首页> 外文会议>International Peat Congress; 20040606-11; Tampere(FI) >NUTRIENT DYNAMICS IN DIFFERENT SUB-TYPES OF OMBROTROPHIC PEAT SWAMP FOREST IN CENTRAL KALIMANTAN, INDONESIA
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NUTRIENT DYNAMICS IN DIFFERENT SUB-TYPES OF OMBROTROPHIC PEAT SWAMP FOREST IN CENTRAL KALIMANTAN, INDONESIA

机译:印度尼西亚中部加里曼丹市不同种类的富营养性泥炭沼泽森林的营养动态

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摘要

Peat swamp forests of Southeast Asia are ombrotrophic ecosystems in which the only input of water and nutrients is from atmospheric deposition and precipitation while outputs are by mass flow of surface drainage water. Internal nutrient transfers are mostly related to maintenance of the forest biomass through gravitational influence (throughflow, stemflow and litterfall) and recycling (decomposition and uptake), and to storage in or release from the surface peat (accumulation or degradation). Comparing of the nutrient dynamics of two subtypes of tropical peat swamp forest, mixed swamp forest and low pole forest shows that nutrient inputs were higher than nutrient losses during a 1-year study period with the greatest nutrient gain for Ca while Mn was the lowest in both sub-types of forest. It is essential that the surplus of nutrients is being stored in currently accumulating peat.
机译:东南亚的泥炭沼泽森林是非营养型生态系统,其中水和养分的唯一输入来自大气层的沉积和降水,而输出则是来自地表排水水的质量流量。内部养分的转移主要与重力影响(通流,茎流和凋落物)和循环利用(分解和吸收)对森林生物量的维持,以及与表层泥炭的存储或释放有关(积累或降解)。比较热带泥炭沼泽森林,混合沼泽森林和低极森林这两种亚型的养分动态,发现在一年的研究期内,养分输入高于养分流失,其中钙的养分吸收最大,而锰在养分吸收最低。两种子类型的森林。必须将多余的营养物存储在当前积累的泥炭中。

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