Measuring Metabolism Using O2 and CO2 1
Total Page:16
File Type:pdf, Size:1020Kb
Load more
Recommended publications
-
Solutes and Solution
Solutes and Solution The first rule of solubility is “likes dissolve likes” Polar or ionic substances are soluble in polar solvents Non-polar substances are soluble in non- polar solvents Solutes and Solution There must be a reason why a substance is soluble in a solvent: either the solution process lowers the overall enthalpy of the system (Hrxn < 0) Or the solution process increases the overall entropy of the system (Srxn > 0) Entropy is a measure of the amount of disorder in a system—entropy must increase for any spontaneous change 1 Solutes and Solution The forces that drive the dissolution of a solute usually involve both enthalpy and entropy terms Hsoln < 0 for most species The creation of a solution takes a more ordered system (solid phase or pure liquid phase) and makes more disordered system (solute molecules are more randomly distributed throughout the solution) Saturation and Equilibrium If we have enough solute available, a solution can become saturated—the point when no more solute may be accepted into the solvent Saturation indicates an equilibrium between the pure solute and solvent and the solution solute + solvent solution KC 2 Saturation and Equilibrium solute + solvent solution KC The magnitude of KC indicates how soluble a solute is in that particular solvent If KC is large, the solute is very soluble If KC is small, the solute is only slightly soluble Saturation and Equilibrium Examples: + - NaCl(s) + H2O(l) Na (aq) + Cl (aq) KC = 37.3 A saturated solution of NaCl has a [Na+] = 6.11 M and [Cl-] = -
SEARCH for EXTANT LIFE THROUGH HUMAN MISSION on the SURFACE of MARS P. Yun (El Camino College 16007 Crenshaw Blvd., Torrance, Ca
Mars Extant Life: What's Next? 2019 (LPI Contrib. No. 2108) 5024.pdf SEARCH FOR EXTANT LIFE THROUGH HUMAN MISSION ON THE SURFACE OF MARS P. Yun (El Camino College 16007 Crenshaw Blvd., Torrance, California 90506 USA, [email protected]) Introduction: NASA Mars missions focus on in- vestigating life in past and present Mars, understanding geological history and climate of Mars, and preparing human mission on the surface of Mars. If Martian ex- tant life exists, then it is expected to be a microorgan- ism due to a high level of radiation and the limited amount of liquid water on surface as well as a high level of carbon dioxide in atmosphere. Through human mission, currently available microbiological sensing technologies on Earth can be implemented on Mars with necessary modification and adjustment to Martian Figure 2. Scanning electron micrographs(SEM) of environment which has a high level of radiation on bacteria found in ice in Greenland and Antarctica surface and a high level of carbon dioxide in atmos- (Credit: Knowlton) phere as well as a low gravity compared to Earth. Mar- Water: Some liquid water may occur transiently on tian extant life may make a home in atmosphere, water, the Martian surface today.[6] Currently available de- ice, soil, or rock of surface or subsurface. tection techniques of microorganism in water include Atmosphere: Microbes consuming carbon- Biosensors, Vibrational Spectroscopy, MALDI/TOF containing chemicals exist in the in the middle-to- mass spectrometry, and Adenosine Tri-phosphate as- upper troposphere (8–15 km altitude) of Earth, and the say.[7] proportion of some microbes in atmosphere is higher Conclusion: Through human mission, currently than in soil and dust.[1] MSL Curiosity’s detection of a available sensing technologies to find microbes in at- seasonal methane cycle suggests that microbes may mosphere, water, ice, soil, rock of surface or subsur- exist in Martian atmosphere, which is composed of face on Earth can be utilized on Mars with necessary 96% carbon dioxide. -
A Novel Technique for the Precise Measurement of CO2 Production Rate in Small Aquatic Organisms As Validated on Aeshnid Dragonfly Nymphs Till S
© 2017. Published by The Company of Biologists Ltd | Journal of Experimental Biology (2017) 220, 964-968 doi:10.1242/jeb.150235 METHODS & TECHNIQUES A novel technique for the precise measurement of CO2 production rate in small aquatic organisms as validated on aeshnid dragonfly nymphs Till S. Harter*, Colin J. Brauner and Philip G. D. Matthews Ṁ in vitro ABSTRACT measuring small aquatic CO2 was validated both and in vivo The present study describes and validates a novel yet simple system using aeshnid dragonfly nymphs. for simultaneous in vivo measurements of rates of aquatic CO2 ̇ ̇ MATERIALS AND METHODS production (MCO2) and oxygen consumption (MO2), thus allowing the calculation of respiratory exchange ratios (RER). Diffusion of CO Animal collection and husbandry 2 Aeshna Anax junius from the aquatic phase into a gas phase, across a hollow fibre Aeshnid dragonfly nymphs ( spp. and ; wet mass ̇ 2.17 mg–1.46 g; n=15) were caught in the experimental ponds at the membrane, enabled aquatic MCO2 measurements with a high- ̇ University of British Columbia (summer 2016), and were held in the precision infrared gas CO2 analyser. MO was measured with a 2 laboratory for several weeks before experiments. Housing was in 1 l PO optode using a stop-flow approach. Injections of known amounts 2 glass containers connected to a recirculation system supplied with of CO2 into the apparatus yielded accurate and highly reproducible 2 dechlorinated Vancouver tap water at room temperature (22°C). measurements of CO2 content (R =0.997, P<0.001). The viability of in vivo measurements was demonstrated on aquatic dragonfly Animals were fed various wild-caught aquatic insects, twice a week. -
The History of Carbon Monoxide Intoxication
medicina Review The History of Carbon Monoxide Intoxication Ioannis-Fivos Megas 1 , Justus P. Beier 2 and Gerrit Grieb 1,2,* 1 Department of Plastic Surgery and Hand Surgery, Gemeinschaftskrankenhaus Havelhoehe, Kladower Damm 221, 14089 Berlin, Germany; fi[email protected] 2 Burn Center, Department of Plastic Surgery and Hand Surgery, University Hospital RWTH Aachen, Pauwelsstrasse 30, 52074 Aachen, Germany; [email protected] * Correspondence: [email protected] Abstract: Intoxication with carbon monoxide in organisms needing oxygen has probably existed on Earth as long as fire and its smoke. What was observed in antiquity and the Middle Ages, and usually ended fatally, was first successfully treated in the last century. Since then, diagnostics and treatments have undergone exciting developments, in particular specific treatments such as hyperbaric oxygen therapy. In this review, different historic aspects of the etiology, diagnosis and treatment of carbon monoxide intoxication are described and discussed. Keywords: carbon monoxide; CO intoxication; COHb; inhalation injury 1. Introduction and Overview Intoxication with carbon monoxide in organisms needing oxygen for survival has probably existed on Earth as long as fire and its smoke. Whenever the respiratory tract of living beings comes into contact with the smoke from a flame, CO intoxication and/or in- Citation: Megas, I.-F.; Beier, J.P.; halation injury may take place. Although the therapeutic potential of carbon monoxide has Grieb, G. The History of Carbon also been increasingly studied in recent history [1], the toxic effects historically dominate a Monoxide Intoxication. Medicina 2021, 57, 400. https://doi.org/10.3390/ much longer period of time. medicina57050400 As a colorless, odorless and tasteless gas, CO is produced by the incomplete combus- tion of hydrocarbons and poses an invisible danger. -
Page 1 of 6 This Is Henry's Law. It Says That at Equilibrium the Ratio of Dissolved NH3 to the Partial Pressure of NH3 Gas In
CHMY 361 HANDOUT#6 October 28, 2012 HOMEWORK #4 Key Was due Friday, Oct. 26 1. Using only data from Table A5, what is the boiling point of water deep in a mine that is so far below sea level that the atmospheric pressure is 1.17 atm? 0 ΔH vap = +44.02 kJ/mol H20(l) --> H2O(g) Q= PH2O /XH2O = K, at ⎛ P2 ⎞ ⎛ K 2 ⎞ ΔH vap ⎛ 1 1 ⎞ ln⎜ ⎟ = ln⎜ ⎟ − ⎜ − ⎟ equilibrium, i.e., the Vapor Pressure ⎝ P1 ⎠ ⎝ K1 ⎠ R ⎝ T2 T1 ⎠ for the pure liquid. ⎛1.17 ⎞ 44,020 ⎛ 1 1 ⎞ ln⎜ ⎟ = − ⎜ − ⎟ = 1 8.3145 ⎜ T 373 ⎟ ⎝ ⎠ ⎝ 2 ⎠ ⎡1.17⎤ − 8.3145ln 1 ⎢ 1 ⎥ 1 = ⎣ ⎦ + = .002651 T2 44,020 373 T2 = 377 2. From table A5, calculate the Henry’s Law constant (i.e., equilibrium constant) for dissolving of NH3(g) in water at 298 K and 340 K. It should have units of Matm-1;What would it be in atm per mole fraction, as in Table 5.1 at 298 K? o For NH3(g) ----> NH3(aq) ΔG = -26.5 - (-16.45) = -10.05 kJ/mol ΔG0 − [NH (aq)] K = e RT = 0.0173 = 3 This is Henry’s Law. It says that at equilibrium the ratio of dissolved P NH3 NH3 to the partial pressure of NH3 gas in contact with the liquid is a constant = 0.0173 (Henry’s Law Constant). This also says [NH3(aq)] =0.0173PNH3 or -1 PNH3 = 0.0173 [NH3(aq)] = 57.8 atm/M x [NH3(aq)] The latter form is like Table 5.1 except it has NH3 concentration in M instead of XNH3. -
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. -
Producing Nitrogen Via Pressure Swing Adsorption
Reactions and Separations Producing Nitrogen via Pressure Swing Adsorption Svetlana Ivanova Pressure swing adsorption (PSA) can be a Robert Lewis Air Products cost-effective method of onsite nitrogen generation for a wide range of purity and flow requirements. itrogen gas is a staple of the chemical industry. effective, and convenient for chemical processors. Multiple Because it is an inert gas, nitrogen is suitable for a nitrogen technologies and supply modes now exist to meet a Nwide range of applications covering various aspects range of specifications, including purity, usage pattern, por- of chemical manufacturing, processing, handling, and tability, footprint, and power consumption. Choosing among shipping. Due to its low reactivity, nitrogen is an excellent supply options can be a challenge. Onsite nitrogen genera- blanketing and purging gas that can be used to protect valu- tors, such as pressure swing adsorption (PSA) or membrane able products from harmful contaminants. It also enables the systems, can be more cost-effective than traditional cryo- safe storage and use of flammable compounds, and can help genic distillation or stored liquid nitrogen, particularly if an prevent combustible dust explosions. Nitrogen gas can be extremely high purity (e.g., 99.9999%) is not required. used to remove contaminants from process streams through methods such as stripping and sparging. Generating nitrogen gas Because of the widespread and growing use of nitrogen Industrial nitrogen gas can be produced by either in the chemical process industries (CPI), industrial gas com- cryogenic fractional distillation of liquefied air, or separa- panies have been continually improving methods of nitrogen tion of gaseous air using adsorption or permeation. -
Arenicola Marina During Low Tide
MARINE ECOLOGY PROGRESS SERIES Published June 15 Mar Ecol Prog Ser Sulfide stress and tolerance in the lugworm Arenicola marina during low tide Susanne Volkel, Kerstin Hauschild, Manfred K. Grieshaber Institut fiir Zoologie, Lehrstuhl fur Tierphysiologie, Heinrich-Heine-Universitat, Universitatsstr. 1, D-40225 Dusseldorf, Germany ABSTRACT: In the present study environmental sulfide concentrations in the vicinity of and within burrows of the lugworm Arenicola marina during tidal exposure are presented. Sulfide concentrations in the pore water of the sediment ranged from 0.4 to 252 pM. During 4 h of tidal exposure no significant changes of pore water sulfide concentrations were observed. Up to 32 pM sulfide were measured in the water of lugworm burrows. During 4 h of low tide the percentage of burrows containing sulfide increased from 20 to 50% in July and from 36 to 77% in October A significant increase of median sulfide concentrations from 0 to 14.5 pM was observed after 5 h of emersion. Sulfide and thiosulfate concentrations in the coelomic fluid and succinate, alanopine and strombine levels in the body wall musculature of freshly caught A. marina were measured. During 4 h of tidal exposure in July the percentage of lugworms containing sulfide and maximal sulfide concentrations increased from 17 % and 5.4 pM to 62% and 150 pM, respectively. A significant increase of median sulfide concentrations was observed after 2 and 3 h of emersion. In October, changes of sulfide concentrations were less pronounced. Median thiosulfate concentrations were 18 to 32 FM in July and 7 to 12 ~.IMin October No significant changes were observed during tidal exposure. -
Discontinuous Co2 Emission in a Small Insect, the Formicine Ant Campoxotus Vicixus
J. exp. Biol. 134, 363-376 (1988) 363 Printed in Great Britain © The Company of Biologists Limited I9SS DISCONTINUOUS CO2 EMISSION IN A SMALL INSECT, THE FORMICINE ANT CAMPOXOTUS VICIXUS BY JOHN R. B. LIGHTON Department of Biology, University of California at Los Angeles, Los Angeles, CA 90024, USA Accepted 21 July 1987 SUMMARY Standard rates of oxygen consumption (VO2) and CO2 production (VCO2) were measured by constant-volume respirometry in the formicine ant, Camponotus vicinus Mayr, at temperatures ranging from 10 to 40°C. Over this range, the Q10 with regard to VO2 was 1-79, and with regard to VCO2, 1-84. Multiple regression equations relating VO2 and VCO2 of inactive ants to mass (0016-0088g) and temperature were calculated. Periodic CO2 emissions ('bursts') were monitored with flow-through respirometry. Burst frequency increased exponentially with tempera- ture (QiO = 3-05), from 814h"' at 15°C to 81-4h~' at 35°C, and was not significantly correlated with body mass over the mass range (0041-0086g) investigated. Burst volume, which could be accurately measured in one ant, decreased with temperature (Qio = 0'61). thus yielding the observed Vcc>2 Q10 °f 1-84. INTRODUCTION The dynamics of external gas exchange in insects has important implications in the measurement of insect metabolic rates; it also provides insights into the functioning of a respiratory system that is complex, efficient, and unique to insects and a few other arthropods. One of the most striking aspects of external gas exchange in insects is its discontinuous, or intermittent, nature. Reports of periodic emissions, or bursts, of CO2 from large insects have been present in the literature for many years (Schneiderman, 1953; Punt, Parser & Kuchlein, 1957; Hamilton, 1964), and such reports have now become commonplace (see reviews by Miller, 1981; Kaars, 1981). -
O2k-Protocols SOP: O2k Quality Control 1
O2k-Protocols SOP: O2k Quality Control 1 Mitochondrial Physiology Network 06.03(19):1-19 (2021) Version 19: 2021-08-19 ©2001-2021 Oroboros Updates: http://wiki.oroboros.at/index.php/MiPNet06.03_POS-Calibration-SOP O2k Quality Control 1: Polarographic oxygen sensors and accuracy of calibration Erich Gnaiger Oroboros Instruments High-Resolution Respirometry Schoepfstrasse 18, 6020 Innsbruck, Austria Email: [email protected] www.oroboros.at Contents 1. Oxygen concentration and partial pressure ............................................................................ 2 2. Polarographic oxygen sensor ........................................................................................................ 2 2.1. Cathode ................................................................................................................................................... 3 2.2. Anode ...................................................................................................................................................... 3 2.3. Electrolyte ............................................................................................................................................. 3 2.4. Membrane ............................................................................................................................................. 4 3. Calibration and quality control (O2k-SOP) .............................................................................. 4 3.1. The O2 sensor test .............................................................................................................................. -
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. -
Dissolved Oxygen in the Blood
Chapter 1 – Dissolved Oxygen in the Blood Say we have a volume of blood, which we’ll represent as a beaker of fluid. Now let’s include oxygen in the gas above the blood (represented by the green circles). The oxygen exerts a certain amount of partial pressure, which is a measure of the concentration of oxygen in the gas (represented by the pink arrows). This pressure causes some of the oxygen to become dissolved in the blood. If we raise the concentration of oxygen in the gas, it will have a higher partial pressure, and consequently more oxygen will become dissolved in the blood. Keep in mind that what we are describing is a dynamic process, with oxygen coming in and out of the blood all the time, in order to maintain a certain concentration of dissolved oxygen. This is known as a) low partial pressure of oxygen b) high partial pressure of oxygen dynamic equilibrium. As you might expect, lowering the oxygen concentration in the gas would lower its partial pressure and a new equilibrium would be established with a lower dissolved oxygen concentration. In fact, the concentration of DISSOLVED oxygen in the blood (the CdO2) is directly proportional to the partial pressure of oxygen (the PO2) in the gas. This is known as Henry's Law. In this equation, the constant of proportionality is called the solubility coefficient of oxygen in blood (aO2). It is equal to 0.0031 mL / mmHg of oxygen / dL of blood. With these units, the dissolved oxygen concentration must be measured in mL / dL of blood, and the partial pressure of oxygen must be measured in mmHg.