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以１９８７年５—６月中日台作黄东海域综合调查的溶解氧资料为主，探讨调查海区溶解氧分布特征与水团的对应关系。指出：近岸水团溶解氧合量高，远海低；上层水团高，下层低。在黄海冷水和东海北部底层冷水的上界出现明显的溶解氧垂直分布最大值及封闭形高氧区。水团边界区，氧跃层明显。溶解氧含量变化与水团温盐特性有关。通过分析发现，溶解氧对鉴别次表层以深各水团，特别对鉴别东海次表层水及黑潮次表层以深各水团，可作为一种有效的指标。
Taking the dissolved oxygen data collected by the Central China, Japan and Taiwan for the Huangdong Sea area from May to June 1987 as the main method, the corresponding relationship between the distribution of dissolved oxygen and the water mass in the sea area was investigated. It is pointed out that the near-shore water mass has high dissolved oxygen content and low sea level. The upper water mass is high and the lower is low. In the upper reaches of the cold water in the Yellow Sea and the northern part of the East China Sea, the maximum vertical distribution of dissolved oxygen and the closed-shaped high-oxygen zone were observed. Water mass boundary area, oxygenated layer obvious. Dissolved oxygen content and water temperature and salt characteristics. Through the analysis, it is found that dissolved oxygen can be used as an effective indicator for identifying deep sub-surface water masses, especially for identifying the deep sub-surface water of the East China Sea sub-surface water and the Kuroshio.