A Review of Greenhouse Gas Emissions by Hydropower Reservoirs

Marco Aurélio Dos Santos
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Abstract

Hydroelectric reservoirs have environmental impacts as many other sources of energy. Regarding hydropower, these effects include flooding cultivated and forest areas, changes in water quality, negative impacts on water biodiversity, conflict with indigenous people and fish migration. In the nineties, researchers put in evidence of another important impact of dam construction: the greenhouse gases generated by flooding organic matter by reservoir flooding. Scientists argue that like natural human water bodies, the hydropower reservoirs emit biogenic gases into the atmosphere. The diffusive gas flux is associated with the difference between gas partial pressure of each chemical substance considering the aquatic system and the atmosphere. Ebullition is a process where some chemical substances are not soluble in water and bubbles are formed in the sediment at the bottom of the reservoir. Ebullition is often the dominant pathway of CH4 that is released from aquatic ecosystems. The phenomenon is episodic and irregular and depends mainly on hydrostatic pressure and other physical influences, such as currents, temperature gradients and the bathymetry of the water body. At hydropower reservoirs, other pathways for gas emanation to the atmosphere are the degassing by water passing through turbines of the powerhouse and the gas diffusion across the river downstream dam. This paper gives a review of the state-of-the-art and advances in the research of greenhouse gas emissions and removals from hydropower reservoirs.
水电水库温室气体排放研究进展
水电水库和许多其他能源一样对环境有影响。就水电而言,这些影响包括耕地和林区的洪水、水质的变化、对水生物多样性的负面影响、与土著居民的冲突以及鱼类洄游。在90年代,研究人员提出了大坝建设的另一个重要影响的证据:水库洪水淹没有机物产生的温室气体。科学家认为,就像人类的天然水体一样,水电站水库也会向大气中排放生物气体。考虑到水生系统和大气,扩散的气体通量与每种化学物质的气体分压之差有关。沸腾是指一些化学物质不溶于水,在水库底部的沉积物中形成气泡的过程。沸腾通常是水生生态系统释放CH4的主要途径。这种现象是间歇性和不规则的,主要取决于静水压力和其他物理影响,如水流、温度梯度和水体的水深。在水电站水库,气体向大气排放的其他途径是水通过电站涡轮机的脱气和气体通过下游大坝的扩散。本文综述了水电水库温室气体排放与清除研究的现状和进展。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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