沙球起源于雨水中的雨滴
Bertil Trottet1,2, Daisuke Noto1, Douglas J Jerolmack1,3
1Department of Earth and Environmental Science, University of Pennsylvania, Philadelphia, PA 19104.
概括
雨滴产生"沙球",通过向下滚动来放大土壤侵蚀. 这种冲击后的过程,与喷侵蚀不同,涉及密集的悬浮形成稳定的形状和堵塞.
科学领域:
- 地球和环境科学 地球和环境科学
- 流体力学 流体力学 流体力学
- 颗粒力学 颗粒力学
背景情况:
- 雨水侵蚀土壤是水循环的关键组成部分.
- 雨滴侵蚀是复杂的,因为它在流体-颗粒力学边界的三相性质.
- 之前的研究重点是雨滴撞击 (喷侵蚀) 时的粒子携带.
研究的目的:
- 为了研究雨滴侵蚀的冲击后阶段.
- 为了揭示土壤浸入的有效机制,超出初始冲击.
- 描述雨滴诱导的土壤聚合物的形成和形态.
主要方法:
- 实验室对干燥,斜坡的颗粒床进行了受控雨滴冲击的实验.
- 对自然降雨事件的现场观测.
- 在不同的落下条件下分析沙球形成,生长和形态.
主要成果:
- 雨滴自发地在颗粒状表面上形成密集,滚动的"沙球".
- 这些沙球有效地吸收沉积物,大大放大了土壤侵蚀.
- 确定了两个稳定的沙球形态:花生状 (水力动力不稳定) 和 toroidal (机械锁定).
结论:
- 撞击后沙球的滚动是一个惊人的高效和占主导地位的土壤侵蚀机制.
- 沙球形成和形态受到水力动力学不稳定性和沉积物负荷的影响.
- 这些发现对理解侵蚀,沉积物运输和生物工程和雪物理等不同领域的相关现象有意义.
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