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Properties of soils in the rehabilitated degraded tropical lowland and hill dipterocarp forests in Peninsular Malaysia

机译:半岛马来西亚恢复石斛土壤土壤的性质

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A study was conducted to characterize the soil properties of two rehabilitated major forest types in Peninsular Malaysia, representing lowland and hill dipterocarp forests located at Bidor and Kinta Forest Reserves, respectively. Twelve soil profileswere dug both in rehabilitated lowland and hill dipterocarp forests including two profiles in natural forest as the control were selected at each site. The significant effect of rehabilitation forests could be seen by the accumulation of organic matter in the uppermost layer, which was assumed to be at an intermediate stage of mineralization. The soils at both sites were acidic, having low activity clay resulting in low CEC, available P, total nitrogen and exchangeable bases, but high in exchangeable Al. High exchangeable Al was the main cause of soil acidity, associated with high rainfall in the humid tropical region. The main source of negative charge was the organic matter, which affect the CEC, PZSE and siga_p values which influence the soil fertility status. The soils are considered as strongly weathered, almost devoid of 2:1 type clay minerals. Kaolinite and gibbsite dominate the clay fraction of the soils at both sites. It is imperative that soil properties should be taken into consideration during rehabilitation of degraded forestland in tropical rainforests.
机译:进行研究在马来西亚半岛表征2种平反主要森林类型的土壤特性,代表位于美罗和近打森林资源低地和山森林龙脑香分别。十二土壤profileswere在恢复低地和山森林龙脑香,包括天然林两个配置文件都挖作为对照,在每个站点选择。康复森林的显著效应可被有机物质在最上面的层,其被假定为在矿化的中间阶段的积累可以看出。两个站点的土壤是酸性的,具有交换性Al导致低CEC低活性粘土,可用P,总氮和可交换的碱,但高。高交换性铝是土壤酸度的主要原因,在潮湿的热带地区强降雨有关。负电荷的主要来源是有机物质,从而影响其影响土壤肥力状态的CEC,PZSE和siga_p值。土壤被认为是强风化,几乎不含2:1型粘土矿物。高岭石,三水铝石支配在两个站点的土壤粘土部分。当务之急是,土壤性质应在热带雨林退化林地康复过程中加以考虑。

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