基于改进的RCA水质模型对珠江口夏季缺氧及初级生产力的数值模拟研究

针对珠江口藻类生长受泥沙遮光限制明显的问题, 对RCA(row and column of Aesop)三维水质模型进行改进, 加入泥沙模块及悬沙遮光对藻类生长的限制作用。应用改进的RCA水质模型, 对珠江口的营养盐、浮游植物及溶解氧进行模拟研究, 结果显示, 改进的RCA水质模型较好地再现了洪季珠江口营养盐、浮游植物和溶解氧在水平及垂向上的空间分布, 这表明该水质模型能较好地反映珠江河口中生态因子的关键过程。珠江口的缺氧现象在物理和生化过程的共同作用下, 被限制在伶仃洋的西滩和中滩及磨刀门海域。在洪季, 大量冲淡水进入珠江口形成锋面, 颗粒态有机物(particulate organic matter, POM)在锋面的影响下, 大量集中沉降在伶仃洋的西滩及中滩特定区域及磨刀门外, 产生较高的底泥耗氧率(sediment oxygen demand, SOD)。而在高SOD的区域, 水体分层通常也较明显, 因而产生缺氧现象。另一方面, 伶仃洋水体中磷的限制作用明显, 加上悬浮泥沙的遮光作用, 不利于浮游植物生长, 使得初级生产力低; 而在陆架上, 悬沙浓度减少使初级生产力增加, 但由于海源颗粒有机碳(particulate organic carbon, POC)的沉积分散于整个陆架上, 无法产生伶仃洋内的高SOD区域, 加上水体分层不明显, 并没有产生缺氧现象。     

Seasonal variations of water system distribution and flow patterns in the southern sea area of Hokkaido,Japan

Hydrographic data and composite current velocity data (ADCP and GEK) were used to examine the seasonal variations of upper-ocean flow in the southern sea area of Hokkaido, which includes the “off-Doto” and “Hidaka Bay” areas separated by Cape Erimo. During the heating season (April–September), the outflow of the Tsugaru Warm Current (TWC) from the Tsugaru Strait first extends north-eastward, and then one branch of TWC turns to the west along the shelf slope after it approaches the Hidaka Shelf. The main flow of TWC evolves continuously, extending eastward as far as the area off Cape Erimo. In the late cooling season (January–March), part of the Oyashio enters Hidaka Bay along the shallower part of the shelf slope through the area off Cape Erimo, replacing almost all of the TWC water, and hence the TWC devolves. It is suggested that the bottom-controlled barotropic flow of the Oyashio, which may be caused by the small density difference between the Oyashio and the TWC waters and the southward migration of main front of TWC, permits the Oyashio water to intrude along the Hidaka shelf slope.     

流速对封闭循环水养殖大菱鲆生长、摄食及水质氮素的影响

在封闭循环水高密度养殖条件下(平均密度14.1 kg/m²±0.51 kg/m²), 设置4 个流速梯度(200, 400,600, 800 L/h,分别以A～D 组表示), 挑选相近体质量(200.3g±7.6 g)的大菱鲆进行42 d 养殖试验, 每个梯度设置3 个重复, 每个重复55 尾鱼, 研究流速对封闭循环水养殖大菱鲆生长、摄食以及水质氮素的影响。试验结果表明: (1) 大菱鲆(Scophthatmus maximus L)特定生长率、增质量率、摄食量随流速增大先快速上升后缓升趋稳, 饲料系数则相反。B、C、D 3 组特定生长率、摄食量分别显著高于A 组30.77%～52.31%、17.30%～22.05%; 饲料系数则显著低于A 组13.83%～22.34%; (2) 养殖水体中总氨氮、非离子氨及亚硝酸氮浓度随流速的增大先快速下降后缓降趋稳。B、C、D 3 组水质总氨氮氨浓度均显著低于A 组53.70%～79.07%; (3) 根据流速对特定生长率、水体总氨氮二者的影响, 得出养殖的生态适宜流速为625 L/h。再结合流速对水循环动力的影响, 得出养殖的生态经济适宜流速为480 L/h。