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Balance of emissions with greenhouse effect in silvopastoral systems in three life zones of Costa Rica

机译:哥斯达黎加三寿命区硅桥系统的温室效应排放平衡

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The greenhouse effect is the result of the gases accumulation in the atmosphere, mainly carbon dioxide (CO_2), methane (CBU) and nitrous oxide (N_2O), that they increase annually 0.5, 0.6 and 0.35% respectively. Approximately 30% of these gases take place for the change in the use of the soil. It is considered that the tropics emit of 10 to 30 million of carbon (C) year~(-1) as a result of decreasing of the organic matter in the soils deforested (Detwiller and Hall 1988). In this sense, the soils with pastures play a very important roll for the great extension that they cover, for the retention and reduction of the emission of C to the atmosphere (Minarni et al. 1993, Fischer et al. 1994).
机译:温室效应是气体在大气中的气体积累,主要是二氧化碳(CO_2),甲烷(CBU)和氧化二氮(N_2O)的结果,即它们每年增加0.5,0.6和0.35%。大约30%的气体发生用于使用土壤的变化。据认为,由于土壤中的有机物(Detwiller和1988年)的有机物降低,热带热带碳(C)年份(C)年(-1)发出10%至3000万碳(C)年。从这个意义上讲,牧场的土壤对于它们覆盖的巨大延伸来说,造成非常重要的卷,以便保留和减少C到大气的发射(Minarni等,1993,Fischer等,1994)。

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