%0 Journal Article %T 滇东岩溶山地不同类型云南松林地土壤团聚体稳定性差异 %T Differences in Soil Aggregate Stability of Different Species of Pinus Yunnanensis in Karst Mountain Area of Eastern Yunnan Province %A 方薇,范弢 %A Fang Wei %A Fan Tao %J 水土保持通报 %J 水土保持通报英文版 %@ 1000-288X %V 40 %N 3 %D 2020 %P 95-102,132 %K 水稳性团聚体;土壤结构稳定性;岩溶山地;滇东;云南松 %K water-stable aggregate;soil structural stability;karst mountains;Eastern Yunnan Province;Pinus yunnanensis %X [目的] 研究滇东岩溶山地不同类型云南松林地土壤团聚体稳定性差异,为岩溶脆弱生境土壤培肥、质量提升、水土固持提供依据。[方法] 通过野外调查和室内分析,研究了滇东岩溶山地云南松纯林、云南松人工混交林、云南松天然混交林、灌丛和原生林5种植被类型水稳性团聚体及团聚体有机碳分布特征,揭示不同类型云南松林团聚体稳定性差异。[结果] ①云南松纯林、人工混交林和天然混交林的<0.25 mm粒径质量分数(5.77%~9.39%)显著低于灌丛(20.92%)和原生林(27.47%)(p<0.05),且人工混交林和天然混交林>5 mm,2~5 mm粒径质量分数高于纯林。②湿筛处理的>0.25 mm水稳性团聚体比例(R0.25)排序为:人工混交林 > 天然混交林 > 纯林>灌丛 > 原生林;平均重量直径(MWD)排序为:人工混交林 > 天然混交林 > 原生林 > 灌丛 > 纯林;几何平均直径(GMD)排序为:人工混交林 > 天然混交林 > 原生林 > 纯林 > 灌丛;分形维数(D)排序为:原生林 > 灌丛 > 纯林 > 天然混交林 > 人工混交林。③纯林、人工混交林、天然混交林的大粒级团聚体(>0.25 mm)对土壤有机碳的贡献率高于小粒级团聚体(<0.25 mm),且>5,2~5,<0.25 mm粒径水稳性土壤团聚体有机碳含量均显著小于灌丛、原生林(p<0.05)。[结论] 云南松人工混交林的土壤团聚体稳定性最高,其养分积累和固碳能力低于灌丛和原生林,高于纯林,作为该区域水土保持的主要植被类型时需要避免人为干扰以提高土壤养分。 %X [Objective] The soil aggregate stability of different species of Pinus yunnanensis in the karst mountain area of Eastern Yunnan Province was studied to provide a basis for soil cultivation, quality improvement, and soil-water conservation of karst fragile habitats.[Methods] Based on the field survey and laboratory analysis, five types of vegetation, namely P. yunnanensis pure forest, P. yunnanensis artificial mixed forest, P. yunnanensis natural mixed forest, shrub, and primeval forest, in the karst mountains of Eastern Yunnan Province were studied in terms of their characteristics of water-stable aggregate and organic carbon distribution in aggregate, which revealed the differences in the soil aggregate stability of different species of P. yunnanensis.[Results] ① The mass fraction of particle size <0.25 mm (5.77%~9.39%) of P. yunnanensis pure forest, artificial mixed forest, and natural mixed forest was significantly lower than that of shrub (20.92%) and primeval forest (27.47%) (p<0.05). The mass fraction of particle size >5 mm and 2~5 mm of artificial mixed forest and natural mixed forest was higher than that of pure forest. ② The proportion order of water-stable aggregate >0.25 mm (R0.25) after wet sieving treatment was P. yunnanensis artificial mixed forest > P. yunnanensis natural mixed forest > P. yunnanensis pure forest > shrub > primeval forest. The mean weight diameter order was P. yunnanensis artificial mixed forest > P. yunnanensis natural mixed forest > primeval forest > shrub > P. yunnanensis pure forest. The geometric mean diameter order was P. yunnanensis artificial mixed forest > P. yunnanensis natural mixed forest > primeval forest > P. yunnanensis pure forest > shrub. The fractal dimension order was primeval forest > shrub > P. yunnanensis pure forest > P. yunnanensis natural mixed forest > P. yunnanensis artificial mixed forest. ③ The contribution rate of large aggregates (>0.25 mm) of P. yunnanensis pure forest, P. yunnanensis artificial mixed forest, and P. yunnanensis natural mixed forest to soil organic carbon was higher than that of small aggregates (<0.25 mm), and the content of organic carbon in soil aggregates with particle sizes of 5, 2~5, and <0.25 mm was significantly lower than that of shrub and primeval forest (p<0.05).[Conclusion] P. yunnanensis artificial mixed forest was observed to have the maximum soil aggregate stability, and its nutrient accumulation and carbon sequestration were lower than those of shrub and primeval forest but higher than those of pure forest. When the P. yunnanensis artificial mixed forest was planted as the main vegetation type for soil and water conservation in this region, it was necessary to avoid human interference for the purpose of improvement of soil nutrients. %R 10.13961/j.cnki.stbctb.2020.03.014 %U http://stbctb.alljournal.com.cn/stbctb/home %1 JIS Version 3.0.0