天然林土壤有机碳及矿化特征研究

通过野外调查和室内分析培养,研究了马尾松林、常绿阔叶林、落叶阔叶林、针阔混交林、红松林和油松林这6种天然林林下土壤有机碳含量及有机碳矿化特征.结果表明,林下土壤有机碳含量都表现出随土壤深度增加而逐渐降低的趋势;双指数方程可以很好拟合出天然林土壤有机碳的矿化过程,准确反映出各天然林土壤的矿化反应特征.天然林各层土壤矿化反应趋势相同,但强度各异.其中,红松林0~10 cm土壤反应强度最为强烈,其下各层土壤的矿化反应强度也显著高于其他天然林的同层土壤;对落叶阔叶林和针阔混交林土壤矿化特征比较发现,凋落物种类差异对土壤活性有机碳含量产生较强烈影响,因此呈现出不同的矿化反应特征.

Organic Carbon and Carbon Mineralization Characteristics in Nature Forestry Soil

Through field investigation and indoor analysis, the organic carbon content and organic carbon mineralization characteristics of six kinds of natural forest soil were studied, including the pine forests, evergreen broad-leaved forest, deciduous broad-leaved forest, mixed needle leaf and Korean pine and Chinese pine forest. The results showed that the organic carbon content in the forest soil showed trends of gradual decrease with the increase of soil depth; Double exponential equation fitted well with the organic carbon mineralization process in natural forest soil, accurately reflecting the mineralization reaction characteristics of the natural forest soil. Natural forest soil in each layer had the same mineralization reaction trend, but different intensity. Among them, the reaction intensity in the 0-10 cm soil of the Korean pine forest was the highest, and the intensities of mineralization reaction in its lower layers were also significantly higher than those in the same layers of other natural forest soil; comparison of soil mineralization characteristics of the deciduous broad-leaved forest and coniferous and broad-leaved mixed forest found that the differences of litter species had a relatively strong impact on the active organic carbon content in soil, leading to different characteristics of mineralization reaction.