OALib Journal期刊
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酸沉降对南亚热带森林土壤主要元素的影响
DOI: 10.3724/SP.J.1145.2013.00255, PP. 255-261
Keywords: 酸沉降,森林土壤,元素动态,亚热带
Abstract:
华南地区的酸沉降可能影响到森林土壤元素循环.采用模拟酸沉降控制实验,研究了鼎湖山自然保护区内不同演替阶段的3种森林土壤在受到酸沉降影响后,土壤ph值和交换性k+、na+、ca2+、mg2+、al3+、h+浓度的动态变化及其相关性.结果表明:3种森林土壤均属于强酸性土壤(ph<4.2),ph值随土层深度增加而上升;除马尾松林k+、na+,土壤交换性阳离子含量与土壤ph均呈显著(p<0.05)或极显著(p<0.01)负相关,其中mg2+的相关性程度及范围最好,其次为ca2+、al3+、k+、na+;3种森林土壤元素含量均表现为al3+>h+>ca2+>mg2+>k+、na+,且它们都是表层高于深层土壤.在混交林和季风林,酸沉降中h+的输入导致土壤铝被活化.3种森林土壤盐基离子(除混交林和季风林na+)含量都很低,尤其是k+、mg2+,最大值分别为0.74mmolkg-1、0.79mmolkg-1.在严重酸沉降影响下,应注意鼎湖山森林土壤是否会出现养分k、mg的缺乏.图3表3参40
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