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首页> 外文期刊>Earth Surface Processes and Landforms: The journal of the British Geomorphological Research Group >Comment on 'A transport-distance approach to scaling erosion rates: III. Evaluating scaling characteristics of MAHLERAN'
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Comment on 'A transport-distance approach to scaling erosion rates: III. Evaluating scaling characteristics of MAHLERAN'

机译:评述“以运输距离方法衡量侵蚀率的方法:III。评估MAHLERAN'的缩放比例特性

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摘要

Wainwright et al. (2008) state that ‘For example, Kinnell (1993) suggests that there should be a peak in detachment at flow depths of two raindrop diameters with lower detachment rates at lesser and greater flow depths, although the data to support his case are also woefully limited in that there are no data to support the initial rise in detachment, other than fitting a point at the origin, which is an artifact of considering sediment concentration in the flow.’ This statement results from incorrectly interpreting the role of the empirical flow depth–drop size function presented in Kinnell (1993).
机译:Wainwright等。 (2008年)指出,“例如,Kinnell(1993年)建议,在两个雨滴直径的水深处应有一个分离峰,在较小和较大水深处有较低的分离率,尽管支持他的情况的数据也很糟糕。局限性在于,除了拟合原点外,没有任何数据支持分离的初始上升,而原点是考虑流中沉积物浓度的假象。'这种说法是由于错误地解释了经验流深度的作用而导致的。 – Kinnell(1993)中提出的液滴大小函数。

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