贵州喀斯特山区人工草地-农田景观土壤温度界面季节性变化  

Seasonal variation of the edge influence of soil temperature on cultivated grassland-cropland boundaries in Karst areas of Guizhou Province

作　　者：郝俊[1] 陈超[1] 王建立[1] 杨丰[1] 刘洪来[1] 

机构地区：[1]贵州大学动物科学学院,贵阳550025

出　　处：《生态学报》2017年第11期3816-3823,共8页Acta Ecologica Sinica

基　　金：国家自然科学基金项目(31560670;31101751);贵州省科技厅项目(黔科合NY字[2012]3011号)

摘　　要：景观界面是生态交错区的重要组成部分,在生态系统的结构、过程和功能中发挥了重要的作用。以贵州喀斯特山区人工草地-农田景观界面为研究对象,对界面表层土壤(0—20 cm)温度进行季节性监测;采用移动窗口法、野外测定和室内统计相结合,对以土壤温度为参数的界面宽度的大小进行了判定;对研究区3个功能区土壤温度进行比较分析。结果表明:贵州人工草地-农田景观界面四季表层土壤的平均温度分别为9.8,26.5,15.4℃和4.8℃;人工草地-农田景观春、夏、秋、冬四季土壤温度界面宽度随土壤温度的变化而变化,表现为由宽变窄的变化规律,分别为37,32,27 m和24 m,土壤温度界面在人工草地系统的影响域变化与总界面宽度保持一致。研究区四季农田功能区系统、人工草地-农田复合功能区系统和人工草地功能区系统的平均土壤温度为14.0,14.1℃和13.9℃,春季、夏季和冬季研究区3个功能区的土壤温度均呈极显著差异,秋季农田功能区系统与人工草地-农田复合功能区系统的土壤温度差异不显著,二者与草地功能区系统差异极显著。建议对研究区采用12—18 m的宽度进行草田间作,为丰富界面理论及"退耕还草"工程提供理论参考和实践措施。The landscape boundary is a transition zone between two or more adjacent ecosystems, or an interface that exists between an organism and abiotic environment; it is also extremely sensitive to climate change and human interference, and plays an essential role in the structure, processes, and functions of ecosystems. Soil temperature affects vegetation growth, and plays an important role in environmental microclimates and plant production, and affects various chemical reactions of soil organic matter and nitrogen accumulation; therefore, it affects plant growth, seed germination, and crop output. Cultivated grassland-cropland boundaries （Maiping County, Guiyang） in Karst areas of Guizhou Province were analyzed, and the surface soil temperature （0-20 cm） of the interface was monitored seasonally. Moving-split window technology （MSWT） was used to compute the variables in adjacent samples along transect data, which was a simple and reliable method for determining the boundary, and MSWT could be used for any type of variable reaction. The width of the cultivated grassland-cropland boundary was determined based on soil temperature by combining the field measurement, indoor statistics, and MSWT in this study. The soil temperature of three functional areas in the study area was compared and analyzed. The results showed that the average annual soil temperature of the cultivated grassland-cropland boundary in Guizhou was 9.8, 26.5, 15.4, and 4.8℃ for spring, summer, autumn, and winter, respectively. The width variation of the soil temperature boundary in cultivated grassland-cropland varied with seasonal shifts and soil temperature, from wide to narrow： 37, 32, 27, and 24 m in spring, summer, autumn, and winter, respectively. This also indicated that the soil temperature-interface width in cultivated grassland systems varied consistently with the total width of the cultivated grassland-cropland boundary, which was categorized as a gradual changing boundary type. The average soil temperature of the cropland f

关 键 词：土壤温度 界面宽度 人工草地-农田界面 季节变化 

分 类 号：S812[农业科学—草业科学]