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Forest vegetation as related to climate and soil conditions at varying altitudes on a humid subtropical mountain, Mount Emei, Sichuan, China

机译:四川峨眉山亚热带湿润山区海拔高度与森林植被相关的气候和土壤条件

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摘要

Altitudinal variations in temperature and soils were analysed on a humid subtropical mountain, Mt Emei (3,099 m a.s.l., 29°34.5′N, 103°21.5′E), in Sichuan, China, to see how the vegetation varies with the environmental factors. As a principal rinding, the coldest mean monthly temperature — 1℃, rather than the warmth index of 85℃·months, emerged as the primary factor that delimited the evergreen broadleaved forest. With regard to soils, properties such as organic C, total N, available P, exchangeable K tended to increase with altitude. The highest values in organic C (26.6%), total N (1.34%) and available P (45.39 ppm) were recorded in surface soils of the mixed forest (2,210 m a.s.l.) including all three tree life forms, i.e. evergreen/deciduous broad-leaved and coniferous trees. The high pH and contents of exchangeable Ca and Mg in the surface soils derived from the parent material, limestone and dolomite, between 900 and 1,200 m, where several Tertiary tree species existed. The C/N ratios of surface soils in the coniferous forests (2,500-3,099 m) were higher than those of the evergreen broadleaved forests (600-1,500 m) and the mixed forests (1,500-2,500 m).
机译:在中国四川湿润的亚热带山峨眉山(3,099 m a.s.l.,29°34.5′N,103°21.5′E)上分析了温度和土壤的垂直变化,以了解植被如何随环境因素变化。作为主要的浸水处理,最冷的平均月气温为1℃,而不是85℃·月的保暖指数,成为界定常绿阔叶林的主要因素。关于土壤,诸如有机碳,总氮,有效磷,可交换钾等特性往往随海拔升高而增加。在混合森林(2,210 m asl)的表层土壤(包括所有三种树的生命形式,即常绿/落叶阔叶林)中,有机碳(26.6%),总氮(1.34%)和有效磷(45.39 ppm)的最高记录。叶和针叶树。源于母体材料石灰岩和白云石的表层土壤的高pH值和可交换的Ca和Mg含量在900至1,200 m之间,那里存在多种第三纪树种。针叶林表层土壤的C / N比(2,500-3,099 m)高于常绿阔叶林(600-1,500 m)和混交林(1,500-2,500 m)。

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