Water: Structure and Properties
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Vibrational Spectra of Light and Heavy Water with Application to Neutron Cross Section Calculations J
CORE Metadata, citation and similar papers at core.ac.uk Provided by CONICET Digital Vibrational spectra of light and heavy water with application to neutron cross section calculations J. I. Marquez Damian, D. C. Malaspina, and J. R. Granada Citation: J. Chem. Phys. 139, 024504 (2013); doi: 10.1063/1.4812828 View online: http://dx.doi.org/10.1063/1.4812828 View Table of Contents: http://jcp.aip.org/resource/1/JCPSA6/v139/i2 Published by the AIP Publishing LLC. Additional information on J. Chem. Phys. Journal Homepage: http://jcp.aip.org/ Journal Information: http://jcp.aip.org/about/about_the_journal Top downloads: http://jcp.aip.org/features/most_downloaded Information for Authors: http://jcp.aip.org/authors Downloaded 11 Jul 2013 to 200.0.233.52. This article is copyrighted as indicated in the abstract. Reuse of AIP content is subject to the terms at: http://jcp.aip.org/about/rights_and_permissions THE JOURNAL OF CHEMICAL PHYSICS 139, 024504 (2013) Vibrational spectra of light and heavy water with application to neutron cross section calculations J. I. Marquez Damian,1,a) D. C. Malaspina,2 and J. R. Granada1,b) 1Neutron Physics Department and Instituto Balseiro, Centro Atómico Bariloche, CNEA, Argentina 2Department of Biomedical Engineering and Chemistry of Life Processes Institute, Northwestern University, 2145 Sheridan Road, Evanston, Illinois 60208, USA (Received 4 June 2013; accepted 19 June 2013; published online 11 July 2013) The design of nuclear reactors and neutron moderators require a good representation of the interac- tion of low energy (E < 1 eV) neutrons with hydrogen and deuterium containing materials. These models are based on the dynamics of the material, represented by its vibrational spectrum. -
The Incredible Lightness of Water Vapor
1 The Incredible Lightness of Water Vapor ∗ 2 Da Yang and Seth Seidel 3 University of California, Davis 4 Lawrence Berkeley National Laboratory, Berkeley ∗ 5 Corresponding author address: Da Yang, 253 Hoagland Hall, Davis, CA 95616. 6 E-mail: [email protected] Generated using v4.3.2 of the AMS LATEX template 1 ABSTRACT 7 The molar mass of water vapor is significantly less than that of dry air. This 8 makes a moist parcel lighter than a dry parcel of the same temperature and 9 pressure. This effect is referred to as the vapor buoyancy effect and has of- 10 ten been overlooked in climate studies. We propose that this effect increases 11 Earth’s outgoing longwave radiation (OLR) and stabilizes Earth’s climate. 12 We illustrate this mechanism in an idealized tropical atmosphere, where there 13 is no horizontal buoyancy gradient in the free troposphere. To maintain the 14 uniform buoyancy distribution, temperature increases toward dry atmosphere 15 columns to compensate reduction of vapor buoyancy. The temperature differ- 16 ence between moist and dry columns would increase with climate warming 17 due to increasing atmospheric water vapor, leading to enhanced OLR and 18 thereby stabilizing Earth’s climate. We estimate that this feedback strength 2 19 is about O(0.2 W/m /K), which compares with cloud feedbacks and surface 20 albedo feedbacks in current climate. 2 21 1. Introduction 22 How fast would Earth’s climate respond to increasing CO2 (Manabe and Wetherald 1975; Flato 23 et al. 2013; Collins et al. 2013)? Why is tropical climate more stable than extratropical climate 24 (Holland and Bitz 2003; Polyakov et al. -
Unique Properties of Water!
Name: _______ANSWER KEY_______________ Class: _____ Date: _______________ Unique Properties of Water! Word Bank: Adhesion Evaporation Polar Surface tension Cohesion Freezing Positive Universal solvent Condensation Melting Sublimation Dissolve Negative 1. The electrons are not shared equally between the hydrogen and oxygen atoms of water creating a Polar molecule. 2. The polarity of water allows it to dissolve most substances. Because of this it is referred to as the universal solvent 3. Water molecules stick to other water molecules. This property is called cohesion. 4. Hydrogen bonds form between adjacent water molecules because the positive charged hydrogen end of one water molecule attracts the negative charged oxygen end of another water molecule. 5. Water molecules stick to other materials due to its polar nature. This property is called adhesion. 6. Hydrogen bonds hold water molecules closely together which causes water to have high surface tension. This is why water tends to clump together to form drops rather than spread out into a thin film. 7. Condensation is when water changes from a gas to a liquid. 8. Sublimation is when water changes from a solid directly to a gas. 9. Freezing is when water changes from a liquid to a solid. 10. Melting is when water changes from a solid to a liquid. 11. Evaporation is when water changes from a liquid to a gas. 12. Why does ice float? Water expands as it freezes, so it is LESS DENSE AS A SOLID. 13. What property refers to water molecules resembling magnets? How are these alike? Polar bonds create positive and negative ends of the molecule. -
Computational Investigation of Surface Freezing in a Molecular Model Of
Computational investigation of surface freezing in a molecular model of water Amir Haji-Akbari ( )a,1 and Pablo G. Debenedettia,2 aDepartment of Chemical and Biological Engineering, Princeton University, Princeton, NJ 08544 Contributed by Pablo G. Debenedetti, February 17, 2017 (sent for review December 21, 2016; reviewed by Christoph Dellago and Angelos Michaelides) Water freezes in a wide variety of low-temperature environ- is therefore one of the major open challenges of atmospheric ments, from meteors and atmospheric clouds to soil and bio- sciences. logical cells. In nature, ice usually nucleates at or near inter- One major difficulty in constructing such predictive frame- faces, because homogenous nucleation in the bulk can only be works is the inability to determine the proper scaling of observed at deep supercoolings. Although the effect of proximal volumetric nucleation rates with the size of microdroplets and surfaces on freezing has been extensively studied, major gaps in nanodroplets that constitute clouds. This is practically impor- understanding remain regarding freezing near vapor–liquid inter- tant because atmospheric clouds are composed of droplets of faces, with earlier experimental studies being mostly inconclu- different sizes. This scaling is determined by whether freezing is sive. The question of how a vapor–liquid interface affects freez- enhanced or suppressed near vapor–liquid interfaces. If freezing ing in its vicinity is therefore still a major open question in ice is suppressed at a free interface, the effective volumetric nucle- physics. Here, we address this question computationally by using ation rate will be independent of r, the droplet radius, and bulk the forward-flux sampling algorithm to compute the nucleation freezing will be dominant at all sizes. -
Case Study: Water and Ice
Case Study: Water and Ice Timothy A. Isgro, Marcos Sotomayor, and Eduardo Cruz-Chu 1 The Universal Solvent Water is essential for sustaining life on Earth. Almost 75% of the Earth’s surface is covered by it. It composes roughly 70% of the human body by mass [1]. It is the medium associated with nearly all microscopic life pro- cesses. Much of the reason that water can sustain life is due to its unique properties. Among the most essential and extreme properties of water is its capabil- ity to absorb large amounts of heat. The heat capacity of water, which is the highest for compounds of its type in the liquid state, measures the amount of heat which needs to be added to water to change its temperature by a given amount. Water, thus, is able to effectively maintain its temperature even 1 when disturbed by great amounts of heat. This property serves to main- tain ocean temperatures, as well as the atmospheric temperature around the oceans. For example, when the sun rises in the morning and a large amount of heat strikes the surface of the Earth, the vast majority of it is absorbed by the ocean. The ocean water, however, does not exhibit a drastic increase in temperature that could make it inhospitable to life. In constrast, when the sun sets in the evening and that heat is taken away, the oceans do not become too cold to harbor life. Water also has high latent heats of vapor- ization and melting, which measure the amount of heat needed to change a certain amount of liquid water to vapor and ice to liquid, respectively. -
Hydrated Sulfate Clusters SO4^2
Article Cite This: J. Phys. Chem. B 2019, 123, 4065−4069 pubs.acs.org/JPCB 2− n − Hydrated Sulfate Clusters SO4 (H2O)n ( =1 40): Charge Distribution Through Solvation Shells and Stabilization Maksim Kulichenko,† Nikita Fedik,† Konstantin V. Bozhenko,‡,§ and Alexander I. Boldyrev*,† † Department of Chemistry and Biochemistry, Utah State University, 0300 Old Main Hill, Logan, Utah 84322-0300, United States ‡ Department of Physical and Colloid Chemistry, Peoples’ Friendship University of Russia (RUDN University), 6 Miklukho-Maklaya St, Moscow 117198, Russian Federation § Institute of Problems of Chemical Physics, Russian Academy of Sciences, Chernogolovka 142432, Moscow Region, Russian Federation *S Supporting Information 2− ABSTRACT: Investigations of inorganic anion SO4 interactions with water are crucial 2− for understanding the chemistry of its aqueous solutions. It is known that the isolated SO4 dianion is unstable, and three H2O molecules are required for its stabilization. In the 2− current work, we report our computational study of hydrated sulfate clusters SO4 (H2O)n (n =1−40) in order to understand the nature of stabilization of this important anion by fi 2− water molecules. We showed that the most signi cant charge transfer from dianion SO4 ≤ 2− to H2O takes place at a number of H2O molecules n 7. The SO4 directly donates its charge only to the first solvation shell and surprisingly, a small amount of electron density of 0.15|e| is enough to be transferred in order to stabilize the dianion. Upon further addition of ff ≤ H2O molecules, we found that the cage e ect played an essential role at n 12, where the fi 2− | | rst solvation shell closes. -
Periodic Table of the Elements Notes
Periodic Table of the Elements Notes Arrangement of the known elements based on atomic number and chemical and physical properties. Divided into three basic categories: Metals (left side of the table) Nonmetals (right side of the table) Metalloids (touching the zig zag line) Basic Organization by: Atomic structure Atomic number Chemical and Physical Properties Uses of the Periodic Table Useful in predicting: chemical behavior of the elements trends properties of the elements Atomic Structure Review: Atoms are made of protons, electrons, and neutrons. Elements are atoms of only one type. Elements are identified by the atomic number (# of protons in nucleus). Energy Levels Review: Electrons are arranged in a region around the nucleus called an electron cloud. Energy levels are located within the cloud. At least 1 energy level and as many as 7 energy levels exist in atoms Energy Levels & Valence Electrons Energy levels hold a specific amount of electrons: 1st level = up to 2 2nd level = up to 8 3rd level = up to 8 (first 18 elements only) The electrons in the outermost level are called valence electrons. Determine reactivity - how elements will react with others to form compounds Outermost level does not usually fill completely with electrons Using the Table to Identify Valence Electrons Elements are grouped into vertical columns because they have similar properties. These are called groups or families. Groups are numbered 1-18. Group numbers can help you determine the number of valence electrons: Group 1 has 1 valence electron. Group 2 has 2 valence electrons. Groups 3–12 are transition metals and have 1 or 2 valence electrons. -
Using Xenon-133 and a Scintillation Camera to Evaluate Pulmonary Function
USING XENON-133 AND A SCINTILLATION CAMERA TO EVALUATE PULMONARY FUNCTION Merle K. Loken and Hugh D. Westgate University of Minnesota Hospitals, Minneapolis, Minnesota During the past several years considerable atten monary-function laboratory (6—9). Thus because of tion has been given to evaluating pulmonary disease their universal availability, the noble gases are being using radioisotopic techniques. The majority of the used more extensively, and, of these gases, ‘33Xehas radioactive preparations used for these studies can the best physical characteristics (5, 10—13). be divided into two general categories : colloidal In this paper we report our preliminary experience aggregates of albumin and radioactive gases. Macro using an Anger scintillation camera to record pul aggregates labeled with 1311or 99@'Tchave been used monary uptake and clearance of ‘33Xein patients extensivelyfor determining regional pulmonary per referred to our service for pulmonary-function evalu fusion and, as such, are useful for evaluating patients ation. The radioactive xenon was administered either with suspected pulmonary emboli (1—5). The dis by inhalation or intravenous injection. tribution of these macroaggregates in the lung is usually determined by conventional rectilinear scan MATERIALS AND METHODS ning although the scintillation camera has also been We obtain 133Xe in 1-curie ampules at approxi used effectively (4,5). mately biweekly intervals from Oak Ridge National To obtain information on ventilation and diffusion Laboratory. The gas is contained in a volume of one of the radioactive gases—oxygen, carbon dioxide, about 5 cc at a pressure of about 10 mmHg (Fig. 1). krypton or xenon—must be used. -
Use of Models for Water Resources Management, Planning, and Policy
Use of Models for Water Resources Management, Planning, and Policy August 1982 NTIS order #PB83-103655 Library of Congress Catalog Card Number 82-600556 For sale by the Superintendent of Documents, U.S. Government Printing Office, Washington, D.C. 20402 Foreword. The Nation'. water resource policies, affect many problem. in the ~$tates today-food production, energy, regional economic development, enviro:,"qual ity, and even our international balance of trade. As the country grows, and ~. ,. _"'I water supplies diminish, it becomes increasingly important to manage existing sup~th the greatest possible efficiency. In re~ent years, successfull11anagement andplanniag of water resources has increasingly been based on the results ,of mathematical~~.: ~~; Leaving aside the mystique of computers and ~pl~_ mathe~atics, mltematical models are simply tools used for understaIJ.ding w~~f~8odIc. and ",at~ re_e man agement activities. This part of water resource manaFm.~~ii thou~ not as apparent as dams and reservoirs or pipes and sewers, is a vital cOlripcmetif inIDetltiJ;lg tlriW'l ation' s water resource needs. Sophisticated analysis, through the ute of models, can improve our understanding of water resources and wat~r resource activities, and helpprev~ wasting both water and money. - This assessment of water resource models is therefore 'DOt an assessment Of_'$tical equations or computers, but of the Nation's ability t~ Use models to more e.·' tly and effectively analyze and solve our water resource prob~,m.. :, I •. ~rn-.' .. :", ',.,e ~ a:'~e, ssment :',.,' •.,:. rs not only the usefulness of the technology-the models-but _ability of Feder -,.,.' State water resource agencies to apply these analytic too1a ~~ly .... -
Ice–Water Interfacial Free Energy for the TIP4P, TIP4P/2005, TIP4P/Ice
Article pubs.acs.org/JPCC Ice−Water Interfacial Free Energy for the TIP4P, TIP4P/2005, TIP4P/ Ice, and mW Models As Obtained from the Mold Integration Technique Jorge R. Espinosa, Carlos Vega, and Eduardo Sanz* Departamento de Química Física, Facultad de Ciencias Químicas, Universidad Complutense de Madrid, 28040 Madrid, Spain ABSTRACT: The freezing of water is greatly influenced by the ice−water interfacial free energy. Yet, no consistent experimental measures of this thermodynamic parameter can be found. In this work we provide estimates for the ice Ih− water interfacial free energy at the normal melting temperature for different crystal planes (basal, primary prismatic, and secondary prismatic) using some widely used water models: TIP4P, TIP4P/2005, TIP4P/Ice, and mW. To compute the interfacial free energy, we use the mold integration method. It consists in calculating the work needed to induce the formation of a crystal slab in the fluid at coexistence conditions with the aid of a mold of potential energy wells whose structure is that of the crystal plane under study. The basal plane has the lowest interfacial free energy in all models of the TIP4P family. For the mW model we could not resolve differences in interfacial free energy between different orientations. The interfacial free energies averaged over all crystal orientations we obtain are 27.2(8), 28.9(8), 29.8(8), and 34.9(8) mJ/m2 for the TIP4P, TIP4P/2005, TIP4P/Ice, and mW models, respectively. The averaged interfacial free energy increases with both the melting temperature and melting enthalpy of the model. Moreover, we compute the interfacial free energy for several crystal orientation of ice Ic using the TIP4P/Ice model and obtain within the accuracy of our calculations the same orientationally averaged interfacial free energy as that of ice Ih. -
The Oxygen and Carbon Dioxide Compensation Points of C3
Proc. Natl. Acad. Sci. USA Vol. 92, pp. 11230-11233, November 1995 Plant Biology The oxygen and carbon dioxide compensation points of C3 plants: Possible role in regulating atmospheric oxygen (photosynthetic carbon/02 inhibition/photorespiration/Nicotiana tobacum/Spinacea oleracea) N. E. TOLBERT*, C. BENKERt, AND E. BECKt *Department of Biochemistry, Michigan State University, East Lansing, MI 48824; and tLehrstuhl Fur Pflanzenphysiologie, Universitat Bayreuth, 95440 Bayreuth, Germany Contributed by N. E. Tolbert, August 15, 1995 ABSTRACT The 02 and CO2 compensation points (02 F bisphosphate to sustain the C2 cycle. Refixation of CO2 and C02 F) of plants in a closed system depend on the ratio of generates the same amount of 02 as taken up during the C2 CO2 and 02 concentrations in air and in the chloroplast and cycle. There is no net CO2 and 02 gas exchange during the specificities of ribulose bisphosphate carboxylase/oxyge- photorespiration (11) unless the complete C2 cycle is blocked nase (Rubisco). The photosynthetic 02 F is defined as the or metabolically interrupted by accumulation or removal of atmospheric 02 level, with a given CO2 level and temperature, products such as glycine or serine. Photorespiration dissipates at which net 02 exchange is zero. In experiments with C3 excess photosynthetic capacity (ATP and NADPH) without plants, the 02 F with 220 ppm CO2 is 23% 02; 02 F increases CO2 reduction or net 02 change. Photosynthetic carbon me- to 27% with 350 ppm CO2 and to 35% 02 with 700 ppm CO2. tabolism is a competition between CO2 and 02 for the dual At 02 levels below the 02 F, C02 uptake and reduction are activities of Rubisco, based on the ratio of CO2 and 02 accompanied by net 02 evolution. -
Signature Properties of Water: Their Molecular Electronic Origins
Signature properties of water: Their molecular electronic origins Vlad P. Sokhana,1, Andrew P. Jonesb, Flaviu S. Cipciganb, Jason Craina,b, and Glenn J. Martynab,c aNational Physical Laboratory, Teddington, Middlesex TW11 0LW, United Kingdom; bSchool of Physics and Astronomy, The University of Edinburgh, Edinburgh EH9 3JZ, United Kingdom; and cIBM Thomas J. Watson Research Center, Yorktown Heights, NY 10598 Edited by Paul Madden, University of Oxford, Oxford, United Kingdom, and accepted by the Editorial Board March 31, 2015 (received for review October 1, 2014) Water challenges our fundamental understanding of emergent combination of multiscale descriptions and statistical sampling have materials properties from a molecular perspective. It exhibits a led to insights into physical phenomena across biology, chemistry, uniquely rich phenomenology including dramatic variations in physics, materials science, and engineering (14). Significant progress behavior over the wide temperature range of the liquid into water’s now requires novel predictive models with reduced empirical input crystalline phases and amorphous states. We show that many-body that are rich enough to embody the essential physics of emergent responses arising from water’s electronic structure are essential mech- systems and yet simple enough to retain intuitive features (14). anisms harnessed by the molecule to encode for the distinguishing Typically, atomistic models of materials are derived from a features of its condensed states. We treat the complete set of these common strategy. Interactions are described via a fixed functional many-body responses nonperturbatively within a coarse-grained elec- form with long-range terms taken from low orders of perturbation tronic structure derived exclusively from single-molecule properties.