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Development of a Three-Layer Steady State Vertical Dissolved Oxygen Model in Grand Lake, Oklahoma
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作者 Josephus F. Borsuah Scott Stoodley +2 位作者 Daniel Storm Andrew Dzialowski Andrew Stoddard 《Natural Resources》 2018年第12期448-467,共20页
Grand Lake O’The Cherokees, the third largest reservoir located in northeastern Oklahoma, provides recreational services, water supply, hydroelectric power, and flood control to residents of Oklahoma and neighboring ... Grand Lake O’The Cherokees, the third largest reservoir located in northeastern Oklahoma, provides recreational services, water supply, hydroelectric power, and flood control to residents of Oklahoma and neighboring states. Grand Lake has experienced major problems?with eutrophication, harmful algal blooms, and dissolved oxygen (DO) depletion during summer. To better understand the dynamics of DO depletion in the hypolimnion of Grand Lake, a three-layer steady state vertical DO model for summer-stratified conditions was used to investigate dissolved oxygen profiles both above and below the thermocline. The DO model was used to determine the relative effects of atmospheric reaeration and phytoplankton production as a source of DO and phytoplankton respiration, decomposition of organic matter, and nitrification as loss terms for DO. Additionally, the importance of sediment oxygen demand (SOD) for hypolimnetic oxygen depletion was investigated at the sediment water-interface under stratified conditions. Observed water quality data, kinetic coefficients from the literature, and physical, biological, and chemical data collected throughout 2013 and 2015 along the spatial gradient of riverine, transition, lacustrine zones and a site close to the Grand Lake Pensacola Dam were used?in the pre-processing calculations to derive estimates of kinetic rates as input parameters to the model. The estimated predictions from the model showed reasonable agreement with the observed vertical profiles of DO. Conclusions from this study indicate that phytoplankton production, high light limitation, and phosphorus were the major terms that controlled DO production in the surface layer, while nitrification and organic carbon decomposition were the major sinks of DO consumption in the bottom layer. Interestingly, SOD did not play a significant role in DO depletion in the water column. 展开更多
关键词 EUTROPHICATION DO Depletion Primary Production MODEL NUTRIENTS Reservoir hypolimnion Central PLAINS
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分层型水库夏季水质对极端厄尔尼诺事件的响应 被引量:3
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作者 邱晓鹏 黄廷林 +2 位作者 曾明正 史建超 曹占辉 《环境科学》 EI CAS CSCD 北大核心 2017年第2期547-554,共8页
为探究极端厄尔尼诺事件对分层型水库夏季水质的影响,分别于正常年(2012年)和厄尔尼诺年(2015年)的5~8月对枣庄周村水库主库区和入库径流的物理和化学指标进行了监测.结果表明,周村水库正常年夏季降雨量明显高于厄尔尼诺年夏季;正常年... 为探究极端厄尔尼诺事件对分层型水库夏季水质的影响,分别于正常年(2012年)和厄尔尼诺年(2015年)的5~8月对枣庄周村水库主库区和入库径流的物理和化学指标进行了监测.结果表明,周村水库正常年夏季降雨量明显高于厄尔尼诺年夏季;正常年夏季水位由124.26 m上升至127.14 m,恒温层厚度增加3.1 m;而厄尔尼诺年夏季水位由121.65 m下降至119.46 m,恒温层厚度减少3.2 m.周村水库入库径流属表层流,其营养盐浓度明显高于库区变温层.正常年夏季外源营养盐的汇入导致库区变温层总氮由1.00 mg·L^(-1)升至2.60 mg·L^(-1),硝态氮由0.19 mg·L^(-1)升至1.28 mg·L^(-1),总磷由0.023mg·L^(-1)升至0.088 mg·L^(-1),而厄尔尼诺年夏季库区变温层营养盐浓度变化不大.厄尔尼诺年夏季恒温层水体还原性污染物浓度明显高于正常年同期水平,其中铁、锰、氨氮和硫化物浓度的最大值分别为0.38、1.36、2.36和1.67 mg·L^(-1),均超过地表水Ⅲ类水质标准.极端厄尔尼诺事件对周村水库夏季变温层水体营养盐浓度和恒温层水体污染物浓度均有较大的影响. 展开更多
关键词 分层 厄尔尼诺 营养盐 恒温层 温跃层
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抽水蓄能电站水库水温简化模型与应用 被引量:3
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作者 孙伟 何蕴龙 +1 位作者 赵鑫 张怀芝 《武汉大学学报(工学版)》 CAS CSCD 北大核心 2013年第4期449-457,共9页
抽水蓄能电站由于其特殊的运行方式,水库水温分布规律与常规电站水库不同.目前有关研究不多,而建立合适的抽水蓄能电站水库水温分布模型,对于确定大坝温度边界条件具有重要意义.采用类比库途径,根据类比库水温实测资料和呼和浩特抽水蓄... 抽水蓄能电站由于其特殊的运行方式,水库水温分布规律与常规电站水库不同.目前有关研究不多,而建立合适的抽水蓄能电站水库水温分布模型,对于确定大坝温度边界条件具有重要意义.采用类比库途径,根据类比库水温实测资料和呼和浩特抽水蓄能电站的特点,对朱伯芳法经验公式进行改进,提出可用于预测严寒地区抽水蓄能电站水库水温分布的简化模型.用简化模型对呼和浩特抽水蓄能电站下水库水温分布进行预测,并将结果作为温度边界条件,计算大坝稳定温度场.结果表明在水气交替范围内,大坝表面温度均匀分布,大坝全断面稳定温度均在10℃以下,符合严寒地区大坝稳定温度场分布规律. 展开更多
关键词 抽水蓄能电站 水温 简化模型 温水层 深水层 温跃层
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