退化高寒草甸恢复对土壤团聚体及其胶结物质的影响

Restoration Effects of Degraded Grassland on Soil Aggregates and Cementing Materials in Alpine Grassland of Qinghai-Tibet Plateau

  • 摘要:
    目的 为探明高寒草甸退化与恢复过程对土壤胶结物质的影响。
    方法 通过研究草地退化与恢复过程(天然嵩草斑块→退化裸土斑块→过渡杂草斑块→自然恢复嵩草斑块/人工修复禾草斑块),分析土壤团聚体稳定性及其胶结物质的含量,且研究各胶结物质对团聚体稳定性的影响。
    结果 ①随草地退化与恢复,表土(0 ~ 10 cm)平均重量直径、几何平均直径和大团聚体比例呈现先降低再升高的趋势(P < 0.05),且自然恢复对团聚体稳定性的提升效果显著优于人工修复方式(P < 0.05);亚表层(10 ~ 20 cm)各指标随草地演替并无显著变化。②草地退化后,表土有机与无机胶结物质均显著减少(P < 0.05);退化草地恢复后,络合态氧化铝、球囊霉素相关土壤蛋白、总有机碳、团聚体有机碳均有显著提升(P < 0.05),其中,自然恢复方式显著提高了不同形态铁铝氧化物含量(P < 0.05);亚表层各指标随草地演替并无显著变化。③结合皮尔逊相关性、冗余与偏相关分析发现,游离态氧化铝和络合态氧化铝是是分别影响表层和亚表层土壤团聚体稳定性关键胶结物质。
    结论 退化高寒草甸的恢复过程通过影响团聚体胶结物质的含量,进而影响了团聚体稳定性,且不同草地恢复方式影响的胶结物质不同。

     

    Abstract:
    Objective Cementing substances in soil represent the most active components and form the foundation and core of soil aggregate formation. The aims were to clarify the effects of alpine meadow degradation and restoration processes on soil cementing substances.
    Method This study investigated the changes in soil aggregate stability and cementing substance content during grassland succession (from natural Kobresia patches → degraded bare patches → transitional weed patches → naturally restored Kobresia patches / artificially restored Gramineae meadow patches), and examined the influence of various cementing substances on aggregate stability.
    Result ① In the surface soil layer (0 - 10 cm), the mean weight diameter, geometric mean diameter and the proportion of macroaggregates decreased initially and then increased along the degradation and restoration gradient (P < 0.05). Moreover, natural restoration significantly improved aggregate stability compared with artificial restoration (P < 0.05). In the subsurface layer (10 - 20 cm), these indicators did not change significantly during the grassland succession. ② After grassland degradation, both organic and inorganic cementing substances in surface soil decreased significantly (P < 0.05). Following restoration, the contents of complexed aluminum oxides, glomalin-related soil proteins, total organic carbon, and aggregate-associated organic carbon significantly increased (P < 0.05). Among them, natural restoration markedly enhanced the levels of various forms of iron and aluminum oxides (P < 0.05). No significant changes were observed in the subsurface layer during the succession. ③ Based on pearson correlation, redundancy analysis, and partial correlation analysis, free aluminum oxides and complexed aluminum oxides were identified as the key cementing substances influencing the stability of surface and subsurface soil aggregates, respectively.
    Conclusion The results demonstrate that the restoration of degraded alpine meadows affects soil aggregate stability by altering the content of cementing substances, and that different restoration approaches influence distinct types of cementing substances.

     

/

返回文章
返回