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首页> 外文期刊>Continental Shelf Research: A Companion Journal to Deep-Sea Research and Progress in Oceanography >Automated detection of sedimentary features using wavelet analysis and neural networks on single beam echosounder data: A case study from the Venice Lagoon, Italy
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Automated detection of sedimentary features using wavelet analysis and neural networks on single beam echosounder data: A case study from the Venice Lagoon, Italy

机译:使用小波分析和神经网络对单波束回波测深仪数据进行沉积特征自动检测:以意大利威尼斯泻湖为例

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摘要

Acoustic methods are well established and widely used for the exploration of the seafloor and the sub-bottom sediments. However, the mapping and reconstruction of the sedimentary features revealed by acoustics can require a very long time because often large acoustic datasets need to be described and interpreted. To reduce the time of the geophysical visual interpretation, we implemented a new procedure for facies classification based on wavelet analysis and neural networks applied to the acoustic profiles. The optimized algorithm applied to a data set of the very shallow Lagoon of Venice classifies automatically the echo shape parameters to identify and map the main lagoon sedimentary features, such as palaeochannels and palaeosurfaces. The classification algorithm contains a set of wavelet transformation parameters as inputs to a neural network analysis based on the self-organizing map (SOM). The analysis was applied on 580. km of acoustic profiles acquired in a very shallow (less than 1. m) and turbid area of the lagoon with a sub-bottom penetration of about 6-7. m under the bottom. Without any special pre-requirement on the data, the algorithm was successfully tested against the results of the visual interpretation and allowed an automated and more efficient full 2D mapping of the sedimentary features of the area. We could distinguish and map different types of palaeochannels, buried creeks, palaeosurfaces as well as areas characterized by homogeneous mudflat facies. The results were validated by comparison with 5 cores sampled in the survey area corresponding with the main sedimentary features revealed by the acoustics.
机译:完善的声学方法已广泛用于海底和地下沉积物的勘探。但是,由于常常需要描述和解释大型声学数据集,因此通过声学揭示沉积特征的绘图和重建可能需要很长时间。为了减少地球物理视觉解释的时间,我们基于小波分析和应用于声波剖面的神经网络实施了一种新的相分类程序。应用于非常浅的威尼斯泻湖数据集的优化算法会自动对回波形状参数进行分类,以识别和绘制主要的泻湖沉积特征,例如古河道和古地表。分类算法包含一组小波变换参数,作为基于自组织映射(SOM)的神经网络分析的输入。该分析应用于在泻湖非常浅(小于1. m)且浑浊的区域中获得的580 km的声学剖面,地下穿透深度约为6-7。底部下方的m。无需对数据进行任何特殊的先决条件,就针对视觉解释的结果成功测试了该算法,并允许对该区域的沉积特征进行自动且高效的全二维地图绘制。我们可以区分和绘制不同类型的古河道,埋入的小溪,古地表以及以均质泥滩相为特征的区域。通过与调查区域采样的5个岩心进行比较,验证了结果,这些岩心对应于声学显示的主要沉积特征。

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