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穿透轨道形态和沉积物参数:地下层对基板性质的变化有很强的抵抗力
Benjamin William Griffin1, Tash L Prescott1, Andréas Jannel1
1School of Biological and Environmental Sciences, Liverpool John Moores University, Liverpool, UK.
Journal of the Royal Society, Interface
|February 27, 2026
概括
沉积物的一致性显著影响地表轨道形态,但不影响地下轨道形态. 这一发现提高了从各种沉积物条件的透轨迹中重建脚部运动的可靠性.
科学领域:
- 古生物学的古生物学
- 地质地质地质地质地质地
- 计算科学 计算科学
背景情况:
- 轨道形态受脚部解剖学,运动和沉积物质的影响.
- 穿透性轨迹提供了有价值的足部运动见解,因为足部和沉积物的相互作用得到了增强.
- 地下轨道形态对于准确的运动恢复至关重要.
研究的目的:
- 研究沉积物的一致性对地下轨道形态学的影响.
- 为了比较地表与地下轨道形态与沉积物变化的强度.
- 评估从透轨道的运动重建的可靠性.
主要方法:
- 使用离散元件方法 (DEM) 模拟.
- 模拟了两种场景:一个垂直入的圆柱体和一个动态的热足类脚.
- 系统地改变了沉积物的摩擦和凝聚力,以观察轨道形态学的影响.
主要成果:
- 沉积物摩擦的增加导致了更明显的移位边缘.
- 更高的沉积物凝聚力导致轨道保持开放,并抵抗填充.
- 低凝聚力导致表面轨迹与实际的脚形态学有显著的偏离.
- 与地表轨道相比,地表轨道形态表现出对沉积物特性变化的更强的弹性.
结论:
- 沉积物的行为大大改变了表面轨道形态,但对地下形态的影响有限.
- 透轨道为运动重建提供可靠的数据,无论沉积物条件如何.
- 这项研究验证了地下轨道形态学用于古运动分析的使用.
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