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Theory and UG for the SurfaceKinetics
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@@ -8,14 +8,17 @@ Bulk physics | |
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H transport | ||
^^^^^^^^^^^ | ||
The model developed by McNabb & Foster :cite:`McNabb1963` is used to model hydrogen transport in materials in FESTIM. The principle is to separate mobile hydrogen :math:`c_\mathrm{m}` and trapped hydrogen :math:`c_\mathrm{t}`. The diffusion of mobile particles is governed by Fick’s law of diffusion where the hydrogen flux is | ||
The model developed by McNabb & Foster :cite:`McNabb1963` is used to model hydrogen transport in materials in FESTIM. | ||
The principle is to separate mobile hydrogen :math:`c_\mathrm{m}\,[\mathrm{m}^{-3}]` and trapped hydrogen :math:`c_\mathrm{t}\,[\mathrm{m}^{-3}]`. | ||
The diffusion of mobile particles is governed by Fick’s law of diffusion where the hydrogen flux is | ||
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.. math:: | ||
:label: eq_difflux | ||
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J = -D \nabla c_\mathrm{m} | ||
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where :math:`D=D(T)` is the diffusivity. Each trap :math:`i` is associated with a trapping and a detrapping rate :math:`k_i` and :math:`p_i`, respectively, as well as a trap density :math:`n_i`. | ||
where :math:`D=D(T)\,[\mathrm{m}^{2}\,\mathrm{s}^{-1}]` is the diffusivity. | ||
Each trap :math:`i` is associated with a trapping and a detrapping rate :math:`k_i\,[\mathrm{m}^{3}\,\mathrm{s}^{-1}]` and :math:`p_i\,[\mathrm{s}^{-1}]`, respectively, as well as a trap density :math:`n_i\,[\mathrm{m}^{-3}]`. | ||
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The temporal evolution of :math:`c_\mathrm{m}` and :math:`c_{\mathrm{t}, i}` are then given by: | ||
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\frac {\partial c_{\mathrm{t}, i}} { \partial t} = k_i c_\mathrm{m} (n_i - c_{\mathrm{t},i}) - p_i c_{\mathrm{t},i} | ||
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where :math:`S_j=S_j(x,y,z,t)` is a source :math:`j` of mobile hydrogen. In FESTIM, source terms can be space and time dependent. These are used to simulate plasma implantation in materials, tritium generation from neutron interactions, etc. | ||
where :math:`S_j=S_j(x,y,z,t)\,[\mathrm{m}^{-3}\,\mathrm{s}^{-1}]` is a source :math:`j` of mobile hydrogen. In FESTIM, source terms can be space and time dependent. These are used to simulate plasma implantation in materials, tritium generation from neutron interactions, etc. | ||
These equations can be solved in cartesian coordinates but also in cylindrical and spherical coordinates. This is useful, for instance, when simulating hydrogen transport in a pipe or in a pebble. FESTIM can solve steady-state hydrogen transport problems. | ||
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Soret effect | ||
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J = -D \nabla c_\mathrm{m} - D\frac{Q^* c_\mathrm{m}}{k_B T^2} \nabla T | ||
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where :math:`Q^*` is the Soret coefficient (also called heat of transport) and :math:`k_B` is the Boltzmann constant. | ||
where :math:`Q^*\,[\mathrm{eV}]` is the Soret coefficient (also called heat of transport) and :math:`k_B` is the Boltzmann constant. | ||
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Conservation of chemical potential at interfaces | ||
^^^^^^^^^^^^^^^^^^^^^^^^^^^^^^^^^^^^^^^^^^^^^^^^ | ||
Continuity of local partial pressure :math:`P` at interfaces between materials has to be ensured. In the case of a material behaving according to Sievert’s law of solubility (metals), the partial pressure is expressed as: | ||
Continuity of local partial pressure :math:`P\,[\mathrm{Pa}]` at interfaces between materials has to be ensured. In the case of a material behaving according to Sievert’s law of solubility (metals), the partial pressure is expressed as: | ||
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.. math:: | ||
:label: eq_Sievert | ||
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P = \left(\frac{c_\mathrm{m}}{K_S}\right)^2 | ||
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where :math:`K_S` is the material solubility (or Sivert's constant). | ||
where :math:`K_S\,[\mathrm{m}^{-3}\,\mathrm{Pa}^{-0.5}]` is the material solubility (or Sivert's constant). | ||
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In the case of a material behaving according to Henry's law of solubility, the partial pressure is expressed as: | ||
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P = \frac{c_\mathrm{m}}{K_H} | ||
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where :math:`K_H` is the material solubility (or Henry's constant). | ||
where :math:`K_H\,[\mathrm{m}^{-3}\,\mathrm{Pa}^{-1}]` is the material solubility (or Henry's constant). | ||
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Two different interface cases can then occur. At the interface between two Sievert or two Henry materials, the continuity of partial pressure yields: | ||
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It appears from these equilibrium equations that a difference in solubilities introduces a concentration jump at interfaces. | ||
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In FESTIM, the conservation of chemical potential is obtained by a change of variables :cite:`Delaporte-Mathurin2021`. The variable :math:`\theta` is introduced and: | ||
In FESTIM, the conservation of chemical potential is obtained by a change of variables :cite:`Delaporte-Mathurin2021`. The variable :math:`\theta\,[\mathrm{Pa}]` is introduced and: | ||
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.. math:: | ||
:label: eq_theta | ||
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k(T) = k_0 \exp \left[-\frac{E_k}{k_B T} \right] | ||
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where :math:`k_0` is the pre-exponential factor, :math:`E_k` is the process activation energy, and :math:`T` is the temperature. | ||
where :math:`k_0` is the pre-exponential factor, :math:`E_k\,[\mathrm{eV}]` is the process activation energy, and :math:`T\,[\mathrm{K}]` is the temperature. | ||
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Heat transfer | ||
^^^^^^^^^^^^^^ | ||
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\rho C_p \frac{\partial T}{\partial t} = \nabla \cdot (\lambda \nabla T) + \sum_i Q_i | ||
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where :math:`T` is the temperature, :math:`C_p` is the specific heat capacity, :math:`\rho` is the material's density, :math:`\lambda` is the thermal conductivity and :math:`Q_i` is a volumetric heat source :math:`i`. As for the hydrogen transport problem, the heat equation can be solved in steady state. In FESTIM, the thermal properties of materials can be arbitrary functions of temperature. | ||
where :math:`T` is the temperature, :math:`C_p\,[\mathrm{J}\,\mathrm{kg}^{-1}\,\mathrm{K}^{-1}]` is the specific heat capacity, :math:`\rho\,[\mathrm{kg}\,\mathrm{m}^{-3}]` is the material's density, | ||
:math:`\lambda\,[\mathrm{W}\,\mathrm{m}^{-1}\,\mathrm{K}^{-1}]` is the thermal conductivity and :math:`Q_i\,[\mathrm{W}\,\mathrm{m}^{-3}]` is a volumetric heat source :math:`i`. As for the hydrogen transport problem, the heat equation can be solved in steady state. In FESTIM, the thermal properties of materials can be arbitrary functions of temperature. | ||
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--------------- | ||
Surface physics | ||
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where :math:`h` is the heat transfer coefficient and :math:`T_{\mathrm{ext}}` is the external temperature. | ||
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--------------- | ||
Kinetic surface model | ||
^^^^^^^^^^^^^^^^^^^^^ | ||
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Modelling hydrogen retention or outgassing might require considering the kinetics of surface processes. | ||
A representative example is the hydrogen uptake from a gas phase, when the energy of incident atoms/molecules is not high enough to | ||
overcome the surface barrier for implantation. The general approach to account for surface kinetics :cite:`Pick1985, Hodille2017, Guterl2019, Schmid2021` consists in | ||
introducing hydrogen surface species :math:`c_\mathrm{s}\,[\mathrm{m}^{-2}]`. | ||
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Evolution of hydrogen surface concentration is determined by the atomic flux balance at the surface, as sketched in the simplified energy diagram below. | ||
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.. thumbnail:: images/potential_diagram.png | ||
:align: center | ||
:width: 800 | ||
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Idealised potential energy diagram for hydrogen near a surface of an endothermic metal. Energy levels are measured from the :math:`\mathrm{H}_2` state | ||
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The governing equation for surface species is: | ||
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.. math:: | ||
:label: eq_surf_conc | ||
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\dfrac{d c_\mathrm{s}}{d t} = J_\mathrm{bs} - J_\mathrm{sb} + J_\mathrm{vs}~\text{on}~\delta\Omega | ||
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where :math:`J_\mathrm{bs}\,[\mathrm{m}^{-2}\,\mathrm{s}^{-1}]` is the flux of hydrogen atoms from the subsurface (bulk region just beneath the surface) onto the surface, | ||
:math:`J_\mathrm{sb}\,[\mathrm{m}^{-2}\,\mathrm{s}^{-1}]` is the flux of hydrogen atoms from the surface into the subsurface, and :math:`J_\mathrm{vs}\,[\mathrm{m}^{-2}\,\mathrm{s}^{-1}]` is the net flux of hydrogen | ||
There was a problem hiding this comment. Choose a reason for hiding this commentThe reason will be displayed to describe this comment to others. Learn more. does J_vs contains the desorbing flux and all abstraction fluxes (ELy Rideal recombination etc) ? There was a problem hiding this comment. Choose a reason for hiding this commentThe reason will be displayed to describe this comment to others. Learn more. In general, yes, but it should be defined by a user. Here is an example from one validation case on how it can be defined: def J_vs(T, surf_conc, t):
phi_atom = SP * Gamma_atom * (1 - surf_conc / n_surf) # adsorption
phi_exc = Gamma_atom * sigma_exc * surf_conc # abstraction
phi_des = 2 * nu0 * (lambda_des * surf_conc) ** 2 * f.exp(-2 * E_des / F.k_B / T) # desorption
return phi_atom - phi_exc - phi_des There was a problem hiding this comment. Choose a reason for hiding this commentThe reason will be displayed to describe this comment to others. Learn more. Maybe this could be explicited then? something like
There was a problem hiding this comment. Choose a reason for hiding this commentThe reason will be displayed to describe this comment to others. Learn more. In this case, should we somehow clarify that the flux comes onto the surface: There was a problem hiding this comment. Choose a reason for hiding this commentThe reason will be displayed to describe this comment to others. Learn more. Probably There was a problem hiding this comment. Choose a reason for hiding this commentThe reason will be displayed to describe this comment to others. Learn more. Maybe just say J_vs = J_in - J_out where J_in is the sum of all fluxes coming from the vacuum to the surface and J_out from the surface to the vacuum Or something like that and then give a few examples There was a problem hiding this comment. Choose a reason for hiding this commentThe reason will be displayed to describe this comment to others. Learn more. A few examples on different processes that can be included? There was a problem hiding this comment. Choose a reason for hiding this commentThe reason will be displayed to describe this comment to others. Learn more. Yes just like you had in your previous comment There was a problem hiding this comment. Choose a reason for hiding this commentThe reason will be displayed to describe this comment to others. Learn more. I updated this part. Let me know what you think. There was a problem hiding this comment. Choose a reason for hiding this commentThe reason will be displayed to describe this comment to others. Learn more. Looks good to me! |
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atoms from the vacuum onto the surface. It worth noticing that the current model does not account for possible surface diffusion and is available only for 1D hydrogen transport simulations. | ||
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The connection condition between surface and bulk domains represents the Robin boundary condition for the hydrogen transport problem. | ||
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.. math:: | ||
:label: eq_subsurf_conc | ||
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-D \nabla c_\mathrm{m} \cdot \mathbf{n} = \lambda_{\mathrm{IS}} \dfrac{\partial c_{\mathrm{m}}}{\partial t} + J_{\mathrm{bs}} - J_{\mathrm{sb}}~\text{on}~\delta\Omega | ||
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where :math:`\lambda_\mathrm{IS}\,[\mathrm{m}]` is the distance between two interstitial sites in the bulk. | ||
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.. note:: | ||
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At the left boundary, the normal vector :math:`\textbf{n}` is :math:`-\vec{x}`. The steady-state approximation of eq. :eq:`eq_subsurf_conc` at the left boundary | ||
is, therefore, :math:`D\frac{\partial c_\mathrm{m}}{\partial x}=J_\mathrm{bs}-J_\mathrm{sb}` representing eq. (12) in the original work of M.A. Pick & K. Sonnenberg :cite:`Pick1985`. | ||
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The fluxes for subsurface-to-surface and surface-to-subsurface transitions are defined as follows: | ||
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.. math:: | ||
:label: eq_Jbs | ||
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J_\mathrm{bs} = k_\mathrm{bs} \lambda_\mathrm{abs} c_\mathrm{m} \left(1-\dfrac{c_\mathrm{s}}{n_\mathrm{surf}}\right) | ||
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.. math:: | ||
:label: eq_Jsb | ||
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J_\mathrm{sb} = k_\mathrm{sb} c_\mathrm{s} \left(1-\dfrac{c_\mathrm{m}}{n_\mathrm{IS}}\right) | ||
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where :math:`n_\mathrm{surf}\,[\mathrm{m}^{-2}]` is the surface concentration of adsorption sites, :math:`n_\mathrm{IS}\,[\mathrm{m}^{-3}]` is the bulk concentration of interstitial sites, | ||
:math:`\lambda_\mathrm{abs}=n_\mathrm{surf}/n_\mathrm{IS}\,[\mathrm{m}]` is the characteristic distance between surface and subsurface sites, :math:`k_\mathrm{bs}\,[\mathrm{s}^{-1}]` | ||
and :math:`k_\mathrm{sb}\,[\mathrm{s}^{-1}]` are the rate constants for subsurface-to-surface and surface-to-subsurface transitions, respectively. | ||
Usually, these rate constants are expressed in the Arrhenius form: :math:`k_i=k_{i,0}\exp(-E_{k,i} / kT)`. Both these processes are assumed to take place | ||
if there are available sites on the surface (in the subsurface). Possible surface/subsurface saturation is accounted for with terms in brackets. | ||
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.. note:: | ||
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In eq. :eq:`eq_Jsb`, the last term in brackets is usually omitted :cite:`Guterl2019, Pick1985, Hodille2017, Schmid2021`, | ||
since :math:`c_\mathrm{m} \ll n_\mathrm{IS}` is assumed. However, this term is included in some works (e.g. :cite:`Hamamoto2020`) | ||
to better reproduce the experimental results. | ||
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------------ | ||
References | ||
--------------- | ||
------------ | ||
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.. bibliography:: bibliography/references.bib | ||
:style: unsrt |
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Vladimir, do you not want to also mention your papers ? I think you implemented and used this kind of model in you laser desorption papers (but it is up to you).
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@ehodille, well, I used, yes. However, I intended to mention here the pioneers, whereas my papers on LID were mainly based on your works.