于兵, 刘子洲, 翟方国, 顾艳镇, 吴文凡. 2020年夏季威海瑜泰海洋牧场底层海水溶解氧的日变化研究[J]. 海洋环境科学, 2022, 41(4): 563-571. DOI: 10.12111/j.mes.2021-x-0070
引用本文: 于兵, 刘子洲, 翟方国, 顾艳镇, 吴文凡. 2020年夏季威海瑜泰海洋牧场底层海水溶解氧的日变化研究[J]. 海洋环境科学, 2022, 41(4): 563-571. DOI: 10.12111/j.mes.2021-x-0070
YU Bing, LIU Zi-zhou, ZHAI Fang-guo, GU Yan-zhen, WU Wen-fan. Study on the diurnal variation in the bottom layer dissolved oxygen in Yutai Marine Ranch off Weihai in the summer of 2020[J]. Chinese Journal of MARINE ENVIRONMENTAL SCIENCE, 2022, 41(4): 563-571. DOI: 10.12111/j.mes.2021-x-0070
Citation: YU Bing, LIU Zi-zhou, ZHAI Fang-guo, GU Yan-zhen, WU Wen-fan. Study on the diurnal variation in the bottom layer dissolved oxygen in Yutai Marine Ranch off Weihai in the summer of 2020[J]. Chinese Journal of MARINE ENVIRONMENTAL SCIENCE, 2022, 41(4): 563-571. DOI: 10.12111/j.mes.2021-x-0070

2020年夏季威海瑜泰海洋牧场底层海水溶解氧的日变化研究

Study on the diurnal variation in the bottom layer dissolved oxygen in Yutai Marine Ranch off Weihai in the summer of 2020

  • 摘要: 利用2020年8月威海瑜泰海洋牧场获取的定点在线观测数据和大面航次观测数据,研究了夏季海洋牧场底层海水溶解氧的日变化特征,并探讨了其影响机制。结果表明,底层海水溶解氧浓度日变化的平均范围为4.02~4.45 mg/L,呈现单峰结构,溶解氧浓度逐时的月标准差则存在多个峰值,溶解氧浓度每日峰值出现的时刻随日期推移向后延迟,其中,浓度最大值多出现在12时;饱和溶解氧浓度主要受到温度的影响,其每日的变化幅度仅为溶解氧浓度的十分之一;表观耗氧量日变化平均值范围为2.75~3.21 mg/L,底层海水始终处于不饱和状态;溶解氧浓度的日变化并不受温度的直接控制,而潮汐引起的水面升降可能会改变到达底层水体的净太阳辐射的强度,从而通过控制光合作用的强弱来影响溶解氧浓度的日变化,此外,平流输运也会对溶解氧浓度的日变化产生影响。本文结果可为进一步研究海洋生态环境及其影响机理提供参考,具有较高的生态与经济价值。

     

    Abstract: Based on the real-time observation data obtained from Yutai Marine Ranch off Weihai in August 2020, as well as the cruise observations, the current study investigated the diurnal variation characteristics of dissolved oxygen (DO) in the bottom layer, with a discussion about its influencing factors. The result indicated that the average diurnal variation of DO concentration in the bottom layer ranged from 4.02 mg/L to 4.45 mg/L, presenting a unimodal structure, but the hourly monthly standard deviation of DO concentration had a few peaks. The everyday occurrence time of the peak of the DO concentration was delayed with the date and the maximum DO concentration mostly appeared at 12. The saturated DO concentration was mainly affected by temperature, and its amplitude of daily variation was only 1/10 of the DO concentration’s amplitude. The average diurnal variation of apparent oxygen utilization ranged from 2.75 mg/L to 3.21 mg/L, so the bottom layer was always in an unsaturated state. The diurnal variation of DO concentration wasn’t directly controlled by temperature. However, the rise and fall of sea surface caused by tide may change the intensity of net solar radiation reaching the bottom layer, so that the photosynthesis altered, and the diurnal variation of DO concentration varied. Moreover, the advection transport also had an impact on the diurnal variation of the DO concentration. The result of this paper can provide a reference for further research on the marine ecological environment and its influence mechanism, which features higher ecological and economic worth.

     

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