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

机译:回应Kinnell的“关于用侵蚀距离的方法腐蚀水垢的方法:III。评估马勒兰水垢的特性”的评论

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摘要

Kinnell comments that we misinterpret his analysis in the development of his empirical relationship relating flow depths and drop sizes (Kinnell, 1993). Beyond any potential misunderstanding of his original paper, Kinnell’s comment is somewhat tangential to the statement he cites. Our issue is simply that the theory is not well supported by the data presented, and furthermore given that his approach is based on assumptions about transport mechanisms that we believe are unwarranted, we felt that it was unwarranted to implement his functional form as a further test of the scaling characteristics of MAHLERAN.
机译:Kinnell认为我们在发展与流量深度和液滴尺寸有关的经验关系时会误解他的分析(Kinnell,1993)。除了对他的原始论文有任何潜在的误解外,金内尔的评论与他引用的陈述有些切合。我们的问题很简单,就是所提供的数据并不能很好地支持该理论,此外,鉴于他的方法是基于我们认为不需要的运输机制假设,因此,我们认为不应该将其功能形式用于进一步的检验MAHLERAN的缩放比例特性。

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