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首页> 外文期刊>Research journal of forestry >Leaf Litter Decomposition Pattern in Dipterocarpus tuberculatus and Dipterocarpus retusus Forests of North East India
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Leaf Litter Decomposition Pattern in Dipterocarpus tuberculatus and Dipterocarpus retusus Forests of North East India

机译:印度东北部Dipterocarpus tuberculatus和Dipterocarpus retusus森林的叶片凋落物分解模式

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Soil is the major reservoir of C in the terrestrial environment and always under dynamic equilibrium due to various bio-geochemical processes active soil development. Litter accumulate forest floor and slowly decompose by the microbial activity to release the nutrients into the surrounding environment. Carbon dioxide is released from the soil to the atmosphere in heterotrophic respiration when the dead organic matter is used for substrates for soil micro-organisms and soil animals. The climatic factors such as rainfall, temperature and seasonal variation s directly influence the occurrence and abundance of microbes that results in the variation of rate of leaf litter decomposition. This work was focused on variation in the rate of leaf litter decomposition in different seasons of the year of two plant species: Dipterocarpus tuberculatus and Dipterocarpus retusus at two different sites and seasonal variation in the microfungal quantity of the decomposed leaf litter was also enumerated. The results revealed a similar trend for the rate of decomposition for both species and a significant correlation between the abiotic factors and leaf litter decomposition.
机译:土壤是陆地环境中碳的主要储集层,由于各种生物地球化学过程,土壤始终活跃于土壤的动态平衡之下。垃圾堆积在森林地面,并由于微生物活动而缓慢分解,从而将养分释放到周围环境中。当死有机物质用作土壤微生物和土壤动物的基质时,二氧化碳会通过异养呼吸从土壤释放到大气中。降雨,温度和季节变化等气候因素直接影响微生物的发生和数量,从而导致凋落物分解速率的变化。这项工作的重点是两种植物物种一年中不同季节的凋落物分解速率的变化,这两个植物是在两个不同的位置上生长的枯萎病和枯萎病,并且还列举了分解后的凋落物的微真菌数量的季节性变化。结果揭示了两种物种分解速率的趋势相似,并且非生物因子与凋落物分解之间存在显着相关性。

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