Lecture 1. Chemical Thermodynamics and Bioenergetics. Fundamentals of Thermochemistry

Total Page:16

File Type:pdf, Size:1020Kb

Lecture 1. Chemical Thermodynamics and Bioenergetics. Fundamentals of Thermochemistry Lecture 1. Chemical thermodynamics and bioenergetics. Fundamentals of thermochemistry. Lecture plan . 1. Types of thermodynamic systems. 2. Thermodynamics functions and parameters of system. 3. The first law of thermodynamics. Internal energy. Enthalpy. 4. Heat of isobaric and isochoric process. Standard heats of the substance formation and combustion. 5. Thermochemistry. Hess law. Thermochemical transformation. 6. Thermochemical calculation and their use for energetic characteristics of biochemical process. 7. Second law of thermodynamic. Entropy. Subject of thermodynamics All chemical reactions are accompanied by transformation of chemical energy to other forms of energy - thermal, electrical, mechanical, etc. Thermodynamics is the branch of physical science that studies all forms of energy and their mutual transformations; therefore it is sometimes called energetics. Bioenergetics is a field of thermodynamics that deals with biosystems. Classical thermodynamics is based on propositions which are confirmed by experiment and does not use knowledge about the molecular structure of substances.The energy of reactions is studied by the branch of thermodynamics which is called thermochemistry or chemical thermodynamics. In thermochemistry two types of chemical reactions are distinguished: exothermic (are accompanied by heat release) and endothermic (are accompanied by heat absorption). There are reactions (not so numerous), which are not accompanied by heat exchange. Chemical reactions can occur at a constant pressure (for example in an open flask) - these are isobaric processes, at a constant volume (in a closed flask or an autoclave) - these are isochoric processes, or at a constant temperature - these are isothermal processes (the names are derived from the Greek words isos - identical, baros - pressure, chorus - space, thermos - heat). Thermodynamics deals with the study of properties of various thermodynamic systems and processes occurring in them. A thermodynamic system is anybody or totality of bodies being in interaction with each other, which may be separated (conditionally or practically) from the surroundings for studying by thermodynamic methods. Different types of thermodynamic systems are known: 1. Homogeneous system – it is uniform in all its parts. For example an aqueous solution of ethanol, or a mixture of gases. 2. Heterogeneous system – it is not uniform and consists of two or more phases, e.g. water-benzene. The term phase means a part of a system with a characteristic chemical composition and macroscopic properties. Phases are separated from each other by physical surfaces, and at transition of these surfaces the properties sharply vary. 3. Physical system – it is a system, in which processes are accompanied by energy change, but the chemical nature of a substance is invariable. For example, changing of the modular condition of a substance at its melting (or crystallization) temperature; condensation of liquid vapor at its boiling temperature (water boils at 373 K). 4. Chemical system – it is a system, in which both phenomena take place: change of the energy content, change of the chemical nature of the system components. For example, interaction of zinc with sulfuric acid and other chemical reactions. 5. Open system – it is a system that may exchange both energy and substance with the surroundings. For example, a bio system - a living organism. 6. Closed system – it is a system that may exchange only energy with other systems, but not substance. For example, an electric range. 7. Isolated system – it is a system, which doesn’t exchange energy or substance with the surroundings. It is very difficult to create an absolutely isolated system. Reactors with good thermoisolation may be reckoned among these systems. At each moment of time the state of a system is characterized by physical properties that do not depend upon the previous history of the system state, for ex- ample: temperature T, pressure P, volume V, energy E, mass m, internal energy U, enthalpy H, entropy S, Gibbs energy G, Helmholtz energy F, etc. Thermodynamics is of great importance for medicine since it helps: • To generate scientific representation of the energy balance of a living organism. • To establish connection between the caloric content of food and energy expenses of the organism. • To develop objective criteria for determining the possibility of realization of separate processes in the human body without carrying out tests. There are some formulations of the first law of thermodynamics. Such concepts as «heat and work», on the one hand, and «internal energy and enthalpy», on the other hand, underlie it. Heat and work are different forms of energy transmission. In thermodynamics heat and work are algebraic values that may be positive and negative. Work is measured in joules. Heat is also expressed in joules in the SI, the unit calorie is also applied. The connection between a joule and a calorie is: 1.00 cal = 4.184 J. When heat is absorbed by a system from the surroundings, it has a positive value, if heat is released by a system into the surroundings, it is taken as negative. Using the concepts heat and work the first law of thermodynamics may be for- mulated as: Energy can neither be created nor destroyed, but only can be converted from one form into another (including heat and work), without changing quantitatively. In fact it is the law of conservation of energy, which was formulated by M. Lo- monosov as long ago as 1748. Other formulation of the first law is: It is impossible to develop a perpetuum mobile of the first kind (i.e. a machine producing work without expenditure of energy). It is possible to formulate the first law of thermodynamics on the basis of other reasons, introducing the concepts internal energy and enthalpy. Internal energy may be considered a sum of different types of energy from atoms, ions and molecules (energy of molecular motion, of intermolecular interac- tion, etc.). According to the law of energy conservation, the heat that is absorbed by a sys- tem is spent to change its internal energy and to produce work: Q = Δ U + A (1) For chemical processes the work against external forces is work against exter- nal pressure and it is equal: A = p(V2 - V1) = p ΔV (2) For an isochoric process (V— const): A = 0 and Qv = U2 - U1 = Δ U (3) It means that the system doesn’t produce external work that is associated with a volume change, and all heat that is released or absorbed is spent on changing the internal energy of a system. For an isobaric process (p — const), excluding internal energy changes, certain work (A) is carried out as a result of volume change in a system, which is equal to the product between pressure (p) and change of the system’s volume (V ): A= p ΔV (4) Qp = Δ U + p ΔV (5) Qp = (U2 - U1) + p(V2 - Vl) (6) or Qp = (U2 + pV2) - (U1 + pV1) (7) Assuming that U + pV = H (8) the heat of the processes taking place at constant temperature and pressure (the most widespread chemical processes) may be represented as: Qp = H2 - H1 = Δ H, (9) where H is the enthalpy of a system. The positive value of enthalpy change (ΔH > 0) corresponds to enthalpy in- crease or to heat absorption by a system (an endothermic process). The negative value of enthalpy change (ΔH< 0) corresponds to enthalpy decrease or to heat release by a system (an exothermic process). So in an isochoricprocess the heat of a reaction is equal to external energy change ΔU: QV = ΔU (10) and in an isobaric process heat is equal to a change of system’s enthalpy: Qp = ΔH (11) It must be noted that Qp > Qv on pΔV value which is the work of expansion. As well as the internal energy of a system U, enthalpy H is also a state function of a system. U and H may be considered as a measure of heat transportation at certain conditions: U at V = const, H at p = const. There is a relationship between internal energy and enthalpy of a system: ΔH = ΔU+pΔV From the equation (5) it follows: ΔU = Qp - pΔV (12) The equation (12) may be interpreted as a mathematical expression of the first law of thermodynamics. An increase of the internal energy of a system is equal to the heat, which is received by the system from the outside, except for the work produced by the system against external forces. All thermochemical calculations are based on Lavoisier and Laplace’s law and Hess’s law. The law of Lavoisier and Laplace (1780): The heat of decomposition of a chemical compound into simple substances is numerically equal and opposite in sign to the heat of formation of this compound from simple substances. Hess’s law (1840): The heat of a reaction is independent of the way, in which this reaction occurs, and only depends upon the initial and final states of a system. The consequences of Hess’s law are of great importance for thermochemical calculations. Consequences of Hess’s law: 1. Enthalpy of a forward reaction is equal and opposite in sign to enthalpy of a reverse reaction. Δ =Δ 2. Reaction enthalpy is equal to the sum of enthalpies of reaction products formation minus the sum of enthalpies of reactant formation. 3. Enthalpy of a combustion reaction is equal to the sum of enthalpies of reactant combustion (Δ ) minus the sum of enthalpies of product combustion. ΔHc = - For a reaction nA + mB = qC + pD Δ Hf = [qΔH°f C + pΔH°f D] - [nΔH°f A + mΔH°f B]; Δ Hc = [nΔHc A + mΔHc B] - [qΔHc C + pΔHc D]. The data on the thermal effects of reactions are used for: calculation of the thermal balances of technological processes, determination of the energy of inter- atomic and intermolecular bonds, ascertainment of the structure and reactionary ability, establishment of the direction of chemical processes, description of the energy balance of an organism.
Recommended publications
  • Chemistry Grade Level 10 Units 1-15
    COPPELL ISD SUBJECT YEAR AT A GLANCE ​ ​ ​ ​​ ​ ​​ ​ ​ ​ ​ ​ ​ GRADE HEMISTRY UNITS C LEVEL 1-15 10 Program Transfer Goals ​ ​ ​ ​ ● Ask questions, recognize and define problems, and propose solutions. ​ ​​ ​ ​ ​ ​ ​ ​ ​ ​ ​ ​ ​ ​ ​ ​ ​ ​ ● Safely and ethically collect, analyze, and evaluate appropriate data. ​ ​ ​ ​ ​ ​ ​ ​ ​ ​ ​ ​ ​ ​ ​ ​ ● Utilize, create, and analyze models to understand the world. ​ ​ ​ ​ ​ ​ ​ ​ ​ ​ ​ ​ ​ ​ ​ ​ ● Make valid claims and informed decisions based on scientific evidence. ​ ​ ​ ​ ​ ​ ​ ​ ​ ​ ​ ​ ​ ​ ​ ​ ​ ​ ● Effectively communicate scientific reasoning to a target audience. ​ ​ ​ ​ ​ ​ ​ ​ ​ ​ ​ ​ ​ ​ PACING 1st 9 Weeks 2nd 9 Weeks 3rd 9 Weeks 4th 9 Weeks ​ ​ ​ ​ ​ ​ ​ ​ ​ ​ ​ ​ ​ ​ ​ ​ Unit 1 Unit 2 Unit 3 Unit 4 Unit 5 Unit 6 Unit Unit Unit Unit Unit Unit Unit Unit Unit ​ ​ ​ ​ ​ ​ ​ ​ ​ ​ ​ ​ 7 8 9 10 11 12 13 14 15 1.5 wks 2 wks 1.5 wks 2 wks 3 wks 5.5 wks ​ ​ ​ ​ ​ ​ ​ ​ ​ ​ ​ ​ 1.5 2 2.5 2 wks 2 2 2 wks 1.5 1.5 ​ ​ ​ ​ wks wks wks wks wks wks wks Assurances for a Guaranteed and Viable Curriculum ​ ​ ​ ​ ​ ​ ​ ​ ​ ​ ​ ​ Adherence to this scope and sequence affords every member of the learning community clarity on the knowledge and skills ​ ​ ​ ​ ​ ​ ​ ​ ​ ​ ​ ​ ​ ​ ​ ​ ​ ​ ​ ​ ​ ​ ​ ​ ​ ​ ​ ​ ​ ​ ​ ​ ​ ​ ​ ​ on which each learner should demonstrate proficiency. In order to deliver a guaranteed and viable curriculum, our team ​ ​ ​ ​ ​ ​ ​ ​ ​ ​ ​ ​ ​ ​ ​ ​ ​ ​ ​ ​ ​ ​ ​ ​ ​ ​ ​ ​ ​ ​ ​ ​ ​ ​ commits to and ensures the following understandings: ​ ​ ​ ​ ​ ​ ​ ​ ​ ​ ​ ​ Shared Accountability: Responding
    [Show full text]
  • Chemistry Courses 2005-2006
    Chemistry Courses 2005-2006 Autumn 2005 Chem 11101 General Chemistry I, Variant A Lee Chem 11102 General Chemistry I, Variant B Norris Chem 12200 Honors General Chemistry I Levy Chem 22000 Organic Chemistry I Yu Chem 22300 Intermediate Organic Chemistry Mrksich Chem 26100 Quantum Mechanics Mazziotti Chem 30100 Advanced Inorganic Chemistry Hopkins Chem 30900 Bioinorganic Chemistry He Chem 32100 Physical Organic Chemistry I Ismagilov Chem 32200 Organic Synthesis and Structure Rawal Chem 32600 Protein Fundamentals Piccirilli Chem 36100 Wave Mechanics & Spectroscopy Butler Chem 36400 Chemical Thermodynamics Dinner Winter 2006 Chem 11201 General Chemistry II, Variant A Scherer Chem 11202 General Chemistry II, Variant B Butler Chem 12300 Honors General Chemistry II Dinner Chem 20100 Inorganic Chemistry I Hillhouse Chem 22100 Organic Chemistry II Rawal Chem 23100 Honors Organic Chemistry II Kozmin Chem 26200 Thermodynamics Norris Chem 26700 Experimental Physical Chemistry Levy Chem 30200 Synthesis & Physical Methods in Inorganic Chemistry Jordan Chem 30400 Organometallic Chemistry Bosnich Chem 32300 Tactics of Organic Synthesis Yamamoto Chem 32400 Physical Organic Chemistry II Mrksich Chem 36200 Quantum Mechanics Freed Chem 36300 Statistical Mechanics Mazziotti Chem 38700 Biophysical Chemistry Lee Spring 2006 Chem 11301 General Chemistry III, Variant A Kozmin Chem 11302 General Chemistry III, Variant B Guyot-Sionnest Chem 20200 Inorganic Chemistry II Jordan Chem 22200 Organic Chemistry III Kent Chem 23200 Honors Organic Chemistry III Yamamoto Chem 22700 Advanced Organic / Inorganic Laboratory (8 students) He Chem 26300 Chemical Kinetics and Dynamics Sibner Chem 26800 Computational Chemistry & Biology Freed Chem 30600 Chemistry of the Elements Hillhouse Chem 31100 Supramolecular Chemistry Bosnich Chem 32500 Bioorganic Chemistry Piccirilli Chem 32900 Polymer Chemistry Yu Chem 33000 Complex Systems Ismagilov Chem 36500 Chemical Dynamics Scherer Chem 36800 Advanced Computational Chemistry & Biology Freed .
    [Show full text]
  • Entropy and Life
    Entropy and life Research concerning the relationship between the thermodynamics textbook, states, after speaking about thermodynamic quantity entropy and the evolution of the laws of the physical world, that “there are none that life began around the turn of the 20th century. In 1910, are established on a firmer basis than the two general American historian Henry Adams printed and distributed propositions of Joule and Carnot; which constitute the to university libraries and history professors the small vol- fundamental laws of our subject.” McCulloch then goes ume A Letter to American Teachers of History proposing on to show that these two laws may be combined in a sin- a theory of history based on the second law of thermo- gle expression as follows: dynamics and on the principle of entropy.[1][2] The 1944 book What is Life? by Nobel-laureate physicist Erwin Schrödinger stimulated research in the field. In his book, Z dQ Schrödinger originally stated that life feeds on negative S = entropy, or negentropy as it is sometimes called, but in a τ later edition corrected himself in response to complaints and stated the true source is free energy. More recent where work has restricted the discussion to Gibbs free energy because biological processes on Earth normally occur at S = entropy a constant temperature and pressure, such as in the atmo- dQ = a differential amount of heat sphere or at the bottom of an ocean, but not across both passed into a thermodynamic sys- over short periods of time for individual organisms. tem τ = absolute temperature 1 Origin McCulloch then declares that the applications of these two laws, i.e.
    [Show full text]
  • Thermochemistry • Spontaneous Process • System • Entropy • Second Law of Thermodynamics • Free Energy • Kinetic Molecular Theory
    Honors Chemistry 3st Grading Period Power Objectives: Academic Vocabulary: • Articulate elemental and molecular properties utilizing physical • Energy • Surroundings structures of the atom and the periodic table. (P.O. #1) • Law of conservation of • Universe energy • Enthalpy • Characterize interactions between matter and energy. • Chemical potential energy • Enthalpy (heat) of reaction (P.O. #2) • Heat • Thermochemical equation • Calorie • Vaporization • Demonstrate how mathematics describes concepts in • Joule • Fusion chemistry. (P.O. #3) • Specific heat • Hess’s law • Design and conduct chemistry investigations. (P.O. #4) • Calorimeter • Standard enthalpy of formation • Thermochemistry • Spontaneous process • System • Entropy • Second law of thermodynamics • Free energy • Kinetic Molecular Theory Thermochemistry Enduring Understandings: Essential Questions: • Temperature is not a form of energy. • What is energy? • Energy is a conserved quantity, which means it cannot be • How do potential and kinetic energy differ? • How can chemical potential energy be related to the heat lost or gained in chemical created or destroyed. reactions? • All of the energy present in the universe was derived from the • How is the amount of heat absorbed or released by a substance calculated as its Big Bang. temperature changes? • Different forms of energy have to do with the motion of atoms • How is a calorimeter used to measure energy that is absorbed or released? • What do enthalpy and enthalpy change mean in terms of chemical reactions and and molecules within a substance. processes? • All chemical reactions require the use of energy in some way, • How are thermochemical equations for chemical reactions and other processes which is why one’s body has a steady temperature and mixing written? • How is energy lost or gained during changes of state? chemicals can cause heat to be released or require heat to react • How is the heat that is absorbed or released in a chemical reaction calculated? (cold).
    [Show full text]
  • Thermochemistry Worksheet #1
    Name: Thermochemistry Worksheet #1 1. The reaction of magnesium with sulfuric acid was carried out in a calorimeter. This reaction caused the temperature of 27.0 grams of liquid water, within the calorimeter, to raise from 25.0C to 76.0C. Calculate the energy associated with this reaction. 2. The reaction of zinc with nitric acid was carried out in a calorimeter. This reaction caused the temperature of 72.0 grams of liquid water, within the calorimeter, to raise from 25.0C to 100.C. Calculate the energy associated with this reaction. 3. A 4.00 gram sample of solid gold was heated from 274K to 314K. How much energy was involved? 4. The reaction of magnesium with hydrochloric acid carried out in a calorimeter caused the temperature of water to change from 25.0C to 36.0C. In this reaction 3760J of energy was released. What mass of water was present? 5. The reaction of magnesium oxide with hydrochloric acid carried out in a calorimeter caused the temperature of water to change from 25.0C to 46.0C. In this reaction 4860J of energy was released. What mass of water was present? 6. A piece of solid gold was heated from 274K to 314K. 35.7J of energy was needed to raise the temperature. What mass of gold was present? Use Hf values (table found in notes) to solve the following problems. 7. Determine the H for each of the following reactions. Classify each reaction as either exothermic or endothermic. a. C3H8(g) + 5O2(g) 3CO2(g) + 4H2O(g) H = ? kJ/mol b.
    [Show full text]
  • Experiment 8 Thermochemistry This Week In
    Experiment 8 Thermochemistry CH 204 Fall 2006 Dr. Brian Anderson What is Thermochemistry? The study of heat in chemical reactions. Forming chemical bonds releases energy. Breaking chemical bonds requires energy. How much energy? Depends on the bond. Add up all the energies to get the heat of reaction, ∆Hrxn . This week in lab We will measure the amount of heat given off by 50 ml of hot water, by some chunks of hot metal, and by two chemical reactions + 2+ Mg + 2H → Mg + H2 + heat + 2+ MgO + 2H → Mg + H2 O + heat We’ll do all these reactions in a coffee cup calorimeter. 1 The basic operation of calorimetry - Start with a known volume of a solution in the calorimeter. - Drop in something hot, or start a reaction that generates heat. - Close the calorimeter and measure the increase in temperature as heat is generated. - Keep measuring the temperature until it finally levels out. Part One: Add hot water to cold 50 mL of cold water (5ºC). Add 50 mL of hot water (75ºC). Final temp should be (75 + 5) ÷ 2 = 40ºC But the final temp will actually be lower than that because the cup itself will absorb a little bit of the heat. Heat Capacity We will use the data in part 1 to calculate the heat capacity of the cup, in units of J/K. This will tell us how many Joules of heat the cup absorbs for every K (or degree C) the water heats up. We know how many Joules of heat we added with the hot water, and we can calculate how many Joules were absorbed by the cold water as it warmed up.
    [Show full text]
  • Chemical Thermodynamics and Staged Unit Operations
    Beginning of Course Memorandum (BOCM) University of Virginia Fall, 2013 CHE 3316 Chemical Thermodynamics and Staged Unit Operations Revised October 22 Instructor: John O'Connell: Office Chemical Engineering 310; Voice (434) 924-3428; E-mail: [email protected] Office Hours: TR1400-1730, Others TBA GTA: Sabra Hanspal: Office CHE 217A; Voice 4-1476; E-mail: [email protected]; Office Hours: MF 12-2 PM Class Meetings: CHE 005, TR 0930-1045, T 1300-1350 Texts: "Lectures in Thermodynamics, Volume 2 (Beta Version)", by J.M. Haile & J.P. O'Connell, 2008 - 12, Electronic copy on CD available from instructor for $15. Total 641 pages. "Separation Process Engineering, 3rd Ed.", by P.C. Wankat, Prentice Hall, 2012. References: “Physical and Chemical Equilibrium for Chemical Engineers, 2nd Ed.” by N. de Nevers, Wiley-Interscience, New York, 2012. "Introduction to Chemical Engineering Thermodynamics, 7th Ed.," by J.M. Smith, H.C. Van Ness, and M.M. Abbott (SVNA). McGraw-Hill, New York, 2005. "Chemical, Biochemical, & Engineering Thermodynamics, 4th Ed.," by S.I. Sandler, John Wiley, 2006. "Schaum's Outline of Thermodynamics with Chemical Applications, 2nd Ed.," by H.C. Van Ness & M.M.Abbott, Schaum's Outlines, McGraw-Hill, 1989. "Lectures in Thermodynamics, Volume 1," by J.M. Haile, Macatea Productions, 2002. “Unit Operations of Chemical Engineering, 7th Ed.”, W. McCabe, J. Smith, & P. Harriott, New York, McGraw-Hill, 2004. “Principles of Chemical Separations with Environmental Applications,” R.D. Noble & P.A. Terry, Cambridge, UK, Cambridge University Press, 2004. “Perry’s Chemical Engineers’ Handbook, 8th Ed.,” D. Green & R. Perry, New York, McGraw-Hill, 2007.
    [Show full text]
  • Oxide Fuel Cells with Hydrocarbon and Syngas Fuels—A Review
    Fundamentals of electro- and thermochemistry in the anode of solid- oxide fuel cells with hydrocarbon and syngas fuels—a review Jeffrey Hanna,∗a Won Yong Lee,a Yixiang Shi,b and Ahmed F. Ghoniema Received Xth XXXXXXXXXX 20XX, Accepted Xth XXXXXXXXX 20XX First published on the web Xth XXXXXXXXXX 200X DOI: 10.1039/b000000x High fuel flexibility of solid-oxide fuel cells (SOFCs) affords the possibility to use relatively cheap, safe, and readily available hydrocarbon (e.g., CH4) or coal syngas (i.e., CO-H2 mixtures) fuels. Utilization of such fuels would greatly lower fuel cost and in- crease the feasibility of SOFC commercialization, especially for near-term adoption in anticipation of the long-awaited so-called “hydrogen economy.” Current SOFC technology has shown good performance with a wide range of hydrocarbon and syngas fu- els, but there are still significant challenges for practical application. In this paper, the basic operating principles, state-of-the-art performance benchmarks, and SOFC-relevant materials are summarized. More in-depth reviews on those topics can be found in Kee and co-workers [Combust. Sci. and Tech., 2008, 180, 1207–1244 and Proc. Combust. Inst., 2005, 30, 2379–2404] and McIntosh and Gorte [Chem. Rev., 2004, 104, 4845–4865]. The focus of this review is on the fundamentals and development of detailed electro- and thermal (or simply, electrothermal) chemistry within the SOFC anode, including electrochemical oxidation mechanisms for H2, CO, CH4, and carbon, as well as the effects of carbon deposition and sulfur poisoning. The interdependence of heterogeneous chemistry, charge-transfer processes, and transport are discussed in the context of SOFC-membrane-electrode assembly (MEA) modeling.
    [Show full text]
  • THERMOCHEMISTRY – 2 CALORIMETRY and HEATS of REACTION Dr
    THERMOCHEMISTRY – 2 CALORIMETRY AND HEATS OF REACTION Dr. Sapna Gupta HEAT CAPACITY • Heat capacity is the amount of heat needed to raise the temperature of the sample of substance by one degree Celsius or Kelvin. q = CDt • Molar heat capacity: heat capacity of one mole of substance. • Specific Heat Capacity: Quantity of heat needed to raise the temperature of one gram of substance by one degree Celsius (or one Kelvin) at constant pressure. q = m s Dt (final-initial) • Measured using a calorimeter – it absorbed heat evolved or absorbed. Dr. Sapna Gupta/Thermochemistry-2-Calorimetry 2 EXAMPLES OF SP. HEAT CAPACITY The higher the number the higher the energy required to raise the temp. Dr. Sapna Gupta/Thermochemistry-2-Calorimetry 3 CALORIMETRY: EXAMPLE - 1 Example: A piece of zinc weighing 35.8 g was heated from 20.00°C to 28.00°C. How much heat was required? The specific heat of zinc is 0.388 J/(g°C). Solution m = 35.8 g s = 0.388 J/(g°C) Dt = 28.00°C – 20.00°C = 8.00°C q = m s Dt 0.388 J q 35.8 g 8.00C = 111J gC Dr. Sapna Gupta/Thermochemistry-2-Calorimetry 4 CALORIMETRY: EXAMPLE - 2 Example: Nitromethane, CH3NO2, an organic solvent burns in oxygen according to the following reaction: 3 3 1 CH3NO2(g) + /4O2(g) CO2(g) + /2H2O(l) + /2N2(g) You place 1.724 g of nitromethane in a calorimeter with oxygen and ignite it. The temperature of the calorimeter increases from 22.23°C to 28.81°C.
    [Show full text]
  • Chapter 19 Chemical Thermodynamics
    Chapter 19 Chemical Thermodynamics Entropy and free energy Learning goals and key skills: Explain and apply the terms spontaneous process, reversible process, irreversible process, and isothermal process. Define entropy and state the second law of thermodynamics. Calculate DS for a phase change. Explain how the entropy of a system is related to the number of possible microstates. Describe the kinds of molecular motion that a molecule can possess. Predict the sign of DS for physical and chemical processes. State the third law of thermodynamics. Compare the values of standard molar entropies. Calculate standard entropy changes for a system from standard molar entropies. Calculate the Gibbs free energy from the enthalpy change and entropy change at a given temperature. Use free energy changes to predict whether reactions are spontaneous. Calculate standard free energy changes using standard free energies of formation. Predict the effect of temperature on spontaneity given DH and DS. Calculate DG under nonstandard conditions. Relate DG°and equilibrium constant (K). Review Chapter 5: energy, enthalpy, 1st law of thermo Thermodynamics: the science of heat and work Thermochemistry: the relationship between chemical reactions and energy changes Energy (E) The capacity to do work or to transfer heat. Work (w) The energy expended to move an object against an opposing force. w = F d Heat (q) Derived from the movements of atoms and molecules (including vibrations and rotations). Enthalpy (H) Enthalpy is the heat absorbed (or released) by a system during a constant-pressure process. 1 0th Law of Thermodynamics If A is in thermal equilibrium with B, and B is in thermal equilibrium with C, then C is also in thermal equilibrium with A.
    [Show full text]
  • Thermochemistry of the Formation of Fossil Fuels
    Fluid-Mineral Interactions: A Tribute to H. P. Eugster © The Geochemical Society, Special Publication No.2, 1990 Editors: R. J. Spencer and I-Ming Chou Thermochemistry of the formation of fossil fuels MOTOAKI SATO U.S. Geological Survey, MS 959, Reston, Virginia 22092, U.S.A. Abstract-Photosynthesis liberatesO2 from a mixture of CO2 and H20 in forming biologicalsubstances. Formation of fossil fuels is also associated with progressive depletion of oxygen from biological substances. The two processes are thus sequential in terms of deoxygenation. To evaluate thermo- chemical relations of the deoxygenation processes in a simple manner, the concept of deoxygenation free energy Gdeox and deoxygenation enthalpy Hdeox (defined as Gibbs energy and enthalpy, respectively, of reaction to release unit mole of O2 in forming a compound CxHyNzOw from CO2, H20, and N2) are computed for over 150 compounds. If compound A changes to compound B by dehydration and/or decarboxylation, and A has a higher Gdeox value than B, energy is released and the transformation can occur spontaneously; likewise heat is released if A has a higher Hdeox' The computed results indicate that energy input is required only for the initial stage of photosynthesis, and progressive deoxygenation and aromatic condensation during diagenesis should decrease free energy and release heat. Catagenesis and metagenesis are also most probably spontaneous and exothermic because both low C-number paraffinic hydrocarbons and polycondensed aromatic kerogens have the lowest Gdeox and Hdeox values among various homologous groups even at room temperature. The ultimate products of the spontaneous evolution of fossilfuelsare methane and graphite. The role of increased temperature associated with deeper burial is not to change the position of equilibrium, but simply to increase the reaction rate exponentially so that the extremely slow reactions would proceed in geologic time.
    [Show full text]
  • The Start of the Abiogenesis: Preservation of Homochirality In
    The start of the Abiogenesis: Preservation of homochirality in proteins as a necessary and sufficient condition for the establishment of the metabolism Søren Toxvaerd Department of Science and Environment, Roskilde University, Postbox 260, DK-4000 Roskilde, Denmark Abstract Biosystems contain an almost infinite amount of vital important details, which together ensure their life. There are, however, some common struc- tures and reactions in the systems: the homochirality of carbohydrates and proteins, the metabolism and the genetics. The Abiogenesis, or the origin of life, is probably not a result of a series of single events, but rather the result of a gradual process with increasing complexity of molecules and chemical reactions, and the prebiotic synthesis of molecules might not have left a trace of the establishment of structures and reactions at the beginning of the evo- lution. But alternatively, one might be able to determine some order in the formation of the chemical denominators in the Abiogenesis. Here we review experimental results and present a model of the start of the Abionenesis, where the spontaneous formation of homochirality in proteins is the precon- dition for the establishment of homochirality of carbohydrates and for the metabolism at the start of the Abiogenesis. Keywords: arXiv:1803.01560v1 [q-bio.BM] 5 Mar 2018 Abiogenesis Homochirality Metabolism 1. The preservation of homochiral structures in millions of years in a prebiotic aqueous environment. There have been many proposals to the establishment of homochirality of carbohydrates and amino acids in a prebiotic environment. It is, however, not the establishment, but rather the preservation of homochirality, which is the problem.
    [Show full text]