对Muñoz Carpena等人关于“复杂降雨模式下浅水位坡面降雨入渗径流过程建模”的评论的答复

IF 3.1 Q2 GEOSCIENCES, MULTIDISCIPLINARY
Songbai Wu , Ting Fong May Chui , Li Chen
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引用次数: 0

摘要

我们感谢Muñoz-Carpena等人(2021)的评论,他们指出了我们的工作和他们的结果之间的一些不一致之处。经过彻底的检查,我们发现Wu等人(2021)应用的土壤水力特性模型描述不准确,并且在第4.1节和图6中参数化模型时存在相关的不一致。校正参数后,我们发现Wu et al.(2021)的模型、SWINGO和Hydrus-1D的模拟入渗速率在稳态和非稳态降雨下都很接近。此外,Wu et al.(2021)利用Vachaud et al.(1974)和Chu(1997)的实验数据进一步验证了Wu et al.(2021)的模型,结果表明Wu et al.(2021)的模型在模拟浅地下水位(WT)土壤的入渗方面表现出令人满意的效果。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Reply to comments by Muñoz-Carpena et al. on “Modeling slope rainfall-infiltration-runoff process with shallow water table during complex rainfall patterns”

We appreciate the comments by Muñoz-Carpena et al. (2021), which pointed out some inconsistency between our work and their results. After a thorough examination, we identified an inaccurate description of the soil hydraulic property model applied in Wu et al. (2021) and an associated inconsistency in parameterizing the model in Section 4.1 and Figure 6. After correcting the parameters, we found that the simulated infiltration rates of Wu et al. (2021)’s model, SWINGO, and Hydrus-1D are close under both steady and unsteady rainfalls. Moreover, Wu et al. (2021)’s model has been further validated using the experimental data of Vachaud et al. (1974) and Chu (1997) and the results show satisfactory performance of Wu et al. (2021)’s model in simulating infiltration in soils with a shallow water table (WT).

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来源期刊
Journal of Hydrology X
Journal of Hydrology X Environmental Science-Water Science and Technology
CiteScore
7.00
自引率
2.50%
发文量
20
审稿时长
25 weeks
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