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机构地区:[1]北京林业大学林学院,北京100083 [2]中国环境科学研究院,北京100012
出 处:《草地学报》2014年第6期1222-1226,共5页Acta Agrestia Sinica
基 金:中央高校基本科研业务费专项资金(BLX2012037)资助
摘 要:利用非线性回归的生态界面测试分析法(BEDA),对华北农牧交错带农田-草地景观土壤的速效氮界面在生长季(5-9月)的时空动态进行分析,为干旱、半干旱地区以植被恢复为主的大规模生态环境建设提供参考。结果表明:农田-草地边界的土壤速效氮生态界面位于草地内。在少雨的5月,农田-草地的边界影响域最小,仅为37.5m;而在雨水较为丰沛的8月,边界影响域最大,为57.5m。相对于少雨期,丰雨期的速效氮生态界面会更靠近草地内部。速效氮素在农田-草地界面上表现出地表生态流季节动态性。In order to provide reference to the vegetation restoration of large scale ecological construction in the arid and semi-arid area,the spatial and temporal variability of soil available nitrogen border at the grassland-farmland ecotone were analyzed by the method of a border-and-ecotone detection analysis (BEDA) based on non-linear regression analysis.The study was located in a mosaic of anthropogenic deciduous grasslands and farmland in the agro-pastoral transition of North China from the dry period (May) to rainy period (September) of 2012.The results showed that the minimum DEI towards the grassland interior was 37.5 m in the dry period (May).The maximum DEI of 57.5 m occurred in the rainy period (August).The amount of precipitation affected the simple diffusion process of available nitrogen,which represented the seasonal dynamics of ecological flows between grassland and farmland.
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