黄河水下三角洲海底粉土微观结构分形特征研究

发布时间：2018-05-10 14:33

本文选题：海底粉土 + SEM　；参考：《海洋科学进展》2017年04期

【摘要】：以黄河水下三角洲海底粉土为研究对象,基于扫描电子显微镜技术获得了大量的海底粉土SEM(scanning electron microscopy)图像,综合运用Image-Pro Plus(IPP)和Photoshop图像处理软件来提取粉土的微观结构参数,以分形理论为指导,运用"周长-面积法"对海底粉土进行了分形特征研究,分析了阈值、放大倍数对粉土分形维数的影响及确定方法,并探讨了分形维数的环境及工程地质意义。研究结果表明,黄河水下三角洲海底粉土的颗粒及孔隙具有特殊的分形特征,分形维数为1.6~1.8;不同分维值在一定程度上反映了波浪扰动强度的不同;分形维数可以表征抗剪强度参数,粉土的黏聚力和内摩擦角随分维值的增大而增大。
[Abstract]:Based on scanning electron microscope (SEM) technique, a large number of SEM(scanning electron microscopyimages of subsea silt in the Yellow River underwater delta were obtained. The microstructural parameters of silt were extracted by using Image-Pro plus IPP) and Photoshop image processing software. Under the guidance of fractal theory, the fractal characteristics of silt are studied by the method of circumference and area, and the influence of threshold value and magnification on fractal dimension of silt is analyzed, and the method of determining the fractal dimension of silt is analyzed. The environmental and engineering geological significance of fractal dimension is also discussed. The results show that the particles and pores of the subsea silt in the Yellow River underwater delta have special fractal characteristics, and the fractal dimension is 1.6 ~ 1.8.The different fractal dimension values reflect the different intensity of wave disturbance to some extent. The fractal dimension can characterize the shear strength parameters, and the cohesive force and internal friction angle of silt increase with the increase of fractal dimension.
【作者单位】：国家海洋局第一海洋研究所;
【基金】：国家海洋公益性行业科研专项——近海海底地质灾害预测评价及防控关键技术研究(201005005) 青岛海洋科学与技术国家实验室鳌山科技创新计划项目——海底地质灾害监测预警与评估关键技术预研究(2015ASKJ03) 中央级公益性科研院所基本科研业务费专项资金资助项目——北黄海海底麻坑群精细地貌特征研究及成因分析(2015G15) 国家自然科学基金项目——基于形态学特征和声学探测技术的北黄海海底麻坑群成因研究(41506069)
【分类号】：P642.1;P736

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