“Body Temperature & Pressure, Saturated” & Ambient Pressure Correction in Air Medical Transport

Total Page:16

File Type:pdf, Size:1020Kb

“Body Temperature & Pressure, Saturated” & Ambient Pressure Correction in Air Medical Transport “Body Temperature & Pressure, Saturated” & Ambient Pressure Correction in air medical transport Mechanical ventilation can be especially challenging during air medical transport, particularly due to the impact of varying atmospheric pressure with changing altitudes. The Oxylog® 3000 plus and Oxylog® 2000 plus help to effectively deal with these challenges. D-33481-2011 Artificial ventilation uses compressed the ventilation volumes delivered by the gas to deliver the required volume to the ventilator. Mechanical ventilation in fixed patient. This breathing gas has normally wing aircraft without a pressurized cabin an ambient temperature level and is very is subject to the same dynamics. In case dry. Inside the human lungs the gas of a pressurized cabin it is still relevant expands due to a higher temperature and to correct the inspiratory volumes, as humidity level. These physical conditions the cabin is usually maintained at MT-5809-2008 are described as “Body Temperature & a pressure of approximately 800 mbar Figure 1: Oxylog® 3000 plus Pressure, Saturated” (BTPS), which (600 mmHg), comparable to an altitude The Oxylog® 3000 plus automatically com- presumes the combined environmental of 8,200 ft/2,500 m. pensates volume delivery and measurement circumstances of – Without BTPS correction, the deli- – a body temperature of 37 °C / 99 °F vered inspiratory volume can deviate up – ambient barometrical pressure to 14 % conditions and (at 14,800 ft/4,500 m altitude) from – breathing gas saturated with water the targeted set volume (i.e. 570 ml vapour (= 100 % relative humidity). instead of 500 ml). – Without ambient pressure correction, Aside from the challenge of changing the inspiratory volume can deviate up temperatures and humidity inside the to 44 % (at 14,800 ft/4,500 m altitude) patient lungs, the ambient pressure is from the targeted set volume also important to consider. Flight altitudes (i.e. 720 ml instead of 500 ml). MT-5869-2008 in air medical transports can reach up to Figure 2: Oxylog® 2000 plus 14,800 ft/4,500 m. Although helicopter The Oxylog 3000 plus and Oxylog 2000 rescue missions rarely go to altitudes plus automatically correct the delivered that require the body to adapt, alterations volume for BTPS and ambient pressure, associated with the changing ambient while also taking atmospheric pressure pressure can have a significant impact on differences into account. 02 | BTPS & AMBIENT PRESSURE CORRECTION IN AIR MEDICAL TRANSPORT D-33403-2011 Figure 3: Example of a medical interior system With BTPS and ambient pressure correction the operator is able to spend more time on patient care. BTPS CORRECTION IN OXYLOG altitudes in volume controlled ventilation The Oxylog 3000 plus and Oxylog 2000 plus modes. As a result, the volume delivered correct the delivered and measured to the patient is kept at a constant level, volume of the breathing gas in order to regardless of the altitude. achieve optimal BTPS conditions within the patient’s lungs, where temperature, The Oxylog 3000 plus and Oxylog 2000 plus humidity and pressure differ from those of measure the ambient air pressure via two the outside environment. The correction is internal pressure sensors and measure based on the assumption that the tempera- the flow rate via an internal flow sen - D-33317-2011 ture of the breathing gas delivered by the sor, which is assumed to be delivered at Figure 4: The Oxylog® 3000 plus in action Oxylog (the inspiratory gas) is 21.1 °C/70 °F 1023 mbar (767 mm Hg) which is the pres- as well as dry and that the temperature of sure at sea level + 10 mbar (10 cm H2O) Air- the breathing gas inside the human lungs way Pressure (PAW). Based on the mea- will be 37 °C/99 °F fully saturated. sured ambient pressure, this measured flow rate is then converted into the correct AMBIENT PRESSURE flow at actual ambient pressure conditions, CORRECTION IN OXYLOG which is required for delivering the set In addition to the BTPS correction, the volume in BTPS. The flow rate correction is Oxylog 3000 plus and Oxylog 2000 plus dynamic and is adjusted breath by breath to automatically compensate ambient pres- compensate for aircraft changing altitudes sure changes. Oxylogs automatically cor- and can vary between 1 % and 44 % (44 % rect the volumetric flow rate for changes at 14,800 ft/4,500 m). in ambient pressure due to changing BTPS & AMBIENT PRESSURE CORRECTION IN AIR MEDICAL TRANSPORT | 03 EXAMPLE BTPS AND Note 2: AMBIENT PRESSURE CORRECTION 1023 mbar (767 mmHg) = 1013 mbar If you set a Vt of 500 ml at sea level, the (760 mmHg) ambient pressure at sea Oxylog 3000 plus and Oxylog 2000 plus level + 10 mbar (10 cmH 2O) PAW. will deliver 447 ml as this volume will 1086 (815 mmHg) mbar = 1023 mbar expand to 500 ml in the patients lungs. (767 mmHg) (see above) + 63 mbar (47 mmHg) of the PH2O at 37 °C/99 °F. Formula: Vt of 500 ml × (294 Kelvin/ 310 Kelvin1) × (1023 mbar (767 mmHg)/ Note 3: 1086 mbar (815 mmHg)2) = 447 ml. 580 mbar (435 mmHg) = 570 mbar MT-5833-2008 (Assumption of PAW mean = 10 mbar (428 mmHg) ambient pressure at Figure 5: Oxylog® 3000 plus BTPS and ambient pressure correction (10 cmH2O) 14,880 ft/4,500 m + 10 mbar (10 cm H2O) is automatically done PAW. 643 mbar (482 mmHg) = 580 mbar If you set a Vt of 500 ml at an altitude of (435 mmHg) (see above) + 63 mbar 14,800 ft/4,500 m, the ventilator will deliv- (47 mmHg) of the P H2O at 37 °C/99 °F. er 428 ml. Oxylog 3000 plus and Oxylog 2000 plus Formula: Vt of 500 ml × (294 Kelvin/ compensate volume delivery and measure- 310 Kelvin1) × (580 mbar (435 mmHg)/ ment for typical environmental influences 643 mbar (482 mmHg) 3) = 428 ml. during air medical transport by applying (Assumption of PAW mean = 10 mbar (10 BTPS and ambient air pressure correction. cmH2O) The corrections are automatic, dynamic and are adjusted breath by breath to Formula’s explained: compensate for aircraft changing altitudes Note 1: and therefore can help preventing baro- 294 Kelvin ≈ 21 °C and 310 Kelvin trauma. As a result the operator is able to ≈ 37 °C/99 °F. spend more time on patient care. 90 51 611 | 15.06-3 | Communications & Sales Marketing | PP | LE | Printed in Germany | Chlorine-free – environmentally compatible | Subject to modifications | © 2015 Drägerwerk AG & Co. KGaA CORPORATE HEADQUARTERS REGION EUROPE CENTRAL REGION MIDDLE EAST, AFRICA REGION CENTRAL Drägerwerk AG & Co. KGaA AND EUROPE NORTH Drägerwerk AG & Co. KGaA AND SOUTH AMERICA Moislinger Allee 53–55 Drägerwerk AG & Co. KGaA Branch Office Dräger Panama Comercial 23558 Lübeck, Germany Moislinger Allee 53–55 P.O. Box 505108 S. de R.L. 23558 Lübeck, Germany Dubai, United Arab Emirates Complejo Business Park, www.draeger.com Tel +49 451 882 0 Tel +971 4 4294 600 V tower, 10th floor Fax +49 451 882 2080 Fax +971 4 4294 699 Panama City [email protected] [email protected] Tel +507 377 9100 Fax +507 377 9130 Manufacturer: REGION EUROPE SOUTH REGION ASIA / PACIFIC [email protected] Drägerwerk AG & Co. KGaA Dräger Médical S.A.S. Draeger Medical Moislinger Allee 53–55 Parc de Haute Technologie South East Asia Pte Ltd. 23558 Lübeck, Germany d’Antony 2 25 International Business Park 25, rue Georges Besse #04-27/29 German Centre 92182 Antony Cedex, France Singapore 609916, Singapore Tel +33 1 46 11 56 00 Tel +65 6572 4388 Fax +33 1 40 96 97 20 Fax +65 6572 4399 [email protected] [email protected] Locate your Regional Sales Representative at: www.draeger.com/contact.
Recommended publications
  • 2007 MTS Overview of Manned Underwater Vehicle Activity
    P A P E R 2007 MTS Overview of Manned Underwater Vehicle Activity AUTHOR ABSTRACT William Kohnen There are approximately 100 active manned submersibles in operation around the world; Chair, MTS Manned Underwater in this overview we refer to all non-military manned underwater vehicles that are used for Vehicles Committee scientific, research, tourism, and commercial diving applications, as well as personal leisure SEAmagine Hydrospace Corporation craft. The Marine Technology Society committee on Manned Underwater Vehicles (MUV) maintains the only comprehensive database of active submersibles operating around the world and endeavors to continually bring together the international community of manned Introduction submersible operators, manufacturers and industry professionals. The database is maintained he year 2007 did not herald a great through contact with manufacturers, operators and owners through the Manned Submersible number of new manned submersible de- program held yearly at the Underwater Intervention conference. Tployments, although the industry has expe- The most comprehensive and detailed overview of this industry is given during the UI rienced significant momentum. Submersi- conference, and this article cannot cover all developments within the allocated space; there- bles continue to find new applications in fore our focus is on a compendium of activity provided from the most dynamic submersible tourism, science and research, commercial builders, operators and research organizations that contribute to the industry and who share and recreational work; the biggest progress their latest information through the MTS committee. This article presents a short overview coming from the least likely source, namely of submersible activity in 2007, including new submersible construction, operation and the leisure markets.
    [Show full text]
  • Optimal Breathing Gas Mixture in Professional Diving with Multiple Supply
    Proceedings of the World Congress on Engineering 2021 WCE 2021, July 7-9, 2021, London, U.K. Optimal Breathing Gas Mixture in Professional Diving with Multiple Supply Orhan I. Basaran, Mert Unal compressors and cylinders, it was limited to surface air Abstract— Professional diving existed since antiquities when supply lines. In 1978, Fleuss introduced the first closed divers collected resources from the bottom of the seas and circuit oxygen breathing apparatus which removed carbon lakes. With technological advancements in the recent century, dioxide from the exhaled gas and did not form bubbles professional diving activities also increased significantly. underwater. In 1943, Cousteau and Gangan designed the Diving has many adverse effects on human physiology which first proper demand-regulated air supply from compressed are widely investigated in order to make dives safer. In this air cylinders worn on the back. The scuba equipment with study, we focus on optimizing the breathing gas mixture minimizing the dive costs while ensuring the safety of the the high-pressure regulator on the cylinder and a single hose divers. The methods proposed in this paper are purely to a demand valve was invented in Australia and marketed theoretical and divers should always have appropriate training by Ted Eldred in the early 1950s [1]. and certificates. Also, divers should never perform dives With the use of Siebe dress, the first cases of decompression without consulting professionals and medical doctors with expertise in related fields. sickness began to be documented. Haldane conducted several experiments on animal and human subjects in Index Terms—-professional diving; breathing gas compression chambers to investigate the causes of this optimization; dive profile optimization sickness and how it can be prevented.
    [Show full text]
  • Ocean Storage
    277 6 Ocean storage Coordinating Lead Authors Ken Caldeira (United States), Makoto Akai (Japan) Lead Authors Peter Brewer (United States), Baixin Chen (China), Peter Haugan (Norway), Toru Iwama (Japan), Paul Johnston (United Kingdom), Haroon Kheshgi (United States), Qingquan Li (China), Takashi Ohsumi (Japan), Hans Pörtner (Germany), Chris Sabine (United States), Yoshihisa Shirayama (Japan), Jolyon Thomson (United Kingdom) Contributing Authors Jim Barry (United States), Lara Hansen (United States) Review Editors Brad De Young (Canada), Fortunat Joos (Switzerland) 278 IPCC Special Report on Carbon dioxide Capture and Storage Contents EXECUTIVE SUMMARY 279 6.7 Environmental impacts, risks, and risk management 298 6.1 Introduction and background 279 6.7.1 Introduction to biological impacts and risk 298 6.1.1 Intentional storage of CO2 in the ocean 279 6.7.2 Physiological effects of CO2 301 6.1.2 Relevant background in physical and chemical 6.7.3 From physiological mechanisms to ecosystems 305 oceanography 281 6.7.4 Biological consequences for water column release scenarios 306 6.2 Approaches to release CO2 into the ocean 282 6.7.5 Biological consequences associated with CO2 6.2.1 Approaches to releasing CO2 that has been captured, lakes 307 compressed, and transported into the ocean 282 6.7.6 Contaminants in CO2 streams 307 6.2.2 CO2 storage by dissolution of carbonate minerals 290 6.7.7 Risk management 307 6.2.3 Other ocean storage approaches 291 6.7.8 Social aspects; public and stakeholder perception 307 6.3 Capacity and fractions retained
    [Show full text]
  • Oxygen Sensors and Their Use Within Rebreathers
    Oxygen sensors and their use within Rebreathers Author – Kevin Gurr Date - 2013 Table of Contents Oxygen sensors and their use within Rebreathers ......................................................... 1 History........................................................................................................................ 2 Concept ...................................................................................................................... 2 Operating Principle ................................................................................................ 3 Concept Summary .................................................................................................. 4 Mechanical Construction ........................................................................................... 6 Sensor Construction ............................................................................................... 7 Electrical Construction............................................................................................... 8 Electronic Functionality ............................................................................................. 8 Interfacing a Sensor to a Rebreather ........................................................................ 10 A Typical Sensor Specification ............................................................................... 11 Understanding a Sensor’s Response Time ............................................................... 13 Sensor Life Span .....................................................................................................
    [Show full text]
  • Quick Reference Guide on the Units of Measure in Hyperbaric Medicine
    Quick Reference Guide on the Units of Measure in Hyperbaric Medicine This quick reference guide is excerpted from Dr. Eric Kindwall’s chapter “The Physics of Diving and Hyperbaric Pressures” in Hyperbaric Medicine Practice, 3rd edition. www.BestPub.com All Rights Reserved 25 THE PHYSICS OF DIVING AND HYPERBARIC PRESSURES Eric P. Kindwall Copyright Best Publishing Company. All Rights Reserved. www.BestPub.com INTRODUCTION INTRODUCTIONThe physics of diving and hyperbaric pressure are very straight forTheward physicsand aofr edivingdefi nanded hyperbaricby well-k npressureown a nared veryacce pstraightforwardted laws. Ga sandu narede r definedpres subyr ewell-knowncan stor eande nacceptedormous laws.ene rgGasy, underthe apressuremount scanof storewhi cenormoush are o fenergy,ten the samountsurprisin ofg. whichAlso, s arema loftenl chan surprising.ges in the pAlso,erce smallntage schangesof the inva rtheiou spercentagesgases use dofa there variousgrea gasestly m usedagni fareied greatlyby ch amagnifiednges in am byb ichangesent pre sinsu ambientre. The pressure.resultan t pTheh yresultantsiologic physiologiceffects d effectsiffer w idifferdely d ewidelypend idependingng on the onp rtheess upressure.re. Thus ,Thus,divi ndivingg or oorpe operatingrating a a hy- perbarichype rfacilitybaric f requiresacility re gainingquires gcompleteaining c oknowledgemplete kn ofow theled lawsge o finvolvedthe law stoin ensurevolved safety.to ensure safety. UNITS OF MEASURE UNITS OF MEASURE This is often a confusing area to anyone new to hyperbaric medicine as both Ameri- This is often a confusing area to anyone new to hyperbaric medicine as can and International Standard of Units (SI) are used. In addition to meters, centimeters, both American and International Standard of Units (SI) are used. In addition kilos,to pounds,meters, andcen feet,time someters, kpressuresilos, po uarend givens, an dinf atmosphereseet, some p rabsoluteessures andare millimetersgiven in of mercury.atmosph Tableeres 1a bgivessolu thete a exactnd m conversionillimeters factorsof me rbetweencury.
    [Show full text]
  • Body Density and Diving Gas Volume of the Northern Bottlenose Whale
    © 2016. Published by The Company of Biologists Ltd | Journal of Experimental Biology (2016) 219, 2962 doi:10.1242/jeb.148841 CORRECTION Correction: Body density and diving gas volume of the northern bottlenose whale (Hyperoodon ampullatus) Patrick Miller, Tomoko Narazaki, Saana Isojunno, Kagari Aoki, Sophie Smout and Katsufumi Sato There was an error published in J. Exp. Biol. 219, 2458-2468. Eqn 1 was presented incorrectly. A ‘−1’ was missing after the ratio of densities, and the subscript of the first instance of the density of seawater (ρsw) was given incorrectly as ‘w’ instead of ‘sw’. The original equation was: C  A r a ¼ :  d  r  v2 þ sw   ðpÞ 0 5 m w r ðdÞ g sin tissue ð1Þ V r À r ð1 þ 0:1  dÞ þ air  g  sinðpÞ sw air ; m ð1 þ 0:1  dÞ where: r ð Þ r ðdÞ¼ tissue 0 : tissue 1 À r ð1 þ 0:1  dÞ101; 325  10À9 The correct equation is as follows: C  A r a ¼ :  d  r  v2 þ sw À   ðpÞ 0 5 m sw r ðdÞ 1 g sin tissue ð1Þ V r À r ð1 þ 0:1  dÞ þ air  g  sinðpÞ sw air ; m ð1 þ 0:1  dÞ where: r ð Þ r ðdÞ¼ tissue 0 : tissue 1 À r ð1 þ 0:1  dÞ101; 325  10À9 This error was corrected on 21 September 2016 in the full-text and PDF versions of this article.
    [Show full text]
  • Equations of Motion Using Thermodynamic Coordinates
    2814 JOURNAL OF PHYSICAL OCEANOGRAPHY VOLUME 30 Equations of Motion Using Thermodynamic Coordinates ROLAND A. DE SZOEKE College of Oceanic and Atmospheric Sciences, Oregon State University, Corvallis, Oregon (Manuscript received 21 October 1998, in ®nal form 30 December 1999) ABSTRACT The forms of the primitive equations of motion and continuity are obtained when an arbitrary thermodynamic state variableÐrestricted only to be vertically monotonicÐis used as the vertical coordinate. Natural general- izations of the Montgomery and Exner functions suggest themselves. For a multicomponent ¯uid like seawater the dependence of the coordinate on salinity, coupled with the thermobaric effect, generates contributions to the momentum balance from the salinity gradient, multiplied by a thermodynamic coef®cient that can be com- pletely described given the coordinate variable and the equation of state. In the vorticity balance this term produces a contribution identi®ed with the baroclinicity vector. Only when the coordinate variable is a function only of pressure and in situ speci®c volume does the coef®cient of salinity gradient vanish and the baroclinicity vector disappear. This coef®cient is explicitly calculated and displayed for potential speci®c volume as thermodynamic coor- dinate, and for patched potential speci®c volume, where different reference pressures are used in various pressure subranges. Except within a few hundred decibars of the reference pressures, the salinity-gradient coef®cient is not negligible and ought to be taken into account in ocean circulation models. 1. Introduction perature surfaces is a potential for the acceleration ®eld, Potential temperature, the temperature a ¯uid parcel when friction is negligible. Because the gradient of this would have if removed adiabatically and reversibly from function gives the geostrophic ¯ow when it balances ambient pressure to a reference pressure, is a valuable Coriolis force, it is also called the geostrophic stream- concept in the study of the atmosphere and oceans.
    [Show full text]
  • Under High Pressure: Spherical Glass Flotation and Instrument Housings in Deep Ocean Research
    PAPER Under High Pressure: Spherical Glass Flotation and Instrument Housings in Deep Ocean Research AUTHORS ABSTRACT Steffen Pausch All stationary and autonomous instrumentation for observational activities in Nautilus Marine Service GmbH ocean research have two things in common, they need pressure-resistant housings Detlef Below and buoyancy to bring instruments safely back to the surface. The use of glass DURAN Group GmbH spheres is attractive in many ways. Glass qualities such as the immense strength– weight ratio, corrosion resistance, and low cost make glass spheres ideal for both Kevin Hardy flotation and instrument housings. On the other hand, glass is brittle and hence DeepSea Power & Light subject to damage from impact. The production of glass spheres therefore requires high-quality raw material, advanced manufacturing technology and expertise in Introduction processing. VITROVEX® spheres made of DURAN® borosilicate glass 3.3 are the hen Jacques Piccard and Don only commercially available 17-inch glass spheres with operational ratings to full Walsh reached the Marianas Trench ocean trench depth. They provide a low-cost option for specialized flotation and W instrument housings. in1960andreportedshrimpand flounder-like fish, it was proven that Keywords: Buoyancy, Flotation, Instrument housings, Pressure, Spheres, Trench, there is life even in the very deepest VITROVEX® parts of the ocean. What started as a simple search for life has become over (1) they need to have pressure- the years a search for answers to basic Advantages and resistant housings to accommodate questions such as the number of spe- Disadvantages sensitive electronics, and (2) they need cies, their distribution ranges, and the of Glass Spheres either positive buoyancy to bring the composition of the fauna.
    [Show full text]
  • Inspiration and Evolution Series of Rebreathers That Are Fitted with Back-Mounted Counterlungs
    RBV05 and RBV05A Rebreather Manual Inflator Maintenance Manual Version 1.0 July 2014 Written by Tino de Rijk Ambient Pressure Diving Ltd. RBV05(A) Rebreather Manual Inflator Maintenance Manual Table of Contents 1. Introduction ........................................................................................... 3! 1.1 Functional description .................................................................................... 3! 1.2 Servicing ......................................................................................................... 3! 1.3 Warranty ......................................................................................................... 3! 1.4 Copyright and Applicable Law ........................................................................ 3! 2. RBV05 Manual Inflator Exploded Diagram and Parts List ................... 4! 2.1 RBV05 (Diluent) and RBV05A (Oxygen) Manual inflators main assembly .... 4! 2.2 RBV05/04 Counterlung Connection Post ....................................................... 5! 3. RBV05B Service Kit Contents and Tools ............................................. 6! 3.1 RBV05B (Diluent) and RBV05B/1 (Oxygen) Service Kit Contents ................. 6! 3.2 Tools Needed ................................................................................................. 7! 4. Disassembly Instructions ...................................................................... 8! 4.1 Remove MP hose and connection post from the counterlung ........................ 8! 4.2 Remove DIN 9/16” UNF adapter
    [Show full text]
  • 1. Temperature and the Ideal Gas Law (Note: This Is a Fairly Long Experiment
    Physics 341 Chapter 1 Page 1-1 1. Temperature and the Ideal Gas Law (Note: This is a fairly long experiment. To save time, much of the graphing can be done “at home”. As always, make sure that you have all the data you need before you leave.) 1.1 Introduction The most important concept at the foundation of thermodynamics is that of thermal equilibrium. We take this for granted in our daily experiences. We know, for instance, that an ice cube will melt when taken out of the freezer – no matter what object “at room temperature” it is brought into contact with. This is the essence of the utility of temperature and thermal equilibrium: the direction of heat flow is independent of the substance involved - it depends on only temperature. In fact, this defines temperature. More precise observations of thermal equilibrium are as follows. First of all, as with the equally familiar notion of mechanical equilibrium, we may say that an isolated macroscopic system is in thermal equilibrium, or thermodynamic equilibrium, whenever it attains a state that is not observed to change with time, at least at a macroscopic level. Obviously, for such a situation to occur, it is also necessary that the system in question is in (internal) mechanical and chemical equilibrium. At the foundations of thermodynamics is the experimental fact that two systems in thermal equilibrium with a third system must also be in thermal equilibrium with each other. This is often referred to as the zeroth law of thermodynamics. It is what leads to the empirical notion of a temperature scale.
    [Show full text]
  • Diving & Subsea Division
    DMS Brochure 2017 #295 #314 #330_Diving, Marine & Sub-Sea 15/11/2017 11:59 Page 1 Diving & Subsea Division Edition two www.divinggauges.co.uk DMS Brochure 2017 #295 #314 #330_Diving, Marine & Sub-Sea 15/11/2017 12:00 Page 2 DMS Brochure 2017 #295 #314 #330_Diving, Marine & Sub-Sea 15/11/2017 12:00 Page 3 INDEX Ashford Instrumentation Ltd was established in 2003 and specialise s in Pressure, Temperature, Level and Flow Measurement. We work in conjunction with many of the largest organisations within Pneumo Gauges 4 the instrumentation field and can therefore find a solution to meet just about any measurement requirement you may have. Our Technical Team has a wealth of application knowledge upon which we can draw when the process demands. Pneumo Gauges 5 Caisson Gauges 6 Diving & Subsea Caisson Gauges 7 Our Diving, Marine & Subsea division has established a product range which is arguably the most comprehensive in the world. We specialise in the supply of Depth, Pneumo, Caisson & Subsea Instrumentation. Dive Panel Gauges 8 Our comprehensive stock and short lead times provide customers with the support they require when the situation demands. Calibration Equipment 9 Diving, Marine & Subsea Sealed Case Subsea Gauges 10 Compensated Subsea Gauges 11 Process, Industrial & Utility Subsea Pressure Process, Industrial & Utility & Depth Transmitters 12 Pressure, Level, Temperature and Flow Instrumentation for the Process and OEM Industries Miscellaneous Instruments 13 HVAC, Plant Room & Utility Subsea Valves 14 HVAC Pressure, Level, Temperature and Flow Instrumentation Calibration & Bespoke Solutions 15 for the HVAC Engineer Specifications and photographs shown in this brochure are representative of our engineering capabilities at the time of printing.
    [Show full text]
  • Gases Boyles Law Amontons Law Charles Law ∴ Combined Gas
    Gas Physics FICK’S LAW Adolf Fick, 1858 Properties of “Ideal” Gases Fick’s law of diffusion of a gas across a fluid membrane: • Gases are composed of molecules whose size is negligible compared to the average distance between them. Rate of diffusion = KA(P2–P1)/D – Gas has a low density because its molecules are spread apart over a large volume. • Molecules move in random lines in all directions and at various speeds. Wherein: – The forces of attraction or repulsion between two molecules in a gas are very weak or negligible, except when they collide. K = a temperature-dependent diffusion constant. – When molecules collide with one another, no kinetic energy is lost. A = the surface area available for diffusion. • The average kinetic energy of a molecule is proportional to the absolute temperature. (P2–P1) = The difference in concentraon (paral • Gases are easily expandable and compressible (unlike solids and liquids). pressure) of the gas across the membrane. • A gas will completely fill whatever container it is in. D = the distance over which diffusion must take place. – i.e., container volume = gas volume • Gases have a measurement of pressure (force exerted per unit area of surface). – Units: 1 atmosphere [atm] (≈ 1 bar) = 760 mmHg (= 760 torr) = 14.7 psi = 0.1 MPa Boyles Law Amontons Law • Gas pressure (P) is inversely proportional to gas volume (V) • Gas pressure (P) is directly proportional to absolute gas • P ∝ 1/V temperature (T in °K) ∴ ↑V→↓P ↑P→↓V ↓V →↑P ↓P →↑V • 0°C = 273°K • P ∝ T • ∴ P V =P V (if no gas is added/lost and temperature
    [Show full text]