Y. H. Wang, C. Su, W. Huang, Y. Kuang, Y. D. Huang, W. L. Wu, C. Chu, Y. J. Chung
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The boundary of this inventory covers the water intake works, impoundment region, the dam, the affiliated hydroelectricity power plant, the administration center and other facilities. In this study, the floating chambers with gas chromatography (GC) were chosen to measure the GHG flux from the water body. For the emission of CH4 and N2O from the water body, there are no significantly difference between the fluxes during the daytime and nighttime. For Original Research Article British Journal of Environment & Climate Change, 4(1): 45-65, 2014 46 carbon dioxide, the instantaneous flux during the nighttime is higher than the daytime flux. The two reservoirs in tropical zone emit more CO2e from the water body than those in subtropical zone. Summarizing the direct and indirect GHG emission, for the four reservoirs, the annual emission quantities ranged from 653 ton of CO2e to 23,146 ton of CO2e. 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引用次数: 0
摘要
摘要本研究旨在评估台湾地区生活用水库原水的碳足迹。为台湾水库系统的温室气体排放提供了初步的测量方法和参考数据库。选取位于亚热带的飞穗(F.T.)和李玉滩(L.Y.T.)水库,以及位于热带的南华(N.H.)和曾文(T.W.)水库作为碳足迹调查的研究对象,包括水体和人类活动产生的温室气体排放。碳足迹清单遵循PAS 2050(2011年商品和服务生命周期温室气体排放评估规范)。水体温室气体排放遵循联合国教科文组织准则。本次清查的范围包括取水工程、蓄水区、坝体、所属水电站、管理中心等设施。本研究采用气相色谱(GC)浮室法测量水体温室气体通量。水体CH4和N2O的排放通量在白天和夜间没有显著差异。英国环境与气候变化学报,4(1):45-65,2014。两个热带水库的水体CO2e排放量高于亚热带水库。综合直接和间接温室气体排放,4个水库年排放总量为653 ~ 23146吨CO2e。家庭用水的碳足迹在0.002 ~ 0.028 kg CO2e/m之间。粗略估计,台湾24个主要水库的温室气体排放总量约为121800吨CO2e,年总出水量为43.5亿m,最高碳足迹为0.028 kg CO2e/m。
A Preliminary Estimation on Carbon Footprint of Raw Water from the Reservoirs for Domestic Use in Taiwan
This study aims to evaluate the carbon footprint of raw water from reservoirs for domestic use in Taiwan. It also provides a preliminary measure and reference database for greenhouse gas (GHG) emission of reservoir systems in Taiwan. Four reservoirs, Feitsui (F.T.) and Liyutan (L.Y.T.) in subtropical zone and Nanhua (N.H.) and Tsengwen (T.W.) in tropical zone, were selected as the cases to be examined for carbon footprint inventory, including the GHG emission from the water body and from human activities. Carbon footprint inventory followed PAS 2050 (2011 Specification for the assessment of the life cycle greenhouse gas emissions of goods and services). GHG emission from water body followed the instruction of UNESCO guidelines. The boundary of this inventory covers the water intake works, impoundment region, the dam, the affiliated hydroelectricity power plant, the administration center and other facilities. In this study, the floating chambers with gas chromatography (GC) were chosen to measure the GHG flux from the water body. For the emission of CH4 and N2O from the water body, there are no significantly difference between the fluxes during the daytime and nighttime. For Original Research Article British Journal of Environment & Climate Change, 4(1): 45-65, 2014 46 carbon dioxide, the instantaneous flux during the nighttime is higher than the daytime flux. The two reservoirs in tropical zone emit more CO2e from the water body than those in subtropical zone. Summarizing the direct and indirect GHG emission, for the four reservoirs, the annual emission quantities ranged from 653 ton of CO2e to 23,146 ton of CO2e. The carbon footprint of water supply for domestic use ranged from 0.002 kg CO2e/m to 0.028 kg CO2e/m. Roughly speaking, the total GHG emission quantity of the 24 main reservoirs in Taiwan was estimated to be around 121,800 ton of CO2e with the total yield of 4.35 billion m of water annually using the highest carbon footprint 0.028 kg CO2e/m.