中非大西洋沿岸喀麦隆河口Wouri-Nkam段水文参数的时空变化

F. Besack, Ebonji Seth Rodrigue, Ajonina Gordon Nwutih, Edikin Roland Dieudonné, Sone Essoh Willy, Nguekeu Brice, Mbang Essome Junior, Hamadou Toume Michel-Remi, O. Raphael, T. Minette
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引用次数: 1

摘要

本研究旨在为可持续管理计划提供有关Wouri Nkam河口河口连续体水文参数动态的相关知识。根据人口密度和人类活动,在11个站点记录了水文参数。使用多个参数收集地下水中的水质参数(温度、盐度、溶解氧、pH、总溶解溶质、氧化还原电位和电导率)。使用漂流器、声纳深度和GPS记录表面洋流和形态测量(深度和宽度)参数。实地测量于2019年5月18日至2020年9月8日进行,分为六(06)次巡航。随后使用XLSTAT 2017(2.7版本)软件对数据进行方差分析(ANOVA)和主成分分析。结果表明,在湿润期,在相对较低的温度(25.5°C-27°C)下,水质参数在空间上更稳定,但不显著(df=9,p 0.05)。在干旱期、春季和洪水潮条件的快照期间,锋面区的界限延伸至S5(Bonalokan,距离S1 8.25km)。相反,在雨季,这一延伸减少到S1(大桥),在本季的小潮和退潮期间,相对略微增加到S3(博南港)。这一结果表明,在季节和潮汐尺度(月球和昼夜周期)期间,轴向梯度分别变化了约八(08)公里和四(04)公里。这些变化还伴随着水质特征的变化,这可能会影响渔业的分布和组成。然而,为了支持这项调查的结果,未来的研究应该集中在更长的时间序列采样方法和模型开发上。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Spatial and Temporal Variation of the Hydrological Parameters in the Wouri-Nkam Section of the Cameroon Estuary, Central African Atlantic Coast
This study aimed to provide relevant knowledge about the dynamics of the hydrological parameters in the river-estuary continuum of the Wouri-Nkam river estuary for a sustainable management program. The hydrological parameters were recorded in eleven stations spanned out on the basis of population density and human activities. Water quality parameters (Temperature, salinity, dissolved oxygen, pH, Total dissolved solutes, Redox potential and conductivity) were collected in subsurface water using a multiple parameter. Surface currents and morphometric (depth and width) parameters were recorded using a drifter, sonar depth and GPS. The field measurements took placed between 18/05/2019 to 08/09/2020 and were divided into six (06) cruises. The data were later subjected to an analysis of variance (ANOVA) and Principle Component Analysis using XLSTAT 2017 (2.7 version) software. Results obtained revealed that, the water quality parameters were spatially more stable notsignficant at (df = 9, p 0.05) with a relatively low temperature (25.5°C - 27°C) during the wet period. The limit of the frontal zone extended to S5 (Bonalokan, 8.25 km from S1) during the snapshot of the dry period, spring phase and flood tide conditions. Inversely, during wet period, this extension reduced to S1 (Bridge) and relatively increases slightly to S3 (Bonangang) during the neap phase and ebb tides of this season. This result revealed a change in the axial gradient of about eight (08) and four (04) kilometers during the seasonal and tidal scales (lunar and diurnal periods) respectively. These changes were also accompanied by changes in the water quality signatures, that may affect the fishery distribution and compositions. However, futures studies to buttress the results of this investigation should focus on longer time series sampling methods and model developments.
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