Diver's Breathing Air Standard and the Frequency of Examination and Tests
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Compressed Air Compressed
Construction Planning, Equipment, and Methods Sixth Edition CHAPTER COMPRESSEDCOMPRESSED AIRAIR • A. J. Clark School of Engineering •Department of Civil and Environmental Engineering By 11 Dr. Ibrahim Assakkaf ENCE 420 – Construction Equipment and Methods Spring 2003 Department of Civil and Environmental Engineering University of Maryland, College Park CHAPTER 11. COMPRESSED AIR Slide No. 1 ENCE 420 ©Assakkaf COMPRESSEDCOMPRESSED AIRAIR 1 CHAPTER 11. COMPRESSED AIR Slide No. 2 ENCE 420 ©Assakkaf INTRODUCTION Compressed air is used for: 9Drilling rock 9Driving piles 9Operating hand tools 9Pumping 9Cleaning PAVING PUMP BREAKER CHAPTER 11. COMPRESSED AIR Slide No. 3 ENCE 420 ©Assakkaf INTRODUCTION In many instances the energy supplied by compressed air is the most convenient method of operating equipment and tools. When air is compressed, it receives energy from the compressor. This energy is transmitted through a pipe or hose to the operating equipment, where a portion of the energy is converted into mechanical work. 2 CHAPTER 11. COMPRESSED AIR Slide No. 4 ENCE 420 ©Assakkaf INTRODUCTION The operations of compressing, transmitting, and using air will always result in a loss of energy, which will give an overall efficiency less than 100%, sometimes considerably less. CHAPTER 11. COMPRESSED AIR Slide No. 5 ENCE 420 ©Assakkaf INTRODUCTION Things to consider: 9Effect of altitude on capacity. 9Loss of air pressure in pipe and hose systems. 9Capacity factors. 3 CHAPTER 11. COMPRESSED AIR Slide No. 6 ENCE 420 ©Assakkaf OVERVIEWOVERVIEW Selecting the right air compressor depends on many factors. ¾ Compressor capacity and operating pressure depend on the tools used. ¾ Engine and compressor lose power and capacity as altitude increases and temperature rises. -
Beach Nourishment Techniques: Report 1: Dredging Systems For
BEACH NOURISHMENT TECHNIQUES R ep ort I DREDGING SYSTEMS FOR BEACH NOURISHMENT FROM OFFSHORE SOURCES by Thomas W. Richardson Hydraulics Laboratory U. S. Army Engineer Waterways Experiment Station P. O. Box 631, Vicksburg, Miss. 39180 September 1976 Report I of a Series Approved For Public Release; Distribution Unlimited TA 7 Prepared for Office, Chief of Engineers, U. S. Army .W34t Washington, D. C. 2 0 3 14 H-76-13 1976 Voi. 1 C . 3 BUREAU OF RECLAMATION LIBRARY DENVER, CO Destroy this report when no longer needed. Do not return it to the originator. P.yi!P.A.y .P f RECLAMATION DENVER LIBRARY 92071163 o'5 i Unclassified SECURITY CLASSIFICATION OF THIS PAGE (When Date Entered) READ INSTRUCTIONS REPORT DOCUMENTATION PAGE BEFORE COMPLETING FORM 1. REPORT NUMBER 2. GOVT ACCESSION NO. 3. RECIPIENT’S CATALOG NUMBER Technical Report H-76-13 4 . T I T L E (and Subtitle) 5. TYPE OF REPORT & PERIOD COVERED BEACH NOURISHMENT TECHNIQUES; Report 1, DREDGING SYSTEMS FOR BEACH NOURISHMENT Report 1 of a series FROM OFFSHORE SOURCES 6. PERFORMING ORG. REPORT NUMBER 7. A U TH O R fsj 8. CONTRACT OR GRANT NUMBERS Thomas W. Richardson 9. PERFORMING ORGANIZATION NAME AND ADDRESS 10. PROGRAM ELEMENT, PROJECT, TASK AREA & WORK UNIT NUMBERS U. S. Army Engineer Waterways Experiment Station Hydraulics Laboratory P. 0. Box 631, Vicksburg, Miss. 39180 11. CONTROLLING OFFICE NAME AND ADDRESS 12. REPORT DATE September 1976 Office, Chief of Engineers, U. S. Army Washington, D. C. 2031** 13. NUMBER OF PAGES 83 1 4 . MONITORING AGENCY NAME & ADDRESSfi/ different from Controlling Office) 15. -
Unit 11 Sound Speed of Sound Speed of Sound Sound Can Travel Through Any Kind of Matter, but Not Through a Vacuum
Unit 11 Sound Speed of Sound Speed of Sound Sound can travel through any kind of matter, but not through a vacuum. The speed of sound is different in different materials; in general, it is slowest in gases, faster in liquids, and fastest in solids. The speed depends somewhat on temperature, especially for gases. vair = 331.0 + 0.60T T is the temperature in degrees Celsius Example 1: Find the speed of a sound wave in air at a temperature of 20 degrees Celsius. v = 331 + (0.60) (20) v = 331 m/s + 12.0 m/s v = 343 m/s Using Wave Speed to Determine Distances At normal atmospheric pressure and a temperature of 20 degrees Celsius, speed of sound: v = 343m / s = 3.43102 m / s Speed of sound 750 mi/h Speed of light 670 616 629 mi/h c = 300,000,000m / s = 3.00 108 m / s Delay between the thunder and lightning Example 2: The thunder is heard 3 seconds after the lightning seen. Find the distance to storm location. The speed of sound is 345 m/s. distance = v t = (345m/s)(3s) = 1035m Example 3: Another phenomenon related to the perception of time delays between two events is an echo. In a canyon, an echo is heard 1.40 seconds after making the holler. Find the distance to the canyon wall (v=345m/s) distanceround trip = vt = (345 m/s )( 1.40 s) = 483 m d= 484/2=242m Applications: Sonar, Ultrasound, and Medical Imaging • Ultrasound or ultrasonography is a medical imaging technique that uses high frequency sound waves and their echoes. -
Compressed Air Engine Swadhinpatnaik Dept
ISSN : 2249-5762 (Online) | ISSN : 2249-5770 (Print) IJRMET VOL . 5, ISSU E 2, MAY - OC T 2015 Compressed Air Engine SwadhinPatnaik Dept. of Mechanical engineering, SRM University, Chennai, India Abstract II. Components This paper work deals with the Compressed-air engine as a • CYLINDER pneumatic actuator that converts one form of energy into another. • PISTON The Air Driven Engine is an eco-friendly engine which operates • COMBUSTION CHAMBER with compressed air. This Engine uses the expansion of compressed • ONNECTING ROD air to drive the pistons of the engine. An Air Driven Engine is • CRANKSHAFT a pneumatic actuator that creates useful work by expanding • CAMSHAFT compressed air. There is no mixing of fuel with air as there is no • CAM combustion. An Air Driven Engine makes use of Compressed Air • PISTON RINGS Technology for its operation The Compressed Air Technology is • GUDGEON PIN quite simple. If we compress normal air into a cylinder the air • INLET would hold some energy within it. This energy can be utilized for • EXHAUST MANIFOLD useful purposes. When this compressed air expands, the energy is • INLET AND EXHAUST VALVE released to do work. So this energy in compressed air can also be • FLYWHEEL utilized to displace a piston. Compressed air propulsion may also be incorporated in hybrid systems, e.g., battery electric propulsion III. Engine Specifications and fuel tanks to recharge the batteries. This kind of system is called Type of fuel used : Petrol hybrid-pneumatic electric propulsion. Additionally, regenerative Cooling system : Air cooled braking can also be used in conjunction with this system. Number of cylinder : Single Number of stroke : Four Stroke Keywords Arrangement : Vertical Air, Compressed, Engine, Energy, Propulsion, Pneumatic Cubic capacity : 100 cc I. -
Atmospheric Cold Front-Generated Waves in the Coastal Louisiana
Journal of Marine Science and Engineering Article Atmospheric Cold Front-Generated Waves in the Coastal Louisiana Yuhan Cao 1 , Chunyan Li 2,* and Changming Dong 1,3,* 1 School of Marine Sciences, Nanjing University of Information Science and Technology, Nanjing 210044, China; [email protected] 2 Department of Oceanography and Coastal Sciences, College of the Coast and Environment, Louisiana State University, Baton Rouge, LA 70803, USA 3 Southern Laboratory of Ocean Science and Engineering (Zhuhai), Zhuhai 519000, China * Correspondence: [email protected] (C.L.); [email protected] (C.D.); Tel.: +1-225-578-2520 (C.L.); +86-025-58695733 (C.D.) Received: 15 October 2020; Accepted: 9 November 2020; Published: 11 November 2020 Abstract: Atmospheric cold front-generated waves play an important role in the air–sea interaction and coastal water and sediment transports. In-situ observations from two offshore stations are used to investigate variations of directional waves in the coastal Louisiana. Hourly time series of significant wave height and peak wave period are examined for data from 2004, except for the summer time between May and August, when cold fronts are infrequent and weak. The intra-seasonal scale variations in the wavefield are significantly affected by the atmospheric cold frontal events. The wave fields and directional wave spectra induced by four selected cold front passages over the coastal Louisiana are discussed. It is found that significant wave height generated by cold fronts coming from the west change more quickly than that by other passing cold fronts. The peak wave direction rotates clockwise during the cold front events. -
A Review of Ocean/Sea Subsurface Water Temperature Studies from Remote Sensing and Non-Remote Sensing Methods
water Review A Review of Ocean/Sea Subsurface Water Temperature Studies from Remote Sensing and Non-Remote Sensing Methods Elahe Akbari 1,2, Seyed Kazem Alavipanah 1,*, Mehrdad Jeihouni 1, Mohammad Hajeb 1,3, Dagmar Haase 4,5 and Sadroddin Alavipanah 4 1 Department of Remote Sensing and GIS, Faculty of Geography, University of Tehran, Tehran 1417853933, Iran; [email protected] (E.A.); [email protected] (M.J.); [email protected] (M.H.) 2 Department of Climatology and Geomorphology, Faculty of Geography and Environmental Sciences, Hakim Sabzevari University, Sabzevar 9617976487, Iran 3 Department of Remote Sensing and GIS, Shahid Beheshti University, Tehran 1983963113, Iran 4 Department of Geography, Humboldt University of Berlin, Unter den Linden 6, 10099 Berlin, Germany; [email protected] (D.H.); [email protected] (S.A.) 5 Department of Computational Landscape Ecology, Helmholtz Centre for Environmental Research UFZ, 04318 Leipzig, Germany * Correspondence: [email protected]; Tel.: +98-21-6111-3536 Received: 3 October 2017; Accepted: 16 November 2017; Published: 14 December 2017 Abstract: Oceans/Seas are important components of Earth that are affected by global warming and climate change. Recent studies have indicated that the deeper oceans are responsible for climate variability by changing the Earth’s ecosystem; therefore, assessing them has become more important. Remote sensing can provide sea surface data at high spatial/temporal resolution and with large spatial coverage, which allows for remarkable discoveries in the ocean sciences. The deep layers of the ocean/sea, however, cannot be directly detected by satellite remote sensors. -
Physical Geography Chapter 5: Atmospheric Pressure, Winds, Circulation Patterns
Physical Geography Chapter 5: Atmospheric Pressure, Winds, Circulation Patterns Torricelli – 1643- first Mercury barometer (76 cm, 29.92 in) – measures response to pressure Pressure – millibars- 1013.2 mb, will cause Hg to rise in tube Unequal heating of Earth’s surface is responsible for differences in pressure to! Variations in Atmospheric Pressure 1. Vertical Variations – increase in elevation, less air pressure Mt. Everest – 8848 m (or 29, 028 ft) – 1/3 pressure 2. Horizontal Variations a. Thermal (determined by T) Warm air is less dense – it rises away from the surface at the equator b. Dynamic: Air from the tropics moves northward and then to the east due to the Coryolis Effect. It collects at this latitude, increasing pressure at the surface. Basic Pressure Systems 1. Low – cyclone – converging air pressure decreases 2. High – anticyclone – Divergins air pressure increases Wind Isobars- line of equal pressure Pressure Gradient - significant difference in pressure Wind- horizontal movement of air in response to differences in pressure ¾ Responsible for moving heat toward poles ¾ 38° Lat and lower: radiation surplus If Earth did not rotate, and if there wasno friction between moving air and the Earth’s surface, the air would flow in a straight line from areas of higher pressure to areas of low pressure. Of course, this is not true, the Earth rotates and friction exists: and wind is controlled by three major factors: 1) PGF- Pressure is measured by barometer 2) Coriolis Effect 3) Friction 1) Pressure Gradient Force (PGF) Pressure differences create wind, and the greater these differences, the greater the wind speed. -
Diving Air Compressor - Wikipedia, the Free Encyclopedia Diving Air Compressor from Wikipedia, the Free Encyclopedia
2/8/2014 Diving air compressor - Wikipedia, the free encyclopedia Diving air compressor From Wikipedia, the free encyclopedia A diving air compressor is a gas compressor that can provide breathing air directly to a surface-supplied diver, or fill diving cylinders with high-pressure air pure enough to be used as a breathing gas. A low pressure diving air compressor usually has a delivery pressure of up to 30 bar, which is regulated to suit the depth of the dive. A high pressure diving compressor has a delivery pressure which is usually over 150 bar, and is commonly between 200 and 300 bar. The pressure is limited by an overpressure valve which may be adjustable. A small stationary high pressure diving air compressor installation Contents 1 Machinery 2 Air purity 3 Pressure 4 Filling heat 5 The bank 6 Gas blending 7 References 8 External links A small scuba filling and blending station supplied by a compressor and Machinery storage bank Diving compressors are generally three- or four-stage-reciprocating air compressors that are lubricated with a high-grade mineral or synthetic compressor oil free of toxic additives (a few use ceramic-lined cylinders with O-rings, not piston rings, requiring no lubrication). Oil-lubricated compressors must only use lubricants specified by the compressor's manufacturer. Special filters are used to clean the air of any residual oil and water(see "Air purity"). Smaller compressors are often splash lubricated - the oil is splashed around in the crankcase by the impact of the crankshaft and connecting A low pressure breathing air rods - but larger compressors are likely to have a pressurized lubrication compressor used for surface supplied using an oil pump which supplies the oil to critical areas through pipes diving at the surface control point and passages in the castings. -
Air Pressure and Wind
Air Pressure We know that standard atmospheric pressure is 14.7 pounds per square inch. We also know that air pressure decreases as we rise in the atmosphere. 1013.25 mb = 101.325 kPa = 29.92 inches Hg = 14.7 pounds per in 2 = 760 mm of Hg = 34 feet of water Air pressure can simply be measured with a barometer by measuring how the level of a liquid changes due to different weather conditions. In order that we don't have columns of liquid many feet tall, it is best to use a column of mercury, a dense liquid. The aneroid barometer measures air pressure without the use of liquid by using a partially evacuated chamber. This bellows-like chamber responds to air pressure so it can be used to measure atmospheric pressure. Air pressure records: 1084 mb in Siberia (1968) 870 mb in a Pacific Typhoon An Ideal Ga s behaves in such a way that the relationship between pressure (P), temperature (T), and volume (V) are well characterized. The equation that relates the three variables, the Ideal Gas Law , is PV = nRT with n being the number of moles of gas, and R being a constant. If we keep the mass of the gas constant, then we can simplify the equation to (PV)/T = constant. That means that: For a constant P, T increases, V increases. For a constant V, T increases, P increases. For a constant T, P increases, V decreases. Since air is a gas, it responds to changes in temperature, elevation, and latitude (owing to a non-spherical Earth). -
Aircraft Performance: Atmospheric Pressure
Aircraft Performance: Atmospheric Pressure FAA Handbook of Aeronautical Knowledge Chap 10 Atmosphere • Envelope surrounds earth • Air has mass, weight, indefinite shape • Atmosphere – 78% Nitrogen – 21% Oxygen – 1% other gases (argon, helium, etc) • Most oxygen < 35,000 ft Atmospheric Pressure • Factors in: – Weather – Aerodynamic Lift – Flight Instrument • Altimeter • Vertical Speed Indicator • Airspeed Indicator • Manifold Pressure Guage Pressure • Air has mass – Affected by gravity • Air has weight Force • Under Standard Atmospheric conditions – at Sea Level weight of atmosphere = 14.7 psi • As air become less dense: – Reduces engine power (engine takes in less air) – Reduces thrust (propeller is less efficient in thin air) – Reduces Lift (thin air exerts less force on the airfoils) International Standard Atmosphere (ISA) • Standard atmosphere at Sea level: – Temperature 59 degrees F (15 degrees C) – Pressure 29.92 in Hg (1013.2 mb) • Standard Temp Lapse Rate – -3.5 degrees F (or 2 degrees C) per 1000 ft altitude gain • Upto 36,000 ft (then constant) • Standard Pressure Lapse Rate – -1 in Hg per 1000 ft altitude gain Non-standard Conditions • Correction factors must be applied • Note: aircraft performance is compared and evaluated with respect to standard conditions • Note: instruments calibrated for standard conditions Pressure Altitude • Height above Standard Datum Plane (SDP) • If the Barometric Reference Setting on the Altimeter is set to 29.92 in Hg, then the altitude is defined by the ISA standard pressure readings (see Figure 10-2, pg 10-3) Density Altitude • Used for correlating aerodynamic performance • Density altitude = pressure altitude corrected for non-standard temperature • Density Altitude is vertical distance above sea- level (in standard conditions) at which a given density is to be found • Aircraft performance increases as Density of air increases (lower density altitude) • Aircraft performance decreases as Density of air decreases (higher density altitude) Density Altitude 1. -
OCN 201 El Nino
OCN 201 El Nino El Nino theme page http://www.pmel.noaa.gov/tao/elnino/nino-home-low.html Reports to the Nation http://www.pmel.noaa.gov/tao/elnino/report/el-nino-report.html This page has all the text and figures and also how to get the booklet 1 El Nino is a major reorganisation of the equatorial climate system that affects regions far from its point of origin in the western Equatorial Pacific Occurs roughly every 6 years around Xmas-time Onset recognised by climatic effects --warm surface waters -- collapse of fisheries -- heavy rains in Peru/Ecuador/central Pacific -- droughts in Indonesia -- change in typhoon tracks Is a good example of how the ocean and atmosphere interact 2 What phase do you think we are in now? A El Nino B La Nina C Normal D I don’t know! A = El Nino 2014 2015 Southern Oscillation Atmospheric pressure differential between Tahiti and Darwin Normally low pressure in Darwin, high in Tahiti Low pressure High pressure Normal El Nino El Nino high pressure in Darwin, low in Tahiti Change in pressure differential results in weakening of easterly equatorial winds 3 Normal conditions in the Equatorial Pacific Strong easterly winds: Pile up warm water in the western Pacific -- thermocline deep in western Pacific, shallow in eastern Pacific Winds drive equatorial upwelling How much higher do you think that sea level is in the western Pacific? A 10cm B 50 cm C 1 metres D 5 metres E More! About 40 cm 4 Satellite image of chlorophyll abundance As thermocline is shallow in eastern Pacific upwelling brings nutrients to surface waters along -
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.