Scalar–tensor theory

In theoretical physics, a scalar–tensor theory is a theory that includes both a scalar field and a tensor field to represent a certain interaction. For example, the Brans–Dicke theory of gravitation uses both a scalar field and a tensor field to mediate the gravitational interaction.

Tensor fields and field theory

Modern physics tries to derive all physical theories from as few principles as possible. In this way, Newtonian mechanics as well as quantum mechanics are derived from Hamilton's principle of least action. In this approach, the behavior of a system is not described via forces, but by functions which describe the energy of the system. Most important are the energetic quantities known as the Hamilton function and the Lagrangian function. Their derivatives in space are known as Hamilton density and Lagrange density. Going to these quantities leads to the field theories.

Modern physics uses field theories to explain reality. These fields can be scalar, vectorial or tensorial. For them:

Scalars are numbers, quantities of the form f(x), like the temperature. Vectors are more general and show a direction. In them, every component of the direction is a scalar. Tensors (degree 2) are a wider generalization, the best known example of which are matrices (that can give equation systems). Higher order tensors are found for example in the deformation theory and in General Relativity.

Gravity as field theory

In physics, forces (as vectorial quantities) are given as the derivative (gradient) of scalar quantities named potentials. In classical physics before Einstein, gravitation was given in the same way, as consequence of a gravitational force (vectorial), given through a scalar potential field, dependent of the mass of the particles. Thus, Newtonian gravity is called a scalar theory. The gravitational force is dependent of the distance r of the massive objects to each other (more exactly, their centre of mass). Mass is a parameter and space and time are unchangeable.

Mathematical formulation

An action of such a gravitational scalar–tensor theory can be written as follows:

 S = \frac{1}{c} \int {d^4 x \sqrt{-g} \frac{1}{2 \mu}} \times \left[ \Phi  R-\frac{\omega(\Phi)}{\Phi} (\partial_\sigma \Phi)^2-V(\Phi)+ 2 \mu~\mathcal{L}_m (g_{\mu \nu}, \Psi)  \right],

where g is the metric determinant, R is the Ricci scalar constructed from the metric g_{\mu \nu}, \mu is a coupling constant with the dimensions L^{-1} M^{-1}T^2, V(\Phi) is the scalar-field potential, \mathcal{L}_m is the material Lagrangian and \Psi represents the non-gravitational fields. Here, the Brans–Dicke parameter \omega has been generalized to a function. Although \mu is often written as being 8 \pi G / c^4, one has to keep in mind that the fundamental constant G there, is not the constant of gravitation that can be measured with, for instance, Cavendish type experiments. Indeed, the empirical gravitational constant is generally no longer a constant in scalar–tensor theories, but a function of the scalar field \Phi. The metric and scalar-field equations respectively write:

R_{\mu \nu}-\frac{1}{2}g_{\mu \nu}R= \frac{\mu}{\Phi}T_{\mu
\nu}+ \frac{1}{\Phi} [\nabla_\mu \nabla_\nu -g_{\mu \nu}\Box]\Phi 
+\frac{\omega(\Phi)}{\Phi^2}(\partial_\mu \Phi \partial_\nu \Phi
- \frac{1}{2}g_{\mu \nu}(\partial_\alpha \Phi)^2)-g_{\mu \nu} \frac{V(\Phi)}{2 \Phi} ,

and

\frac{2\omega(\Phi)+3}{\Phi}\Box \Phi=  \frac{\mu}{\Phi} T   - \frac{\omega'(\Phi)}{\Phi} (\partial_\sigma \Phi)^2 + V'(\Phi) - 2 \frac{V(\Phi)}{\Phi} .

Also, the theory satisfies the following conservation equation, implying that test-particles follow space-time geodesics such as in general relativity:

\nabla_\sigma T^{\mu \sigma} = 0,

where  T^{\mu \sigma} is the stress-energy tensor defined as

T_{\mu \nu}=-\frac{2}{\sqrt{-g}} \frac{\delta(\sqrt{-g}\mathcal{L}_m)}{\delta g^{\mu \nu}}.

The Newtonian approximation of the theory

Developing perturbatively the theory defined by the previous action around a Minkowskian background, and assuming non-relativistic gravitational sources, the first order gives the Newtonian approximation of the theory. In this approximation, and for a theory without potential, the metric writes

g_{00}=-1+ 2 \frac{U}{c^2}+\mathcal{O}(c^{-3}),~ g_{0i}=\mathcal{O}(c^{-2}),~ g_{ij}=\delta_{ij}+\mathcal{O}(c^{-1}),

with U satisfying the following usual Poisson equation at the lowest order of the approximation:

\triangle U = 8 \pi G_\mathrm{eff}~ \rho+\mathcal{O}(c^{-1}),

where  \rho is the density of the gravitational source and  G_\mathrm{eff}= \frac{2 \omega_0 +4}{2 \omega_0 +3} \frac{G}{\Phi_0} (the subscript _0 indicates that the corresponding value is taken at present cosmological time and location). Therefore, the empirical gravitational constant is a function of the present value of the scalar-field background  \Phi_0 and therefore theoretically depends on time and location. However until now, no deviation from the constancy of the Newtonian gravitational constant has been measured , implying that the scalar-field background  \Phi_0 is pretty stable over time. Such a stability is not theoretically generally expected but can be theoretically explained by several mechanisms (e.g. ).

The first post-Newtonian approximation of the theory

Developing the theory at the next level leads to the so-called first post-Newtonian order. For a theory without potential and in a system of coordinates respecting the weak isotropy condition (i.e. g_{ij} \propto \delta_{ij}+\mathcal{O}(c^{-3})), the metric takes the following form:

g_{00}=-1+\frac{2 W}{c^2} - \beta \frac{2 W^2}{c^4}+\mathcal{O}(c^{-5})
g_{0i}=-(\gamma+1) \frac{2W_i}{c^3}+\mathcal{O}(c^{-4})
g_{ij}=\delta_{ij} \left(1+\gamma \frac{2 W}{c^2} \right)+\mathcal{O}(c^{-3})

with

\Box W+\frac{1+2\beta -3\gamma }{c^2} W\triangle W+\frac{2}{c^2}(
1+\gamma) \partial_t J =-4\pi G_\mathrm{eff}\Sigma+ \mathcal{O}(c^{-3}) ,
\triangle W_i-\partial x_i J =-4\pi G_\mathrm{eff}\Sigma^i + \mathcal{O}(c^{-1}),

where J is a function depending on the coordinate gauge

J =\partial_t W+\partial_k W_k+\mathcal{O}(c^{-1}).

It corresponds to the remaining diffeomorphism degree of freedom that is not fixed by the weak isotropy condition. The sources are defined as

\Sigma =\frac{1}{c^2} (T^{00}+\gamma T^{kk}), ~~~\Sigma^i =\frac{1}{c} T^{0i},

the so-called post-Newtonian parameters are

\gamma = \frac{\omega_0 +1}{\omega_0 +2}, ~~\beta = 1+\frac{\omega_0^{\prime}}{( 2\omega_0 +3) (2\omega_0+4)^2},

and finally the empirical gravitational constant G_\mathrm{eff} is given by

G_\mathrm{eff}= \frac{2\omega_0+4}{2\omega_0+3}G,

where G is the (true) constant that appears in the coupling constant \mu defined previously.

Observational constraints on the theory

Current observations indicate that \gamma-1=(2.1 \pm 2.3)\times 10^{-5} . It means that \omega_0 > 40 000. Although explaining such a value in the context of the original Brans–Dicke theory is impossible, Damour and Nordtvedt found that the field equations of the general theory often lead to an evolution of the function \omega toward infinity during the evolution of the universe . Hence, according to them, the current high value of the function \omega could be a simple consequence of the evolution of the universe.

The best current constraint on the post-Newtonian parameter \beta comes from Mercury's perihelion shift and is |\beta-1|<3 \times 10^{-3} .

Both constraints show that while the theory is still a potential candidate to replace general relativity, the scalar field must be very weakly coupled in order to explain current observations.

Higher-dimensional relativity and scalar–tensor theories

After the postulation of the General Relativity of Einstein and Hilbert, Theodor Kaluza and Oskar Klein proposed in 1917 a generalization in a 5-dimensional manifold: Kaluza–Klein theory. This theory possesses a 5-dimensional metric (with a compactified and constant 5th metric component, dependent on the gauge potential) and unifies gravitation and electromagnetism, i.e. there is a geometrization of electrodynamics.

This theory was modified in 1955 by P. Jordan in his Projective Relativity theory, in which, following group-theoretical reasonings, Jordan took a functional 5th metric component that lead to a variable gravitational constant G. In his original work, he introduced coupling parameters of the scalar field, to change energy conservation as well, according to the ideas of Dirac.

Following the Conform Equivalence theory, multidimensional theories of gravity are conform equivalent to theories of usual General Relativity in 4 dimensions with an additional scalar field. One case of this is given by Jordan's theory, which, without breaking energy conservation (as it should be valid, following from microwave background radiation being of a black body), is equivalent to the theory of C. Brans and Robert H. Dicke of 1961, so that it is usually spoken about the Brans–Dicke theory. The Brans–Dicke theory follows the idea of modifying Hilbert-Einstein theory to be compatible with Mach's principle. For this, Newton's gravitational constant had to be variable, dependent of the mass distribution in the universe, as a function of a scalar variable, coupled as a field in the Lagrangian. It uses a scalar field of infinite length scale (i.e. long-ranged), so, in the language of Yukawa's theory of nuclear physics, this scalar field is a massless field. This theory becomes Einsteinian for high values for the parameter of the scalar field.

In 1979, R. Wagoner proposed a generalization of scalar–tensor theories using more than one scalar field coupled to the scalar curvature.

JBD theories although not changing the geodesic equation for test particles, change the motion of composite bodies to a more complex one. The coupling of a universal scalar field directly to the gravitational field gives rise to potentially observable effects for the motion of matter configurations to which gravitational energy contributes significantly. This is known as the "Dicke–Nordtvedt" effect, which leads to possible violations of the Strong as well as the Weak Equivalence Principle for extended masses.

JBD-type theories with short-ranged scalar fields use, according to Yukawa's theory, massive scalar fields. The first of this theories was proposed by A. Zee 1979. He proposed a Broken-Symmetric Theory of Gravitation, combining the idea of Brans and Dicke with the one of Symmetry Breakdown, which is essential within the Standard Model SM of elementary particles, where the so-called Symmetry Breakdown leads to mass generation (as a consequence of particles interacting with the Higgs field). Zee proposed the Higgs field of SM as scalar field and so the Higgs field to generate the gravitational constant.

The interaction of the Higgs field with the particles that achieve mass through it is short-ranged (i.e. of Yukawa-type) and gravitational-like (one can get a Poisson equation from it), even within SM, so that Zee's idea was taken 1992 for a scalar–tensor theory with Higgs field as scalar field with Higgs mechanism. There, the massive scalar field couples to the masses, which are at the same time the source of the scalar Higgs field, which generates the mass of the elementary particles through Symmetry Breakdown. For vanishing scalar field, this theories usually go through to standard General Relativity and because of the nature of the massive field, it is possible for such theories that the parameter of the scalar field (the coupling constant) does not have to be as high as in standard JBD theories. Though, it is not clear yet which of these models explains better the phenomenology found in nature nor if such scalar fields are really given or necessary in nature. Nevertheless, JBD theories are used to explain inflation (for massless scalar fields then it is spoken of the inflaton field) after the Big Bang as well as the quintessence. Further, they are an option to explain dynamics usually given through the standard cold dark matter models, as well as MOND, Axions (from Breaking of a Symmetry, too), MACHOS,...

Connection to string theory

A generic prediction of all string theory models is that the spin-2 graviton has a spin-0 partner called "dilaton" . Hence, string theory predicts that the actual theory of gravity is a scalar–tensor theory rather than general relatity. However, the precise form of such a theory is not currently known because one does not have the mathematical tools in order to address the corresponding non-perturbative calculations. Besides, the precise effective 4-dimensional form of the theory is also confronted to the so-called landscape issue.

Other possible scalar–tensor theories

Theories with non-minimal scalar-matter coupling

References

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