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Publié parharona haronaa Modifié depuis plus de 7 années
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DIFFUSION IN SOLIDS FICK’S LAWS KIRKENDALL EFFECT ATOMIC MECHANISMS Diffusion in Solids P.G. Shewmon McGraw-Hill, New York (1963)
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ArH2H2 Movable piston with an orifice H 2 diffusion direction Ar diffusion direction Piston motion Piston moves in the direction of the slower moving species
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AB Inert Marker – thin rod of a high melting material which is basically insoluble in A & B Kirkendall effect Materials A and B welded together with Inert marker and given a diffusion anneal Usually the lower melting component diffuses faster (say B) Marker motion
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Diffusion Mass flow process by which species change their position relative to their neighbours Driven by thermal energy and a gradient Thermal energy → thermal vibrations → Atomic jumps Concentration / chemical potential ElectricGradient Magnetic Stress
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Assume that only B is moving into A Assume steady state conditions → J f(x,t) (No accumulation of matter) Flux (J) (restricted definition) → Flow / area / time [Atoms / m 2 / s]
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Fick’s I law No. of atoms crossing area A per unit time Cross-sectional area Concentration gradient Matter transport is down the concentration gradient Diffusion coefficient/ diffusivity A Flow direction As a first approximation assume D f(t)
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Fick’s first law
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Diffusivity (D) → f(A, B, T) D = f(c) D f(c) C1C1 C2C2 Steady state diffusion x → Concentration →
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Diffusion Steady state J f(x,t) Non-steady state J = f(x,t) D = f(c) D f(c)
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Fick’s II law JxJx J x+ x xx Fick’s first law D f(x)
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RHS is the curvature of the c vs x curve x → c → x → c → +ve curvature c ↑ as t ↑ ve curvature c ↓ as t ↑ LHS is the change is concentration with time
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Solution to 2 o de with 2 constants determined from Boundary Conditions and Initial Condition Erf ( ) = 1 Erf (- ) = -1 Erf (0) = 0 Erf (-x) = -Erf (x) u → Exp( u 2 ) → 0 Area
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A B Applications based on Fick’s II law x → Concentration → C avg ↑ t t 1 > 0 | c(x,t 1 ) t 2 > t 1 | c(x,t 1 ) t = 0 | c(x,0) A & B welded together and heated to high temperature (kept constant → T 0 ) Flux f(x)| t f(t)| x Non-steady state If D = f(c) c(+x,t) c(-x,t) i.e. asymmetry about y-axis C(+x, 0) = C 1 C( x, 0) = C 2 C1C1 C2C2 A = (C 1 + C 2 )/2 B = (C 2 – C 1 )/2 Determination of Diffusivity
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Temperature dependence of diffusivity Arrhenius type
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Applications based on Fick’s II law Carburization of steel Surface is often the most important part of the component, which is prone to degradation Surface hardenting of steel components like gears is done by carburizing or nitriding Pack carburizing → solid carbon powder used as C source Gas carburizing → Methane gas CH 4 (g) → 2H 2 (g) + C (diffuses into steel) x → 0 C1C1 CSCS C(+x, 0) = C 1 C(0, t) = C S A = C S B = C S – C 1
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Approximate formula for depth of penetration
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ATOMIC MODELS OF DIFFUSION 1. Interstitial Mechanism
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2. Vacancy Mechanism
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3. Interstitialcy Mechanism
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4. Direct Interchange and Ring
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Interstitial Diffusion 1 2 12 HmHm At T > 0 K vibration of the atoms provides the energy to overcome the energy barrier H m (enthalpy of motion) → frequency of vibrations, ’ → number of successful jumps / time
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1 2 Vacant site c = atoms / volume c = 1 / 3 concentration gradient dc/dx = ( 1 / 3 )/ = 1 / 4 Flux = No of atoms / area / time = ’ / area = ’ / 2 On comparison with
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Substitutional Diffusion Probability for a jump (probability that the site is vacant). (probability that the atom has sufficient energy) H m → enthalpy of motion of atom ’ → frequency of successful jumps As derived for interstitial diffusion
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Element HfHf HmHm H f + H m Q Au9780177174 Ag9579174184 Calculated and experimental activation energies for vacancy Diffusion
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Interstitial Diffusion Substitutional Diffusion D (C in FCC Fe at 1000ºC) = 3 10 11 m 2 /s D (Ni in FCC Fe at 1000ºC) = 2 10 16 m 2 /s
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DIFFUSION PATHS WITH LESSER RESISTANCE Q surface < Q grain boundary < Q lattice Experimentally determined activation energies for diffusion Core of dislocation lines offer paths of lower resistance → PIPE DIFFUSION Lower activation energy automatically implies higher diffusivity Diffusivity for a given path along with the available cross-section for the path will determine the diffusion rate for that path
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Comparison of Diffusivity for self-diffusion of Ag → single crystal vs polycrystal 1/T → Log (D) → Schematic Polycrystal Single crystal ← Increasing Temperature Q grain boundary = 110 kJ /mole Q Lattice = 192 kJ /mole
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