Use Nitrogen Safely
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Air Pressure
Name ____________________________________ Date __________ Class ___________________ SECTION 15-3 SECTION SUMMARY Air Pressure Guide for ir consists of atoms and molecules that have mass. Therefore, air has Reading A mass. Because air has mass, it also has other properties, includ- ing density and pressure. The amount of mass per unit volume of a N What are some of substance is called the density of the substance. The force per unit area the properties of air? is called pressure. Air pressure is the result of the weight of a column of N What instruments air pushing down on an area. The molecules in air push in all directions. are used to mea- This is why air pressure doesn’t crush objects. sure air pressure? Falling air pressure usually indicates that a storm is approaching. Rising N How does increas- air pressure usually means that the weather is clearing. A ing altitude affect barometer is an instrument that measures changes in air pressure. There air pressure and are two kinds of barometers: mercury barometers and aneroid density? barometers. A mercury barometer consists of a glass tube open at the bottom end and partially filled with mercury. The open end of the tube rests in a dish of mercury, and the space above the mercury in the tube contains no air. The air pressure pushing down on the surface of the mer- cury in the dish is equal to the weight of the column of mercury in the tube. At sea level, the mercury column is about 76 centimeters high, on average. An aneroid barometer has an airtight metal chamber that is sen- sitive to changes in air pressure. -
Effect of Tropospheric Air Density and Dew Point Temperature on Radio (Electromagnetic) Waves and Air Radio Wave Refractivity
International Journal of Scientific & Engineering Research, Volume 7, Issue 6, June-2016 356 ISSN 2229-5518 Effect of Tropospheric Air density and dew point temperature on Radio (Electromagnetic) waves and Air radio wave refractivity <Joseph Amajama> University of Calabar, Department of Physics, Electronics and Computer Technology Unit Etta-agbor, Calabar, Nigeria [email protected] Abstract: Signal strengths measurements were obtained half hourly for some hours and simultaneously, the atmospheric components: atmospheric temperature, atmospheric pressure, relative humidity and wind direction and speed were registered to erect the effects of air density and dew point temperature on radio signals (electromagnetic waves) as they travel through the atmosphere and air radio wave refractivity. The signal strength from Cross River State Broadcasting Co-operation Television (CRBC-TV), (4057'54.7''N, 8019'43.7''E) transmitted at 35mdB and 519.25 MHz (UHF) were measured using a Cable TV analyzer in a residence along Ettaabgor, Calabar, Nigeria (4057'31.7''N, 8020'49.7''E) using the digital Community – Access (Cable) Television (CATV) analyzer with 24 channels, spectrum 46 – 870 MHz, connected to a domestic receiver antenna of height 4.23 m. Results show that: on the condition that the wind speed and direction are the same or (0 mph NA), the radio signal strength is near negligibly directly proportional to the air density, mathematically Ss / ∂a1.3029 = K, where Ss is Signal Strength in dB, ∂a is Density of air Kg/m3 and K is constant; radio -
Air Infiltration Glossary (English Edition)
AIRGLOSS: Air Infiltration Glossary (English Edition) Carolyn Allen ~)Copyrlght Oscar Faber Partnership 1981. All property rights, Including copyright ere vested In the Operating Agent (The Oscar Faber Partnership) on behalf of the International Energy Agency. In particular, no part of this publication may be reproduced, stored in a retrieval system or transmitted in any form or by any means, electronic, mechanical, photocopying, recording or otherwise, without the prior written permluion of the operat- ing agent. Contents (i) Preface (iii) Introduction (v) Umr's Guide (v) Glossary Appendix 1 - References 87 Appendix 2 - Tracer Gases 93 Appendix 3 - Abbreviations 99 Appendix 4 - Units 103 (i) (il) Preface International Energy Agency In order to strengthen cooperation In the vital area of energy policy, an Agreement on an International Energy Program was formulated among a number of industrialised countries In November 1974. The International Energy Agency (lEA) was established as an autonomous body within the Organisation for Economic Cooperation and Development (OECD) to administer that agreement. Twenty-one countries are currently members of the lEA, with the Commission of the European Communities participating under a special arrangement. As one element of the International Energy Program, the Participants undertake cooperative activities in energy research, development, and demonstration. A number of new and improved energy technologies which have the potential of making significant contributions to our energy needs were identified for collaborative efforts. The lEA Committee on Energy Research and Development (CRD), assisted by a small Secretariat staff, coordinates the energy research, development, and demonstration programme. Energy Conservation in Buildings and Community Systems The International Energy Agency sponsors research and development in a number of areas related to energy. -
Calculation Exercises with Answers and Solutions
Atmospheric Chemistry and Physics Calculation Exercises Contents Exercise A, chapter 1 - 3 in Jacob …………………………………………………… 2 Exercise B, chapter 4, 6 in Jacob …………………………………………………… 6 Exercise C, chapter 7, 8 in Jacob, OH on aerosols and booklet by Heintzenberg … 11 Exercise D, chapter 9 in Jacob………………………………………………………. 16 Exercise E, chapter 10 in Jacob……………………………………………………… 20 Exercise F, chapter 11 - 13 in Jacob………………………………………………… 24 Answers and solutions …………………………………………………………………. 29 Note that approximately 40% of the written exam deals with calculations. The remainder is about understanding of the theory. Exercises marked with an asterisk (*) are for the most interested students. These exercises are more comprehensive and/or difficult than questions appearing in the written exam. 1 Atmospheric Chemistry and Physics – Exercise A, chap. 1 – 3 Recommended activity before exercise: Try to solve 1:1 – 1:5, 2:1 – 2:2 and 3:1 – 3:2. Summary: Concentration Example Advantage Number density No. molecules/m3, Useful for calculations of reaction kmol/m3 rates in the gas phase Partial pressure Useful measure on the amount of a substance that easily can be converted to mixing ratio Mixing ratio ppmv can mean e.g. Concentration relative to the mole/mole or partial concentration of air molecules. Very pressure/total pressure useful because air is compressible. Ideal gas law: PV = nRT Molar mass: M = m/n Density: ρ = m/V = PM/RT; (from the two equations above) Mixing ratio (vol): Cx = nx/na = Px/Pa ≠ mx/ma Number density: Cvol = nNav/V 26 -1 Avogadro’s -
Guidance Document Cryogenic Liquids
Guidance Document Cryogenic Liquids [This is a brief and general summary. Read the full MSDS for more details before handling.] Introduction: All cryogenic liquids are gases at normal temperature and pressure. The liquids are formed by cooling the gases below room temperature, followed by compression which liquefies them. Cryogenic liquids are kept in the liquid state at very low temperatures. Cryogenic liquids have boiling points below -73°C (-100°F). The most common cryogenic liquids currently on campus are liquid nitrogen, liquid argon and liquid helium. The different cryogens become liquids under different conditions of temperature and pressure. But all have two very important properties in common. First, the liquids and their vapors are extremely cold. The risk of destructive freezing of tissues is always present. In addition, when they vaporize the liquids expand to enormous volumes. For example, liquid nitrogen will expand 696 times as it vaporizes. Vaporization in a sealed container could rupture the vessel. Vaporization in an enclosed workspace could cause asphixiation by displacing air needed to support life. All of the cryogenic liquids on campus are inert, colorless, odorless, non-corrosive and non- flammable. Not all cryogens fit this description. Special permission would be required to use other cryogenic liquids. Liquid oxygen could produce an oxygen-rich atmosphere which could accelerate combustion of other materials. Liquid hydrogen, liquid methane or liquefied natural gas could form an extremely flammable mixture with air. Liquid carbon monoxide is extremely toxic and extremely flammable. Cryogenic liquids are received from the vendor in special vacuum jacketed cylinders, which allows for storage of the liquefied gas for a long time. -
CE-087 Calculation of Gas Density and Viscosity
CE‐087 Calculation of Gas Density and Viscosity Instructor: Harlan Bengtson, PhD, P.E. Course ID: CE‐087 PDH Hours: 2 PDH PDH Star | T / F: (833) PDH‐STAR (734‐7827) | E: [email protected] Calculation of Gas Density and Viscosity Harlan H. Bengtson, PhD, P.E. COURSE CONTENT 1. Introduction The density and/or viscosity of a gas is often needed for some other calculation, such as pipe flow or heat exchanger calculations. This course contains discussion of, and example calculation of, the density and viscosity of a specified gas at a given temperature and pressure. If the gas temperature is high relative to its critical temperature and the gas pressure is low relative to its critical pressure, then it can be treated as an ideal gas and its density can be calculated at a specified temperature and pressure using the ideal gas law. If the density of a gas is needed at a temperature and pressure at which it cannot be treated as an ideal gas law, however, then the compressibility factor of the gas must be calculated and used in calculating its density. In this course, the Redlich Kwong equation will be used for calculation of the compressibility factor of a gas. The Sutherland formula can be used to calculate the viscosity of a gas at a specified temperature and pressure if the Sutherland constants are available for the gas. It will be discussed and used in example calculations. Another method for calculating the viscosity of air at a specified temperature and pressure will also be presented and discussed. -
Air Separation Plants. History and Technological Progress in the Course of Time
Air separation plants. History and technological progress in the course of time. History and technological progress of air separation 03 When and how did air separation start? In May 1895, Carl von Linde performed an experiment in his laboratory in Munich that led to his invention of the first continuous process for the liquefaction of air based on the Joule-Thomson refrigeration effect and the principle of countercurrent heat exchange. This marked the breakthrough for cryogenic air separation. For his experiment, air was compressed Linde based his experiment on findings from 20 bar [p₁] [t₄] to 60 bar [p₂] [t₅] in discovered by J. P. Joule and W. Thomson the compressor and cooled in the water (1852). They found that compressed air cooler to ambient temperature [t₁]. The pre- expanded in a valve cooled down by approx. cooled air was fed into the countercurrent 0.25°C with each bar of pressure drop. This Carl von Linde in 1925. heat exchanger, further cooled down [t₂] proved that real gases do not follow the and expanded in the expansion valve Boyle-Mariotte principle, according to which (Joule-Thomson valve) [p₁] to liquefaction no temperature decrease is to be expected temperature [t₃]. The gaseous content of the from expansion. An explanation for this effect air was then warmed up again [t₄] in the heat was given by J. K. van der Waals (1873), who exchanger and fed into the suction side of discovered that the molecules in compressed the compressor [p₁]. The hourly yield from gases are no longer freely movable and this experiment was approx. -
Hazard Analysis CONSEQUENCE ANALYSIS for CHEVRON HYDROGEN PLANT
Appendix C Hazard Analysis CONSEQUENCE ANALYSIS FOR CHEVRON HYDROGEN PLANT Prepared For Environmental Audit, Inc. 1000-A Ortega Way Placentia, California 92670-7125 Prepared By Quest Consultants Inc.® 908 26th Avenue N.W. Norman, Oklahoma 73069 Telephone: 405-329-7475 Fax: 405-329-7734 03-04-6477 April 21, 2003 QUEST CONSEQUENCE ANALYSIS FOR CHEVRON HYDROGEN PLANT Introduction Quest Consultants Inc. has performed a series of release, vapor dispersion, and fire radiation calculations in an effort to quantify the consequences following a release from various process lines on the premises of Chevron’s proposed Hydrogen Plant in the El Segundo Refinery. The releases were designed to simulate what would happen if one of several lines containing either anhydous ammonia (AnNH3), aqueous ammonia (AqNH3), natural/fuel gas, hydrogen (H2), or pentanes was to fully fail and the material contained therein was released to the environment. Site-Specific Information Several of the parameters defined in the analysis are: Toxic Material Pipelines Proposed AnNH 3 Proposed AqNH Parameters Current AnNH Feed to 3 3 to New Hydrogen Plant Hydrogen Plant Pipeline diameter 2-inch 2-inch 2-inch Aqueous ammonia Material composition Anhydrous ammonia Anhydrous ammonia (30% by weight in water) Temperature 87°F 87°F 87°F Pressure 170 psig 170 psig 180 psig Average flow rate 13 gpm 13 gpm 216 gpd Approximate length of pipeline 5,000 ft 1,100 ft 750 ft Fuel Gas and Pentanes Pipelines Proposed Proposed Proposed Parameters Natural Gas Line Fuel Gas Line Pentanes Line Pipeline -
The Noble Gases
INTERCHAPTER K The Noble Gases When an electric discharge is passed through a noble gas, light is emitted as electronically excited noble-gas atoms decay to lower energy levels. The tubes contain helium, neon, argon, krypton, and xenon. University Science Books, ©2011. All rights reserved. www.uscibooks.com Title General Chemistry - 4th ed Author McQuarrie/Gallogy Artist George Kelvin Figure # fig. K2 (965) Date 09/02/09 Check if revision Approved K. THE NOBLE GASES K1 2 0 Nitrogen and He Air P Mg(ClO ) NaOH 4 4 2 noble gases 4.002602 1s2 O removal H O removal CO removal 10 0 2 2 2 Ne Figure K.1 A schematic illustration of the removal of O2(g), H2O(g), and CO2(g) from air. First the oxygen is removed by allowing the air to pass over phosphorus, P (s) + 5 O (g) → P O (s). 20.1797 4 2 4 10 2s22p6 The residual air is passed through anhydrous magnesium perchlorate to remove the water vapor, Mg(ClO ) (s) + 6 H O(g) → Mg(ClO ) ∙6 H O(s), and then through sodium hydroxide to remove 18 0 4 2 2 4 2 2 the carbon dioxide, NaOH(s) + CO2(g) → NaHCO3(s). The gas that remains is primarily nitrogen Ar with about 1% noble gases. 39.948 3s23p6 36 0 The Group 18 elements—helium, K-1. The Noble Gases Were Kr neon, argon, krypton, xenon, and Not Discovered until 1893 83.798 radon—are called the noble gases 2 6 4s 4p and are noteworthy for their rela- In 1893, the English physicist Lord Rayleigh noticed 54 0 tive lack of chemical reactivity. -
Revised Formula for the Density of Moist Air (CIPM-2007)
IOP PUBLISHING METROLOGIA Metrologia 45 (2008) 149–155 doi:10.1088/0026-1394/45/2/004 Revised formula for the density of moist air (CIPM-2007) A Picard1,RSDavis1,MGlaser¨ 2 and K Fujii3 1 Bureau International des Poids et Mesures, Pavillon de Breteuil, F-92310 Sevres` Cedex, France 2 Physikalisch-Technische Bundesanstalt, Bundesallee 100, D-38116 Braunschweig, Germany 3 National Metrology Institute of Japan, National Institute of Advanced Industrial Science and Technology (NMIJ/AIST), Central 3, 1-1, Umezono 1-chome, Tsukuba, Ibaraki 305-8563, Japan Received 8 January 2008 Published 18 February 2008 Online at stacks.iop.org/Met/45/149 Abstract Measurements of air density determined gravimetrically and by using the CIPM-81/91 formula, an equation of state, have a relative deviation of 6.4 × 10−5. This difference is consistent with a new determination of the mole fraction of argon xAr carried out in 2002 by the Korea Research Institute of Standards and Science (KRISS) and with recently published results from the LNE. The CIPM equation is based on the molar mass of dry air, which is dependent on the contents of the atmospheric gases, including the concentration of argon. We accept the new argon value as definitive and amend the CIPM-81/91 formula accordingly. The KRISS results also provide a test of certain assumptions concerning the mole fractions of oxygen and carbon dioxide in air. An updated value of the molar gas constant R is available and has been incorporated in the CIPM-2007 equation. In making these changes, we have also calculated the uncertainty of the CIPM-2007 equation itself in conformance with the Guide to the Expression of Uncertainty in Measurement, which was not the case for previous versions of this equation. -
Direct Determination of Air Density in a Balance Through Artifacts
JOURNAL OF RESEARCH of the National Bureau of Standards Vol. 83, No.5, Septem ber- October 197B ::> I Dired Detennination of Air Density in a Balance Through Artifads Charaderized in an Evacuated Weighing Chamber. W. F. Koch Center for AnalytiCXJI Oremistry, National Bureau of Standards, Washington, DC 20234 R. S. Davis and V. E. Bower Centerfor Absolute Physirol Quantities, National Bureau of Standards, Washington, DC 20234 June 29, 1978 This paper describes a s imple device wh ich permit s mass comparisons in air without appea l to the correction for ai r buoyancy. The device consists of a ca nister which is evacuated and weighed on a laboratory balance with a mass inside. A second we ighing of another mass in the evacuated cani ster provides th e des ired ma ss com parison. The method was used to deter'm ine the mass difference between two sta inl ess steel weights of widel y differing densi ties. With knowledge of this mass difference and of the volume difference one may, by a simple air weighing of the two objects, determine directl y the densit y of the ai r in the balance case. Densiti es of air d etermin ed by this method were compared with those calc ul ate d from the barometric pressure, the temperature, and the relati ve humidity of the laboratory a ir. The experime nt a l and calculated va lues agree th roughout to within 1.0 fL g cm- 3 (w here the norm al air densit y is about 1.2 mg cm- 3). -
Renewable Energy Carriers: Hydrogen Or Liquid Air / Nitrogen? Yongliang Li, Haisheng Chen, Xinjing Zhang, Chunqing Tan, Yulong Ding
Renewable energy carriers: Hydrogen or liquid air / nitrogen? Yongliang Li, Haisheng Chen, Xinjing Zhang, Chunqing Tan, Yulong Ding To cite this version: Yongliang Li, Haisheng Chen, Xinjing Zhang, Chunqing Tan, Yulong Ding. Renewable energy carriers: Hydrogen or liquid air / nitrogen?. Applied Thermal Engineering, Elsevier, 2010, 30 (14-15), pp.1985. 10.1016/j.applthermaleng.2010.04.033. hal-00660111 HAL Id: hal-00660111 https://hal.archives-ouvertes.fr/hal-00660111 Submitted on 16 Jan 2012 HAL is a multi-disciplinary open access L’archive ouverte pluridisciplinaire HAL, est archive for the deposit and dissemination of sci- destinée au dépôt et à la diffusion de documents entific research documents, whether they are pub- scientifiques de niveau recherche, publiés ou non, lished or not. The documents may come from émanant des établissements d’enseignement et de teaching and research institutions in France or recherche français ou étrangers, des laboratoires abroad, or from public or private research centers. publics ou privés. Accepted Manuscript Title: Renewable energy carriers: Hydrogen or liquid air / nitrogen? Authors: Yongliang Li, Haisheng Chen, Xinjing Zhang, Chunqing Tan, Yulong Ding PII: S1359-4311(10)00196-1 DOI: 10.1016/j.applthermaleng.2010.04.033 Reference: ATE 3093 To appear in: Applied Thermal Engineering Received Date: 29 October 2009 Revised Date: 24 April 2010 Accepted Date: 30 April 2010 Please cite this article as: Y. Li, H. Chen, X. Zhang, C. Tan, Y. Ding. Renewable energy carriers: Hydrogen or liquid air / nitrogen?, Applied Thermal Engineering (2010), doi: 10.1016/ j.applthermaleng.2010.04.033 This is a PDF file of an unedited manuscript that has been accepted for publication.