...
首页> 外文期刊>Earth Surface Processes and Landforms: The journal of the British Geomorphological Research Group >A simple model accounting for the uptake, transport, and deposition of wind-eroded mineral particles in the hyperarid coastal Atacama Desert of northern Chile
【24h】

A simple model accounting for the uptake, transport, and deposition of wind-eroded mineral particles in the hyperarid coastal Atacama Desert of northern Chile

机译:一个简单的模型说明了智利北部高干旱沿海阿塔卡马沙漠中风蚀矿物颗粒的吸收,运输和沉积

获取原文
获取原文并翻译 | 示例
           

摘要

As previously observed in marine sediments collected downwind of African or South American continental sources, recent studies of sediment cores collected at the bottom of Mejillones Bay in north Chile (23°S) show a laminated structure in which the amount of particles of aeolian origin and their size create significant differences between the layers. This suggests inter-annual to inter-decadal variations in the strength of the local southerly winds responsible for (1) the erosion of the adjacent hyperarid surface of the Mejillones Pampa, and (2) the subsequent transport of the eroded particles towards the bay. A simple model accounting for the vertical uptake, transport, and deposition of the particles initially set into motion by wind at the surface of the pampa is proposed. This model, which could be adapted to other locations, assumes that the initial rate of (vertical) uptake is proportional to the (horizontal) saltation flux quantified by means of White's equation, that particles are lifted to a height (H), increasing with the magnitude of turbulence, and that sedimentation progressively removes the coarsest particles from the air column as it moves towards the bay. In this model, the proportionality constant (A) linking the vertical flux of particles with the horizontal flux, and the injection height (H) control the magnitude and size distribution of the deposition flux in the bay. Their values are determined using the wind speed measured over the pampa and the size distribution of particles collected in sediment traps deployed in the bay as constraints. After calibration, the model is used to assess the sensitivity of the deposition flux to the wind intensity variations. The possibility of performing such quantitative studies is necessary for interpreting precisely the variability of the aeolian material in the sediment cores collected at the bottom of Mejillones Bay.
机译:如先前在非洲或南美大陆来源的顺风处收集的海洋沉积物中所观察到的那样,最近对智利北部Mejillones湾底部(23°S)收集的沉积物芯进行的研究显示出一种层状结构,其中大量的风成因和它们的大小会在各层之间产生明显差异。这表明造成(1)Mejillones Pampa相邻高干旱表面的侵蚀,以及(2)随后被侵蚀的颗粒向海湾的迁移,造成的南风的强度在年际至年代际变化。提出了一个简单的模型,该模型考虑了最初在风中在风中开始在风中运动的粒子的垂直吸收,运输和沉积。该模型可以适用于其他位置,它假设(垂直)摄取的初始速率与通过怀特方程量化的(水平)盐化通量成正比,即颗粒被提升至高度(H),随湍流的大小,并且随着沉降物向海湾移动,沉降物逐渐将其从气柱中去除。在此模型中,将颗粒的垂直通量与水平通量联系起来的比例常数(A)和注入高度(H)控制隔室中沉积通量的大小和大小分布。它们的值是根据在潘帕上测得的风速和在海湾中部署的沉积物捕集器中收集的颗粒尺寸分布作为约束条件来确定的。校准后,该模型用于评估沉积通量对风强度变化的敏感性。进行这样的定量研究的可能性对于准确解释梅吉永斯湾底部收集的沉积岩心中风沙物质的变异性是必要的。

著录项

相似文献

  • 外文文献
  • 专利
获取原文

客服邮箱:kefu@zhangqiaokeyan.com

京公网安备:11010802029741号 ICP备案号:京ICP备15016152号-6 六维联合信息科技 (北京) 有限公司©版权所有
  • 客服微信

  • 服务号