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Physico-Chemical Parameters Profile During Dry and Wet Seasons in Southern South China Sea: Brunei Bay

机译:南海南部干湿季期间的理化参数分布:文莱湾

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摘要

The physico-chemical parameters were assessed in the Brunei hay water column in order to provide scientific data on these parameters during the dry and wet seasons. The parameters measured were salinity, temperature, dissolved oxygen, pH and total suspended solids. The results showed that most of the parameters showed seasonal variations between the dry and wet seasons. Lower surface values of salinity, temperature, dissolved oxygen and pH were observed in the wet season and vice versa for total suspended solids. In addition, the vertical profiles between surface and bottom waters varied during the wet season and this was more noticeable for salinity and dissolved oxygen. Lower salinities were recorded in the surface water compared to bottom water due to the greater river discharge and rainfall. Decreasing of dissolved oxygen were observed in going from surface to bottom waters. Lower dissolved oxygen in bottom water might be mainly due to degradation of organic wastes and restricted current circulation. The results of this study provide helpful data that enables the decision makers to effectively manage activities in the bay.
机译:在文莱干草水柱中评估了理化参数,以便在干旱和潮湿季节提供有关这些参数的科学数据。测量的参数是盐度,温度,溶解氧,pH和总悬浮固体。结果表明,大多数参数显示出干燥季节和潮湿季节之间的季节性变化。在湿季观察到盐度,温度,溶解氧和pH值较低的表面,总悬浮固体反之亦然。此外,在湿季,地表水和底水之间的垂直剖面也有所不同,这对于盐度和溶解氧更为明显。由于河水流量和降雨增加,地表水中的盐度比底部水低。从地表水到底水时,观察到溶解氧的减少。底部水中溶解氧较低可能主要是由于有机废物的降解和电流流通受限。这项研究的结果提供了有用的数据,使决策者能够有效地管理海湾中的活动。

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