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First Law of Thermodynamics Physics 313 Professor Lee Carkner Lecture 8
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Exercise #6 Spring Work done on spring W = F dx = kx dx = ½kx 2 = ½k(x 2 2 –x 1 2 ) If the spring is initially unstretched, x 1 = 0 Spring and gas work displacement of spring V = A X 0.025 = 0.25 x, x = 0.1 m, x 2 = 0.1 m W = ½kx 2 2 = (½)(150)(0.1) 2 = P = W/ V = 0.75/0.025 = 30 kPa PV = nRT T = PV/nR = (30000)(0.025)/(1)(8.31) =
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Heat What is heat? Heat is not a state variable No heat transfer if: Heat is energy and can occur with different processes
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Isochoric Heat If heat is added the temperature of the system will rise Any heat exchange directly affects the internal energy
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Adiabatic Work In an adiabatic system no heat can flow For any adiabatic process by which the system move from state 1 to state 2 the total amount of work is a constant This is not normally true This work changes the internal energy
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Internal Energy When heat flows into the system or work is done on a system the system gains energy The internal energy is a property of a system and can be expressed in terms of thermodynamic coordinates We will often discuss a change in internal energy ( U or dU)
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First Law of Thermodynamics Energy is conserved Can write in differential form as dU is a change in internal energy dQ and dW are small amounts of heat or work
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Notes on the First Law Heat is defined thermodynamically by the first law: Can also write for work: Sign Convention Heat into a system is positive Work done on the system is positive This convention can be changed but the first law then also must be changed
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Notes on Heat Heat was once thought to be a fluid within a body People began to suspect that heat was a form of energy in the early 1800’s, but couldn’t prove it Joule demonstrated the equivalence of heat and work in the 1840’s
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Special Cases Adiabatic: U = W Isochoric: U = Q
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Heat and Internal Energy If a Styrofoam block and a steel block are both heated the same amount which is hotter? Why? Q = C T
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Specific Heat We will also use the heat capacity per mole: Where n is number of moles or (m/M) total mass divided by molar mass
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Heat Capacities We can express the heat capacity in terms of differential changes in temperature and heat C = dQ/dT We can then define two specific quantities: C V = (dQ/dT) V C P = (dQ/dT) P Note that C is a function of temperature
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Internal Energy We can write the heat flow into a system as: For an isochoric system So: The change in internal energy is a function of the change in temperature
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Heat Conservation All objects within the boundary will exchange heat until they are in thermodynamic equilibrium (equal T) Lost to surroundings
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Calorimetry A calorimeter must : produce a well defined amount of heat Monitor temperature Heat produced must all go into raising temperature of sample
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