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Long-term changes in post-cooling water loads from power plants and thermal and oxygen conditions in stratified lakes

机译:发电厂的后冷却水负荷以及分层湖中的热和氧气条件的长期变化

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Trends in thermal and oxygen conditions were identified in three stratified lakes that are part of the cooling system of two Power Plants. The total water uptake and discharge by the power plants decreased from approximately 60.0 m-3s-1 in 1995-1999 to approximately 50.0 m-3s-1 in 2005-2010, while, simultaneously, the degree of water heating decreased. Changes in the hydrological conditions influenced an increase in the mean and maximum water retention times in the lakes. Decelerated water flow rates and lower inertia decreased the thickness of the epilimnion and water temperature and oxygen content in Lake Licheńskie, the shallowest of the lakes studied. Oxygen conditions deteriorated in the deeper, isolated waters of Lake ?lesińskie. The more advantageous morphometric conditions in Lake Mikorzyńskie contributed to improved oxygen conditions in the near-bottom water layer and decreased levels of oxygen deficits in the spring-summer period.
机译:在两个电厂冷却系统的三个分层湖泊中,确定了热和氧气条件的趋势。发电厂的总取水和取水量从1995-1999年的约60.0 m-3s-1下降到2005-2010年的约50.0 m-3s-1,同时,水的加热程度下降。水文条件的变化影响了湖泊中平均和最大保水时间的增加。水流速度的降低和惯性的降低降低了利琴斯基湖(最浅的湖泊)的lim水厚度以及水温和氧气含量。弗莱森斯基湖的较深的孤立水域中的氧气状况恶化。 Mikorzyńskie湖中更有利的形态学条件有助于改善近底部水层中的氧气状况,并减少春夏季的氧气不足水平。

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