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河西走廊不同土地利用方式下土壤团聚体组成与稳定性特征OA

Characteristics of soil aggregate composition and stability under different land-use types in the Hexi Corridor

中文摘要英文摘要

探究河西走廊不同土地利用方式下土壤团聚体的组成与稳定性特征,有助于揭示干旱区土壤结构对人为干扰的响应机制,为土壤质量评估与可持续管理提供科学依据.在河西走廊选取耕地、园地、林地和草地四种代表性土地利用方式,采集0~20 cm和20~40 cm土层的土壤样品,将土壤团聚体采用湿筛法分离为>2 mm、0.25~2 mm、0.053~0.25 mm、<0.053 mm 4个粒级,测定其质量分数,并计算几何平均直径(Geometric Mean Diameter,GMD)、平均重量直径(Mean Weight Diameter,MWD)、组分质量分数(R0.25)及大团聚体/微团聚体比值(AR),解析不同土地利用方式下土壤团聚体组成与稳定性特征及其影响因子.研究区各土地利用方式下土壤团聚体组成均以<0.053 mm粒级为主,其次为0.053~0.25 mm粒级,>2 mm和0.25~2 mm粒级占比相对较低.林地两个土层中>2 mm和0.25~2 mm粒级的质量分数均显著高于耕地和草地,而耕地、园地和草地各粒级团聚体的质量分数差异不显著.土壤团聚体稳定性总体按照林地>园地>耕地>草地的趋势递减.在0~20 cm土层,林地的团聚体稳定性显著高于其他三种土地利用类型;而在20~40 cm土层,林地的团聚体稳定性仍显著高于耕地和草地,但与园地差异不显著.此外,在同一土地利用类型下,两个土层间的团聚体稳定性不存在显著差异.相关性分析表明,河西走廊土壤团聚体稳定性与土壤pH值无显著相关性,但与土壤有机质含量和全氮含量呈显著的正相关.河西走廊林地的土壤团聚体稳定性显著高于耕地、园地和草地,土壤有机质与全氮的积累水平是影响该区域土壤团聚体形成与稳定性的关键因素.

An understanding of soil aggregate composition and stability under different land-use types in the Hexi Corridor can reveal how soil structure responds to anthropogenic disturbances in arid regions and provides a sci-entific basis for soil quality assessment and sustainable land management.Four representative land-use types in the Hexi Corridor were selected:cropland,orchard,forestland,and grassland.Soil samples were collected from the 0-20 and 20-40 cm depth intervals.Wet sieving was employed to separate soil aggregates into the following four size fractions:>2,0.25-2,0.053-0.25,and<0.053  mm.The mass proportions of each fraction were deter-mined,and aggregate stability indices were calculated,including mean weight diameter,geometric mean diame-ter,proportion of macroaggregates(R0.25),and the ratio of macroaggregates to microaggregates.Soil aggregate composition,stability,and their driving factors under different land-use types were analyzed.Across all land-use types in the study area,soil aggregates were dominated by the<0.053  mm fraction,followed by the 0.053-0.25  mm fraction;the>2 mm and 0.25-2  mm fractions constituted relatively lower proportions.The mass pro-portions of the>2  mm and 0.25-2  mm aggregates were significantly higher at both soil depths in forestland com-pared with cropland and grassland,whereas no significant differences were observed among cropland,orchard,and grassland.Generally,aggregate stability followed the pattern of forestland>orchard>cropland>grassland.In the 0-20  cm layer,forestland exhibited significantly greater stability than all other land-use types.In the 20-40  cm layer,forestland was significantly more stable than cropland and grassland but did not differ significantly from orchard.However,within each land-use type,aggregate stability did not vary significantly between the two depth intervals.Correlation analysis indicated that aggregate stability was unrelated to soil pH but was positively correlated with soil organic matter and total nitrogen content.Overall,forestland in the Hexi Corridor exhibits sig-nificantly higher soil aggregate stability than cropland,orchard,and grassland;this is primarily due to the accu-mulation of soil organic matter and total nitrogen,which are key determinants of aggregate formation and stabili-ty in this region.

张旭斌;张德明;白玲;莫玉娟;杨全;舒龙飞;陈天坤;马玉欣

中国地质调查局西宁自然资源综合调查中心,青海 西宁 810021中国地质调查局西宁自然资源综合调查中心,青海 西宁 810021中国地质调查局西宁自然资源综合调查中心,青海 西宁 810021中国地质调查局西宁自然资源综合调查中心,青海 西宁 810021中国地质调查局西宁自然资源综合调查中心,青海 西宁 810021中国地质调查局西宁自然资源综合调查中心,青海 西宁 810021中国地质调查局西宁自然资源综合调查中心,青海 西宁 810021中国地质调查局西宁自然资源综合调查中心,青海 西宁 810021

土壤团聚体土地利用河西走廊干旱区

soil aggregatesland-useHexi Corridorarid region

《干旱区研究》 2026 (5)

978-987,10

中国地质调查局调查项目"全国国土变更调查国家级外业核查(西宁中心)"(DD20230800309)

10.13866/j.azr.2026.05.08

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