Boyle's Law: Registering the Pressure Changes of Gas Held in a Closed
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History of Hyperbaric Medicine ROBERT S
American Osteopathic College of Occupational and Preventive Medicine 2015 Mid Year Educational Conference, Ft. Lauderdale, Florida How Did We Get From Here History of Hyperbaric Medicine ROBERT S. MICHAELSON, DO, MPH MARCH 14, 2015 To Here 3 History of Hyperbaric Medicine Discuss history of diving Discovery of the atmosphere Five major milestones in the development of hyperbaric medicine Triger’s caisson Eads and Brooklyn Bridge Haldane and staged decompression Rescue of the USS Squalus Donnell and Norton 5 Gourd Breathing About 375 AD Diving as a Profession Salvage Operations From as early as 9th century BC Pay scale based on depth of dive Military Operations Early attempts to bore into hull of ships or attach crude explosives to vessels Confined to shallow waters and for short duration dives Very Hard to be Stealthy and Effective T-1 American Osteopathic College of Occupational and Preventive Medicine 2015 Mid Year Educational Conference, Ft. Lauderdale, Florida DivingHood by Flavius Vegetius Renatus about 375 AD in Leonardo’s (1452-1519) Design For Swim Fins Epitome Institutionum Rei Militaris Diving Rig of Niccolo Tartaglia Canon Recovery Mid-1600’s about 1551 Probably First Diving Bell Mid-1600’s T-2 American Osteopathic College of Occupational and Preventive Medicine 2015 Mid Year Educational Conference, Ft. Lauderdale, Florida T-3 American Osteopathic College of Occupational and Preventive Medicine 2015 Mid Year Educational Conference, Ft. Lauderdale, Florida Diving as a Profession Salvage Operations From as early as 9th century BC Pay scale based on depth on dive Military Operations Early attempts to bore into hull of ships or attach crude explosives to vessels Confined to shallow waters and for short duration dives Very Hard to be Stealthy and Effective Diving Bell-1664 Klingert’s Diving Suit -1797 The Vasa, a Swedish ship sunk within a This equipment is the first to be called mile of her maidenvoyage in 1628. -
Role and Important of Hydrogen in Plant Metabolism
Kheyrodin and Kheyrodin, World J. Biol. Med. Science Volume 4 (3) 13-20, 2017 Indexed, Abstracted and Cited: Index Copernicus International (Poland), ISRA Journal Impact Factor, International Impact Factor Services (IIFS), Directory of Research Journals Indexing (DRJI), International Institute of Organized Research and Scientific Indexing Services, Cosmos Science Foundation (South-East Asia), International Innovative Journal Impact Factor, Einstein Institute for Scientific Information {EISI}, Directory of Open Access Scholarly Resources, Science Indexing Library (UAE), Swedish Scientific Publication (Sweden), citefactor.org journals indexing, Directory Indexing of International Research Journals World Journal of Biology and Medical Sciences Published by Society for Advancement of Science® ISSN 2349-0063 (Online/Electronic) Volume 4, Issue-3, 13-20, July to September, 2017 Journal Impact Factor: 4.197 WJBMS 04/03/119/2017 All rights reserved www.sasjournals.com A Double Blind Peer Reviewed Journal / Refereed Journal [email protected]/[email protected] REVIEW ARTICLE Received: 04/08/2017 Revised: 04/09/2017 Accepted: 05/09/2017 Role and Important of Hydrogen in Plant Metabolism Hamid Kheyrodin and *Sadaf Kheyrodin Faculty of Desert Science, Semnan University, Iran *Urban Planning in Mashad Azad University, Iran ABSTRACT Hydrogen is the simplest and most abundant element in the entire universe. According to astrophysicist David Palmer, about 75 percent of all the known elemental matter that exists is composed of hydrogen. The nucleus of a hydrogen atom is made out of a single proton, which is a positively charged particle. One electron orbits around the outside of the nucleus. Neutrons, which can be found in all other elements, do not exist in the most common form of hydrogen.Hydrogen peroxide (H2O2) is produced predominantly in plant cells during photosynthesis and photorespiration, and to a lesser extent, in respiration processes. -
Scuba Diving History
Scuba diving history Scuba history from a diving bell developed by Guglielmo de Loreno in 1535 up to John Bennett’s dive in the Philippines to amazing 308 meter in 2001 and much more… Humans have been diving since man was required to collect food from the sea. The need for air and protection under water was obvious. Let us find out how mankind conquered the sea in the quest to discover the beauty of the under water world. 1535 – A diving bell was developed by Guglielmo de Loreno. 1650 – Guericke developed the first air pump. 1667 – Robert Boyle observes the decompression sickness or “the bends”. After decompression of a snake he noticed gas bubbles in the eyes of a snake. 1691 – Another diving bell a weighted barrels, connected with an air pipe to the surface, was patented by Edmund Halley. 1715 – John Lethbridge built an underwater cylinder that was supplied via an air pipe from the surface with compressed air. To prevent the water from entering the cylinder, greased leather connections were integrated at the cylinder for the operators arms. 1776 – The first submarine was used for a military attack. 1826 – Charles Anthony and John Deane patented a helmet for fire fighters. This helmet was used for diving too. This first version was not fitted to the diving suit. The helmet was attached to the body of the diver with straps and air was supplied from the surfa 1837 – Augustus Siebe sealed the diving helmet of the Deane brothers’ to a watertight diving suit and became the standard for many dive expeditions. -
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. -
Pressure Diffusion Waves in Porous Media
Lawrence Berkeley National Laboratory Lawrence Berkeley National Laboratory Title Pressure diffusion waves in porous media Permalink https://escholarship.org/uc/item/5bh9f6c4 Authors Silin, Dmitry Korneev, Valeri Goloshubin, Gennady Publication Date 2003-04-08 eScholarship.org Powered by the California Digital Library University of California Pressure diffusion waves in porous media Dmitry Silin* and Valeri Korneev, Lawrence Berkeley National Laboratory, Gennady Goloshubin, University of Houston Summary elastic porous medium. Such a model results in a parabolic pressure diffusion equation. Its validity has been Pressure diffusion wave in porous rocks are under confirmed and “canonized”, for instance, in transient consideration. The pressure diffusion mechanism can pressure well test analysis, where it is used as the main tool provide an explanation of the high attenuation of low- since 1930th, see e.g. Earlougher (1977) and Barenblatt et. frequency signals in fluid-saturated rocks. Both single and al., (1990). The basic assumptions of this model make it dual porosity models are considered. In either case, the applicable specifically in the low-frequency range of attenuation coefficient is a function of the frequency. pressure fluctuations. Introduction Theories describing wave propagation in fluid-bearing porous media are usually derived from Biot’s theory of poroelasticity (Biot 1956ab, 1962). However, the observed high attenuation of low-frequency waves (Goloshubin and Korneev, 2000) is not well predicted by this theory. One of possible reasons for difficulties in detecting Biot waves in real rocks is in the limitations imposed by the assumptions underlying Biot’s equations. Biot (1956ab, 1962) derived his main equations characterizing the mechanical motion of elastic porous fluid-saturated rock from the Hamiltonian Principle of Least Action. -
Metabolism Picton, 2019
History of Science Metabolism Picton, 2019 Metabolism An Experiment on a Bird in the Air Pump Joseph Wright of Derby, 1768 In a previous presentation we followed studies of how the human body works up to the 17th Century. As the Scientific Revolution proceeded the old dogmas such as the humors were cast aside and experiments became the way to understand the processes of life. The painting shows the new scientific approach to understanding life. The scientist removes air from a glass container and shows that the bird can no longer live without air. The painting was based on one of the experiments conducted in by Robert Boyle (1627-1691) and published in 1660. Oxygen in the air is essential to human life. Metabolism is the name given to the chemical reactions that occur in living organisms. It derives from the Greek meta (beyond) and ballein (throw) – it signifies the changes that are effected. It is composed of anabolism (ana, upward) – the production of new compounds – and catabolism (cato, down) – the breakdown of compounds. From the Wikipedia notes on the painting The witnesses display various emotions: one of the girls worriedly watches the fate of the bird, while the other is too upset to observe and is comforted by her father; two gentlemen (one of them dispassionately timing the experiment) and a boy look on with interest, while the young lovers to the left of the painting are absorbed only in each other. The scientist himself looks directly out of the picture, as if challenging the viewer to judge whether the pumping should continue, killing the bird, or whether the air should be replaced and the cockatoo saved. -
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. -
What Is High Blood Pressure?
ANSWERS Lifestyle + Risk Reduction by heart High Blood Pressure BLOOD PRESSURE SYSTOLIC mm Hg DIASTOLIC mm Hg What is CATEGORY (upper number) (lower number) High Blood NORMAL LESS THAN 120 and LESS THAN 80 ELEVATED 120-129 and LESS THAN 80 Pressure? HIGH BLOOD PRESSURE 130-139 or 80-89 (HYPERTENSION) Blood pressure is the force of blood STAGE 1 pushing against blood vessel walls. It’s measured in millimeters of HIGH BLOOD PRESSURE 140 OR HIGHER or 90 OR HIGHER mercury (mm Hg). (HYPERTENSION) STAGE 2 High blood pressure (HBP) means HYPERTENSIVE the pressure in your arteries is higher CRISIS HIGHER THAN 180 and/ HIGHER THAN 120 than it should be. Another name for (consult your doctor or immediately) high blood pressure is hypertension. Blood pressure is written as two numbers, such as 112/78 mm Hg. The top, or larger, number (called Am I at higher risk of developing HBP? systolic pressure) is the pressure when the heart There are risk factors that increase your chances of developing HBP. Some you can control, and some you can’t. beats. The bottom, or smaller, number (called diastolic pressure) is the pressure when the heart Those that can be controlled are: rests between beats. • Cigarette smoking and exposure to secondhand smoke • Diabetes Normal blood pressure is below 120/80 mm Hg. • Being obese or overweight If you’re an adult and your systolic pressure is 120 to • High cholesterol 129, and your diastolic pressure is less than 80, you have elevated blood pressure. High blood pressure • Unhealthy diet (high in sodium, low in potassium, and drinking too much alcohol) is a systolic pressure of 130 or higher,or a diastolic pressure of 80 or higher, that stays high over time. -
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. -
The Development of the Chlorinity-Salinity Concept in Oceanography
AN ABSTRACT OF THE THESIS OF WILLIAM JOHN WALLACE, JR. for the Ph. D. (Name) (Degree) in GENERAL SCIENCE presented on April 7,1971 (Major) (Date) Title: THE DEVELOPMENT OF THE CHLORINITY-SALINITY CONCEPT INOCEANOGRAM Redacted for Privacy Abstract approved: Vert J. Moris This study traces the historical foundations of the concept of constant ionic proportionality and the equation (Salinity[S°700] = 1.805 Chlorinity [C1700] + 0.030) which has been in general use in ocean- ography since 1902 until 1969 and which is based upon this constancy, The notion that the constituents present in sea water exist in constant proportions was first clearly stated by Marcet in 1819.The germ of the idea may be found, however, in the worksof Bergmann in the late eighteenth century and implied in other works.Maury, in the mid-nineteenth century, popularized the concept and Forchhammer, in 1865, strengthened this idea by quantifying it and introducing the use of the "coefficient" of chlorine to determine salinity,Although he determined a slightly different value for the coefficient, Dittmar regarded his analysis of the sea water samples from the Challenger expedition as a vindication of Forchhammer's work.Knudsen, Forch and Sorensen, in 1902 gave a lengthy gravimetric definition for salinity based on the analysis of nine water samples.As this proce- dural definition was in practice too time-consuming to perform, the above equation was presented which relates the determination of salinity to that of chlorinity.The work of Knudsen, Forch and Sorensen, and that of Dittmar before them, wasaccepted as demonstrating the constancy of ionic proportionality, and the equation was a cornerstone of chemical oceanographyfrom 1902 to 1958. -
Cotton Mather's Relationship to Science
Georgia State University ScholarWorks @ Georgia State University English Theses Department of English 4-16-2008 Cotton Mather's Relationship to Science James Daniel Hudson Follow this and additional works at: https://scholarworks.gsu.edu/english_theses Part of the English Language and Literature Commons Recommended Citation Hudson, James Daniel, "Cotton Mather's Relationship to Science." Thesis, Georgia State University, 2008. https://scholarworks.gsu.edu/english_theses/33 This Thesis is brought to you for free and open access by the Department of English at ScholarWorks @ Georgia State University. It has been accepted for inclusion in English Theses by an authorized administrator of ScholarWorks @ Georgia State University. For more information, please contact [email protected]. COTTON MATHER’S RELATIONSHIP TO SCIENCE by JAMES DANIEL HUDSON Under the Direction of Dr. Reiner Smolinski ABSTRACT The subject of this project is Cotton Mather’s relationship to science. As a minister, Mather’s desire to harmonize science with religion is an excellent medium for understanding the effects of the early Enlightenment upon traditional views of Scripture. Through “Biblia Americana” and The Christian Philosopher, I evaluate Mather’s effort to relate Newtonian science to the six creative days as recorded in Genesis 1. Chapter One evaluates Mather’s support for the scientific theories of Isaac Newton and his reception to natural philosophers who advocate Newton’s theories. Chapter Two highlights Mather’s treatment of the dominant cosmogonies preceding Isaac Newton. The Conclusion returns the reader to Mather’s principal occupation as a minister and the limits of science as informed by his theological mind. Through an exploration of Cotton Mather’s views on science, a more comprehensive understanding of this significant early American and the ideological assumptions shaping his place in American history is realized. -
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.