Based on secular fixed_site data in the artificial sand_fixing vegetation district at the southeast fringe of the Tengger Desert, the formative characteristics of soil microbiotic crusts and its influences on vegetati...Based on secular fixed_site data in the artificial sand_fixing vegetation district at the southeast fringe of the Tengger Desert, the formative characteristics of soil microbiotic crusts and its influences on vegetation dynamics were analyzed. Once sand barrier and artificial vegetation have stabilized the surface of the sifting sand, could form aeolian deposition crust and then evolve into algae_dominated crust. Such processes result from the interactions of physical effects of atmospheric dust and silt deposition on sand surface, sinking and raindrop impact, and soil microorganism activities. Under the condition of less than 200 mm precipitation, the presence of microbiotic crust changes the soil hydraulic conductivity, alters the temporal and spatial distribution of the limited precipitation in sand layer and leads to the decline of deep_rooted shrubs. The development of microbiotic crust and subsurface soil affects the plant growth and seed rain distribution, as a result, the diversity of plant species gradually tend to become saturated and finally affects the vegetation stability.展开更多
陆地表面的腾发量分布具有很大的空间变异性,而传统方法只能进行点上的计算。为反映表面腾发量的空间特征,引入遥感技术和SEBAL(surface energy balance algorithm for land)模型。遥感技术能够方便、快捷地获取地面信息,而SEBAL模型则...陆地表面的腾发量分布具有很大的空间变异性,而传统方法只能进行点上的计算。为反映表面腾发量的空间特征,引入遥感技术和SEBAL(surface energy balance algorithm for land)模型。遥感技术能够方便、快捷地获取地面信息,而SEBAL模型则利用Landsat TM/ETM影像获取的遥感信息计算区域腾发量。该文在SEBAL模型的基础上,针对具体研究区域的客观情况进行参数改进,在ERDAS软件支持下,计算获得了研究区域地面反照率、地面温度以及各能量分量的空间分布。结果分析表明,参数改进后模型计算过程简捷,结果基本合理,具有广阔的应用前景,尤其对于缺乏观测资料的地区,更是一种行之有效的方法。展开更多
文摘Based on secular fixed_site data in the artificial sand_fixing vegetation district at the southeast fringe of the Tengger Desert, the formative characteristics of soil microbiotic crusts and its influences on vegetation dynamics were analyzed. Once sand barrier and artificial vegetation have stabilized the surface of the sifting sand, could form aeolian deposition crust and then evolve into algae_dominated crust. Such processes result from the interactions of physical effects of atmospheric dust and silt deposition on sand surface, sinking and raindrop impact, and soil microorganism activities. Under the condition of less than 200 mm precipitation, the presence of microbiotic crust changes the soil hydraulic conductivity, alters the temporal and spatial distribution of the limited precipitation in sand layer and leads to the decline of deep_rooted shrubs. The development of microbiotic crust and subsurface soil affects the plant growth and seed rain distribution, as a result, the diversity of plant species gradually tend to become saturated and finally affects the vegetation stability.
文摘陆地表面的腾发量分布具有很大的空间变异性,而传统方法只能进行点上的计算。为反映表面腾发量的空间特征,引入遥感技术和SEBAL(surface energy balance algorithm for land)模型。遥感技术能够方便、快捷地获取地面信息,而SEBAL模型则利用Landsat TM/ETM影像获取的遥感信息计算区域腾发量。该文在SEBAL模型的基础上,针对具体研究区域的客观情况进行参数改进,在ERDAS软件支持下,计算获得了研究区域地面反照率、地面温度以及各能量分量的空间分布。结果分析表明,参数改进后模型计算过程简捷,结果基本合理,具有广阔的应用前景,尤其对于缺乏观测资料的地区,更是一种行之有效的方法。
