Abstract
Polarization of dispersive and dissipative dielectric media with smoothed-out inhomogeneities is studied with the goal to clarify the question of renormalizability of electromagnetic stress–energy tensor. The stress tensor is computed with the Lifshitz approach to van der Waals forces in the non-retarded limit, which accounts for dominant effects at the distances from the interface shorter than the absorption wavelength. After the substraction of the leading free space ultraviolet divergencies, there still remain two types of divergencies. First, contributions diverging in the sharp interface case become finite once it is smoothed out. Second, new subleading ultraviolet cut-off-dependent contributions appear due to the interface internal structure. The Hadamard expansion, based on the heat kernel method, is applied to systematically single out both finite and subleading contributions and to demonstrate incomplete renormalizability of the Lifshitz theory. The above approach also allows us to reveal the purely quantum mechanical nature of surface tension, which consists of finite cut-off-independent as well as cut-off-dependent contributions. The deduced theory of surface tension and its calculations for real dielectric media are favourably compared to the available experimental data. The problem of surface tension proves to be of a distinguished limit type because the sharp interface formulation loses the critical information about the internal structure of an interface. The general theory offered here is illustrated with an exactly solvable model representing a smooth transition between two different dielectric media, which relies upon a solution of the Schrödinger equation with the Scarf potential.
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Notes
Because in the time domain the relation between the displacement vector \({\varvec{D}}\) and the electric field vector \({\varvec{E}}\) is nonlocal, \({\varvec{D}}(t,{\varvec{x}}) = {\varvec{E}}(t,{\varvec{x}}) + \int _{0}^{\infty }{f(\tau ) {\varvec{E}}(t-\tau ,{\varvec{x}}) \, \mathrm {d}\tau }\), while in the frequency-domain it becomes \(\widehat{{\varvec{D}}}(\omega ;{\varvec{x}}) = \varepsilon (\omega ) \widehat{{\varvec{E}}}(\omega ;{\varvec{x}}), \ \varepsilon (\omega ) = 1 + \int _{0}^{\infty }{f(\tau ) \, e^{\mathrm {i}\omega \tau } \, \mathrm {d}\tau }\).
The sign convention [57, 58] used here is dictated by the need to regularize the Feynman path integral via an analytic continuation from real t to complex t with negative imaginary part. However, the opposite sign convention is often used [54], which also transforms the Lorentzian into the Euclidean metric.
Consider deformation of a small volume with fixed number of molecules as an example.
The power \(-12\) was chosen by Lennard-Jones for convenience: in reality, the actual potential may have a mixed polynomial-exponential form, cf. [67] and references therein. For example, in the case of helium atoms the repulsive interaction between them is caused by a depletion in electron density in the overlap region that descreens the nuclei from each other resulting in internuclear repulsion. In general, while the \(r^{-12}\) term is often attributed to the Pauli exclusion principle for fermions due to anti-symmetry of their wave functions resulting in an exchange interaction between identical particles (which also applies to bosons)—this interaction is different from Coulomb electrostatic repulsion and, in fact, stronger on shorter distances and ultimately responsible for the stability of matter [68, 69]—it could also originate from the Heisenberg principle of uncertainty [70].
Physically, this absorption of electrostriction to the renormalized isotropic pressure follows from the chemical potential [14, 62], which must be constant for media in equilibrium. One may think of the electrostriction stress as analogous to the gravity in the ocean compensated by the mechanical stresses in water: if it is balanced in the r-direction, then due to isotropy it must be balanced in the \(\theta \)-direction as well. Notably, the \(\theta \)-dependence of the electrostriction stress leads to non-uniform compression of the matter which is stronger near the interface. However, due to isotropy, electrostriction does not contribute to ST (Sect. 4).
Because from now on we will work mostly with the Fourier transforms of all quantities, we implicitly assume that they depend on the Matsubara frequencies \(\zeta _n\) and q, and, for simplicity, we omit these arguments in functions. Thus, in these notations we have \(\varepsilon (\mathrm {i}\zeta ;{\varvec{x}})\equiv \varepsilon ({\varvec{x}})\), \({\widehat{G}}(\zeta ;{\varvec{x}},{\varvec{x'}})\equiv {\widehat{G}}({\varvec{x}},{\varvec{x'}})\), etc. Since \(\varepsilon \) is already dimensionless, we use the same letter for the functions \(\varepsilon =\varepsilon ({\overline{z}})=\varepsilon (\mathrm {i}\zeta ;{w}{\overline{z}})\).
Recall that the pressure is the force per unit area of the wall should it be bounding the medium, while normal stress is the force per unit area acting on the medium itself.
In the case of the Scarf model, \(\gamma ^{ \text{(div) }}\) can be calculated explicitly:
$$\begin{aligned} \gamma ^{ \text{(div) }}={23\over 6 (4\pi )^{3/2} \beta \lambda _{0}w}\sum _n \frac{(\ln \varepsilon _{\infty })^2}{(\ln \varepsilon _{\infty })^2+4\pi ^2}\frac{1+\sqrt{\varepsilon _{\infty }}}{\sqrt{\varepsilon _{\infty }}}. \end{aligned}$$First, this leads to the Keesom effect [82] contributing to vdW forces due to attraction of permanent dipoles with moments \(\mathrm {p}\)—in the case of water the ratio of the Keesom to London energies of interaction \(\varphi _{K}/\varphi _{L} = 4 \mathrm {p}^{4}/(9 h_{{ \text{ B }}} T \alpha _{w}^{2} \omega _{a}) \approx 6.32\), where \(\alpha _{w}\) is the water molecular polarizability; most importantly, the hydrogen bond energy \(3.82 \cdot 10^{-20} \, \mathrm {J}\) per bond is comparable to that of the latent heat of evaporation per molecule \(6.78 \cdot 10^{-20} \, \mathrm {J}\) and much larger than \(k_{{ \text{ B }}} T \approx 4.14 \cdot 10^{-21} \, \mathrm {J}\) thus indeed being capable of affecting the value of ST. Second, the water molecule polarity may give rise to a local structure in the bulk and potentially at the interface thus, in particular, invalidating assumptions behind the isotropy of the dielectric permittivity upon which the Lifshitz theory is based—if one thinks of water molecules as permanent dipoles, they may orient themselves along the interface thus increasing ST as opposed to, say, surfactants, which, when added to water, stick their polar heads in water and thus orient themselves perpendicularly to the interface, thus decreasing ST due to repulsion between themselves.
This is typical for non-closed theories, e.g. the Navier–Stokes equations require the empirically measured viscosity coefficient.
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This work was partially supported by the Natural Sciences and Engineering Research Council of Canada (NSERC). A.Z. also acknowledges financial support by the Killam Trust.
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Heat kernel calculations
Heat kernel calculations
Let us define the new field
and the corresponding Green’s function
where \(\upphi ({\varvec{x}})\) is the operator corresponding to the field \(\phi ({\varvec{x}})\). Then, the inner product for this new field takes the covariant form \(\int \mathrm {d}{\varvec{x}}\, \varPhi _1 \varPhi _2=\int \mathrm {d}{\varvec{x}}\,\varepsilon ^{-3/2}\, \phi _1 \phi _2=\int \mathrm {d}{\varvec{x}}\sqrt{\mathrm {g}}\, \phi _1 \phi _2\). Equation (3) transforms to
Taking into account that
the new operator \({\mathbb {O}}\) becomes
Note that
and the covariant Laplacian in metric \(\mathrm {g}_{ij}\) reads
Therefore, we obtain the covariant form for the operator in (80)
which is Hermitian with the covariant measure \(\sqrt{\mathrm {g}}\). The potential \({\mathbb {V}}\) can also be obtained following the computations in [31, 64], which require the knowledge of the Christoffel symbols
and the connection
Heat kernel corresponding to operator \({\widehat{O}}\) is \({\widehat{K}}(s|{\varvec{x}},{\varvec{x'}})=\mathrm {g}^{1/4}({\varvec{x}})\mathrm {g}^{1/4}({\varvec{x}}'){\mathbb {K}}(s|{\varvec{x}},{\varvec{x'}})\), where
here s is the proper time, \(\sigma ({\varvec{x}},{\varvec{x}}')\) a world function defined as one half of the square of geodesic distance between points in the metric \(\mathrm {g}_{ij}\) and \(\varDelta ^{1/2}({\varvec{x}},{\varvec{x}}') \equiv \mathrm {g}^{-1/2}({\varvec{x}}) \mathfrak {D}({\varvec{x}},{\varvec{x}}') \mathrm {g}^{-1/2}({\varvec{x}}')\), where \(\mathfrak {D}({\varvec{x}},{\varvec{x}}') = -\det \left( -\sigma _{;\mu \nu '}\right) \) is the van Vleck–Morette determinant. For the computation of the heat kernel of this operator, we need to know \(\varDelta ^{1/2}({\varvec{x}},{\varvec{x}}')\), \(a_0({\varvec{x}},{\varvec{x}}')\), and \(a_1({\varvec{x}},{\varvec{x}}')\) and their derivatives. In particular they include the curvature terms:
here we used the relations
The regularized Green’s function (79), in the original notation, assumes the form
where \(\lambda _{0}\) is the cut-off parameter, and can be expanded as
Derivation of the regularized stress tensor then reduces to the following steps:
-
i)
Compute \(\varDelta ^{1/2}({\varvec{x}},{\varvec{x}}')\), \(a_0({\varvec{x}},{\varvec{x}}')\), and \(a_1({\varvec{x}},{\varvec{x}}')\);
-
ii)
Compute the second partial derivative of the Green’s function \(\partial _{{\varvec{x}}}\partial _{{\varvec{x}}'}{\widehat{G}}_{\lambda _{0}}(\zeta ;{\varvec{x}},{\varvec{x'}})\);
-
iii)
Take the limit \({\varvec{x}}={\varvec{x'}}\);
-
iv)
Integrate over the proper time s and then expand the result in the cut-off \(\lambda _{0}\);
-
v)
Compute \({\widehat{\sigma }}_{ij}(\zeta ;{\varvec{x}})\) by substituting the result to (11).
For the quantities in the limit of coincident points, we introduce notation \([\dots ]\equiv (\dots )|_{{\varvec{x}}={\varvec{x'}}}\). The expressions that we need to compute divergent parts (33) of the Green’s function \({\widehat{G}}_{\lambda _{0}}(\zeta ;{\varvec{x}},{\varvec{x'}})\) are [111]
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Zelnikov, A., Krechetnikov, R. Scarf for Lifshitz. Eur. Phys. J. Plus 136, 755 (2021). https://doi.org/10.1140/epjp/s13360-021-01714-3
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DOI: https://doi.org/10.1140/epjp/s13360-021-01714-3