使用剪切波弹性学,核记录和显微镜技术进行表面泥平沉积物的表征)
Gabriel R Venegas1,2, Jane McCue2, Yu-Hsuan Chao3
1Center for Acoustics Research and Education, University of New Hampshire, Durham, New Hampshire 03824, USA.
The Journal of the Acoustical Society of America
|September 3, 2025
概括
剪切波弹性图 (SWE) 不侵入地绘制了沉积物的异质性,揭示了孔隙连接的硬性和变化. 这种方法可以了解表面沉积物中的弹性波形特性.
科学领域:
- 地质学
- 听力学
- 沉积物学
背景情况:
- 表面沉积物由于物理,生物和化学过程而表现出复杂的异质性.
- 这种异质性显著影响弹性波的传输和散射.
- 需要使用非侵入性技术来描述这些微妙的表面层.
研究的目的:
- 在表面沉积物中应用剪切波弹性图像 (SWE) 来获得剪切速度异质性的高分辨率成像.
- 将弹性特性与微观结构特征相关联.
- 研究沉积物结构与波浪传播之间的关系.
主要方法:
- 在新罕布什尔州的泥中采集的样本.
- 声波辐射力产生了剪切波 (50-200赫兹).
- 高率超声波成像剪切波传播,创建2D剪切速度地图.
- 分析了沉积物微观结构的显微镜技术.
主要成果:
- 在较软的矩阵 (~2 m/s) 中,SWE 发现了毫米级的硬 (高达16 m/s).
- 空间光谱分析显示切割速度强度在-42到-38dB/m之间.
- 阳性剪切速度梯度与孔隙连接性降低和谷物连接性增加相关.
结论:
- 剪切波弹性学对于表层沉积物的细度异质性是有效的.
- 沉积物微观结构,特别是颗粒接触和有机粘土含量,影响弹性波特性.
- 这些发现支持对滑,符合标准的接触者的粒度剪切模型.
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