首页> 外文期刊>Transport in Porous Media >Reply to Comments by Veling on 'A Semi-Analytical Solution for Large-Scale Injection-Induced Pressure Perturbation and Leakage in a Laterally Bounded Aquifer-Aquitard System' by Zhou, Birkholzer,and Tsang
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Reply to Comments by Veling on 'A Semi-Analytical Solution for Large-Scale Injection-Induced Pressure Perturbation and Leakage in a Laterally Bounded Aquifer-Aquitard System' by Zhou, Birkholzer,and Tsang

机译:对Veling的评论答复,周,Birkholzer和Tsang提出了“一种在侧向界含水层-阿奎塔尔系统中大规模注入引起的压力扰动和泄漏的半解析解决方案”

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摘要

Veling (2010) pointed to "a serious mistake" and "mathematical inconsistency" in Zhou et al. (2009) because the dimensionless flow equations in Equation 4 (in terms of dimensionless hydraulic head rise in the aquifer and the aquitard) would give rise to additional terms when back converting to the groundwater flow equations, in the case that initial conditions for hydraulic head were spatially variable. He added, however, that the conclusions of the paper remain valid when uniform initial conditions are assumed. We accept this comment because we have indeed assumed uniform initial conditions in the system but failed to state this explicitly in the publication, partially because this assumption is very common in groundwater hydrology when deriving analytical and semi-analytical solutions.
机译:Veling(2010)在Zhou等人的文章中指出“严重错误”和“数学上的矛盾”。 (2009年),因为在水头的初始条件下,方程4中的无量纲流方程(根据含水层和无水层中无量纲的水头扬程)在转换回地下水流量方程时会产生附加项。在空间上是可变的。但是,他补充说,当假设统一的初始条件时,本文的结论仍然有效。我们接受此评论是因为我们确实假设系统中存在统一的初始条件,但未能在出版物中明确说明这一点,部分原因是推导分析和半分析解决方案时该假设在地下水水文学中非常普遍。

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    《Transport in Porous Media》 |2011年第1期|p.357-358|共2页
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    Earth Sciences Division, Lawrence Berkeley National Laboratory, University of California, Berkeley, CA 94720, USA,One Cyclotron Road, Berkeley, MS 90-1116, USA;

    Earth Sciences Division, Lawrence Berkeley National Laboratory, University of California, Berkeley, CA 94720, USA;

    Earth Sciences Division, Lawrence Berkeley National Laboratory, University of California, Berkeley, CA 94720, USA;

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