感谢齐璞和孙赞盈教授对我们关于“非漫滩高含沙洪水异常传播机理和临界条件”的研究感兴趣,他们的讨论有益于对学术问题的深入研究。但须说明的是,他们的批评实际上是对流体力学基本概念的误解和对我们的论文的误读导致的。我们的研究是针对黄河下游高含沙紊流进行的,通过分析充分发展的紊流中具有屈服应力的层流底层(黏性底层)对洪水波稳定性的影响,探讨了黄河下游非漫滩高含沙洪水增值的一种机理,所涉及的基本假设、分析和结论更与“层流”、“浆河”现象无 Thanks to Prof. Qi Pu and Prof. Sun Zanying for their interest in our research on the mechanism and critical conditions for the abnormal transmission of highly sediment-laden floodplains in non-floodplains. Their discussions are good for further research on academic issues. However, it should be noted that their criticism is actually caused by the misunderstanding of the basic concepts of fluid mechanics and the misreading of our dissertation. Our research is aimed at the high turbulent flow in the lower Yellow River. By analyzing the influence of yield stress on the stability of the flood wave in the fully developed turbulent flow, the paper discusses the non-floodplain in the lower Yellow River One of the mechanisms for the value added of silt floods involves the underlying assumptions, analyzes and conclusions that are more relevant to the “laminar flow”, “slurry river”