SAR图像河流分割的加权指数区域能量模型

传统主动轮廓模型很难实现精确的SAR图像河流分割。针对这一问题,本文提出了一种加权指数区域能量主动轮廓模型,以精确地提取SAR图像中的河流。该模型在Chan-Vese(CV)模型能量泛函中引入了指数区域能量,能更好地衡量分割图像和原始图像的差异程度,提高模型的分割准确性。此外,利用目标区域和背景区域内像素灰度的最大绝对差取代模型中常值区域能量权重,自适应地调节目标区域和背景区域的能量比重,加速曲线运动到目标区域的边缘,获得更高的分割效率。针对实际河流SAR图像进行了分割试验,结果表明:与传统主动轮廓模型相比,本文提出的模型能更快速、精确地分割SAR图像中的河流,在分割结果和分割效率两方面具有优势。

基于自监督学习的河流分割方法

针对水上桥梁图像受地形、天气、环境的影响,河流情况复杂且形式较多,无法事先采集所有图像中的河流样本等问题,本文提出一种基于自监督学习的河流分割方法,利用K均值聚类与Harris角点相结合的方法自动提取部分河流区域作为自监督学习的河流样本,以及河流样本的颜色和纹理特征,再根据提取的图像的河流特征利用支持向量机(SVM)的单分类功能进行训练学习,通过训练好的分类器完成河流的分割。实验结果表明,本文的河流分割方法能较好地分割出河流并适应不同场景的水上桥梁图像。

基于L_(1)范数混合主动轮廓的河流SAR图像分割

为解决现有主动轮廓模型难以准确分割河流SAR图像的问题,提出一种基于L_(1)范数的混合主动轮廓模型。首先,计算轮廓曲线内外区域像素灰度的中值作为区域拟合中心,以抑制SAR图像中干扰区域对其准确性的影响;然后,利用L_(1)范数构建新的能量约束项并在模型能量泛函中引入边缘指示函数,进一步提升模型的分割性能;最后,将基于L_(1)范数的中值和均值能量约束项结合起来并添加额外的区域拟合中心约束项,以提高模型的整体稳定性。针对实际河流SAR图像进行分割试验,结果表明,与现有分割方法相比,本文模型能更准确、稳定地分割河流SAR图像。

ADAPTIVE RIVER SEGMENTATION IN SAR IMAGES

There is difficulty for distinguishing of river and shadow in Synthetic Aperture Radar (SAR) images. A method of river segmentation in SAR images based on wavelet energy and gradient is proposed in this paper. It mainly includes two algorithms: coarse segmentation and refined segmen- tation. Firstly, The river regions are coarsely segmented by the wavelet energy feature,and then refined segmented accurately by the gradient threshold which is got adaptively. The experimental results show the validity of the method, which provides a good foundation for targets detection above the river.

Numerical simulation of deposit in confluence zone of debris flow and mainstream

Abundant solid materials were formed as a result of landslide and collapse due to Wenchuan earthquake.The solid source around mountains would form a debris flow when appropriate rain condition occurs.Such a debris flow is structurally very large and strong,and the river flow can hardly wash away the deposit when the debris flow enters into the mainstream.As a result,the deposit on the river bed due to debris flow will cause a series of hazards.Based on the previous researches and relevant data,this paper simplified the interaction between debris flow and current of the main river,and adopted the finite element characteristic-based-split algorithm which is favorable to the stabilization of dealing with the convection.Finally,the numerical model of the confluence of debris flow deposit and main river was developed,and the deposit progress of the mega-debris flow from Wenjiagou in Mianyuan river was reproduced.Furthermore,the influence of the deposit on the flow route of the main river,and distribution of velocity and water depth were analyzed.The results showed that the simulation deposit terrain qualitatively agreed with the field data through comparison,including the deposit area and depth distribution.Furthermore,the improvement of the model in future was discussed.