期刊文献+

千岛湖水体稳定度和热分层结构对溶解氧垂向分布的影响

Effects of water stability and thermal stratification on the vertical distribution of dissolved oxygen at Lake Qiandao
下载PDF
导出
摘要 基于2017年1月—2020年2月千岛湖大坝前水质高频监测数据与湖心区气象数据,使用Lake Analyzer(LA)软件计算了水体稳定度指标(“施密特稳定度”和“浮力频率”)和热分层指标(“温跃层深度”和“温跃层厚度”),并与溶解氧垂向分布指标(“氧跃层深度”和“氧跃层强度”)结合分析。结果表明千岛湖存在时间长且稳定的热力分层和溶解氧分层,分层期为每年4—12月,根据结构变化可分为形成期(4—6月)、稳定期(7—9月)和减弱期(10—12月)三个阶段。水体稳定度指标、热分层指标和溶解氧垂向分布指标间相关分析结果表明:水体混合状态是影响溶解氧垂向分布的重要因素,湖体存在热分层则是氧跃层出现的根本原因,水体稳定度升高与热分层结构形成均阻碍溶解氧的垂向交换,促进氧跃层的形成。基于回归分析,发现温跃层深度与氧跃层深度具有良好的线性关系,拟合精度高(R^(2)=0.81,N=25),说明在千岛湖可通过温跃层深度推断氧跃层态势。研究结果同时证明LA在千岛湖的可适用性,以及在其它湖泊的可推广性,提供了水体稳定度和热分层指标定量化计算的工具。 To provide substantial information of vertical distribution of dissolved oxygen(DO)at Lake Qiandao,oxycline depth(OD)and oxycline intensity(OI)were defined and calculated for January 2017 to February 2020.Lake Analyzer(LA)was used to calculate Schmidt Stability(St),Buoyancy frequency(N_(2)),thermocline depth(thermD)and thermocline thickness(thermT)based on the high-frequency monitoring water quality(WQ)data and the meteorological data at Lake Qiandao for the same period.The results demonstrated that there were long-lasting thermal stratification and DO stratification from April to December through the year.Thermal stratifications showed obvious seasonality with stratifications initially formed during April-June,strengthened during July-September,and weakened during October-December.According to Spearman correlation analysis among the parameters for water stability,thermal stratification and vertical DO distribution,water stability was a key factor for vertical DO distribution,and the thermal stratification was a key factor for oxycline formation.Intensive thermal stratification decreased vertical DO exchange between the upper and lower layers,and promoted the oxycline formation.ThermD and OD was closely correlated with R^(2) of 0.81(N=25).Successful application of LA to Lake Qiandao showed that LA was a reliable and adaptive tool for quantitatively estimating the parameters for thermal and oxycline stratifications and water stability not only for Lake Qiandao but also for other lakes.
作者 张如枫 兰佳 王裕成 满小明 吴松涛 吴志旭 李慧赟 罗潋葱 李加龙 龚发露 殷鑫星 孙婷 ZHANG Rufeng;LAN Jia;WANG Yucheng;MAN Xiaoming;WU Songtao;WU Zhixu;LI Huiyun;LUO Liancong;LI Jialong;GONG Falu;YIN Xinxing;SUN Ting(Institute for International Rivers and Eco-security,Yunnan University,Kunming 650500,China;Chun’an Branch of Hangzhou Bureau of Ecology and Environment,Hangzhou 311700,China;Potevio Information Technology Co.,Ltd.,Beijing 100086,China;Pujiang Meteorology Bureau,Jinhua 322200,China;Nanjing Institute of Geography and Limnology,Chinese Academy of Sciences,Nanjing 210008,China;Institute for Ecological Research and Pollution Control of Plateau Lakes,School of Ecology and Environmental Sciences,Yunnan University,Kunming 650500,China)
出处 《生态科学》 CSCD 北大核心 2024年第1期160-169,共10页 Ecological Science
基金 云南大学人才引进启动项目(C176220100043) 国家自然科学基金(NSFC-41671205)。
关键词 水体稳定度 热分层 溶解氧 氧跃层 Lake Analyzer 千岛湖 water stability thermal stratification dissolved oxygen oxycline Lake Analyzer Lake Qiandao
  • 相关文献

参考文献33

二级参考文献484

共引文献752

相关作者

内容加载中请稍等...

相关机构

内容加载中请稍等...

相关主题

内容加载中请稍等...

浏览历史

内容加载中请稍等...
;
使用帮助 返回顶部