Gases: a Review Kinetic Molecule Theory (KMT): Traits of an Ideal Gas
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THE SOLUBILITY of GASES in LIQUIDS Introductory Information C
THE SOLUBILITY OF GASES IN LIQUIDS Introductory Information C. L. Young, R. Battino, and H. L. Clever INTRODUCTION The Solubility Data Project aims to make a comprehensive search of the literature for data on the solubility of gases, liquids and solids in liquids. Data of suitable accuracy are compiled into data sheets set out in a uniform format. The data for each system are evaluated and where data of sufficient accuracy are available values are recommended and in some cases a smoothing equation is given to represent the variation of solubility with pressure and/or temperature. A text giving an evaluation and recommended values and the compiled data sheets are published on consecutive pages. The following paper by E. Wilhelm gives a rigorous thermodynamic treatment on the solubility of gases in liquids. DEFINITION OF GAS SOLUBILITY The distinction between vapor-liquid equilibria and the solubility of gases in liquids is arbitrary. It is generally accepted that the equilibrium set up at 300K between a typical gas such as argon and a liquid such as water is gas-liquid solubility whereas the equilibrium set up between hexane and cyclohexane at 350K is an example of vapor-liquid equilibrium. However, the distinction between gas-liquid solubility and vapor-liquid equilibrium is often not so clear. The equilibria set up between methane and propane above the critical temperature of methane and below the criti cal temperature of propane may be classed as vapor-liquid equilibrium or as gas-liquid solubility depending on the particular range of pressure considered and the particular worker concerned. -
Dysbarism - Barotrauma
DYSBARISM - BAROTRAUMA Introduction Dysbarism is the term given to medical complications of exposure to gases at higher than normal atmospheric pressure. It includes barotrauma, decompression illness and nitrogen narcosis. Barotrauma occurs as a consequence of excessive expansion or contraction of gas within enclosed body cavities. Barotrauma principally affects the: 1. Lungs (most importantly): Lung barotrauma may result in: ● Gas embolism ● Pneumomediastinum ● Pneumothorax. 2. Eyes 3. Middle / Inner ear 4. Sinuses 5. Teeth / mandible 6. GIT (rarely) Any illness that develops during or post div.ing must be considered to be diving- related until proven otherwise. Any patient with neurological symptoms in particular needs urgent referral to a specialist in hyperbaric medicine. See also separate document on Dysbarism - Decompression Illness (in Environmental folder). Terminology The term dysbarism encompasses: ● Decompression illness And ● Barotrauma And ● Nitrogen narcosis Decompression illness (DCI) includes: 1. Decompression sickness (DCS) (or in lay terms, the “bends”): ● Type I DCS: ♥ Involves the joints or skin only ● Type II DCS: ♥ Involves all other pain, neurological injury, vestibular and pulmonary symptoms. 2. Arterial gas embolism (AGE): ● Due to pulmonary barotrauma releasing air into the circulation. Epidemiology Diving is generally a safe undertaking. Serious decompression incidents occur approximately only in 1 in 10,000 dives. However, because of high participation rates, there are about 200 - 300 cases of significant decompression illness requiring treatment in Australia each year. It is estimated that 10 times this number of divers experience less severe illness after diving. Physics Boyle’s Law: The air pressure at sea level is 1 atmosphere absolute (ATA). Alternative units used for 1 ATA include: ● 101.3 kPa (SI units) ● 1.013 Bar ● 10 meters of sea water (MSW) ● 760 mm of mercury (mm Hg) ● 14.7 pounds per square inch (PSI) For every 10 meters a diver descends in seawater, the pressure increases by 1 ATA. -
Nitrogen Narcosis
WHAT IS IT? A reversible alteration in consciousness that occurs while at depth (usually noticeable around 30 meters or 100 ft) Caused by the anesthetic effect of certain gases at high pressure NITROGEN NARCOSIS Depths Beyond 100 Feet! Individual Variability Day-to-Day Variability Signs and Symptoms of N2 Narcosis Impaired performance mental/manual work Dizziness, euphoria, intoxication Overconfidence Uncontrolled laughter Overly talkative Memory loss/post-dive amnesia Perceptual narrowing Impaired sensory function Loss of consciousness > 300 ft Deep Scuba Dives Breathing Air YEAR DIVER DEPTH 1943 Dumas 203 feet 1948 Dumas 307 feet 1967 Watts 390 feet 1968 Watson 437 feet 1989 Gilliam 452 feet Prevention of Nitrogen Narcosis Restrict diving depth to less than 100 fsw If affected, return immediately to surface Plan dive beforehand − Max time to be on bottom − Any decompression required − Minimum air required for ascent − Emergency action in event of accident Breathe helium/oxygen mixture How to Beat Narcosis (Francis 2006) Be sober, no hangover and drug free Be rested and confident Use a high quality regulator Avoid task loading Be over trained Approach limits gradually Use a slate to plan dive Schedule gauge checks and buddy checks Be positive, well motivated and prudent Oxygen Characteristics: − Colorless − Odorless − Tasteless Disadvantage: − Toxic when Oxygen is the only gas excessive amounts metabolized by the human body are breathed under pressure Too much or too little oxygen is dangerous! Oxygen Toxicity -
AP Chemistry Chapter 5 Gases Ch
AP Chemistry Chapter 5 Gases Ch. 5 Gases Agenda 23 September 2017 Per 3 & 5 ○ 5.1 Pressure ○ 5.2 The Gas Laws ○ 5.3 The Ideal Gas Law ○ 5.4 Gas Stoichiometry ○ 5.5 Dalton’s Law of Partial Pressures ○ 5.6 The Kinetic Molecular Theory of Gases ○ 5.7 Effusion and Diffusion ○ 5.8 Real Gases ○ 5.9 Characteristics of Several Real Gases ○ 5.10 Chemistry in the Atmosphere 5.1 Units of Pressure 760 mm Hg = 760 Torr = 1 atm Pressure = Force = Newton = pascal (Pa) Area m2 5.2 Gas Laws of Boyle, Charles and Avogadro PV = k Slope = k V = k P y = k(1/P) + 0 5.2 Gas Laws of Boyle - use the actual data from Boyle’s Experiment Table 5.1 And Desmos to plot Volume vs. Pressure And then Pressure vs 1/V. And PV vs. V And PV vs. P Boyle’s Law 3 centuries later? Boyle’s law only holds precisely at very low pressures.Measurements at higher pressures reveal PV is not constant, but varies as pressure varies. Deviations slight at pressures close to 1 atm we assume gases obey Boyle’s law in our calcs. A gas that strictly obeys Boyle’s Law is called an Ideal gas. Extrapolate (extend the line beyond the experimental points) back to zero pressure to find “ideal” value for k, 22.41 L atm Look Extrapolatefamiliar? (extend the line beyond the experimental points) back to zero pressure to find “ideal” value for k, 22.41 L atm The volume of a gas at constant pressure increases linearly with the Charles’ Law temperature of the gas. -
THE SOLUBILITY of GASES in LIQUIDS INTRODUCTION the Solubility Data Project Aims to Make a Comprehensive Search of the Lit- Erat
THE SOLUBILITY OF GASES IN LIQUIDS R. Battino, H. L. Clever and C. L. Young INTRODUCTION The Solubility Data Project aims to make a comprehensive search of the lit erature for data on the solubility of gases, liquids and solids in liquids. Data of suitable accuracy are compiled into data sheets set out in a uni form format. The data for each system are evaluated and where data of suf ficient accuracy are available values recommended and in some cases a smoothing equation suggested to represent the variation of solubility with pressure and/or temperature. A text giving an evaluation and recommended values and the compiled data sheets are pUblished on consecutive pages. DEFINITION OF GAS SOLUBILITY The distinction between vapor-liquid equilibria and the solUbility of gases in liquids is arbitrary. It is generally accepted that the equilibrium set up at 300K between a typical gas such as argon and a liquid such as water is gas liquid solubility whereas the equilibrium set up between hexane and cyclohexane at 350K is an example of vapor-liquid equilibrium. However, the distinction between gas-liquid solUbility and vapor-liquid equilibrium is often not so clear. The equilibria set up between methane and propane above the critical temperature of methane and below the critical temperature of propane may be classed as vapor-liquid equilibrium or as gas-liquid solu bility depending on the particular range of pressure considered and the par ticular worker concerned. The difficulty partly stems from our inability to rigorously distinguish between a gas, a vapor, and a liquid, which has been discussed in numerous textbooks. -
CEE 370 Environmental Engineering Principles Henry's
CEE 370 Lecture #7 9/18/2019 Updated: 18 September 2019 Print version CEE 370 Environmental Engineering Principles Lecture #7 Environmental Chemistry V: Thermodynamics, Henry’s Law, Acids-bases II Reading: Mihelcic & Zimmerman, Chapter 3 Davis & Masten, Chapter 2 Mihelcic, Chapt 3 David Reckhow CEE 370 L#7 1 Henry’s Law Henry's Law states that the amount of a gas that dissolves into a liquid is proportional to the partial pressure that gas exerts on the surface of the liquid. In equation form, that is: C AH = K p A where, CA = concentration of A, [mol/L] or [mg/L] KH = equilibrium constant (often called Henry's Law constant), [mol/L-atm] or [mg/L-atm] pA = partial pressure of A, [atm] David Reckhow CEE 370 L#7 2 Lecture #7 Dave Reckhow 1 CEE 370 Lecture #7 9/18/2019 Henry’s Law Constants Reaction Name Kh, mol/L-atm pKh = -log Kh -2 CO2(g) _ CO2(aq) Carbon 3.41 x 10 1.47 dioxide NH3(g) _ NH3(aq) Ammonia 57.6 -1.76 -1 H2S(g) _ H2S(aq) Hydrogen 1.02 x 10 0.99 sulfide -3 CH4(g) _ CH4(aq) Methane 1.50 x 10 2.82 -3 O2(g) _ O2(aq) Oxygen 1.26 x 10 2.90 David Reckhow CEE 370 L#7 3 Example: Solubility of O2 in Water Background Although the atmosphere we breathe is comprised of approximately 20.9 percent oxygen, oxygen is only slightly soluble in water. In addition, the solubility decreases as the temperature increases. -
Ideal Gasses Is Known As the Ideal Gas Law
ESCI 341 – Atmospheric Thermodynamics Lesson 4 –Ideal Gases References: An Introduction to Atmospheric Thermodynamics, Tsonis Introduction to Theoretical Meteorology, Hess Physical Chemistry (4th edition), Levine Thermodynamics and an Introduction to Thermostatistics, Callen IDEAL GASES An ideal gas is a gas with the following properties: There are no intermolecular forces, except during collisions. All collisions are elastic. The individual gas molecules have no volume (they behave like point masses). The equation of state for ideal gasses is known as the ideal gas law. The ideal gas law was discovered empirically, but can also be derived theoretically. The form we are most familiar with, pV nRT . Ideal Gas Law (1) R has a value of 8.3145 J-mol1-K1, and n is the number of moles (not molecules). A true ideal gas would be monatomic, meaning each molecule is comprised of a single atom. Real gasses in the atmosphere, such as O2 and N2, are diatomic, and some gasses such as CO2 and O3 are triatomic. Real atmospheric gasses have rotational and vibrational kinetic energy, in addition to translational kinetic energy. Even though the gasses that make up the atmosphere aren’t monatomic, they still closely obey the ideal gas law at the pressures and temperatures encountered in the atmosphere, so we can still use the ideal gas law. FORM OF IDEAL GAS LAW MOST USED BY METEOROLOGISTS In meteorology we use a modified form of the ideal gas law. We first divide (1) by volume to get n p RT . V we then multiply the RHS top and bottom by the molecular weight of the gas, M, to get Mn R p T . -
Partial Liquid Ventilation Versus Conventional Mechanical Ventilation with High PEEP and Moderate Tidal Volume in Acute Respiratory Failure in Piglets
0031-3998/02/5202-0225 PEDIATRIC RESEARCH Vol. 52, No. 2, 2002 Copyright © 2002 International Pediatric Research Foundation, Inc. Printed in U.S.A. Partial Liquid Ventilation Versus Conventional Mechanical Ventilation with High PEEP and Moderate Tidal Volume in Acute Respiratory Failure in Piglets SIEGFRIED RÖDL, BERNDT URLESBERGER, IGOR KNEZ, DRAGO DACAR, AND GERFRIED ZOBEL Departments of Pediatrics [S.R., G.Z.], Neonatology [B.U.] and Cardiac Surgery [I.K., D.D.], University of Graz, A-8036 Graz, Austria ABSTRACT This prospective randomized pilot study aimed to test the measurements. When compared with control animals, partial hypotheses that partial liquid ventilation combined with a high liquid ventilation resulted in significantly better oxygenation positive end-expiratory pressure (PEEP) and a moderate tidal with improved cardiac output and oxygen delivery. Dead space volume results in improved gas exchange and lung mechanics ventilation appeared to be lower during partial liquid ventilation without negative hemodynamic influences compared with con- compared with conventional mechanical ventilation. No signifi- ventional mechanical ventilation in acute lung injury in piglets. cant differences were observed in airway pressures, pulmonary Acute lung injury was induced in 12 piglets weighing 9.0 Ϯ 2.4 compliance, and airway resistance between both groups. The kg by repeated i.v. injections of oleic acid and repeated lung results of this pilot study suggest that partial liquid ventilation lavages. Thereafter, the animals were randomly assigned either combined with high PEEP and moderate tidal volume improves to partial liquid ventilation (n ϭ 6) or conventional mechanical oxygenation, dead space ventilation, cardiac output, and oxygen ϭ ventilation (n 6) at a fractional concentration of inspired O2 of delivery compared with conventional mechanical ventilation in 1.0, a PEEP of 1.2 kPa, a tidal volume Ͻ 10 mL/kg body weight acute lung injury in piglets but has no significant influence on (bw), a respiratory rate of 24 breaths/min, and an inspiratory/ lung mechanics. -
Outta Gas (From the 2007: Exploring the Inner Space of the Celebes Sea
2007: Exploring the Inner Space of the Celebes Sea Outta Gas FOCUS MAXIMUM NUMBER OF STUDENTS Gas laws 30 GRADE LEVEL KEY WORDS 9-12 (Chemistry/Physics) Celebes Sea SCUBA diving FOCUS QUESTION Gas laws How can Boyle’s Law, Charles’ Law, Gay-Lussac’s Ideal Gas Law Law, Henry’s Law, and Dalton’s Law be used to Boyle’s Law predict the behavior of gases used in SCUBA div- Charles’ Law ing? Gay-Lussac’s Law Henry’s Law LEARNING OBJECTIVES Dalton’s Law Students will define Boyle’s Law, Charles’ Law, Pressure Gay-Lussac’s Law, Henry’s Law, and Dalton’s Law. Worksheet Mathematics Students will use Boyle’s Law, Charles’ Law, Gay- Lussac’s Law, Henry’s Law, and Dalton’s Law to BACKGROUND INFORMATION solve practical problems related to SCUBA diving. Indonesia is well-known as one of Earth’s major centers of biodiversity. Although Indonesia cov- MATERIALS ers only 1.3 percent of Earth’s land surface, it “Blue Water Diving Worksheet,” one copy for includes: each student or student group • 10 percent of the world’s flowering plant species; AUDIO/VISUAL MATERIALS • 12 percent of the world’s mammal species; None • 16 percent of all reptile and amphibian species; and TEACHING TIME • 17 percent of the world’s bird species. One or two 45-minute class periods plus time for students to complete worksheet In addition, together with the Philippines and Great Barrier Reef, this region has more species SEATING ARRANGEMENT of fishes, corals, mollusks, and crustaceans than Classroom style any other location on Earth. -
Respiration (Physiology) 1 Respiration (Physiology)
Respiration (physiology) 1 Respiration (physiology) In physiology, respiration (often mistaken with breathing) is defined as the transport of oxygen from the outside air to the cells within tissues, and the transport of carbon dioxide in the opposite direction. This is in contrast to the biochemical definition of respiration, which refers to cellular respiration: the metabolic process by which an organism obtains energy by reacting oxygen with glucose to give water, carbon dioxide and ATP (energy). Although physiologic respiration is necessary to sustain cellular respiration and thus life in animals, the processes are distinct: cellular respiration takes place in individual cells of the animal, while physiologic respiration concerns the bulk flow and transport of metabolites between the organism and the external environment. In unicellular organisms, simple diffusion is sufficient for gas exchange: every cell is constantly bathed in the external environment, with only a short distance for gases to flow across. In contrast, complex multicellular animals such as humans have a much greater distance between the environment and their innermost cells, thus, a respiratory system is needed for effective gas exchange. The respiratory system works in concert with a circulatory system to carry gases to and from the tissues. In air-breathing vertebrates such as humans, respiration of oxygen includes four stages: • Ventilation, moving of the ambient air into and out of the alveoli of the lungs. • Pulmonary gas exchange, exchange of gases between the alveoli and the pulmonary capillaries. • Gas transport, movement of gases within the pulmonary capillaries through the circulation to the peripheral capillaries in the organs, and then a movement of gases back to the lungs along the same circulatory route. -
Masteringphysics: Assignmen
MasteringPhysics: Assignment Print View http://session.masteringphysics.com/myct/assignmentPrint... Manage this Assignment: Chapter 18 Due: 12:00am on Saturday, July 3, 2010 Note: You will receive no credit for late submissions. To learn more, read your instructor's Grading Policy A Law for Scuba Divers Description: Find the increase in the concentration of air in a scuba diver's lungs. Find the number of moles of air exhaled. Also, consider the isothermal expansion of air as a freediver diver surfaces. Identify the proper pV graph. Associated medical conditions discussed. SCUBA is an acronym for self-contained underwater breathing apparatus. Scuba diving has become an increasingly popular sport, but it requires training and certification owing to its many dangers. In this problem you will explore the biophysics that underlies the two main conditions that may result from diving in an incorrect or unsafe manner. While underwater, a scuba diver must breathe compressed air to compensate for the increased underwater pressure. There are a couple of reasons for this: 1. If the air were not at the same pressure as the water, the pipe carrying the air might close off or collapse under the external water pressure. 2. Compressed air is also more concentrated than the air we normally breathe, so the diver can afford to breathe more shallowly and less often. A mechanical device called a regulator dispenses air at the proper (higher than atmospheric) pressure so that the diver can inhale. Part A Suppose Gabor, a scuba diver, is at a depth of . Assume that: 1. The air pressure in his air tract is the same as the net water pressure at this depth. -
Shaffer CV 010419.Pdf
CURRICULUM VITAE Name: Thomas H. Shaffer, MS.E., Ph.D. Office Address: Temple University School of Medicine Department of Physiology 3420 North Broad Street Philadelphia, PA 19140 Office Address: Nemours Research Lung Center Department of Biomedical Research Alfred I. duPont Hospital for Children 1600 Rockland Road, A/R 302 Wilmington, DE 19803 Present Academic and Hospital Appointments: 2004 – Present Director, Nemours Center for Pediatric Research Nemours Biomedical Research Alfred I duPont Hospital for Children 1600 Rockland Road Wilmington, DE 19803 2001 - Present Associate Director , Nemours Biomedical Research Nemours Children’s Clinic – Wilmington of The Nemours Foundation Alfred I. duPont Hospital for Children, Wilmington, DE 19803 Director, Nemours Pediatric Lung Center Nemours Children's Clinic - Wilmington of The Nemours Foundation Alfred I. duPont Hospital for Children, Wilmington, DE Director, Office of Technology Transfer Nemours Children's Clinic - Wilmington of The Nemours Foundation Alfred I. duPont Hospital for Children, Wilmington, DE Professor, Pediatrics, Department of Pediatrics Thomas Jefferson University, College of Medicine, Philadelphia, PA 2001-Present Professor Emeritus, Physiology and Pediatrics, Departments of Physiology and Pediatrics Temple University School of Medicine, Philadelphia, PA 1 Training, Awards, Societies, and Membership: Education: 1963-1968 B.S. Mechanical Engineering, Drexel University, Philadelphia, PA 1968 Mathematics, Pennsylvania State University, State College, PA 1969-1970 MSE. Applied