沾河干流水能開發(fā)工程地質條件分析
發(fā)布時間:2018-05-26 06:36
本文選題:沾河干流 + 水能開發(fā); 參考:《吉林大學》2014年碩士論文
【摘要】:水能是一種無污染、可再生、運行費用低的清潔能源。水能發(fā)電便于電力調峰,能夠提高資源利用率和經濟社會的綜合效益。面對地球傳統(tǒng)資源日益緊張趨勢,世界各國紛紛優(yōu)先選擇和大力開發(fā)利用水能資源。目前,水能發(fā)電作為電力行業(yè)中最重要的清潔能源和可再生能源之一,發(fā)展的潛力巨大。我國已探明的水能資源蘊藏量和可能開發(fā)的水能資源量都位居世界第一,也是目前世界上建設規(guī)模最大、水電裝機容量最多和發(fā)展速度最快的國家。 沾河海撥高程100m~700m,河流全長250km,流域面積6551km2,,水能開發(fā)潛力巨大。因此,有必要在沾河選擇建壩條件較好的河段建立水壩。 本文將針對沾河中游河段干流的水能開發(fā)進行規(guī)劃研究,主要開展三方面研究:一是沾河干流工程地質條件勘察與分析,規(guī)劃河段內出露的主要地層為古生界二迭系地層和中生界侏羅系地層及新生界第三系與第四系地層;侵入巖主要為華力西早期侵入巖和華力西晚期侵入巖及印支期侵入巖。二是沾河干流大壩施工用建筑材料勘查與分析,主要對各規(guī)劃梯級方案中水電站水庫區(qū)、壩址、引水建筑物、廠房等工程地質條件進行深入勘查和調研,對砂礫石料、土料等天然建筑材料的產地進行了普查,最后得出客觀合理的沾河中游河段干流各水電站區(qū)域的地質、地震、工程地質結論,為科學合理開發(fā)沾河干流水能提供可靠和寶貴的基礎資料。三是沾河干流水能開發(fā)方案選擇,擬定三個梯級開發(fā)方案,分別為二級開發(fā)方案、三級開發(fā)方案及四級開發(fā)方案。二級開發(fā)方案,由沾北水電站、新鄂水電站組成;三級開發(fā)方案,由沾北水電站、義氣敏水電站、新鄂水電站組成;四級開發(fā)方案,由都魯河口水電站、沾北水電站、義氣敏水電站、新鄂水電站組成。
[Abstract]:Water energy is a kind of clean energy without pollution, renewable and low operating cost. Water power generation is convenient for power peak adjustment. It can improve the utilization of resources and the comprehensive benefits of economy and society. In the face of the increasingly tense trend of the earth's traditional resources, all countries in the world have chosen and vigorously developed the resources of water energy. At present, the hydropower generation is used as the power industry. One of the most important clean and renewable energy sources has great potential for development. Our country's proven water resources and potential water resources are the first in the world, and the largest country in the world, with the largest capacity and the fastest development speed in the world.
Zhanhe sea allocates 100m ~ 700m, the total length of the river is 250km, the area of the river basin is 6551km2, and the potential of water energy development is great. Therefore, it is necessary to establish the dam in the river section with the better condition of selecting the dam in the river.
In this paper, the water energy development of the main stream in the middle reaches of Zhan He River will be studied in three aspects: first, the investigation and analysis of the geological conditions of the Zhan River main stream, the main strata exposed in the river section are the two superposition strata of the Paleozoic and the Mesozoic Jurassic strata and the third and Quaternary strata of the new birth boundary, and the intrusive rock owners. Two is the exploration and analysis of the construction materials for the construction of Zhan he main stream dam, and the geological conditions for the hydropower station reservoir area, the dam site, the diversion building, the factory building and other engineering geological conditions are carried out in depth. According to the survey of the producing area of the building materials, the objective and reasonable geological, earthquake, and engineering geological conclusions of the area of the main stream of the middle reaches of the river in the middle reaches of the river are obtained, which can provide the reliable and valuable basic data for the scientific and rational exploitation of the dry water of the river, three is the selection of the water energy development scheme of Zhan He River, and the three cascade development schemes are drawn up. Not for the two level development scheme, three level development scheme and four level development scheme. The two level development scheme is composed of die North hydropower station and new Hubei hydropower station; the three level development scheme is composed of die North hydropower station, Yi Qi Min hydropower station, and new Hubei hydropower station; the four level development scheme is made up of the Du Lu River mouth water power station, the Zhi Bei hydropower station, the Yi gas sensitive hydropower station, the new Hubei hydropower station. The station is made up.
【學位授予單位】:吉林大學
【學位級別】:碩士
【學位授予年份】:2014
【分類號】:TV221.2;TV72;P642
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