分层湖库温跃层溶解氧极值现象研究进展
A Review of Metalimnetic Dissolved Oxygen Maximum and Minimum in Stratified Lakes and Reservoirs
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摘要: 分层湖库温跃层溶解氧(DO)极值现象包括温跃层DO极大和温跃层DO极小(metalimnetic dissolved oxygen minima, MOM)两类。通过系统调研国内外文献,详细梳理了温跃层DO极值现象的形成原因、形成过程、研究方法及其对环境造成的影响;从形成因素、研究方法、湖库形态、生化过程和物理过程等方面比较分析了温跃层DO极大和温跃层DO极小现象的异同点;归纳出MOM的6方面成因:浮游生物呼吸耗氧、有机物分解耗氧、边坡沉积物耗氧、DO垂向输移、温跃层或温跃层下部取水、混合层或滞温层人工增氧。基于当前研究进展,认为研究方法上应强化三维水动力-生物化学耦合数学模型的应用,研究内容上应进一步从多维度(垂向和水平)研究分层湖库DO动力学过程,探究气候变化、极端天气对DO分层结构的影响。Abstract: The extreme values of dissolved oxygen (DO) in thermocline include metalimnetic dissolved oxygen maximum and metalimnetic dissolved oxygen minimum (MOM) in stratified lakes and reservoirs. On the basis of systematic investigation of domestic and foreign literatures, the formation causes, formation process, research methods and its impact on the environment of metalimnetic DO maximum and minimum are reviewed; Their similarities and differences from the aspects of formation factors, research methods, lake morphology, biological process and physical process are compared and analyzed. Six causes of MOM are summarized : plankton respiration consumption, organic matter decomposition oxygen consumption, side-slope sediment oxygen consumption, DO vertical transport, water intake from thermocline and its lower position, artificial oxygenation in epilimnetic and hypolimnetic. In conclusion, the application of three dimensional hydrodynamic-biochemical coupling mathematical model should be strengthened in the research methods. In terms of research content, the DO dynamics process of stratified lakes and reservoirs should be further studied from multi-dimensional (vertical and horizontal), and explore the impacts of climate change and extreme weather on DO structure.
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