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Visibility in airborne volcanic ash: considerations for surface transportation using a laboratory-based method

机译:空气中火山灰的可见性:使用基于实验室的方法的表面运输的考虑因素

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摘要

All modes of surface transportation can be disrupted by visibility degradation caused by airborne volcanic ash. Despite much qualitative evidence of low visibility on roads following historical eruptions worldwide, there have been few detailed studies that have attempted to quantify relationships between visibility conditions and observed impacts on network functionality and safety. In the absence of detailed field observations, such gaps in knowledge can be filled by developing empirical datasets through laboratory investigations. Here, we use historical eruption data to estimate a plausible range of ash-settling rates and ash particle characteristics for Auckland city, New Zealand. We propose and implement a new experimental set-up in controlled laboratory conditions, which incorporates a dual-pass transmissometer and solid aerosol generator, to reproduce these ash-settling rates and calculate visual ranges through the associated airborne volcanic ash. Our findings demonstrate that visibility is most impaired for high ash-settling rates (i.e. & 500 g m(-2) h(-1)) and particle size is deemed the most influential ash characteristic for visual range. For the samples tested (all & 320 mu m particle diameter), visibility was restricted to similar to 1-2 m when ash settling was replicated for very high rates (i.e. similar to 4000 g m(-2) h(-1)) and was especially low when ash particles were fine-grained, more irregular in shape and lighter in colour. Finally, we consider potential implications for disruption to surface transportation in Auckland through comparisons with existing research which investigates the consequences of visual range reduction for other atmospheric hazards such as fog. This includes discussing how our approach might be utilised in emergency and transport management planning. Finally, we summarise strategies available for the mitigation of visibility degradation in environments contaminated with volcanic ash.
机译:所有表面运输模式都可以通过空气中的火山灰引起的可视性降解来破坏。尽管在全球历史爆发后道路上有很大的定性证据,但仍有很少的详细研究,试图量化能见度条件之间的关系,并观察到对网络功能和安全影响的影响。在没有详细的现场观察的情况下,通过通过实验室调查开发经验数据集可以填充知识中的这种差距。在这里,我们使用历史爆发数据来估计新西兰奥克兰市的灰度稳定率和灰分粒子特征。我们提出并在受控实验室条件下实施了新的实验设置,该方法包括双通透射仪和固体气溶胶发生器,以再现这些灰分稳定速率并通过相关的空气载火山灰计算视觉范围。我们的研究结果表明,对于高灰分稳定速率(即& 500g m(-2)H(-1))和粒度被认为是视觉范围最有影响力的特征的能力最受损。对于测试的样品(所有& LT; LT;320μm粒径),当复制灰分沉降时,可视地仅达到1-2μm(即类似于4000克(-2)H(-1) )),当灰分颗粒细粒细粒,形状更不规则,颜色较轻时,特别低。最后,我们考虑通过与现有研究的比较来考虑对奥克兰地表运输的潜在影响,通过对现有的研究来调查视觉范围减少对雾等其他大气危害的后果。这包括讨论如何在紧急和运输管理计划中使用我们的方法。最后,我们总结了在用火山灰污染的环境中减轻可见性降解的策略。

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