赵强, 曹维, 邢健, 龙绍桥. 基于现场观测数据的三门核电站冬季温排水时空特征分析[J]. 海洋环境科学, 2022, 41(6): 847-856. DOI: 10.12111/j.mes.2022-x-0074
引用本文: 赵强, 曹维, 邢健, 龙绍桥. 基于现场观测数据的三门核电站冬季温排水时空特征分析[J]. 海洋环境科学, 2022, 41(6): 847-856. DOI: 10.12111/j.mes.2022-x-0074
ZHAO Qiang, CAO Wei, XING Jian, LONG Shao-qiao. Spatio-temporal characteristics of thermal discharge from Sanmen Nuclear Power Plant in winter based on field observations[J]. Chinese Journal of MARINE ENVIRONMENTAL SCIENCE, 2022, 41(6): 847-856. DOI: 10.12111/j.mes.2022-x-0074
Citation: ZHAO Qiang, CAO Wei, XING Jian, LONG Shao-qiao. Spatio-temporal characteristics of thermal discharge from Sanmen Nuclear Power Plant in winter based on field observations[J]. Chinese Journal of MARINE ENVIRONMENTAL SCIENCE, 2022, 41(6): 847-856. DOI: 10.12111/j.mes.2022-x-0074

基于现场观测数据的三门核电站冬季温排水时空特征分析

Spatio-temporal characteristics of thermal discharge from Sanmen Nuclear Power Plant in winter based on field observations

  • 摘要: 基于2022年冬季三门湾海域20个定点站和2条走航测线的水温观测数据,分析了三门核电站冬季温排水的时空特征。受温排水影响,冬季观测海域表层水温通常为10 ℃~19 ℃。从垂向上看,位于排水口东侧的分层水温测站存在温度层化,表底温差平均值在大、小潮期间分别为0.16 ℃~1.21 ℃和0.51 ℃~2.37 ℃,小潮期间温度层化较强且持续时间较大潮期间长3~13 h;其余分层水温测站的水体总体呈混合均匀状态。涨急和涨憩时刻,温排水主要被限制在排水口外较小的区域,并向北经猫头水道进入蛇蟠水道;落急和落憩时刻,温排水则向南影响南部滩涂及其以东海域。以1 ℃温升为标准,涨潮时段温排水最远可影响到排水口西北约3 km处,落潮时段温排水最远可影响到排水口东南约5 km处。三门核电厂址以南各测站小潮期典型潮时水温通常比大潮期高0.5 ℃~5.0 ℃,说明三门核电站以南海域在小潮期受温排水的影响更大。

     

    Abstract: Based on the water temperature data from 20 fixed-point stations and 2 voyage lines in the Sanmen Bay in the winter of 2022, the spatio-temporal characteristics of thermal discharge from the Sanmen Nuclear Power Plant (SNPP) in winter are analyzed. Affacted by the thermal discharge, the SSTs of the observation area are usually in the range of 10 ℃ to 19 ℃. In vertical, water temperature is stratified at the station located on the east of the outlet, and the averaged differences of tempetature between surface and bottom are in the rage of 0.16 ℃ to 1.21 ℃ during the spring tide and 0.51 ℃ to 2.37 ℃ during the neap tide. At the other stations, the water is well mixed. At the time of flood peak tide and flood slack tide, thermal discharge is limited to a small area outside the outlet and is transported northward to the Shepan Waterway through the Maotou Waterway. While at the time of ebb peak tide and ebb slack tide, thermal discharge is transported southward to the tidal flats and their eastern area. Taking the temperature rise of 1 ℃ as the standard, the thermal discharge can affect about 3 km northwest of the outlet during the flood tide and about 5 km southeast of the outlet during the ebb tide. The difference of the water temperature at the north of the SNPP between the spring tide and the neap tide is usually 0 to 0.8 ℃, and the water temperature at the south of the SNPP is usually 0.5 ℃ to 5.0 ℃ higher during the neap tide than that during the spring tide, indicating that the water at the south of the SNPP is more affected by the thermal discharge during the neap tide.

     

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