The low acoustic noise and turbulence wind tunnel of the University of Sao Paulo

2021 ◽  
pp. 1-33
Author(s):  
F.R. Amaral ◽  
J.C. Serrano Rico ◽  
C.S. Bresci ◽  
M.M. Beraldo ◽  
V.B. Victorino ◽  
...  

Abstract This paper introduces the Low Acoustic Noise and Turbulence (LANT) wind tunnel of the Sao Carlos School of Engineering, University of Sao Paulo (USP-EESC), Brazil. The closed-loop wind tunnel features several devices to improve flow uniformity, reduce swirl, and lower the background acoustic noise and turbulence, enabling stability and aeroacoustic experiments. The design criteria was based on the best practices reported, in particular for low turbulence wind tunnels. Yet, these criteria are conflicting and we discuss the decisions that had to be made and present flow quality results that were achieved. The 16-bladed axial fan with 13-blade stators is driven by a variable-speed electric motor. At the corners, 100 mm dense acoustic foam is installed on the vertical walls, floor and ceiling, and the turning vanes are filled with acoustic-absorbing material. The long settling chamber contains a 3.175 mm mesh hexagonal honeycomb and five fine mesh nylon screens, ending in a 7:1 area ratio short contraction. The 3-m long closed-working section has a $1\times 1\ {\rm m}^2$ cross-section area. At 15 m/s the working section wall boundary layer is less than 100 mm thick, providing an area of at least $800\times 800\ \mathrm{mm}^2$ where the streamwise flow uniformity was within 1%. In the 10–30 m/s flow speed range, the turbulence intensity ranged from 0.05% to 0.071% and the background acoustic noise level, obtained with an inflow microphone, ranged from 90 and 110 dB. A benchmark experiment on a flat plate boundary layer produced an almost perfect two-dimensional Blasius profile up to $Re_x \approx 2.5 \times 10^6$ . A beamforming benchmark experiment on aeroacoustics accurately identified the sound emitted by a cylinder immersed in the flow.

1978 ◽  
Vol 100 (1) ◽  
pp. 91-96 ◽  
Author(s):  
V. de Brederode ◽  
P. Bradshaw

Measurements in the entry region of a square duct (specifically, a wind-tunnel working section) show that the direct effect of stress-induced secondary flows in the corners on the center-plane boundary layer is negligible for boundary layers thinner than about one-fourth of the duct width. Further, the effects of streamwise pressure gradient and of quasi-collinear lateral convergence tend to cancel so that the velocity profiles and skin friction are quite close to those on a flat plate. This shows that the boundary layer on the floor of a wind tunnel of constant, square cross section can be used to simulate a flat-plate flow even when the boundary layer thickness is as large as one-fourth of the tunnel height.


1998 ◽  
Vol 37 (3) ◽  
pp. 269-287 ◽  
Author(s):  
I. Bischoff-Gauß ◽  
N. Kalthoff ◽  
F. Fiedler

Abstract The area between the Atlantic Ocean and São Paulo is highly polluted due to high emission rates at Cubatão, a city situated 15 km inland at a steep slope. It was expected that secondary circulations would develop caused by the land–sea contrast and strong orographic changes, which influence the transport and diffusion of air pollutants. In 1994–95, surface stations were operated and radiosonde ascents were performed to analyze the characteristic features of the land–sea-breeze circulation. The stations make evident a land–sea-breeze system that arrived in the suburbs of São Paulo in the early afternoon. The upslope winds favor the propagation of the sea breeze at the steep slope. During the measurement period, large-scale northwesterly winds prevailed that advected warm air from the plateau to the coastal area in the afternoon and resulted in a limitation of the boundary layer growth. The data were used to initialize a three-dimensional mesoscale model for calculation of the transport and deposition of SO2 emitted at Cubatão. The boundary layer height was found to be a limitation for vertical mixing of the air pollutants. However, a step between the coastal boundary layer and the boundary layer over the plateau causes SO2 to be vented into the free atmosphere at the slope and then transported toward the Atlantic Ocean with the large-scale northwesterly winds. Thus, over the coastal area, the SO2 concentrations in the free atmosphere were even higher than within the mixed layer. The deposition, summed up over a day, was calculated and found to be strongest at the slope and over the Atlantic Ocean.


2018 ◽  
Vol 214 ◽  
pp. 174-188 ◽  
Author(s):  
Flávia N.D. Ribeiro ◽  
Amauri P. de Oliveira ◽  
Jacyra Soares ◽  
Regina M. de Miranda ◽  
Michael Barlage ◽  
...  

2019 ◽  
Vol 34 (3) ◽  
pp. 331-340
Author(s):  
Lucas Caixeta Vieira ◽  
João de Deus Godinho Junior ◽  
Renato Adriane Alves Ruas ◽  
Vinícius Ribeiro Faria ◽  
Alberto Carvalho Filho

Interações entre adjuvante e pontas hidráulicas no controle da deriva de glifosato   LUCAS CAIXETA VIEIRA1, JOÃO DE DEUS GODINHO JUNIOR2, RENATO ADRIANE ALVES RUAS3, VINÍCIUS RIBEIRO FARIA4, ALBERTO CARVALHO FILHO5   1 Departamento de Produção Vegetal, Universidade de São Paulo, Av. Pádua Dias, N0: 11, Agronomia, CEP: 13418-900, Piracicaba – São Paulo, Brasil, [email protected] 2 Departamento de Engenharia Rural, Universidade Estadual Paulista, Via de Acesso Professor Paulo Donato Castelane Castellane S/N - Vila Industrial, CEP: 14884-900, Jaboticabal – São Paulo, Brasil, [email protected] 3  Instituto de Ciências Agrárias, Universidade Federal de Viçosa, Rodovia MG-230 - Km 7, Zona Rural, CEP: 38810-000, Rio Paranaíba – Minas Gerais, Brasil, [email protected] 4  Instituto de Ciências Agrárias, Universidade Federal de Viçosa, Rodovia MG-230 - Km 7, Zona Rural, CEP: 38810-000, Rio Paranaíba – Minas Gerais, Brasil, [email protected] 5 Instituto de Ciências Agrárias, Universidade Federal de Viçosa, Rodovia MG-230 - Km 7, Zona Rural, CEP: 38810-000, Rio Paranaíba – Minas Gerais, Brasil, [email protected]   RESUMO: Objetivou-se com este trabalho analisar as interações entre adjuvante e pontas hidráulicas no controle da deriva de glifosato. Primeiramente, avaliou-se o espectro de gotas, empregando-se o delineamento inteiramente casualizado (DIC), em parcela subdividida, avaliando-se quatro soluções de aplicação (Parcelas): água; água + óleo mineral; água + glifosato; água + óleo mineral + glifosato e três modelos de pontas tipo leque(Subparcelas): simples (SL); duplo (DL) e duplo com indução de ar (DLI), com seis repetições. Determinou-se o diâmetro da mediana volumétrica; densidade de gotas; amplitude relativa e o potencial risco de deriva. Na etapa seguinte à deriva foi quantificada em túnel de vento, empregando o DIC em parcela sub subdividida, sendo avaliadas as quatro soluções de aplicação (Parcelas), os três modelos de pontas (Subparcelas), em duas velocidades de vento (Sub subparcelas): 1,0 e 2,0 m s-1, com quatro repetições. Independentemente da solução de aplicação, a ponta DL apresentou os maiores valores de deriva, seguida da SL e DLI, respectivamente. A solução de aplicação água + óleo mineral + glifosato, proporcionou os menores valores de deriva para todas pontas hidráulicas avaliadas. A interação do glifosato com o óleo mineral, aplicado com a ponta DLI, tem potencial para reduzir a deriva no campo.   Palavras-chave: tecnologia de aplicação, túnel de vento, espectro de gotas, redução de perdas, controle de qualidade.   Interactions between adjuvant and hydraulic nozzles in the control of glyphosate drift   ABSTRACT: The aim of this work was to analyze the interactions between adjuvant and the hydraulic nozzle in glyphosate drift control. Firstly, the droplet spectrum was evaluated using a completely randomized design (DIC) in a split plot, evaluating four application solutions (plots): water; water + mineral oil; water + glyphosate; water + mineral oil + glyphosate and three nozzle spray models (subplots): simple (SL); double (DL) and double with air induction (DLI), with six repetitions. The diameter of the volumetric median was determined; droplet density; relative amplitude and the potential risk of drift. In the following stage the drift was quantified in a wind tunnel, using the sub-subdivided DIC, being evaluated the four application solutions (parcels), the three nozzle spray models (subplots), in two wind speeds (sub-plots): 1.0 and 2.0 m s-1, with four repetitions. Regardless of the application solution, the DL tip presented the highest drift values, followed by SL and DLI, respectively. The application solution water + mineral oil + glyphosate, provided the lowest drift values ​​for all hydraulic tips evaluated. The interaction of glyphosate with mineral oil, applied with the DLI tip, has the potential to reduce drift in the field.   Keywords: application technology, wind tunnel, spectrum of drops, loss reduction, quality control.


2000 ◽  
pp. 167
Author(s):  
K. Narayanan Nair ◽  
Edmilson Dias de Freitas ◽  
Odon R. C. Sanchez ◽  
Maria Assunção Faus da Silva Dias ◽  
Maria De Fátima Andrade

As variações espaciais e temporais da Camada Limite planetária (CLP) da Área Metropolitana da cidade de São Paulo (RMSP) durante o período de 23 de julho a 15 de Agosto de 1999 são estudas utilizando dados de um Sodar Doppler. RMSP (λ = 23º34’ S e φ = 46º44’ W) está numa altitude de 800 m acima do nível médio do mar, localizada 60 km à noroeste do oceano Atlântico, limitada por cadeias de montanhas ao norte, tendo uma orografia complexa e configura-se numa ilha de calor urbana.Este trabalho tem o objetivo de entender o impacto da urbanização sobre os processos de CLP particularmente durante a estação de inverno. Um número de diferentes tipos de experimentos estiveram em operação durante uma campanha de inverno organizada pelo IAG-USP. O Sodar Doppler fornece dados sobre (i) função estrutura de temperatura, CT2, (ii) velocidade do vento horizontal, u, (iii) velocidade do vento vertical, w, (iv) desvios padrão do vento horizontal e vertical, σu, σv e σw, e (v) altura da inversão de temperatura, Zi.A análise dos dados fornecidos pelo Sodar mostra claramente as variações desses parâmetros em alturas indo de 50 m até 1500 m com intervalos de 50 m num intervalo de tempo de 15 minutos. Existe grande variação desses parâmetros com a altura.O aumento noturno no campo do vento horizontal com a altura é bem marcado indicando a quase ausência de transporte vertical de momento horizontal durante a noite em condições estáveis. Durante as horas da manhã a aceleração na velocidade do vento é evidente. O aumento anormal em Zi durante a noite sob condições estáveis prevalece durante o inverno com valores mais altos em agosto do que em julho.


2010 ◽  
Vol 49 (12) ◽  
pp. 2574-2590 ◽  
Author(s):  
Eduardo Barbaro ◽  
Amauri P. Oliveira ◽  
Jacyra Soares ◽  
Georgia Codato ◽  
Maurício J. Ferreira ◽  
...  

Abstract This work describes the seasonal and diurnal variations of downward longwave atmospheric irradiance (LW) at the surface in São Paulo, Brazil, using 5-min-averaged values of LW, air temperature, relative humidity, and solar radiation observed continuously and simultaneously from 1997 to 2006 on a micrometeorological platform, located at the top of a 4-story building. An objective procedure, including 2-step filtering and dome emission effect correction, was used to evaluate the quality of the 9-yr-long LW dataset. The comparison between LW values observed and yielded by the Surface Radiation Budget project shows spatial and temporal agreement, indicating that monthly and annual average values of LW observed in one point of São Paulo can be used as representative of the entire metropolitan region of São Paulo. The maximum monthly averaged value of the LW is observed during summer (389 ± 14 W m−2; January), and the minimum is observed during winter (332 ± 12 W m−2; July). The effective emissivity follows the LW and shows a maximum in summer (0.907 ± 0.032; January) and a minimum in winter (0.818 ± 0.029; June). The mean cloud effect, identified objectively by comparing the monthly averaged values of the LW during clear-sky days and all-sky conditions, intensified the monthly average LW by about 32.0 ± 3.5 W m−2 and the atmospheric effective emissivity by about 0.088 ± 0.024. In August, the driest month of the year in São Paulo, the diurnal evolution of the LW shows a minimum (325 ± 11 W m−2) at 0900 LT and a maximum (345 ± 12 W m−2) at 1800 LT, which lags behind (by 4 h) the maximum diurnal variation of the screen temperature. The diurnal evolution of effective emissivity shows a minimum (0.781 ± 0.027) during daytime and a maximum (0.842 ± 0.030) during nighttime. The diurnal evolution of all-sky condition and clear-sky day differences in the effective emissivity remain relatively constant (7% ± 1%), indicating that clouds do not change the emissivity diurnal pattern. The relationship between effective emissivity and screen air temperature and between effective emissivity and water vapor is complex. During the night, when the planetary boundary layer is shallower, the effective emissivity can be estimated by screen parameters. During the day, the relationship between effective emissivity and screen parameters varies from place to place and depends on the planetary boundary layer process. Because the empirical expressions do not contain enough information about the diurnal variation of the vertical stratification of air temperature and moisture in São Paulo, they are likely to fail in reproducing the diurnal variation of the surface emissivity. The most accurate way to estimate the LW for clear-sky conditions in São Paulo is to use an expression derived from a purely empirical approach.


2018 ◽  
Vol 176 ◽  
pp. 06015 ◽  
Author(s):  
Márcia T. A. Marques ◽  
Gregori de A. Moreira ◽  
Maciel Pinero ◽  
Amauri P. Oliveira ◽  
Eduardo Landulfo

This study aims to compare the planetary boundary layer height (PBLH) values estimated by radiosonde data through the bulk Richardson number (BRN) method and by Doppler lidar measurements through the Carrier to Noise Ratio (CNR) method, which corresponds to the maximum of the variance of CNR profile. The measurement campaign was carried during the summer of 2015/2016 in the city of São Paulo. Despite the conceptual difference between these methods, the results show great agreement between them.


2010 ◽  
Vol 43 (5) ◽  
pp. 596-598 ◽  
Author(s):  
Vidal Haddad Junior ◽  
Ivan Sazima

In recent years, attacks by piranhas have become a common problem in dammed portions of rivers and streams in the State of Sao Paulo, Southeastern Brazil. In two outbreaks recorded in two neighboring counties in the Northwest region of the state, 74 bathers were bitten. Only one bite per person was recorded during a short period of the year. The bites were related to parental care and/or defense of spawning territory, which confirms previous studies and demystify the attacks by these legendary fish, as they are perceived by most people. Placement of fine mesh nets and removal of aquatic vegetation stopped the attacks.


2020 ◽  
Vol 7 (2) ◽  
Author(s):  
Maciel Piñero Sánchez ◽  
Amauri Pereira Oliveira ◽  
Ramón Pérez Varona ◽  
Janet Valdés Tito ◽  
Georgia Codato ◽  
...  

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