Surface thermodynamics, surface stress, equations at surfaces and triple lines for deformable bodies
Juan Olives (CINaM)

TL;DR
This paper develops a comprehensive thermodynamic and mechanical framework for deformable surfaces, introducing new definitions and equations that extend classical theories to include surface stress, triple line equilibrium, and modifications to Young's law.
Contribution
It refines Gibbs' approach by defining surface stress and deriving new thermodynamic and mechanical equations for deformable bodies, including triple line equilibrium conditions.
Findings
New definition of surface stress for deformable bodies
Generalized surface equilibrium equations including surface stress
Modified Young's equation at triple contact lines
Abstract
The thermodynamics and mechanics of the surface of a deformable body are studied here, following and refining the general approach of Gibbs. It is first shown that the 'local' thermodynamic variables of the state of the surface are only the temperature, the chemical potentials and the surface strain tensor (true thermodynamic variables, for a viscoelastic solid or a viscous fluid). A new definition of the surface stress is given and the corresponding surface thermodynamics equations are presented. The mechanical equilibrium equation at the surface is then obtained. It involves the surface stress and is similar to the Cauchy equation for the volume. Its normal component is a generalization of the Laplace equation. At a (body-fluid-fluid) triple contact line, two equations are obtained, which represent: (i) the equilibrium of the forces (surface stresses) for a triple line fixed on the…
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Surface thermodynamics, surface stress, equations at surfaces and triple lines for deformable bodies
**Juan Olives
CINaM-CNRS, Campus de Luminy, case 913, 13288 Marseille cedex 9, France
E-mail: [email protected]** Associated to Aix-Marseille Université.
Abstract
The thermodynamics and mechanics of the surface of a deformable body are studied here, following and refining the general approach of Gibbs. It is first shown that the ‘local’ thermodynamic variables of the state of the surface are only the temperature, the chemical potentials and the surface strain tensor (true thermodynamic variables, for a viscoelastic solid or a viscous fluid). A new definition of the surface stress is given and the corresponding surface thermodynamics equations are presented. The mechanical equilibrium equation at the surface is then obtained. It involves the surface stress and is similar to the Cauchy equation for the volume. Its normal component is a generalization of the Laplace equation. At a (body–fluid–fluid) triple contact line, two equations are obtained, which represent: (i) the equilibrium of the forces (surface stresses) for a triple line fixed on the body; (ii) the equilibrium relative to the motion of the line with respect to the body. This last equation leads to a strong modification of Young’s classical capillary equation.
1 Introduction
Thermodynamic, chemical and mechanical properties of the surfaces of deformable bodies, with various applications, e.g., on nanostructures, thin films, adhesions or coating, have been continually investigated, from the early work of Gibbs [1] until recent mechanical [2, 6] or thermodynamic [3, 4, 5, 7, 8, 9] approaches. However, some basic questions, such as the exact determination of the thermodynamic variables of state of the surface, still persist, as shown, e.g., in the recent expression of the work of deformation of the surface [3, 8]. This shows that there is a real need for a rigorous and general thermodynamic approach, in order to determine the thermodynamic variables of state and to obtain the corresponding equations of surface thermodynamics and mechanics. Another problem arises at a (body–fluid–fluid) triple contact line, where the classical elastic theory predicts a singularity of the deformation (namely, an infinite displacement). Generally, authors have assumed some finite thickness of the fluid–fluid interface [10, 11], only considered what occurs outside some neighbourhood of this line [12, 13], or proposed a new force derived from the volume stresses of the solid [14]. Nevertheless, the validity of Young’s classical capillary equation remains problematic and the equilibrium equations at the triple line are in fact completely unknown.
In this paper, the general thermodynamic approach of Gibbs is applied and refined, leading to (i) the determination of the ‘local’ thermodynamic variables of state of the surface, (ii) a new definition of the surface stress, (iii) the surface thermodynamics equations, (iv) the equilibrium equations at the surfaces and (v) the equilibrium equations at the triple lines, which imply a strong modification of Young’s equation (as in [4, 5]).
2 Thermodynamic equilibrium conditions
Let us consider a general deformable body in contact with various immiscible fluids , ,… (figure 1).
No mass exchange is assumed between the body and the fluids, but there may be mass exchanges between all the fluids and the body–fluid (, ,…) and fluid–fluid (,…) surfaces. For simplicity’s sake, we suppose that the body consists of a substance c, the fluids and the fluid–fluid surfaces are composed of the substances 1, 2,…, , with all these components c, 1, 2,…, being independent. We first recall Gibbs’s definition of dividing surfaces, and then define the corresponding ‘ideal’ states and ‘ideal’ transformations.
2.1 Dividing surfaces, ideal states and ideal transformations
In the actual state, a body–fluid interface may be considered as a heterogeneous thin film across which the physical quantities may vary rapidly from their values in the homogeneous body to their values in the homogeneous fluid (‘homogeneous’ here means ‘with slow and continuous variations of the physical properties’). Following Gibbs [1], this actual state is replaced by an ideal state in which the body–fluid interface is replaced by a mathematical dividing surface (without thickness), the body and its physical properties being extrapolated (from their values in the homogeneous body) up to this dividing surface, and the same being made for the fluid on the other side of this surface. For any extensive physical quantity, the surface value of this quantity is then defined as the excess of this physical quantity in the actual state over that of the two homogeneous phases in the ideal state. It is expressed per unit area of the dividing surface, and its value depends on the exact position of this surface, which is arbitrary within (or very close to) the actual interface film. In the present paper, the position of the dividing surface is defined so that the surface mass density of the substance c of the body vanishes. Thus, the body–fluid dividing surfaces only contain (as mass excesses) the substances 1, 2,…, , as in the fluids and the fluid–fluid surfaces. In addition, for each component (= 1, 2,…, ), all the fluid regions and the body–fluid and fluid–fluid surfaces which contain are supposed to be connected. We also assume that, in the actual interface film, the physical quantities present slow and continuous variations (as those occurring in the homogeneous body or fluid) along the directions parallel to the interface (in contrast to the possible rapid variations of these quantities along the normal to the interface).
Let us now consider two arbitrary states of the body , e.g., in contact with the fluid , and call ‘initial’ and ‘final’ these two states. In the actual initial state, the body is homogeneous up to a surface , beyond which the interface film takes place (see figure 2).
Note that a precise definition of is not necessary; in fact, we only need that the body is homogeneous up to and that this surface is close to the interface. On , the volume mass density of the substance c of the body has some value . Then, crossing the interface film, varies rapidly, and finally vanishes in the homogeneous fluid region. We denote the surface such that is generally between and , and beyond (fluid side). The dividing surface, as defined above (no excess of mass of the substance c), is denoted . In a similar way, the surfaces , and are defined in the final state. Between the initial and final states, there is an actual transformation , defined in the initial state of the body up to , which maps the position of a material point of the body in the actual initial state, to its position in the actual final state. Clearly, . In addition, and may be chosen so that . Indeed, such a choice for is justified if the surface is not situated in the interface film region (in the final state). This last condition can always be satisfied, by choosing—if necessary—a surface slightly separated from the interface film (in the initial state).
If and are two points very close to each other (i.e., at a small angle from the normal to ), we assume that and will also remain very close to each other. If and are two other such points (thus, ; this equality and the other ones which follow, have to be considered as good approximations, when the thickness of the interface film is very small), this implies that . By taking infinitesimal vectors , it means that (restrictions to P of the linear mappings ), where is the plane tangent to the interface. More generally, we assume that remains unchanged when crosses the interface (from to ).
If the actual initial state is replaced by the ideal one, with respect to the dividing surface , an ideal transformation may then be defined in the (ideal initial state of the) body up to , in the following way: it coincides with in the homogeneous part of the body, up to , and its derivative (linear mapping) in the region between and is extrapolated from the value of the derivative in the homogeneous body. Three assertions will now be proved.
- The surface is generally not the image of by the actual transformation . This may be shown with the following simple example. Let the interface be plane, the normal axis, and the respective positions of and , and a linear decreasing function of , with values at and 0 at , i.e. with , which leads to the position of . Let the actual transformation be a simple compression along the axis, such that linearly decreases from the value 1 at to the small value at (i.e. ), and then remains constant () for . Under this transformation, the volume mass density in the actual final state will be
[TABLE]
Since is constant for , the dividing surface in the final state will be situated at such that , i.e. very close to 1. The surface being situated at , this shows that cannot be the image of by .
- The surface is the image of by the ideal transformation . In order to prove this assertion, let us consider, in the actual initial state, , (with at a small angle from the normal to ), a small parallelepiped with edge , limited by and , and a similar parallelepiped limited by and (figure 3).
In the final state, is transformed into , which is not a parallelepiped, since its (curved) ‘edge’ suffered an heterogeneous deformation. Nevertheless, all the sections of by the planes parallel to represent the same parallelogram (up to a translation), since remains unchanged when moves from to (as noted above; ). Let us consider the straight line (with ) tangent to the curved edge at , and the parallelepiped with edge , having the same face on as (see figure 3). By the definition of , is constant and equal to , between and , in , which implies that is a parallelepiped which, like , rests on the edge and has the same face on as .
By the definition of (no excess of mass of the constituent c), the mass of c contained in (in the actual state) is equal to the mass of c contained in in the ideal state (i.e., if is filled with only the substance c, with a constant density , equal to ). Note that this property does not depend on the choice of the parallelepiped (i.e., its face on and the orientation of ).
Under the transformation , the mass of c contained in is equal to that contained in (for the actual states). In addition, if is ‘cut up’ into very thin slices parallel to , then, by appropriate sliding of these slices (with respect to each other), we can obtain the parallelepiped , which shows that the mass of c contained in is equal to that contained in (for the actual state).
Now, let us transport by the substance c contained in in the ideal state: will thus contain the same mass of c as that contained in (in the ideal state). In addition, the density will be constant in , and equal to (since and are constant in , and respectively equal to and ). The various preceding mass equalities finally lead to: the mass of c contained in (filled with only the substance c, with a constant density , equal to ) is equal to that contained in in the actual state. This exactly means that the parallelepiped is limited by the surface (defined by: no excess of mass of the constituent c), i.e., that . We may also say that the mass density in (resulting from the transport) is that of the ideal final state (as defined at the beginning of the section).
- The volume mass density of the substance c of the body in the ideal final state results from the transport by the ideal transformation of the mass density of this substance in the ideal initial state. This is a consequence of the previous last conclusion.
Let us now consider a third arbitrary state of the body , called ‘reference state’, and define, as above for the initial and final states, the corresponding surfaces , and (subscript 0 for the reference state). The actual and ideal transformations are respectively denoted and , between the reference and initial states, and and , between the reference and final states. We have the new assertion:
- The ideal transformation between the reference and final states is equal to the ideal transformation between the reference and initial states composed with the ideal transformation between the initial and final states: . Indeed, let be situated between and , be very close to , and denote , , , . Then, , hence , i.e. .
2.2 Thermodynamic equilibrium conditions
We consider that the system is closed and bounded by a closed surface , and write the Gibbs equilibrium criterion
[TABLE]
( is the internal energy and the work of the external forces), for all variations of the system such that the entropy and the masses of the various components ( = 1,…, ) are constant. If the bounding surface , the points of the body which belong to this surface, and the lines in which the fluid–fluid surfaces meet this surface, are all fixed, then is reduced to the work of the forces of gravity (there is no work of the fluid pressures on , since they are normal to and the fluid displacements are tangent to ), and the criterion may be written
[TABLE]
where is the potential energy of gravity. Note that, in this variation, we exclude the formation of new fluids or new (body–fluid or fluid–fluid) surfaces.
We thus have two states of the system: the present state and the (arbitrary) varied state, i.e., after the variation . Let us respectively call these two states ‘initial’ and ‘final’ and then apply the definitions and results of the preceding section. We may thus write the internal energy of the actual present state as
[TABLE]
where refers to an element of volume or surface, and are the energies of the homogeneous phases in the ideal state (i.e., extrapolated up to the dividing surfaces), and and the excesses of the energy for the corresponding dividing surfaces ( as defined by Gibbs; as defined above). Note that, in the present approach, we only take into account the volume and the surface effects (as a first approximation, intrinsic line effects, such as line energy, line tension,… are here neglected). Similarly, for the varied state,
[TABLE]
with respect to the dividing surfaces of this state, i.e., (as defined by Gibbs) and (as defined above). In the difference , the first term is
[TABLE]
In the last integral, we may consider that the body , in its ideal present state (up to ), has been divided into infinitesimal elements of volume (of energy ). The assertions 2 and 3 of the preceding section show that the body , in its ideal varied state (up to ), may be exactly divided into the elements which are the images of the preceding ones by the ideal transformation (from the ideal present state to the ideal varied state). If refers to an element of the ideal present state and its corresponding image by , we may then write
[TABLE]
and since each element is a closed ‘system’ (with respect to the geometrical transformation ), for any infinitesimal reversible thermodynamic transformation :
[TABLE]
(in the ideal states; refers to ; all the quantities are extrapolated up to the dividing surfaces), where is the temperature, the volume, the stress tensor at equilibrium and the strain tensor corresponding to . According to assertion 4 of the preceding section, this may also be written in the Lagrangian representation, with respect to a given reference state of the body:
[TABLE]
where is the volume in the reference state, the Piola–Kirchhoff stress tensor (relative to the reference state) at equilibrium, and the Green–Lagrange strain tensor (relative to the reference state, i.e., associated to ; ).
For the and terms in , the expressions of Gibbs are used:
[TABLE]
(in the ideal states; in the integrals on , the quantities are extrapolated up to the dividing surfaces; the integrals refer to the dividing surfaces, , and being surface excesses and an element of area), where is the fluid pressure, the fluid–fluid surface tension and the chemical potential per unit mass of component . Note that, in this case, each element of volume or surface is treated as an open ‘system’.
The above arguments may similarly be applied to the potential energy of gravity:
[TABLE]
where and correspond to the homogeneous phases in the ideal state (i.e., extrapolated up to the dividing surfaces: , ), and are the excess quantities for these dividing surfaces, is the gravity field (supposed constant), the height and the mass. In the and integrals, represents the surface excess for the dividing surfaces (the excess of is equal to , since, crossing the interface film, remains almost constant whereas the volume mass density varies rapidly). Then,
[TABLE]
each element being a closed ‘system’ with respect to the transformation ( refers to ), and
[TABLE]
(in the ideal states; the elements of volume or surface are here treated as open ‘systems’).
Finally, the Gibbs equilibrium criterion may be written
[TABLE]
and the associated conditions of constant and are
[TABLE]
Note that these expressions, and all the following ones, refer to the ideal states, which means that all the quantities of the volume integrals are extrapolated up to the dividing surfaces (and, in the integrals, refers to ), and the surface integrals refer to these dividing surfaces (, , and being surface excesses).
From this point, we may follow the proof given in [4] (extension of the approach of Gibbs [1]), here applied to the case of a general deformable body, which first shows that the equilibrium (2)–(4) of the system is equivalent to
(i) the thermal and chemical equilibrium equations:
[TABLE]
(ii) the mechanical equilibrium equations concerning only the system of the fluids:
in each fluid
[TABLE]
in each surface
[TABLE]
in each triple line
[TABLE]
( is the mass per unit volume, the mass per unit area (surface excess); refers to , to ; and are the principal curvature radii of the surface, considered positive when the centres are on the side; is the angle between the O axis and the normal to the surface, oriented from to ; at the line, and for each surface, is the unit vector normal to the line, tangent to the surface, and oriented from the line to the interior of ; in (7) and (8), , , and only depend on ; all these equations (5)–(10) were written by Gibbs [1]) and
(iii) the following new mechanical equilibrium condition (of variational form) which concerns only the body, the body–fluid surfaces and the body–fluid–fluid lines:
[TABLE]
where is the (constant) gravity vector field, the displacement of a material point of the body (by , up to the dividing surfaces ), the unit vector normal to the surface, oriented from to ( also represents the normal displacement of the surface, from to , positively measured from to ), the unit vector normal to the line, tangent to the surface, and oriented from the line to the interior of , the length of a line element, and the (vector) displacement of the line, perpendicular to the line (figure 4).
Note that (7) and (8) are consequences of (5) and (6), since and are functions of and which satisfy [1]
[TABLE]
(the subscripts and respectively denote the volume density and the surface density).
The terms of the last line of (11) may be calculated in the (ideal) reference state of the body (i.e., on ). With the help of the above assertions 2 (, and ) and 4 (), we may write, e.g., for the first term
[TABLE]
where the subscript 0 is used for the reference state, , is the variation at a fixed point of , and the (scalar) displacement of the line, measured in the reference state, perpendicular to that line in the reference state, and positively considered from to (figure 4). Then,
[TABLE]
The two last terms of the last line of (11) only depend on the variations of the masses and the geometrical positions. In particular, they do not depend on (or ), and we may thus use, e.g., (i.e., ) to calculate these terms:
[TABLE]
By applying the same method as above (with instead of ), and according to , we finally obtain for the last line of (11):
[TABLE]
where is the excess of grand potential (on , for ), per unit area in the reference state (on ). The equilibrium condition (11) may then be written as
[TABLE]
in which is an arbitrary variation such that, on the surface which bounds the system, the points of the body and the points of the body–fluid–fluid lines remain fixed. Note that is the displacement by (up to the dividing surfaces ).
3 Surface thermodynamics and surface stress
Now, let us take a bounding surface which only encloses one fluid and the body . The surface enclosed in is bounded by the closed curve . The above equilibrium condition (13) takes the form:
[TABLE]
for any variation such that the points of the body which belong to remain fixed (by the actual transformation ; then, also, by the ideal transformation , since is the extrapolation of , between and ); and respectively denote the parts of the body and the surface enclosed in . Let us use the usual Eulerian representations of stress () and strain (, where ), and Green’s formula:
[TABLE]
The preceding equilibrium condition is then equivalent to
(i) the mechanical equilibrium equations of the body
[TABLE]
(obtained by fixing the points of the surface, and their thermodynamic state, in (14); note that, with the presence of volume couples of forces, of moment ( written as an antisymmetric tensor), the new term would appear in (14), and (17) would become = 0; in our case, , and and are symmetric) and
(ii) the following mechanical equilibrium condition for :
[TABLE]
for any variation such that the points of the body which belong to remain fixed.
From this condition, we are now able to determine the set of the ‘local’ (see below, after (21)) thermodynamic variables of state of the surface. The expression clearly depends on the variations of the thermodynamic variables of state of , for a given point (). What is shown in the preceding condition (18) is that , and then also at a given point , only depend on the vector field defined on the surface, i.e., on the variation of only one geometrical variable: the field of the positions of the points of the surface. Since a thermodynamic variable of state is geometrically local, this geometrical variable must be, in fact, at the point ( is the covariant differential of , on the surface ; is the restriction of to ). Obviously, cannot be a variable of state, because the thermodynamic state of the surface may remain unchanged under any translation, , whereas is changed into . The variable is then reduced to , i.e., at the first order, . Let be an isometry of onto , such that is a direct linear mapping on , and use the classical decomposition , where is a positive symmetric tensor and a rotation in . With respect to another isometry , such that is direct, the decomposition would be , with and , which shows that the symmetric tensor only depends on (and not on ). We thus have the unique decomposition , where is an isometry. In addition, under a rotation (of the whole space), , is changed into ( being the associated vectorial rotation), but the symmetric tensor remains unchanged, since , with . Since the thermodynamic state of the surface may remain unchanged under such an arbitrary rotation, whereas is changed into , but remains unchanged, we may conclude that the true geometrical variable of state is . Other variables equivalent to are (because is symmetric and positive) or the (Lagrangian) surface strain ( = identity operator), all these tensors being associated to the deformation of the surface (change of the scalar product), e.g., for :
[TABLE]
for arbitrary vectors . In conclusion, we may take (at ) as the geometrical variable of state and, as mentioned above (as a consequence of (18)), is then proportional to its variation :
[TABLE]
The ‘coefficient’ of will be called the (Lagrangian) surface stress tensor at equilibrium, and the work of deformation of the surface, expressed per unit area in the reference state. Note that (20) actually defines the symmetric part of the tensor , because is symmetric. Here, we consider that the surface stress (, and its Eulerian form , below) is symmetric, but this may not be always the case (e.g., in the presence of surface couples of forces, acting on the interface; as for the case of volume stress: see the comment after (17)). In an equivalent form,
[TABLE]
Finally, this expression gives us the set of the ‘local’ thermodynamic variables of state of the surface: , and . ‘Local’ here means: for the subset of the thermodynamic states which can be reached by reversible transformations, from a given thermodynamic state. In such a subset of thermodynamic states, the surface stress is then the partial derivative of with respect to the surface strain :
[TABLE]
(components , with arbitrary coordinates on the surface; the two variables and —although equal—being formally distinguished in (22)).
If the above subset of thermodynamic states of the surface is equal to the set of all thermodynamic states, then the above ‘local’ variables are the true (‘global’) thermodynamic variables of state of the surface. This occurs if any thermodynamic state can be reached by a reversible transformation from any other thermodynamic state. We know that such a property is valid for some volume bodies, such as viscoelastic solids or viscous fluids, for which any transformation becomes reversible when achieved at vanishing speed. We may assume that the surface of such bodies has the same property, in which case the above variables are the true thermodynamic variables of state of the surface.
From the definition of and (20), we may also write
[TABLE]
which gives another equivalent set of ‘local’ thermodynamic variables of state: , and . The surface stress here appears as the partial derivative of with respect to the surface strain:
[TABLE]
(a Shuttleworth type equation [15]; its Eulerian version is expressed in (29), below).
As above, for the usual volume stress and strain tensors, we have a similar Eulerian representation for the surface stress and strain tensors ( and , respectively; , for ), and the work of deformation of the surface:
[TABLE]
Equation (21) may also be written, with fixed:
[TABLE]
(, etc; compare with (1) for a fluid–fluid surface, where ; is the identity operator on ) or
[TABLE]
(since , etc and ); and with variable:
[TABLE]
in which the surface stress is associated with the deformation of a given element , and the surface grand potential with the creation of a new element of surface . The Eulerian form of (23) is, with fixed:
[TABLE]
since and (compare with (12) for a fluid–fluid surface).
Note that, although the three variables are independent, it may occur, in some particular cases, that fewer variables are necessary. For example, if we a priori know that the tensor is isotropic (as for the isotropic pressure in a fluid, or the surface tension in a fluid–fluid surface), i.e., (eigenvalue also denoted ), then the expression (25) is reduced to . In this case, we only need one variable, namely .
Moreover, note that the expression (25) obtained for the work of deformation of the surface, differs from that proposed in [3, 8]:
[TABLE]
where and are the volume stress and strain tensors, the subscripts and respectively refer to the tangential and normal components, and the symbol indicates an excess quantity on the surface. Since , the comparison of the two expressions shows that the surface stress here defined differs from its usual definition as the excess of tangential stress . There are, in fact, too many variables in (30): 3 variables + 3 variables . The above thermodynamic approach showed that there are only 3 geometrical (‘local’) variables of state for the surface, namely the 3 components of (or ). Note also that the continuity of the normal stress , when crossing the interface, is assumed in (30): however, the next section will show that there is generally a discontinuity of the normal stress, due to the presence of surface stress and gravity.
4 Equations at surfaces and triple lines
4.1 Surfaces
With (20) and (25), the mechanical equilibrium condition (18) for the surface takes the form:
[TABLE]
for any variation such that on . By application of Green’s formula to the last term, this leads to the mechanical equilibrium equation of the surface:
[TABLE]
With Cartesian coordinates for the whole space and arbitrary curvilinear coordinates for the surface (for , and must be clearly distinguished), it may be written
[TABLE]
where refer to space coordinates, to surface coordinates, summation is performed on repeated indices, and are the Christoffel’s symbols. A similar equation was obtained in a purely mechanical approach [2]. Note the similarity of this equation (32) with the Cauchy volume one (16).
Note also that (32) may easily be generalized at the surface between two deformable bodies ( and ):
[TABLE]
where is the stress tensor in , and is oriented from to .
Equation (32) may be separated into tangential and normal components. The tangential component is
[TABLE]
where the subscript indicates the vector component tangent to the surface and is the surface divergence:
[TABLE]
The normal component of (32) is
[TABLE]
where , and is the ‘fundamental form’
[TABLE]
the eigenvalues of which are the principal curvatures, and , of the surface (a curvature being considered positive, when its center is on the side of ). This equation (37) generalizes the classical Laplace equation (9) for a fluid–fluid surface. Indeed, represents the difference of the normal pressures and, for isotropic surface stresses, (eigenvalue also denoted ).
Equation (32) also shows that there is a discontinuity of the normal stress at the interface, the jump of which, , is due both to surface stress (term , with components and ) and to gravity (term ).
4.2 Triple lines
Let us now consider a bounding surface which encloses two fluids ( and ) and the body , and apply the general equilibrium condition (13), using the above expressions (15), (20) and (25). Note that Green’s formula applied to the work of deformation of the surface leads to the new term at the triple line, where and is the unit vector normal to the line, tangent to the surface, and oriented from the line to the interior of (here, , and refer to the side). With the help of the equilibrium equations (16)–(17) for , and (32) for and , the general equilibrium condition is then reduced to:
[TABLE]
for any variation such that the two points of the line which belong to remain fixed (both in space, and as points of the body).
The transformation restricted to the body–fluid surface, between the (ideal) reference and present states of the body, is continuous, but its differential is not continuous at the triple line, since the plane tangent to the surface and the plane tangent to the surface (at the triple line) are different (figure 5).
Its variation will also be discontinuous at the triple line. From the side point of view, and if , the displacement of the line would be equal to . On the other hand, if on , and , this displacement would be ( belongs to ; is here considered as a vector). In the general case, the displacement of the triple line will then be
[TABLE]
(expression from the side, in the second line; see figure 5; the component of this normal to is the of (39), but this has no effect on ).
From (40) and the Eulerian form of the last term of (39) (; is the excess of grand potential on the surface, per unit area in the present state), the equilibrium condition (39) takes the form
[TABLE]
which leads to two equilibrium equations at the triple line:
[TABLE]
(by considering the triple line as fixed with respect to the body, i.e., , hence ) and
[TABLE]
Equation (42) represents the equilibrium of the forces acting on the triple line, considered as fixed on the body (), whereas (43) expresses the equilibrium relative to the motion of the triple line with respect to the body (). A similar situation was found in the case of the thin plate [4, 5]. Note that it was proposed [14] that the equilibrium at the triple line involves not only the (, and ) surface forces, but also a force which originates from the volume stresses in the body and the singularity at the triple line. The obtained equation (42) shows that there is no body volume contribution, and that the equilibrium only involves the forces exerted by the three surfaces (, and ) on the triple line. This equation shows that surface stresses are forces acting on a line fixed on the body, and may easily be generalized to a line of contact between three deformable bodies (, and ):
[TABLE]
(equilibrium of the forces acting on the triple line, considered as fixed with respect to the three bodies).
Let be a unit vector tangent to the triple line, , the components of in the basis , and use similar notations for with the basis . Equation (42) may then be separated into its normal and tangential components (with respect to the line):
[TABLE]
Equation (43) may also be viewed as the expression of the equilibrium (41), when and : this means that the triple line is fixed in space, but moves with respect to the body; in other words, the body moves with respect to the triple line, which remains fixed in space (the body then also moves with respect to its singularity, attached to the triple line). Since implies that and , (43) may then be written as
[TABLE]
This equilibrium equation has a clear physical meaning: it states that the variation of surface energy (grand potential) due to the motion of the triple line with respect to the body (e.g., increase in bf area and decrease in bf’ area) is equal to the work of the surface stresses acting on the triple line (although the triple line does not move in space, the points of the body situated at this line move by in the side, and by in the side).
From the expressions (40) of and , equation (43):
[TABLE]
may be written as
[TABLE]
(in this last equation, the covariant forms of the tensors and are used, and denotes the covariant metric tensors on and , respectively).
In the reference state, let be the unit vector normal to the line, tangent to the or surface (in the reference state, there is no singularity at the triple line, and the planes tangent to and are identical), and oriented from to , and the unit vector tangent to , with the same orientation as . With the notations
[TABLE]
(, , ), (48) or (49) is equivalent to the two equations
[TABLE]
The second equation is the same as (46) (which shows that (48) does not depend on the component of along ), and the first one may be written as
[TABLE]
i.e.,
[TABLE]
Another form of this equation is obtained after multiplication by :
[TABLE]
since
[TABLE]
Let us show that the preceding equations do not depend on the reference state. Since
[TABLE]
where
[TABLE]
is the ‘relative’ differential of the transformation, on the side with respect to the side (this concept was defined in [16]), the above equation (48) takes the form
[TABLE]
(with the covariant forms of , and , as above for (49)), which does not depend on the reference state. Indeed, if the previous reference state 0 (indicated by the subscript 0) is replaced by a new reference state 1 (subscript 1), such that is continuous at the triple line, then
[TABLE]
(at the triple line), hence
[TABLE]
which shows that does not depend on the reference state. Using the bases , and , (55) may be written in the matrix form:
[TABLE]
which shows that
[TABLE]
and leads to another form of (56) or (53):
[TABLE]
4.3 Modified Young’s equation
If the body is a rigid solid, (42) cannot be obtained from (41), because it is not possible to move the triple line in the space () while this line remains fixed to the solid (). In fact, (41) takes the form
[TABLE]
(, since ), and leads to
[TABLE]
(since and ; is the angle of contact measured in the fluid ), which is Young’s classical equation. This shows that Young’s classical equation only refers to the surface energies (and not to the surface stresses ) and is related to the displacement of the triple line with respect to the solid.
Then, in the present case of a deformable body, (42) cannot be compared with Young’s classical equation (since it refers to the surface stresses and the triple line fixed on the body). The present generalization of Young’s equation is in fact related to (43) (or (48), (49), (53), (56), (57)), because this equation contains the surface energies and is related to the displacement of the triple line with respect to the body. In order to eliminate the surface stresses in (57), we use the projections of (45) onto and :
[TABLE]
(, and are the three angles of contact, respectively measured in , and ), which give
[TABLE]
(using ). By introducing these expressions in (57), we obtain the following modified form of Young’s equation:
[TABLE]
or
[TABLE]
(using ). A modified form of Young’s equation was previously presented in the case of the thin plate [4, 5]. Obviously, if and (or if and ), this equation takes the form
[TABLE]
which leads to the Young’s classical equation (59) when tends to .
5 Conclusions
This paper deals with the thermodynamic (and mechanical) equilibrium of a deformable body in contact with fluids, specially at the surfaces and the triple contact lines of the body. We have applied the ‘dividing surface’ Gibbs approach [1], here refined with a new concept: the ‘ideal transformation’ between two ‘ideal’ states, which defines the ‘ideal’ displacement of the material points, within the interface film, up to the dividing surface. The approach is based on a careful application of the general thermodynamic equilibrium criterion of Gibbs. The classical thermal and chemical equilibrium equations (5), (6), and the mechanical equations concerning the fluids (7)–(10) and the (volume part of the) body (16), (17) are first separated. We thus obtain a new equilibrium condition which only refers to the surfaces and the triple contact lines of the body. As a first consequence of this condition, it is shown that the ‘local’ thermodynamic variables of state of the surface are only the temperature, the chemical potentials and the surface strain tensor (these are the true thermodynamic variables of state, if, e.g., the body is a viscoelastic solid or a viscous fluid). This leads to a new definition of the surface stress tensor (which differs from the usual definition as the excess of tangential stress) and to the corresponding surface thermodynamic equations (21)–(29), with the simple expression (25) for the work of deformation of the surface (which differs from the expression (30) of [3, 8]). The mechanical equilibrium equation of the surface (32) is then obtained. This equation, similar to the classical Cauchy one for the volume, may be separated into tangential (35) and normal (37) components. This normal component is in fact a generalization of the classical Laplace equation for a fluid–fluid surface. Finally, at the (body–fluid–fluid) triple contact lines, we show that there are two mechanical equilibrium equations. The first one (42) (or (45), (46)) represents the equilibrium of the forces which act on the triple line, considered as a line fixed on the body (these forces are the surface stresses; there is no contribution from the volume stresses of the body, as proposed in [14]). The very original second equation (48) (or (49), (53), (56), (57)) expresses the equilibrium relative to the motion of the triple line with respect to the body, while the line remains fixed in space: i.e., the body moves with respect to the triple line (and with respect to the singularity of the body, attached to this line), which remains fixed in space. This equation involves the surface energies, the surface stresses, and the ‘relative deformation’ [16] between the two sides of the body surface separated by the triple line. It leads to a strong modification of the Young’s classical capillary equation, as shown in the equations (62) or (63). A similar situation was found in the case of the thin plate [4, 5]. An approximate solution of these equations, for an elastic solid, will be given in a future paper.
Acknowledgments
We acknowledge financial support from CINaM-CNRS and ANR-08-NANO-036.
The reference list from the paper itself. Each links out to its DOI / PubMed record.
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