黄土丘陵区生物结皮覆盖对土壤团聚体分布特征及稳定性影响

Effect of Biological Crust Mulching on Distribution Characteristics and Stability of Soil Aggregates in Loess Hilly Region

  • 摘要:
      目的  以吕梁离石区结皮覆盖(藻结皮、藓结皮、藓草混生结皮,裸地为对照)下土壤为研究对象,研究结皮种类对其下层土壤有机碳及土壤团聚体稳定性的影响。
      方法  通过干筛和湿筛法对土壤团聚体分级,探究土壤容重、土壤有机碳含量和土壤静水崩解速率与团聚体稳定的相关性。
      结果  在0 ~ 5 cm和5 ~ 10 cm深度,3种结皮下土壤容重与裸地间均达到显著差异;土壤有机碳含量表现为藓草混生结皮和藓结皮分别比裸地显著增加。不同深度土层,团聚体破坏率、分形维数表现为裸地 > 藻结皮 > 苔藓结皮 > 藓草混生结皮;平均重量直径和几何平均直径变化规律正好相反。相关性分析表明,> 0.25 mm土壤团聚体含量与土壤容重呈显著负相关关系;团聚体破坏率、分形维数与土壤容重、土壤静水崩解速率呈极显著正相关关系,与土壤有机碳含量呈极显著负相关关系;平均重量直径、几何平均直径与土壤容重呈极显著负相关关系,与土壤静水崩解速率呈显著负相关关系,与土壤有机碳含量呈极显著正相关关系。
      结论  黄土丘陵吕梁随结皮层次提高,土壤团聚体形成能力和土壤团聚体水稳定性逐渐增高,对土壤水稳定性起主导作用的是土壤有机碳含量。

     

    Abstract:
      Objective  The effects of soil crusts types on the soil organic carbon and the stability of soil aggregates were studied under the soil crust mulching (algal crust, moss crust, mixed soil crust and bare soil) in the rocky area of Lüliang.
      Method  The relationships between soil bulk density (SBD) , soil organic carbon (SOC) and soil static water disintegration rate (B) and the stability of soil aggregates were investigated by dry and wet sieving methods.
      Result  The results showed that there were significant differences between SBD and bare land at the depth of 0 ~ 5 cm and 5 ~ 10 cm. The SOC of Moss mixed crust and Moss crust increased significantly than that of bare soil. In different depth of soil layers, the aggregate broken rate (PAD) and fractal dimension (D) were Bare Land > Algal Crust > Moss Crust > Moss Mixed Crust, but the mean weight diameter (MWD) and geometric mean diameter (GMD) were opposite. The correlation analysis showed that the contents of soil aggregate (R0.25) were negatively correlated with SBD, and the contents of PAD, D were positively correlated with SBD and B, and negatively correlated with SOC. MWD, GMD and SBD showed a significant negative correlation, a significant negative correlation with B, and a significant positive correlation with SOC.
      Conclusion  With the increase of soil crust succession, the ability of soil aggregate formation and the water stability of soil aggregate increase gradually in Lüliang Loess Hilly region, and the content of soil organic carbon plays a dominant role in soil water stability.

     

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