Guide to Understanding Condensation
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Role of the Dew Water on the Ground Surface in HONO Distribution: a Case Measurement in Melpitz
Atmos. Chem. Phys., 20, 13069–13089, 2020 https://doi.org/10.5194/acp-20-13069-2020 © Author(s) 2020. This work is distributed under the Creative Commons Attribution 4.0 License. Role of the dew water on the ground surface in HONO distribution: a case measurement in Melpitz Yangang Ren1, Bastian Stieger2, Gerald Spindler2, Benoit Grosselin1, Abdelwahid Mellouki1, Thomas Tuch2, Alfred Wiedensohler2, and Hartmut Herrmann2 1Institut de Combustion, Aérothermique, Réactivité et Environnement (ICARE), CNRS (UPR 3021), Observatoire des Sciences de l’Univers en région Centre (OSUC), 1C Avenue de la Recherche Scientifique, 45071 Orléans CEDEX 2, France 2Leibniz Institute for Tropospheric Research (TROPOS), Permoserstraße 15, 04318 Leipzig, Germany Correspondence: Abdelwahid Mellouki ([email protected]) and Hartmut Herrmann ([email protected]) Received: 25 November 2019 – Discussion started: 30 January 2020 Revised: 27 August 2020 – Accepted: 13 September 2020 – Published: 9 November 2020 Abstract. To characterize the role of dew water for the eas that provide a large amount of ground surface based on ground surface HONO distribution, nitrous acid (HONO) the OH production rate calculation. measurements with a Monitor for AeRosols and Gases in am- bient Air (MARGA) and a LOng Path Absorption Photome- ter (LOPAP) instrument were performed at the Leibniz In- 1 Introduction stitute for Tropospheric Research (TROPOS) research site in Melpitz, Germany, from 19 to 29 April 2018. The dew water Nitrous acid (HONO) is important in atmospheric chemistry was also collected and analyzed from 8 to 14 May 2019 using as its photolysis (Reaction R1) is an important source of OH a glass sampler. The high time resolution of HONO measure- radicals. -
Electricity Demand Reduction in Sydney and Darwin with Local Climate Mitigation
P. Rajagopalan and M.M Andamon (eds.), Engaging Architectural Science: Meeting the Challenges of Higher Density: 52nd 285 International Conference of the Architectural Science Association 2018, pp.285–293. ©2018, The Architectural Science Association and RMIT University, Australia. Electricity demand reduction in Sydney and Darwin with local climate mitigation Riccardo Paolini UNSW Built Environment, UNSW Sydney, Australia [email protected] Shamila Haddad UNSW Built Environment, UNSW Sydney, Australia [email protected] Afroditi Synnefa UNSW Built Environment, UNSW Sydney, Australia [email protected] Samira Garshasbi UNSW Built Environment, UNSW Sydney, Australia [email protected] Mattheos Santamouris UNSW Built Environment, UNSW Sydney, Australia [email protected] Abstract: Urban overheating in synergy with global climate change will be enhanced by the increasing population density and increased land use in Australian Capital Cities, boosting the total and peak electricity demand. Here we assess the relation between ambient conditions and electricity demand in Sydney and Darwin and the impact of local climate mitigation strategies including greenery, cool materials, water and their combined use at precinct scale. By means of a genetic algorithm, we produced two site-specific surrogate models, for New South Wales and Darwin CBD, to compute the electricity demand as a function of air temperature, humidity and incoming solar radiation. For Western Sydney, the total electricity savings computed under the different mitigation scenarios range between 0.52 and 0.91 TWh for the summer of 2016/2017, namely 4.5 % of the total, with the most relevant saving concerning the peak demand, equal to 9 % with cool materials and water sprinkling. -
A Comprehensive Review of Thermal Energy Storage
sustainability Review A Comprehensive Review of Thermal Energy Storage Ioan Sarbu * ID and Calin Sebarchievici Department of Building Services Engineering, Polytechnic University of Timisoara, Piata Victoriei, No. 2A, 300006 Timisoara, Romania; [email protected] * Correspondence: [email protected]; Tel.: +40-256-403-991; Fax: +40-256-403-987 Received: 7 December 2017; Accepted: 10 January 2018; Published: 14 January 2018 Abstract: Thermal energy storage (TES) is a technology that stocks thermal energy by heating or cooling a storage medium so that the stored energy can be used at a later time for heating and cooling applications and power generation. TES systems are used particularly in buildings and in industrial processes. This paper is focused on TES technologies that provide a way of valorizing solar heat and reducing the energy demand of buildings. The principles of several energy storage methods and calculation of storage capacities are described. Sensible heat storage technologies, including water tank, underground, and packed-bed storage methods, are briefly reviewed. Additionally, latent-heat storage systems associated with phase-change materials for use in solar heating/cooling of buildings, solar water heating, heat-pump systems, and concentrating solar power plants as well as thermo-chemical storage are discussed. Finally, cool thermal energy storage is also briefly reviewed and outstanding information on the performance and costs of TES systems are included. Keywords: storage system; phase-change materials; chemical storage; cold storage; performance 1. Introduction Recent projections predict that the primary energy consumption will rise by 48% in 2040 [1]. On the other hand, the depletion of fossil resources in addition to their negative impact on the environment has accelerated the shift toward sustainable energy sources. -
Chapter 3 Bose-Einstein Condensation of an Ideal
Chapter 3 Bose-Einstein Condensation of An Ideal Gas An ideal gas consisting of non-interacting Bose particles is a ¯ctitious system since every realistic Bose gas shows some level of particle-particle interaction. Nevertheless, such a mathematical model provides the simplest example for the realization of Bose-Einstein condensation. This simple model, ¯rst studied by A. Einstein [1], correctly describes important basic properties of actual non-ideal (interacting) Bose gas. In particular, such basic concepts as BEC critical temperature Tc (or critical particle density nc), condensate fraction N0=N and the dimensionality issue will be obtained. 3.1 The ideal Bose gas in the canonical and grand canonical ensemble Suppose an ideal gas of non-interacting particles with ¯xed particle number N is trapped in a box with a volume V and at equilibrium temperature T . We assume a particle system somehow establishes an equilibrium temperature in spite of the absence of interaction. Such a system can be characterized by the thermodynamic partition function of canonical ensemble X Z = e¡¯ER ; (3.1) R where R stands for a macroscopic state of the gas and is uniquely speci¯ed by the occupa- tion number ni of each single particle state i: fn0; n1; ¢ ¢ ¢ ¢ ¢ ¢g. ¯ = 1=kBT is a temperature parameter. Then, the total energy of a macroscopic state R is given by only the kinetic energy: X ER = "ini; (3.2) i where "i is the eigen-energy of the single particle state i and the occupation number ni satis¯es the normalization condition X N = ni: (3.3) i 1 The probability -
לב שלם Siddur Lev Shalem לשבת ויום טוב for Shabbat & FESTIVALS
סדור לב שלם Siddur Lev Shalem לשבת ויום טוב for shabbat & fEstIVaLs For restricted use only: March-April 2020 Do not copy, sell, or distribute the rabbinical assembly Copyright © 2016 by The Rabbinical Assembly, Inc. First edition. All rights reserved. No part of this book may be reproduced or transmitted in any form The Siddur Lev Shalem Committee or by any means, electronic or mechanical, including photocopy, recording or any information storage or retrieval system, except Rabbi Edward Feld, Senior Editor and Chair for brief passages in connection with a critical review, without permission in writing from: Rabbi Jan Uhrbach, Associate Editor The Rabbinical Assembly Rabbi David M. Ackerman 3080 Broadway New York, NY 10027 Ḥazzan Joanna Dulkin www.rabbinicalassembly.org Rabbi Amy Wallk Katz Permissions and copyrights for quoted materials may be found on pages 463–465. Rabbi Cantor Lilly Kaufman isbn: 978-0-916219-64-2 Rabbi Alan Lettofsky Library of Congress Cataloging-in-Publication Data is available. Rabbi Robert Scheinberg Designed, composed, and produced by Scott-Martin Kosofsky at The Philidor Company, Rabbi Carol Levithan, ex officio Rhinebeck, New York. www.philidor.com The principal Hebrew type, Milon (here in its second and third Rabbi Julie Schonfeld, ex officio iterations), was designed and made by Scott-Martin Kosofsky; it was inspired by the work of Henri Friedlaender. The principal roman and italic is Rongel, by Mário Feliciano; the sans serif is Cronos, by Robert Slimbach. The Hebrew sans serif is Myriad Hebrew, by Robert Slimbach with Scott-Martin Kosofsky. Printed and bound by LSC Communications, Crawfordsville, Indiana. -
Initial Start-Up When Starting up the Cooler Refrigeration System for the First Time, the Following Events Occur
SEQUENCE OF OPERATION COOLERS AND FREEZERS COOLERS All standard units are equipped with an adjustable thermostat located on the lower right hand side of the evaporator coil, on the inside of the walk-in. All units are set at the factory to the temperature requested by the customer. Minor adjustments in operating temperature may be made to suit your needs by a qualified refrigeration technician. Polar King recommends that you do not set the temperature colder than required, as this will cause unnecessary power consumption. Recommended temperature for a cooler ranges from +34° to +37° F, unless specified otherwise for special applications. Refrigeration - Initial Start-Up When starting up the cooler refrigeration system for the first time, the following events occur. The operating sequence is as follows: (1) Thermostat calls for refrigerant. (2) Liquid line solenoid valve opens, allowing refrigerant to flow. (3) Pressure control makes the control circuit and the condensing unit operates. (4) When the room thermostat is satisfied, the liquid line solenoid will close, and the compressor will pump down and turn off. (Fan on unit cooler will continue to run.) These units are designed for application conditions 33°F and above. CAUTION: DO NOT SET A COOLER BELOW 32°F OR DAMAGE MAY OCCUR. Defrost Defrost is accomplished during refrigeration off cycle. Four defrost cycles per day are programmed at the factory (4 a.m., 10 a.m., 4 p.m., and 10:00 p.m.). It may be necessary to change the defrost cycle times to fit your work schedule. The interior temperature may rise slightly during the defrost cycle. -
Disparities in Ammonia, Temperature, Humidity, and Airborne Particulate Matter Between the Micro-And Macroenvironments of Mice in Individually Ventilated Caging
Journal of the American Association for Laboratory Animal Science Vol 49, No 2 Copyright 2010 March 2010 by the American Association for Laboratory Animal Science Pages 177–183 Disparities in Ammonia, Temperature, Humidity, and Airborne Particulate Matter between the Micro-and Macroenvironments of Mice in Individually Ventilated Caging Matthew D Rosenbaum,1 Susan VandeWoude,2 John Volckens,3 and Thomas E Johnson3,* Animal room environmental parameters typically are monitored with the assumption that the environment within the cage closely mirrors the room environment. This study evaluated that premise by examining macro- (room) and microenvi- ronmental (cage) parameters in individually ventilated cages housing mice with variable amounts of bedding over a period of 17 d without cage changes. Intracage ammonia levels remained within recommended human guidelines but were higher than room levels, confirming that microisolation caging is efficient at preventing ammonia generated from animal waste from escaping into the room. Humidity and temperature within cages were consistently higher than room levels. Particles in the room predominantly consisted of fine particles (diameter less than 2.5 µm), presumably from the ambient atmosphere; some of these particles were found in the cage microenvironment. In addition, mouse activity within cages produced larger particles, and these particles contributed to substantially higher aerosol mass concentrations within the cage. These findings demonstrate that, although cage and room environmental parameters differ, knowledge of room environmental conditions can be used to predict certain conditions within the cage. This association is relevant in that typical animal care standard operat- ing procedures rely on room measurements, not intracage measurements, which arguably are more important for assessing animal welfare. -
At the Request of the District, Environmental Control Systems, Inc, the District's Environmental Risk Engineers, Visited Charl
Environmental Control Systems, Inc. Indoor Air Quality Investigation Charles F. Patton Middle School Executive Summary At the request of the district, Environmental Control Systems, Inc, the district’s environmental risk engineers, visited Charles F. Patton Middle School to visually assess surfaces and test the air quality in various regions of the school building. This process was completed on Wednesday, November 21 during the regular school day when school was in session. Upon their professional inspection and review, Environmental Control Systems concluded that there is no evidence of mold at Charles F. Patton Middle School. Below is a summary of the report provided by Environmental Control Systems, Inc. You may view the complete report by clicking here. Indoor Air Quality Investigation Report Summary - November 21, 2018 1. Currently, there are no EPA, CDC or OSHA regulations or standards for airborne mold contaminants, therefore, there are no quantitative health-based guidelines, values, or thresholds for acceptable, tolerable, or normal concentrations for airborne fungi spores. 2. Generally speaking, indoor mold types should be similar to, and airborne concentrations should be no greater than, those found outdoors and in non-complaint areas. 3. According to the EPA, there is no practical way to eliminate all mold and mold spores in an indoor environment. Spores can be found almost anywhere and can grow on virtually any substance, providing moisture is present. 4. Mold may begin growing indoors when mold spores land on wet surfaces. There are many types of mold, but none of them will grow without water. At the time of this investigation, there was no condensation on any horizontal or vertical surfaces as all surfaces were equal to or higher than room temperature. -
It's Just a Phase!
BASIS Lesson Plan Lesson Name: It’s Just a Phase! Grade Level Connection(s) NGSS Standards: Grade 2, Physical Science FOSS CA Edition: Grade 3 Physical Science: Matter and Energy Module *Note to teachers: Detailed standards connections can be found at the end of this lesson plan. Teaser/Overview Properties of matter are illustrated through a series of demonstrations and hands-on explorations. Students will learn to identify solids, liquids, and gases. Water will be used to demonstrate the three phases. Students will learn about sublimation through a fun experiment with dry ice (solid CO2). Next, they will compare the propensity of several liquids to evaporate. Finally, they will learn about freezing and melting while making ice cream. Lesson Objectives ● Students will be able to identify the three states of matter (solid, liquid, gas) based on the relative properties of those states. ● Students will understand how to describe the transition from one phase to another (melting, freezing, evaporation, condensation, sublimation) ● Students will learn that matter can change phase when heat/energy is added or removed Vocabulary Words ● Solid: A phase of matter that is characterized by a resistance to change in shape and volume. ● Liquid: A phase of matter that is characterized by a resistance to change in volume; a liquid takes the shape of its container ● Gas: A phase of matter that can change shape and volume ● Phase change: Transformation from one phase of matter to another ● Melting: Transformation from a solid to a liquid ● Freezing: Transformation -
ESSENTIALS of METEOROLOGY (7Th Ed.) GLOSSARY
ESSENTIALS OF METEOROLOGY (7th ed.) GLOSSARY Chapter 1 Aerosols Tiny suspended solid particles (dust, smoke, etc.) or liquid droplets that enter the atmosphere from either natural or human (anthropogenic) sources, such as the burning of fossil fuels. Sulfur-containing fossil fuels, such as coal, produce sulfate aerosols. Air density The ratio of the mass of a substance to the volume occupied by it. Air density is usually expressed as g/cm3 or kg/m3. Also See Density. Air pressure The pressure exerted by the mass of air above a given point, usually expressed in millibars (mb), inches of (atmospheric mercury (Hg) or in hectopascals (hPa). pressure) Atmosphere The envelope of gases that surround a planet and are held to it by the planet's gravitational attraction. The earth's atmosphere is mainly nitrogen and oxygen. Carbon dioxide (CO2) A colorless, odorless gas whose concentration is about 0.039 percent (390 ppm) in a volume of air near sea level. It is a selective absorber of infrared radiation and, consequently, it is important in the earth's atmospheric greenhouse effect. Solid CO2 is called dry ice. Climate The accumulation of daily and seasonal weather events over a long period of time. Front The transition zone between two distinct air masses. Hurricane A tropical cyclone having winds in excess of 64 knots (74 mi/hr). Ionosphere An electrified region of the upper atmosphere where fairly large concentrations of ions and free electrons exist. Lapse rate The rate at which an atmospheric variable (usually temperature) decreases with height. (See Environmental lapse rate.) Mesosphere The atmospheric layer between the stratosphere and the thermosphere. -
Capillary Condensation of Colloid–Polymer Mixtures Confined
INSTITUTE OF PHYSICS PUBLISHING JOURNAL OF PHYSICS: CONDENSED MATTER J. Phys.: Condens. Matter 15 (2003) S3411–S3420 PII: S0953-8984(03)66420-9 Capillary condensation of colloid–polymer mixtures confined between parallel plates Matthias Schmidt1,Andrea Fortini and Marjolein Dijkstra Soft Condensed Matter, Debye Institute, Utrecht University, Princetonplein 5, 3584 CC Utrecht, The Netherlands Received 21 July 2003 Published 20 November 2003 Onlineatstacks.iop.org/JPhysCM/15/S3411 Abstract We investigate the fluid–fluid demixing phase transition of the Asakura–Oosawa model colloid–polymer mixture confined between two smooth parallel hard walls using density functional theory and computer simulations. Comparing fluid density profiles for statepoints away from colloidal gas–liquid coexistence yields good agreement of the theoretical results with simulation data. Theoretical and simulation results predict consistently a shift of the demixing binodal and the critical point towards higher polymer reservoir packing fraction and towards higher colloid fugacities upon decreasing the plate separation distance. This implies capillary condensation of the colloid liquid phase, which should be experimentally observable inside slitlike micropores in contact with abulkcolloidal gas. 1. Introduction Capillary condensation denotes the phenomenon that spatial confinement can stabilize a liquid phase coexisting with its vapour in bulk [1, 2]. In order for this to happen the attractive interaction between the confining walls and the fluid particles needs to be sufficiently strong. Although the main body of work on this subject has been done in the context of confined simple liquids, one might expect that capillary condensation is particularly well suited to be studied with colloidal dispersions. In these complex fluids length scales are on the micron rather than on the ångstrom¨ scale which is typical for atomicsubstances. -
Heat Index Climatology for the North-Central United States
HEAT INDEX CLIMATOLOGY FOR THE NORTH-CENTRAL UNITED STATES Todd Rieck National Weather Service La Crosse, Wisconsin 1. Introduction middle Mississippi River Valleys, and the western Great Lakes. Also, the physiological Heat is an underrated danger, with an response to heat will be briefly investigated, average of 175 Americans losing their lives including a review of how heat acclimatization annually from heat-related causes. According to affects the human body’s biology. This the Centers for Disease Control and Prevention, protective biological response is an important from 1979-2003 excessive heat exposure consideration when evaluating the impact of the caused 8,015 deaths in the United States. heat on those that are, or are not, acclimatized During this period, more people died from to the heat. extreme heat than from hurricanes, lightning, tornadoes, and floods combined. In this study, 95°F will be used as the start for the climatological analysis as prolonged Heat kills by taxing the human body beyond exposure to heat this warm increases the risk of its ability to cool itself. Cooling is primarily sunstroke, heat cramps, and heat exhaustion accomplished by the evaporation of perspiration. (Table 1) . How efficiently this process functions is directly related to the amount of water vapor in the air. 2. Data High moisture content reduces the evaporative cooling rate of perspiration, making it difficult for All available weather observations from the the body to maintain a steady and safe internal National Climatic Data Center were used from temperature. One way to measure the 192 locations (Fig. 1), extending from Utah to combined effect of temperature and moisture on Michigan, and from the Canadian-U.S.