Greenhouse Gas Diffusive Flux Assessment from Few Indian Reservoirs

G. Anvesh, C. Giriprasad, M. Rafi
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Abstract

There is a growing interest and concern regarding Green House Gas (GHG) emissions as these is the major contributors of global warming. Carbon dioxide (CO2) and Methane (CH4) are two main GHGs which get emitted from both natural aquatic and terrestrial ecosystems as well as from anthropogenic activities. In natural aquatic system water storage is an important aspect for meeting the requirements of drinking water, food, and energy. However, development of such water bodies will impact the environment. Recent studies have shown that water bodies play a significant role as the sources of GHG emission, particularly in tropical climatic zones. One possible reason for this is the annual water temperature is much higher in tropical climates. This means that the rate of decomposition is faster leading to higher CO2 and CH4 flux in the water. Indian reservoirs indicate the complete spectrum of different types of reservoir found in the world. Their performance in terms of emission of GHGs is more difficult to trace out. In this paper pathways of GHG emission from a reservoir have been discussed and a tool as suggested by UNESCO/IHA has been used to assess the GHG emission from four existing reservoirs in India. These reservoirs are of different age and are located in different parts and climatic zones of India. Predicted diffusive fluxes in CO2eq have been estimated for the year 2013 as well as over the 100 years of their existence in terms of Tonnes CO2 eq.
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几个印度储层的温室气体扩散通量评估
温室气体(GHG)排放是全球变暖的主要原因,人们对它的兴趣和关注日益增加。二氧化碳(CO2)和甲烷(CH4)是自然水生和陆地生态系统以及人类活动排放的两种主要温室气体。在天然水生系统中,储水是满足饮用水、食物和能源需求的一个重要方面。然而,这些水体的开发会对环境造成影响。最近的研究表明,水体作为温室气体排放源发挥着重要作用,特别是在热带气候带。一个可能的原因是热带地区的年水温要高得多。这意味着分解速度更快,导致水中CO2和CH4通量更高。印度的水库显示了世界上发现的各种不同类型的水库的完整谱。它们在温室气体排放方面的表现更难以追踪。本文讨论了一个水库的温室气体排放途径,并使用教科文组织/印度水文研究所建议的一种工具来评估印度四个现有水库的温室气体排放。这些水库年龄不同,位于印度不同的地区和气候带。以CO2当量吨为单位估算了2013年的CO2当量预测扩散通量以及它们存在的100年内的扩散通量。
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