Raj Phani K
Technology & Management Systems, Inc., 102 Drake Road, Burlington, MA 01803, USA.
J Hazard Mater. 2007 Apr 11;142(3):720-9. doi: 10.1016/j.jhazmat.2006.06.130. Epub 2006 Jul 6.
Spectral description of thermal emission from fires provides a fundamental basis on which the fire thermal radiation hazard assessment models can be developed. Several field experiments were conducted during the 1970s and 1980s to measure the thermal radiation field surrounding LNG fires. Most of these tests involved the measurement of fire thermal radiation to objects outside the fire envelope using either narrow-angle or wide-angle radiometers. Extrapolating the wide-angle radiometer data without understanding the nature of fire emission is prone to errors. Spectral emissions from LNG fires have been recorded in four test series conducted with LNG fires on different substrates and of different diameters. These include the AGA test series of LNG fires on land of diameters 1.8 and 6m, 35 m diameter fire on an insulated concrete dike in the Montoir tests conducted by Gaz de France, a 1976 test with 13 m diameter and the 1980 tests with 10 m diameter LNG fire on water carried out at China Lake, CA. The spectral data from the Montoir test series have not been published in technical journals; only recently has some data from this series have become available. This paper presents the details of the LNG fire spectral data from, primarily, the China Lake test series, their analysis and results. Available data from other test series are also discussed. China Lake data indicate that the thermal radiation emission from 13 m diameter LNG fire is made up of band emissions of about 50% of energy by water vapor (band emission), about 25% by carbon dioxide and the remainder constituting the continuum emission by luminous soot. The emissions from the H2O and CO2 bands are completely absorbed by the intervening atmosphere in less than about 200 m from the fire, even in the relatively dry desert air. The effective soot radiation constitutes only about 23% during the burning period of methane and increases slightly when other higher hydrocarbon species (ethane, propane, etc.) are burning in the LNG fire. The paper discusses the procedure by which the fire spectral data are used to predict the thermal emission from large LNG fires. Unfortunately, no direct measurements of the soot density or smoke characteristics were made in the tests. These parameters have significant effect on the thermal emission from large LNG fires.
火灾热辐射的光谱描述为火灾热辐射危害评估模型的开发提供了一个基本依据。在20世纪70年代和80年代进行了几次现场试验,以测量液化天然气火灾周围的热辐射场。这些试验大多涉及使用窄角或广角辐射计测量火灾热辐射到火灾范围外的物体。在不了解火灾辐射特性的情况下外推广角辐射计数据容易出错。在四个不同试验系列中记录了液化天然气火灾的光谱辐射,这些试验是在不同基材上、不同直径的液化天然气火灾中进行的。其中包括美国燃气协会在陆地上进行的直径为1.8米和6米的液化天然气火灾试验系列、法国燃气公司在蒙图瓦尔试验中在隔热混凝土堤上进行的直径35米的火灾试验、1976年进行的直径13米的试验以及1980年在美国加利福尼亚州中国湖进行的直径10米的水上液化天然气火灾试验。蒙图瓦尔试验系列的光谱数据尚未在技术期刊上发表;直到最近,该系列的一些数据才得以公开。本文主要介绍了来自中国湖试验系列的液化天然气火灾光谱数据的详细情况、分析及结果。同时也讨论了其他试验系列的可用数据。中国湖的数据表明,直径13米的液化天然气火灾的热辐射由水蒸气(带状辐射)贡献约50%的能量的带状辐射、二氧化碳贡献约25%的能量以及其余由发光烟灰构成的连续辐射组成。即使在相对干燥的沙漠空气中,来自水和二氧化碳波段的辐射在距离火灾不到约200米的范围内就会被中间的大气完全吸收。在甲烷燃烧期间,有效烟灰辐射仅占约23%,当液化天然气火灾中有其他高碳氢化合物(乙烷、丙烷等)燃烧时,有效烟灰辐射会略有增加。本文讨论了利用火灾光谱数据预测大型液化天然气火灾热辐射的方法。遗憾的是,试验中没有对烟灰密度或烟雾特性进行直接测量。这些参数对大型液化天然气火灾的热辐射有显著影响。