海拔对藏东南山地土壤有机碳垂直分布格局的影响分析

    Analysis of Impact of Altitude on Vertical Distribution Pattern of Soil Organic Carbon in Mountainous Regions of Southeastern Tibet

    • 摘要:
      目的 分析藏东南地区高山生态系统在垂直分布带上的空间异质性,研究不同海拔土壤有机碳(SOC)储量的分布特征及其影响因子。
      方法 以高寒半湿润区藏东南典型山地色季拉山为研究对象,在海拔3 400~4 600 m每隔200 m海拔梯度展开采样,通过野外调查与室内分析相结合的方法,探讨海拔对SOC垂直分布特征的影响及其与其他理化指标的相关性。
      结果 色季拉山土壤物理指标之间存在很大的空间异质性,在海拔3 400~4 600 m土壤容重、总孔隙度、毛管孔隙度和非毛管孔隙度的变化范围分别为0.72~1.08 g/cm3、51.76%~67.06%、47.11%~58.03% 和9.03%~11.04%;SOC主要集中分布在0~60 cm土层中,不同海拔梯度SOC含量(1.57%~8.24%)随着土层深度的增加呈下降趋势,以海拔4 618 m高寒草甸的SOC含量最高,为其他海拔的1.76~3.07倍;SOC储量范围为117.14~220.63 t/hm2,以海拔4 255 m土层的SOC储量显著高于其他海拔高度,相当于海拔3 393 m的2倍;不同海拔显著影响0~60 cm土层的SOC储量,整体上呈现单峰曲线变化趋势。
      结论 色季拉山不同植被类型土壤的SOC垂直分布差异显著,海拔梯度变化会直接或间接影响SOC的精准估算,进而影响SOC的空间分布和预测。

       

      Abstract:
      Objective The spatial heterogeneity of alpine ecosystems in southeastern Tibet in the vertical distribution zone was analyzed, and the distribution characteristics and influencing factors of soil organic carbon(SOC)reserves at different altitudes were studied.
      Methods Taking the Sejila Mountain, a typical mountain in southeastern Tibet in the alpine and semi-humid region, as the research object, sampling was carried out at an altitude of 3 400-4 600 m with an altitude gradient of 200 m, and the altitude was investigated by combining field investigation and indoor analysis. The impact of altitude on the vertical distribution characteristics of SOC and its correlation with other physical and chemical indicators.
      Result There was a great spatial heterogeneity among the soil physical indexes in the Sejila Mountain at an altitude of 3 400~4 600 m. The soil bulk density, total porosity, capillary porosity and non-capillary porosity varied 0.72-1.08 g/cm3, 51.76%-67.06%, 47.11%-58.03% and 9.03%-11.04%. SOC was mainly distributed in the 0-60 cm soil layer, and the SOC contents of different altitude gradients(1.57%-8.24%)showed a downward trend with the increase of soil depth, and the SOC content of the alpine meadow at an altitude of 4 618 m was the highest, which was 1.76-3.07 times that of other altitudes; SOC reserve was 117.14-220.63 t/hm2, among which the SOC reserve in the soil layer at an altitude of 4 255 m was significantly higher than that at other altitudes, equivalent to 2 times that at an altitude of 3 393 m; different altitudes significantly affected the SOC reserves in the 0-60 cm soil layer, showing a single peak as a whole curve change trend.
      Conclusion There are significant differences in the vertical distribution of SOC under different vegetation types in the Sejila Mountain, and the change of altitude gradient will directly or indirectly affects the accurate estimation of SOC, and then affects the spatial distribution and prediction of SOC.

       

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