| 土地利用变化对西南喀斯特土壤团聚体组成、稳定性以及C、N、P化学计量特征的影响 |
| 摘要点击 1899 全文点击 587 投稿时间：2021-09-23 修订日期：2021-11-17 |
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| 中文关键词 生态化学计量学 土壤团聚体 喀斯特 土地利用 稳定性 |
| 英文关键词 ecological stoichiometry soil aggregate Karst land use stability |
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| 中文摘要 |
| 土壤团聚体稳定性和养分化学计量特征对土地利用变化的响应研究，以及对当前脆弱生态环境保护与修复具有重要意义.为探明西南喀斯特山地土地利用方式变化对土壤团聚体组成、稳定性与C、N、P养分化学计量特征的影响规律，选取了西南喀斯特典型区域为研究区，针对7种主要土地利用方式建立了系列样地，开展了土壤团聚体组成与稳定性、团聚体C、N、P含量与计量比特征研究.结果表明，土地利用变化显著影响了土壤团聚体稳定性.玉米地和撂荒地的土壤团聚体稳定性相对较高，草地和裸地的团聚体稳定性相对较低，土壤团聚体稳定性总体随土层增加呈现降低趋势.不同土地利用方式土壤团聚体C、N和P含量存在显著差异.疏林地和撂荒地土壤团聚体C和N含量较高，草地土壤团聚体C和N含量较低，裸地和撂荒地土壤团聚体P含量相对较高.土地利用变化对土壤团聚体C、N和P计量比也存在明显影响.乔木林地、疏林地和撂荒地土壤团聚体C：N相对较高，草地土壤团聚体C：N最低；乔木林地和疏林地土壤团聚体C：P较高，明显高于其他土地利用方式；乔木林地、疏林地和灌木林地土壤团聚体N：P较高，明显高于裸地和撂荒地.喀斯特土壤团聚体组成和稳定性与土壤C、N和P化学计量特征存在显著或极显著的相关性.土壤团聚体稳定性与大团聚体所占质量分数呈正相关.土壤大团聚体质量分数增加，团聚体稳定性增加，有利于土壤C、N和P养分的保持和积累.研究结果对喀斯特生态系统植被修复、水土保持和土地利用调控具有重要意义. |
| 英文摘要 |
| Responses of soil aggregate stability and nutrient stoichiometry to land use change are of great significance to the protection and restoration of fragile ecosystems. In order to explore the influence of the law of land use change on soil aggregate stability and C, N, and P nutrient stoichiometric characteristics in the karst ecosystem of Southwest China, a typical region of the Southwest China Karst was selected as the study area. A series of sample plots were established for the seven typical land use types, and the constitution; stability; and C, N, and P contents and stoichiometric ratios of soil aggregates were studied. The results showed that land use change significantly affected the soil aggregate stability. The soil aggregate stability of corn fields and abandoned land was relatively high, whereas that of grassland and bare land was relatively low. The soil aggregate stability generally decreased with the increase in soil layer. There were significant differences in the C, N, and P contents of soil aggregates between different land use types. The C and N contents of soil aggregates of open woodland and abandoned land were higher, the C and N contents of grassland were lower, and the P contents of soil aggregates of bare land and abandoned land were relatively higher. Land use change also significantly affected the stoichiometric ratio of soil aggregate C, N, and P. The C:N of soil aggregates of arbor forest land, open forest land, and abandoned land was relatively high, and that of grassland was the lowest. The C:P of soil aggregates of arbor woodland and open woodland was higher than that in shrub woodland and grassland. The soil aggregate N:P of arbor forest land, open forest land, and shrub forest land was higher and was significantly higher than that of bare land and abandoned land. There were significant or extremely significant correlations between the constitution and stability of soil aggregates and the stoichiometric characteristics of soil aggregate C, N, and P. Soil aggregate stability was positively correlated with the mass fraction of large soil aggregates. The mass fraction of large soil aggregates increased, and the stability of aggregates correspondingly increased, which was conducive to the maintenance and accumulation of soil C, N, and P nutrients. These results are of great significance for vegetation restoration, soil and water conservation, and land use regulation in karst ecosystems of Southwest China. |
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