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应用分解网袋法对亚热带常绿阔叶林7种常见林冠树种落叶分解过程中矿质元素(K, Na, Ca, Mg, Al, Fe, Mn, Cu和Zn)动态变化进行了为期2年的研究.这些树种是研究地区森林植被的代表种,且不同树种的落叶化学组成差异明显.研究结果表明:落叶分解速率(落叶干重残留百分率和分解常数k)与矿质元素初始浓度之间没有明显的相关性.但是,大多数情况下,落叶干重残留百分率与残留落叶的矿质元素浓度之间有着显著的相关关系.落叶分解过程中不同矿质元素的迁移性大小依次为: Na = K > Mg ≥ Ca > N ≥ Mn ≥ Zn ≥ P > Cu >> Al >> Fe.各树种的K和Na浓度在分解中均表现为下降趋势,Ca和Mg浓度亦表现为下降趋势, 但在分解初期偶有升高倾向. 而各树种中的其它元素(Zn, Cu, Al, Fe)浓度在分解中都表现出升高趋势,唯有Mn例外,在不同树种间,其浓度的变化模式存在一定差异. 大多数树种的Cu,Al和Fe等3元素在分解试验末期的绝对重量均比初始重量显著提高,其机理在很大程度上可能归因于这些元素与腐殖质的结合,而不是生物固定.表2图1参40.“,”Dynamical patterns of mineral elements during decomposition processes were investigated for seven common canopy species in a subtropical evergreen broad-leaved forest by means of litterbag technique over 2 years. The species studied are representative for the vegetation in the study area and differed significantly in chemical qualities of their litter. No significant relationships were found between decomposition rate (percentage dry mass remaining and decomposition constant k) and initial element concentrations. However, there were significant correlations between the percentage of dry mass remaining and the mineral element concentrations in the remaining litter for most cases. The rank of the element mobility in decomposition process was as follows: Na = K > Mg ≧ Ca > N ≧ Mn ≧ Zn ≧ P > Cu >> Al >> Fe. Concentrations of K and Na decreased in all species as decomposition proceeded. Calcium and Mg also decreased in concentration but with a temporal increase in the initial phase of decomposition, while the concentrations of other elements (Zn, Cu, Al, and Fe) increased for all species with exception of Mn which revealed a different pattern in different species. In most species, microelements (Cu, Al, and Fe) significantly increased in absolute amounts at the end of the litterbag incubation, which could be ascribed to a large extent to the mechanism of abiotic fixation to humic substances rather than biological immobilization.