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Study of physico-chemical parameters of water in the Loukkos river estuary (Larache, Morocco)

机译:Loukkos河口(摩洛哥拉拉什)水的理化参数研究

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Background In the context of the knowledge of the functioning of estuaries and the evolution of abiotic factors on the basis of the marine dynamics, a study was conducted at the level of the Loukkos river estuary. Results Water samples were collected seasonally from March to September during 2006 in 5 stations, spread throughout the estuary. Monitoring of several parameters showed significant variations. Indeed, the temperature of water ranging from 19.20 at 29.70°C, the pH is alkaline fluctuating from 7.02 to 7.99, salinity reach 29.50mg/l, dissolved oxygen fluctuated between 2.17 and 12.33mg/l and conductivity which follows the profile of salinity indicating the degree of mineralization of mean ranging from 593 to 54700μs/cm. Conclusions This research reveals to identify a spatial and temporal functional dynamism of the study estuary denoting the existence of two gradients: the first, upstream downstream, very marked at high tide, linked to marine and ocean inflow hydrodynamics and the second that in relation to the upstream water intake is very marked at low tide.
机译:背景技术在了解河口功能和基于海洋动力学的非生物因子演变的背景下,在Loukkos河口一级进行了研究。结果2006年3月至9月,在5个站点中按季节收集了水样,分布在整个河口。监测几个参数显示出明显的变化。实际上,水的温度在29.70°C时为19.20,pH在7.02至7.99之间呈碱性波动,盐度达到29.50mg / l,溶解氧在2.17至12.33mg / l之间波动,并且电导率遵循盐度曲线平均矿化度范围为593至54700μs/ cm。结论本研究揭示了确定研究河口的时空动态性,表明存在两个梯度:第一个,上游下游,在涨潮时非常明显,与海洋和海洋流入水动力有关,第二个与退潮时上游取水口非常明显。

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