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首页> 外文期刊>Geologica Carpathica >Application of grain-size trend analysis and spatio-temporal changes of sedimentation, as a tool for lagoon management. Case study: the Kotychi lagoon (western Greece)
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Application of grain-size trend analysis and spatio-temporal changes of sedimentation, as a tool for lagoon management. Case study: the Kotychi lagoon (western Greece)

机译:运用粒度趋势分析和沉积物的时空变化作为泻湖管理的工具。案例研究:Kotychi泻湖(希腊西部)

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摘要

The Kotychi lagoon is located on the northwest Peloponnese Greece, along a wave dominated and microtidalcoast. The lagoon is one of the most important ecological areas in Greece, with international significance as it is protectedby the Ramsar International Convention and is listing in the Natura (E.C.) Catalogue. For the present study 59 surficialsamples were collected from the bottom of the lagoon, on a grid basis (approximately 300 m spacing) using a grab andwere analysed for their grain size distribution as well as grain size parameters, mean, variance and skewness. Using themoment measures, grain-size trend analysis was made and the definition of trend vectors were estimated. Grain-size trendanalysis indicates that the sediments of the lagoon are mainly sandy mud. Application of trend analysis indicates that thesediment pathways along the lagoon can be related to a) the sediments source area of the lagoon (small river supplies), b)wind related water circulation and c) the NW and SW wind directions. Moreover, comparing 1990 and 2000 satelliteimages we have detected three major areas where the shallow waters show a significant increase: area (a) in the northeastpart of the lagoon, area (b) in the middle-west part and area (c) in the southern part. All these changes are related to riverdischarges and to the winnowing effect. Detection of changes in the coastline of the lagoon, showed a total reduction ofareas covered by water by up to 13.8 %. The biggest change was detected in the northeast and in the southeast area of thelagoon and is related to the sediment supply from the periphery of the lagoon and to a minor degree to the bottom sedimentpathway and winnowing effect. The rate of change of the area covered by water shows a rapid filling up of the lagoon andthat additional measures have to applied forthe protection of the lagoon ecosystem.
机译:科蒂奇泻湖位于希腊伯罗奔尼撒西北部,沿波为主的微潮海岸。泻湖是希腊最重要的生态区之一,具有国际意义,因为它受到《拉姆萨尔国际公约》的保护,并被列入《自然法典》(Natura(E.C.)Catalogue)。在本研究中,使用抓斗从网格的底部(大约300 m的间隔)上,从泻湖底部收集了59个表面样本,并对其粒度分布以及粒度参数,均值,方差和偏度进行了分析。使用矩量度法,进行了晶粒尺寸趋势分析,并估计了趋势矢量的定义。粒度趋势分析表明,泻湖的沉积物主要是沙泥。趋势分析的应用表明,沿泻湖的这些泥沙通道可能与a)泻湖的沉积物源区(小河流供应),b)与风有关的水循环以及c)西北风和西南风的方向有关。此外,通过比较1990年和2000年的卫星图像,我们发现了浅水显着增加的三个主要区域:泻湖东北部的区域(a),中西部地区的区域(b)和西部地区的区域(c)。南部。所有这些变化与河水流量和风选效果有关。对泻湖海岸线变化的检测表明,被水覆盖的区域总共减少了多达13.8%。在泻湖的东北和东南地区发现了最大的变化,这与泻湖外围的沉积物供应有关,而对底部沉积物通道和风吹作用的影响较小。被水覆盖的区域的变化率表明泻湖正在迅速填满,必须采取其他措施来保护泻湖的生态系统。

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