slope aspects. Partial least squares regression (PLSR) was used to explore the main driving factors of short-term soil organic carbon changes on slopes.
      Results 1) The density of the Cajanus cajan community on the shady slope is much higher than that on the sunny and semi-sunny slopes, which also results in a significant increase in the total biomass of the vegetation community on the shady slope compared to other slopes. The soil organic carbon content on shady slopes is 4.3 and 4.7 times higher than that on sunny and semi-sunny slopes, respectively, while there is no significant difference between sunny and semi-sunny slopes. 2) The soil moisture content and available nutrient content of the shady slope are significantly higher than those of other slope aspects, and there are also significant differences in soil bacterial community structure and enzyme activity among different slope aspects. 3) In addition to soil moisture and nutrient content, the relative abundance of Actinobacteria is also the main factor affecting short-term changes in soil organic carbon.
      Conclusions The differences in hydrothermal conditions between different slope aspects have an impact on the short-term soil organic carbon recovery of slopes by changing soil moisture, nutrient content, and bacterial community composition. Changing the composition of soil bacterial communities through microbial agents may affect the short-term accumulation process of soil organic carbon on slopes.

       

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