Flame Structure and Scalar Properties in Microgravity Laminar Fires

Recent results from microgravity combustion experiments conducted in the Zero Gravity Facility (ZGF) 5.18 second drop tower are reported. Emission mid-infrared spectroscopy measurements have been completed to quantitatively determine the flame temperature, water and carbon dioxide vapor concentrations, radiative emissive power, and soot concentrations in a microgravity laminar ethylene/air flame. The ethylene/air laminar flame conditions are similar to previously reported experiments including the Flight Project, Laminar Soot Processes (LSP). Soot concentrations and gas temperatures are in reasonable agreement with similar results available in the literature. However, soot concentrations and flame structure dramatically change in long duration microgravity laminar diffusion flames as demonstrated in this paper

Popular Agitation and British Parliamentary Reform, 1866-1867

This paper demonstrated that the force of public opinion as expressed by pro-reform agitations played a critical role in the attainment of working-class voting rights with the Reform Act of 1867. This Reform Act, which passed after more than a year of political disputes and public demands, gave most of the urban English working class the right to vote. In 1866 a modest reform bill sponsored by William Gladstone’s Liberal government had been defeated by a combination of Conservative and conservative Liberal opposition. After months of popular demonstrations, Benjamin Disraeli’s new Conservative government introduced another reform bill that initially was very restrictive. But after further public demonstrations and political conflict in parliament, the bill emerged as a radical measure that more than doubled the size of the electorate. The paper followed the course of the reform controversy and public agitations, and established that the working-class agitations in favor of parliamentary reform were a critical force in compelling parliament to enact comprehensive working class enfranchisement. The project used original source material, including the parliamentary debates, The Times and the Manchester Guardian, working class and radical newspapers such as the Beehive, Commonwealth and the e National Reformer, magazines such as Blackwood’s, Contemporary Review, and Quarterly Review, trade union minutes, memoirs, speeches, and private letters

Classical generalized constant coupling model for geometrically frustrated antiferromagnets

A generalized constant coupling approximation for classical geometrically frustrated antiferromagnets is presented. Starting from a frustrated unit we introduce the interactions with the surrounding units in terms of an internal effective field which is fixed by a self consistency condition. Results for the magnetic susceptibility and specific heat are compared with Monte Carlo data for the classical Heisenberg model for the pyrochlore and kagome lattices. The predictions for the susceptibility are found to be essentially exact, and the corresponding predictions for the specific heat are found to be in very good agreement with the Monte Carlo results.Comment: 4 pages, 3 figures, 2 columns. Discussion about the zero T value of the pyrochlore specific heat correcte

Modelagem do balanço hídrico em microbacia cultivada com plantio comercial de Eucalyptus grandis x urophylla no leste de Minas Gerais, Brasil

No Brasil, o número de plantios comerciais de espécies florestais de crescimento rápido vem aumentando consideravelmente nas últimas décadas. Contudo, os possíveis impactos desse aumento sobre os recursos hídricos ainda são desconhecidos. O objetivo deste estudo foi realizar a modelagem do balanço hídrico em uma microbacia cultivada com plantio comercial de híbridos de Eucalyptus grandis x urophylla no Leste de Minas Gerais, Brasil. O trabalho foi realizado em uma microbacia experimental com área total de 40 ha durante o ano hidrológico, compreendido entre outubro de 2009 e setembro de 2010. A principal entrada de água no sistema via precipitação pluvial e os dados meteorológicos foram coletados por uma estação automática instalada no interior da área de estudo. As principais saídas foram estimadas pela equação modificada de Penman-Monteith e pela mensuração do deflúvio gerado na saída da bacia. Do total precipitado (1.123 mm) durante o ano, 9% (106 mm) retornaram à atmosfera via interceptação, 66% (740 mm) via transpiração da cultura e 11% (119 mm) pela evaporação do solo, que somados corresponderam à aproximadamente 86% da entrada de água na microbacia. Do deflúvio total gerado (~147 mm), apenas 4,29 mm (0,4%) foram convertidos em escoamento superficial. Pode-se concluir que durante o ano hidrológico monitorado o balanço entre as principais entradas e as saídas de água na microbacia foi equalizado, não comprometendo a disponibilidade hídrica natural no curso d'água