Hydrogen is ubiquitous and can be found in all commercial metals. Even small amounts of hydrogen can lead to embrittlement, loss of ductility, and premature failure of metal components in service. Thus, techniques to measure low solubilities of hydrogen in metals are desirable.
If unimpeded hydrogen will move within, into, and out of metals. The driving force for hydrogen movement is the negative gradient of the chemical potential. In this study, hydrogen gas will be produced at high pressure (fugacity), between 60 and 280 MPa (70 and 600 MPa), in situ from the confined thermal decomposition of zirconium hydride powder, ZrH2, distributed on the surface of a probe made of zirconium metal. The hydrogen in the gas will move into the metal and the probe until the zirconium hydride powder is depleted or equilibrium is reached. In both instances, the chemical potential gradients are zero and there is no further net movement of hydrogen:
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The chemical potential gradients are zero when the hydride powder is depleted because the means of transporting hydrogen between the metal and the probe is lost when the production of hydrogen gas ceases; the chemical potentials could be different, but there are no gradients if there is no means of transport.
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Chemical potential gradients at equilibrium are zero for hydrogen as atoms in solid solutions, in the gas phase as H2, and as metal hydrides if these forms of hydrogen can interact in a mixture.
The probe introduced in this study exploits these features of chemical potentials to determine the solubility of atomic hydrogen in metal in equilibrium with hydrogen gas: the Sieverts solubility. At equilibrium, the chemical potentials of hydrogen gas and atomic hydrogen in solid solution are equal. Adding a probe introduces more chemical potentials to consider, but the probe does not affect the metal-hydrogen equilibrium. The chemical potentials of hydrogen gas and atomic hydrogen in the metal will simultaneously have to equal the chemical potentials of all interacting forms of hydrogen in the probe and in any residual zirconium hydride powder. Whether hydrogen movement stops because of depletion of the zirconium hydride or because of equilibrium, the hydrogen that partitions to the probe provides a proxy measurement of the solubility of hydrogen in the metal in equilibrium with hydrogen gas by mass balance.
In this study the solubility of hydrogen in copper is examined. Copper has been proposed for use as the outer shell of containers for spent nuclear fuel. The effects of hydrogen on copper are being studied to identify diffusion-controlled degradation mechanisms that might take place during storage over thousands of years.
The Sieverts solubility, S, of hydrogen in copper at equilibrium with hydrogen gas has been described by an Arrhenius expression determined from experimentally measured values that span 2 orders of magnitude between 1000 to 400 °C[1,2,3,4,5,6,7] and values calculated from permeability data and optimized thermodynamic parameters from a CALPHAD study[7]:
$$ S = 2600\exp \left( { - \frac{48550}{RT}} \right){\text{ [mol H}}_{2} /{\text{m}}^{3} \sqrt {\text{MPa}} ] $$
(1)
where R is 8.314 J/mol K. The solubility of hydrogen in copper is low and there are few direct measurements below 500 °C and no data below 400 °C,[7] so mass-transport calculations that require solubilities at temperatures relevant to storage of spent fuel (< 200 °C) require extrapolation of Eq 1. The effectiveness of this extrapolation is challenged by the apparent incompatibility of Eq 1 with a similar equation determined from diffusivity and hydrogen-gas permeation studies.
Diffusivities for hydrogen in copper spanning 6 orders of magnitude have been measured between 1000 °C and room temperature using electrochemical permeation and outgassing techniques.[1,8,9,10,11,12] The diffusivities were fitted to an Arrhenius expression[7]:
$$ D = 1.74 \times 10^{ - 6} \exp \left( { - \frac{42000}{RT}} \right){\text{ [m}}^{2} /{\text{s}}]. $$
(2)
Hydrogen-gas permeation studies in copper have been reported spanning 10 orders of magnitude between 700 °C and room temperature.[9,11,12,13,14,15] In these studies, high-pressure hydrogen gas is on one surface of a thin foil of copper, and low pressure is on the other surface. Hydrogen gas dissociates at the metal surface on the high-pressure side into atomic hydrogen that moves into solid solution in the metal:
$$ \frac{1}{2}H_{2} \rightleftharpoons H_{\text{solid\,solution}}. $$
(3)
The activity coefficient for hydrogen in the metal is assumed to be unity because the concentrations are low (< 3 ppm by mass in copper, wppm). The concentration of hydrogen at the metal surface is related to the fugacity of hydrogen gas, \( f_{{{\text{H}}_{ 2} }} , \) by a modified Sieverts equation[16]:
$$ c_{\text{H\,in\,Cu}} = S\left( {\frac{{2M_{\text{H}} }}{{\rho_{\text{Cu}} }}} \right)\sqrt {f_{{{\text{H}}_{2} }} } {\text{ [wppm]}} $$
(4)
where MH is the molar mass of hydrogen, \( \rho_{\text{Cu}}\) is the density of copper. The flux of atoms through the metal is given by an approximation to Fick’s Law for thin foils with thickness \( \delta x \):
$$ {\text{J}} = - D\frac{\Delta c}{\delta x} $$
(5)
where Δc is the difference in the concentrations of hydrogen in solution at the two surfaces of the foil.
Substituting Eq 4 into Eq 5 yields the equation for the permeation flux through a thin foil:
$$ {\text{J}} = - DS\left( {\frac{{2M_{\text{H}}}}{{\rho_{\text{Cu}}}}} \right)\frac{{\sqrt {f_{{{\text{H}}_{2} }} } }}{\delta x} $$
(6)
where the assumption has been made that the fugacity of hydrogen on the low-pressure side of the foil is zero and the hydrogen that moves through the metal is replenished from the gas at steady state. The permeability constant, P, determined from experiments is defined:
Experimental permeabilities were fitted to an Arrhenius expression[7]:
$$ P = 1.4 \times 10^{ - 3} \exp \left( { - \frac{84320}{RT}} \right){\text{ [mol H}}_{2} /{\text{m s }}\sqrt {\text{MPa}} ]. $$
(8)
The solubility can be determined from Eq 7 and the permeability and diffusivity relations given by Eqs 2 and 8:
$$ S_{\text{H\,in\,Cu}} \equiv P/D = 812 \cdot \exp \left( { - \frac{42300}{RT}} \right){\text{ [mol H}}_{2} /{\text{m}}^{3} \sqrt {\text{MPa}} ]. $$
(9)
Comparing the values from Eq 9 with those from Eq 1 demonstrates the inconsistency of these Arrhenius equations for S, D and P: they do not satisfy the defining relationship P = DS (Eq 7). It is commonly believed[7] that this discrepancy can be attributed to the solubility because of trapping of hydrogen at crystalline defects such as vacancies, dislocations, grain boundaries, porosity, but these defects would affect values of diffusivity and permeation, not just solubility. The equation for solubility is the most likely of S, D and P to be in error because it was partially calculated from ab initio models that do not include crystalline defects, whereas the equations for diffusivity and permeation were determined solely from experimental data. Experimentally determined solubilities will be higher in metals containing large numbers of defects because more hydrogen will partition to the defects. Ab initio models that do not include partitioning to defects will always underpredict experimental solubilities.
In this study we introduce an indirect method to determine hydrogen solubilities in copper between 350 and 450 °C that will support empirical extrapolations to temperatures more relevant to nuclear spent fuel storage (< 200 °C). The method based on chemical potential uses a zirconium metal probe, in situ generation of molecular hydrogen, and high-pressure partitioning between molecular hydrogen and atomic hydrogen in copper and zirconium at various temperatures. A Sieverts expression written in Arrhenius form will be determined from the solubilities measured in this study and compared with Eqs 1 and 9.