下水道系统间歇泉形成的新认识

IF 1.2 Q4 WATER RESOURCES
S. Wright
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引用次数: 3

摘要

先前对在经历雨水间歇泉的地点收集的压力和速度数据的分析提出了发生的机制。试图重现间歇泉的实验室实验很有希望,但由于小规模实验中潜在的规模效应,结果不确定。随后的研究人员通常将这一早期工作作为后续实验室实验的起点。多年来,人们获得了许多实际系统中间歇泉的视频,对这些视频中重要特征的回顾对原始假设的某些方面提出了质疑。对这一现象的另一种解释已经发展出来,并且已经确定了一种实验系统,这可能有助于解决一些问题。然而,实验室实验也可能受到规模效应的影响,必须进行一些初步研究,以确定在推进我们对这一现象的认识方面是否有一条富有成效的道路。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
A New Look at Geyser Formation in Sewer Systems
Previous analysis of pressure and velocity data collected at a site experiencing stormwater geysers suggested a mechanism for the occurrence. Laboratory experiments attempting to reproduce the geysers were promising but inconclusive due to potential scale effects in the small scale experiments. Subsequent researchers have generally used this early work as the starting point for subsequent laboratory experiments. Over the years, a number of videos of geysers in actual systems have been obtained and a review of important features from these videos calls into question certain aspects of the original hypothesis. An alternative explanation for the phenomenon has been developed and an experimental system has been identified that may help resolve some questions. However, laboratory experiments may also be impacted by scale effects and several preliminary studies must be conducted to determine whether there is a fruitful path forward in advancing our knowledge of this phenomenon.
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来源期刊
CiteScore
1.30
自引率
0.00%
发文量
8
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