Comments on 'Turbulent boundary layer shear flows as an approximation of base surges at Campi Flegrei (Southern Italy), by Dellino et al. (2004)'

J.P. Le Roux

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Comments on 'Turbulent boundary layer shear flows as an approximation of base surges at Campi Flegrei (Southern Italy), by Dellino et al. (2004)'

机译：Dellino等人对“ Campi Flegrei（意大利南部）基础湍流的近似湍流边界层剪切流”的评论。（2004）”

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To summarize, it appears that Dellino et al. (2004) obtained remarkable results in spite of some erroneous assumptions, which shows that caution should be exercised in this kind of estimation. It so happens that virtually any fluid density between 0.001 and 0.01 g cm~(-3) could have been used to give the same result for both equations, which would yield widely different shear and mean velocities for these base-surges.

机译：总而言之，看来Dellino等人。（2004）尽管有一些错误的假设也取得了显着的结果，这表明在这种估计中应该谨慎行事。碰巧的是，对于这两个方程，几乎任何流体密度在0.001和0.01 g cm〜（-3）之间的流体都可以用来给出相同的结果，这对于这些基本波动会产生截然不同的剪切力和平均速度。

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《Journal of Volcanology and Geothermal Research》 |2005年第4期|p.331-332|共2页
作者
J.P. Le Roux;
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作者单位

Departamento de Geologia, Facultad de Ciencias Fisicas y Matematicas, Universidad de Chile, Casilla 13518, Correo 21, Santiago, Chile;

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正文语种 eng
中图分类天文学、地球科学;
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Comments on 'Turbulent boundary layer shear flows as an approximation of base surges at Campi Flegrei (Southern Italy), by Dellino et al. (2004)'

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