在热带环境中回收有机废物产品

F. Feder
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引用次数: 1

摘要

有机废物被定义为农业中强调的有机性质和农业、城市或农业-工业来源的所有残留物。堆肥是一种转化有机物的好氧过程。厌氧消化(或甲烷化)也是有机物降解的一种生物过程,但发生在缺氧的情况下。有机废弃物输入后,土壤生物特性的变化主要体现在大型动物(膜翅目动物等)、微生物(细菌、真菌、藻类等)及其活动上。除了影响有机废物的实际肥料价值外,氨挥发导致的氮损失还有助于生态系统的富营养化和酸雨的形成。热带土壤有机质含量的持续下降主要与高温、高湿变化和土壤类型导致的土壤快速矿化有关。沙质土壤的养分保持能力和有机质积累能力较低,尤其脆弱。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Recycling Organic Waste Products in a Tropical Context
Organic waste products are defined as all residues of an organic nature and of agricultural, urban or agricultural‐industrial origin emphasized in agriculture. Composting is an aerobic process of transforming organic matter. Anaerobic digestion (or methanation) is also a biological process of degradation of organic matter, but which takes place in the absence of oxygen. Changes in the biological characteristics of soils, after the input of organic waste products, are revealed on macrofauna (hymenoptera, etc.), microorganisms (bacteria, fungi, algae, etc.) and their activities. Beyond affecting the actual fertilizer value of organic waste products, nitrogen losses through ammonia volatilization contribute to the eutrophication of ecosystems and the genesis of acid rain. The inexorable decline in the organic matter content of tropical soils is mainly linked to their rapid mineralization due to high temperature and humidity variations as well as soil types. Sandy soils, ferrasols, with low nutrient retention and organic matter accumulation capacities, are particularly vulnerable.
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