The Discovery of Boyle's Law, and the Concept of the Elasticity of Air in The
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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. -
Thermodynamics Notes
Thermodynamics Notes Steven K. Krueger Department of Atmospheric Sciences, University of Utah August 2020 Contents 1 Introduction 1 1.1 What is thermodynamics? . .1 1.2 The atmosphere . .1 2 The Equation of State 1 2.1 State variables . .1 2.2 Charles' Law and absolute temperature . .2 2.3 Boyle's Law . .3 2.4 Equation of state of an ideal gas . .3 2.5 Mixtures of gases . .4 2.6 Ideal gas law: molecular viewpoint . .6 3 Conservation of Energy 8 3.1 Conservation of energy in mechanics . .8 3.2 Conservation of energy: A system of point masses . .8 3.3 Kinetic energy exchange in molecular collisions . .9 3.4 Working and Heating . .9 4 The Principles of Thermodynamics 11 4.1 Conservation of energy and the first law of thermodynamics . 11 4.1.1 Conservation of energy . 11 4.1.2 The first law of thermodynamics . 11 4.1.3 Work . 12 4.1.4 Energy transferred by heating . 13 4.2 Quantity of energy transferred by heating . 14 4.3 The first law of thermodynamics for an ideal gas . 15 4.4 Applications of the first law . 16 4.4.1 Isothermal process . 16 4.4.2 Isobaric process . 17 4.4.3 Isosteric process . 18 4.5 Adiabatic processes . 18 5 The Thermodynamics of Water Vapor and Moist Air 21 5.1 Thermal properties of water substance . 21 5.2 Equation of state of moist air . 21 5.3 Mixing ratio . 22 5.4 Moisture variables . 22 5.5 Changes of phase and latent heats . -
Introduction to Hydrostatics
Introduction to Hydrostatics Hydrostatics Equation The simplified Navier Stokes equation for hydrostatics is a vector equation, which can be split into three components. The convention will be adopted that gravity always acts in the negative z direction. Thus, and the three components of the hydrostatics equation reduce to Since pressure is now only a function of z, total derivatives can be used for the z-component instead of partial derivatives. In fact, this equation can be integrated directly from some point 1 to some point 2. Assuming both density and gravity remain nearly constant from 1 to 2 (a reasonable approximation unless there is a huge elevation difference between points 1 and 2), the z- component becomes Another form of this equation, which is much easier to remember is This is the only hydrostatics equation needed. It is easily remembered by thinking about scuba diving. As a diver goes down, the pressure on his ears increases. So, the pressure "below" is greater than the pressure "above." Some "rules" to remember about hydrostatics Recall, for hydrostatics, pressure can be found from the simple equation, There are several "rules" or comments which directly result from the above equation: If you can draw a continuous line through the same fluid from point 1 to point 2, then p1 = p2 if z1 = z2. For example, consider the oddly shaped container below: By this rule, p1 = p2 and p4 = p5 since these points are at the same elevation in the same fluid. However, p2 does not equal p3 even though they are at the same elevation, because one cannot draw a line connecting these points through the same fluid. -
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. -
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. -
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. -
Module 2: Hydrostatics
Module 2: Hydrostatics . Hydrostatic pressure and devices: 2 lectures . Forces on surfaces: 2.5 lectures . Buoyancy, Archimedes, stability: 1.5 lectures Mech 280: Frigaard Lectures 1-2: Hydrostatic pressure . Should be able to: . Use common pressure terminology . Derive the general form for the pressure distribution in static fluid . Calculate the pressure within a constant density fluids . Calculate forces in a hydraulic press . Analyze manometers and barometers . Calculate pressure distribution in varying density fluid . Calculate pressure in fluids in rigid body motion in non-inertial frames of reference Mech 280: Frigaard Pressure . Pressure is defined as a normal force exerted by a fluid per unit area . SI Unit of pressure is N/m2, called a pascal (Pa). Since the unit Pa is too small for many pressures encountered in engineering practice, kilopascal (1 kPa = 103 Pa) and mega-pascal (1 MPa = 106 Pa) are commonly used . Other units include bar, atm, kgf/cm2, lbf/in2=psi . 1 psi = 6.695 x 103 Pa . 1 atm = 101.325 kPa = 14.696 psi . 1 bar = 100 kPa (close to atmospheric pressure) Mech 280: Frigaard Absolute, gage, and vacuum pressures . Actual pressure at a give point is called the absolute pressure . Most pressure-measuring devices are calibrated to read zero in the atmosphere. Pressure above atmospheric is called gage pressure: Pgage=Pabs - Patm . Pressure below atmospheric pressure is called vacuum pressure: Pvac=Patm - Pabs. Mech 280: Frigaard Pressure at a Point . Pressure at any point in a fluid is the same in all directions . Pressure has a magnitude, but not a specific direction, and thus it is a scalar quantity . -
Pressure Vs. Volume and Boyle's
Pressure vs. Volume and Boyle’s Law SCIENTIFIC Boyle’s Law Introduction In 1642 Evangelista Torricelli, who had worked as an assistant to Galileo, conducted a famous experiment demonstrating that the weight of air would support a column of mercury about 30 inches high in an inverted tube. Torricelli’s experiment provided the first measurement of the invisible pressure of air. Robert Boyle, a “skeptical chemist” working in England, was inspired by Torricelli’s experiment to measure the pressure of air when it was compressed or expanded. The results of Boyle’s experiments were published in 1662 and became essentially the first gas law—a mathematical equation describing the relationship between the volume and pressure of air. What is Boyle’s law and how can it be demonstrated? Concepts • Gas properties • Pressure • Boyle’s law • Kinetic-molecular theory Background Open end Robert Boyle built a simple apparatus to measure the relationship between the pressure and volume of air. The apparatus ∆h ∆h = 29.9 in. Hg consisted of a J-shaped glass tube that was Sealed end 1 sealed at one end and open to the atmosphere V2 = /2V1 Trapped air (V1) at the other end. A sample of air was trapped in the sealed end by pouring mercury into Mercury the tube (see Figure 1). In the beginning of (Hg) the experiment, the height of the mercury Figure 1. Figure 2. column was equal in the two sides of the tube. The pressure of the air trapped in the sealed end was equal to that of the surrounding air and equivalent to 29.9 inches (760 mm) of mercury. -
1 Introduction
Cambridge University Press 978-0-521-88707-6 - An Introduction to the Chemistry of the Sea: Second Edition Michael E. Q. Pilson Excerpt More information 1 Introduction A complete working model of the earth is still a rather distant goal. HOLLAND 1978 Those magnificent pictures of Earth from space, among the most humanly important and evocative results from the placing of manned and unmanned satellites in orbit during the last several decades, have shown us that underneath the clouds most of the world is blue. Viewed in this way from space, Earth is seen as a planet covered mostly by water, and most of that water is seawater. This thin layer of water, covering 71% of Earth, affects or controls much of its climate and chemistry. The blue color of the sea tells us that most sunlight on the ocean is absorbed and not reflected. The absorption of sunlight warms the planet. The warmth evaporates water, especially from the tropical ocean. Water in the atmosphere is a greenhouse gas, and this also helps to warm Earth. Some atmos- pheric water forms clouds; by reflecting sunlight clouds help to cool Earth. The balance between heating and cooling is always changing as clouds form and dissipate, so exact calculation of the balance is difficult. The water in the ocean is a vast reservoir of heat, which buffers and slows global change. Both the currents in the ocean and the winds in the atmosphere carry heat from low latitudes, where there is a net input, towards the poles, where there is a net loss of heat to space. -
Measurement of Human Metabolism
Measurement of Human Metabolism BY ROBERT BRYCHTA, ERICA WOHLERS, JON MOON, AND KONG CHEN besity is one of the most prevalent chronic diseases globally, especially in the United States. While the United States gained an early lead in unneces- sary weight gain, most other countries are quickly closing the gap. The lat- Oest U.S. National Health and Nutrition Examination Survey (NHANES, http://www.cdc.gov/nchs/nhanes.htm) documents that about one third of adults in the United States are now overweight [a body-mass index (BMI) between 25 and 30 kg/m2] and another one third (61 million) are considered obese (BMI > 30 kg/m2). Being obese is a strong risk factor for cardiovascular diseases, type 2 diabetes, osteoporosis, some cancers, and depression. The economic impact of this condition is staggering: in 2008, more than 147 billion dollars were spent just in the United States for medical costs related to obesity. Time lost from work and spending on weight loss costs even more. Obesity is influenced to some extent by genetic and environmental fac- tors. However, two centuries of research has repeatedly confirmed that the basic principle of energy balance (Figure 1) governs the accumula- tion of fat. Obesity results from years of slightly higher energy intake from food than energy expended (EE). The path to obesity leads from a positive energy balance of approximately 100–125 kcal per day to between 2 and 6 kg of weight gain per year (Figure 2; [1]). In other words, you can become overweight by eating just one or two cookies or drinking a can of sugar soda a day.