State of Surface and Vertical Salinity in Puttalam Lagoon during North-East Monsoon

Perera H.A.S.D, Jayathilake R.M.
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Abstract

Puttalam Lagoon which covers 226 km2 located in Sri Lanka‘s Northwest coast, plays an important role in aquaculture and lagoon capture fisheries. Kala oya and Mee oya are the major freshwater sources which empties into the Lagoon by eastern bank. Salinity variability is an important environmental variable in lagoon system that has an impact on aquaculture and aquatic resources. During the Northeast monsoon (NEM) in 2021, the spatial and vertical fluctuation of salinity in the lagoon was studied using SBE 19plus V2 CTD profiler. Field measurements show that the vertical salinity stratification in the lagoon was substantial during the study period. The lagoon has a significant spatial variability of salinity, ranging from 15 psu to 26 psu and Kala Oya river mouth has a salinity of 22 psu which impacted by freshwater and sea water circulation. The Salinity stratification in eastern section of the lagoon where the Kala Oya and Mee Oya streamflow reach is observed with surface salinity of 15 psu. During the NEM season, the average discharge of Kala Oya and Mee Oya to the lagoon was 10.8 m3/s and 9.4 m3/s, respectively, with a mean monthly precipitation of 48.89 mm. Fresh water from the Kala and Mee oya rivers flows into the lagoon during the season, while low evaporation and significant rainfall led the salinity to decline during the wet season, influencing the structure and function of lagoon ecosystems. The study reveals that a significant area of the lagoon is covered by the 20-30 psu salinity range, which is more appropriate for brackish water fisheries, particularly for shrimp and prawns during NEM.  Keywords: Salinity, CTD profiling, Northeast Monsoon, Freshwater 
东北季风期间普特拉姆泻湖的地表和垂直盐度状况
普塔兰泻湖位于斯里兰卡西北海岸,面积 226 平方公里,在水产养殖和泻湖捕捞渔业中发挥着重要作用。Kala oya 和 Mee oya 是淡水的主要来源,淡水从东岸流入泻湖。盐度变化是泻湖系统中的一个重要环境变量,对水产养殖和水产资源有影响。在 2021 年东北季风(NEM)期间,使用 SBE 19plus V2 CTD 剖面仪研究了泻湖盐度的空间和垂直波动。实地测量结果表明,在研究期间,泻湖的垂直盐度分层现象严重。泻湖盐度的空间变化很大,从 15 psu 到 26 psu 不等,卡拉奥亚河口的盐度为 22 psu,受到淡水和海水循环的影响。在 Kala Oya 和 Mee Oya 溪流流经的泻湖东段,观察到盐度分层现象,表层盐度为 15 psu。在 NEM 季节,Kala Oya 和 Mee Oya 流向泻湖的平均排水量分别为每秒 10.8 立方米和 9.4 立方米,月平均降水量为 48.89 毫米。季节性淡水从 Kala Oya 和 Mee oya 河流入泻湖,而低蒸发量和大量降雨导致盐度在雨季下降,从而影响泻湖生态系统的结构和功能。研究表明,泻湖的相当大面积被 20-30 psu 的盐度范围所覆盖,而这一盐度范围更适合咸水渔业,尤其是对虾和对虾的近海捕捞。 关键词盐度 CTD 分析 东北季风 淡水
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