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从大坝实现生态系统安全的水电。

Realizing ecosystem-safe hydropower from dams.

作者信息

Ahmad Shahryar Khalique, Hossain Faisal

机构信息

Dept. of Civil and Environmental Engineering, Univ. of Washington, More Hall 201, Seattle, WA 98195 USA.

出版信息

Renew Wind Water Sol. 2020;7(1):2. doi: 10.1186/s40807-020-00060-9. Epub 2020 Jun 1.

DOI:10.1186/s40807-020-00060-9
PMID:32647609
原文链接:https://pmc.ncbi.nlm.nih.gov/articles/PMC7325499/
Abstract

For clean hydropower generation while sustaining ecosystems, minimizing harmful impacts and balancing multiple water needs is an integral component. One particularly harmful effect not managed explicitly by hydropower operations is thermal destabilization of downstream waters. To demonstrate that the thermal destabilization by hydropower dams can be managed while maximizing energy production, we modelled thermal change in downstream waters as a function of decision variables for hydropower operation (reservoir level, powered/spillway release, storage), forecast reservoir inflow and air temperature for a dam site with in situ thermal measurements. For data-limited regions, remote sensing-based temperature estimation algorithm was established using thermal infrared band of Landsat ETM+ over multiple dams. The model for water temperature change was used to impose additional constraints of tolerable downstream cooling or warming (1-6 °C of change) on multi-objective optimization to maximize hydropower. A reservoir release policy adaptive to thermally optimum levels for aquatic species was derived. The novel concept was implemented for Detroit dam in Oregon (USA). Resulting benefits to hydropower generation strongly correlated with allowable flexibility in temperature constraints. Wet years were able to satisfy stringent temperature constraints and produce substantial hydropower benefits, while dry years, in contrast, were challenging to adhere to the upstream thermal regime.

摘要

为了在维持生态系统的同时实现清洁水电发电,将有害影响降至最低并平衡多种用水需求是一个不可或缺的组成部分。水电运营未明确管理的一种特别有害的影响是下游水域的热不稳定。为了证明在最大化能源生产的同时可以管理水电大坝造成的热不稳定,我们将下游水域的热变化建模为水电运营决策变量(水库水位、发电/溢洪道泄流量、蓄水量)、预测的水库入库流量以及具有现场热测量数据的大坝站点的气温的函数。对于数据有限的地区,利用陆地卫星增强型专题绘图仪(Landsat ETM+)的热红外波段,在多个大坝上建立了基于遥感的温度估算算法。水温变化模型被用于在多目标优化中施加可容忍的下游冷却或升温(变化1 - 6摄氏度)的额外约束,以最大化水电产量。得出了一种适应水生物种热最佳水平的水库泄流政策。这一新颖概念在美国俄勒冈州的底特律大坝得到了实施。水电发电所产生的效益与温度约束下的允许灵活性密切相关。湿润年份能够满足严格的温度约束并产生可观的水电效益,而相比之下,干旱年份则难以维持上游的热状况。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/f294/7325499/37c6894e6152/40807_2020_60_Fig13_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/f294/7325499/ca042ffa0a22/40807_2020_60_Fig1_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/f294/7325499/83dd51b29c36/40807_2020_60_Fig2_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/f294/7325499/1264b1d5f476/40807_2020_60_Fig3_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/f294/7325499/aa847af4be62/40807_2020_60_Fig4_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/f294/7325499/6b9bec2fb3a7/40807_2020_60_Fig5_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/f294/7325499/6597c157a109/40807_2020_60_Fig6_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/f294/7325499/6902cf402823/40807_2020_60_Fig7_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/f294/7325499/024a5fe36cfa/40807_2020_60_Fig8a_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/f294/7325499/caa8d9ed4fbd/40807_2020_60_Fig9_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/f294/7325499/c1de465e4c67/40807_2020_60_Fig10_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/f294/7325499/e14e8bdde5e3/40807_2020_60_Fig11a_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/f294/7325499/750ed17c5c93/40807_2020_60_Fig12_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/f294/7325499/37c6894e6152/40807_2020_60_Fig13_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/f294/7325499/ca042ffa0a22/40807_2020_60_Fig1_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/f294/7325499/83dd51b29c36/40807_2020_60_Fig2_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/f294/7325499/1264b1d5f476/40807_2020_60_Fig3_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/f294/7325499/aa847af4be62/40807_2020_60_Fig4_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/f294/7325499/6b9bec2fb3a7/40807_2020_60_Fig5_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/f294/7325499/6597c157a109/40807_2020_60_Fig6_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/f294/7325499/6902cf402823/40807_2020_60_Fig7_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/f294/7325499/024a5fe36cfa/40807_2020_60_Fig8a_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/f294/7325499/caa8d9ed4fbd/40807_2020_60_Fig9_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/f294/7325499/c1de465e4c67/40807_2020_60_Fig10_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/f294/7325499/e14e8bdde5e3/40807_2020_60_Fig11a_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/f294/7325499/750ed17c5c93/40807_2020_60_Fig12_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/f294/7325499/37c6894e6152/40807_2020_60_Fig13_HTML.jpg

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