首页> 中文期刊> 《海洋与湖沼》 >沙海蜇(Nemopilema nomurai)消亡过程中海水溶解氧变化的模拟研究

沙海蜇(Nemopilema nomurai)消亡过程中海水溶解氧变化的模拟研究

         

摘要

To understand the influence of the decaying process after a large jellyfish bloom on marine environment, laboratory simulation experiments were performed to study the variations of dissolved oxygen (DO) during the decompo- sition process of Nemopilema nomurai at different temperature, pH, salinity, and N/P ratios. The results suggested that the decomposition ofN. nomurai needed a great deal of oxygen, and the extents of DO decrease were not significantly differ- ent under different temperature, pH, salinity, and N/P ratio conditions. Complete decomposition of N. nomurai generally took about 6--7 days and more time was needed under high N/P conditions. The decomposition of N. nomurai caused se- vere hypoxia of the seawater and the oxygen concentration was below 20% of saturation. Oxygen consumption in the simulation experiments dramatically increased from the second day to the third day and it peaked on the sixth or the sev- enth day. However, the high DO consumption rates under different N/P conditions appeared in the second day and contin- ued to the seventh day. Different temperature, salinity, pH and N/P ratios in the seawaters caused variations in the extents of DO consumption during the decomposition process. The extents of DO consumption were in the order of temperature (23--30℃) 〉 pH (5.0--9.0) 〉 salinity (21--33) 〉 N/P ratio (16:1--240:1), and the values of 39.9, 39.7, 38.0, and 35.9 mg/(kg·d), respectively. Consequently, the influence of temperature and pH on the DO consumption was more significant and the influence of N/P ratio and salinity was relatively small.%采用实验室模拟的方法,研究了不同海水温度、盐度、pH、N/P比下,沙海蜇消亡过程中海水溶解氧的变化特征,这对探讨水母灾害性暴发后消亡的环境影响有重要的科学意义。研究结果表明,沙海蜇的消亡可引起海水溶解氧浓度的显著降低,不同海水温度、盐度、pH、N/P比条件下沙海蜇消亡引起的海水溶解氧浓度的降低无显著差异,但与没有沙海蜇消亡时,海水溶解氧的变化相比则差异显著。沙海蜇消亡一般需要6—7天时间,在高N/P比的海水中,沙海蜇的消亡时间延长。沙海蜇的消亡造成水体的严重缺氧,水体氧饱和度低于20%,从第2天到第3天,本底海水、不同过程温度、盐度、pH条件下,消耗水体氧的量剧增,第6天达到峰值,但不同N/P比条件下,水体溶解氧的降低在第2天即可达到一个耗氧的高值,一直持续到第7天出现峰值;海水温度、盐度、pH、N/P比变化,可导致沙海蜇的消亡过程中水体氧消耗量的变化,就这四种影响因素而言,其平均最大耗氧量从大到小的顺序是:温度(23—30℃区间段)〉pH(5.0—9.0区间段)〉盐度(21~33区间段)〉N/P比(16:1—240:1区间段),分别为39.9、39.7、38.0和35.9mg/(kg·d),相对而言,水体温度和pH对沙海蜇消亡过程中氧消耗量影响较大,水体N/P比和盐度影响较小。所以,沙海蜇消亡过程中,由于海水温度和pH的变化形成的低氧区更为严重,而且在当今富营养化(高N/P比)的近海水域中,水母的消亡高耗氧的时间加长,对海水环境造成的影响更为严重。

著录项

  • 来源
    《海洋与湖沼》 |2012年第3期|502-506|共5页
  • 作者单位

    中国科学院海洋研究所海洋生态与环境科学重点实验室,青岛266071;

    中国科学院海洋研究所海洋生态与环境科学重点实验室,青岛266071 中国科学院研究生院,北京100049;

    中国科学院海洋研究所海洋生态与环境科学重点实验室,青岛266071;

    中国科学院海洋研究所海洋生态与环境科学重点实验室,青岛266071;

    中国科学院海洋研究所海洋生态与环境科学重点实验室,青岛266071;

    中国科学院海洋研究所海洋生态与环境科学重点实验室,青岛266071;

    中国科学院海洋研究所海洋生态与环境科学重点实验室,青岛266071 中国科学院研究生院,北京100049;

  • 原文格式 PDF
  • 正文语种 chi
  • 中图分类 水生生物生态学;
  • 关键词

    溶解氧; 环境影响; 消亡过程; 沙海蜇; 模拟研究;

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