In the following subsections, we will present the different measurements used to constrain the SME coefficients. Each subsection contains a brief description of the principle of the experiment, how it can be used to search for Lorentz symmetry violations, what are the current best constraints obtained with such measurements and eventually how it can be improved in the future.
4.1. Atomic Gravimetry
The most sensitive experiments on Earth searching for Lorentz Invariance Violation (LIV) in the minimal SME gravity sector are gravimeter tests. As Earth rotates, the signal recorded in a gravimeter, i.e., the apparent local gravitational acceleration
g of a laboratory test body, would be modulated in the presence of LIV in gravity. This was first noted by Nordtvedt and Will in 1972 [
87] and used soon after with gravimeter data to constrain preferred-frame effects in the PPN formalism [
88,
89] at the level of
.
This test used a superconducting gravimeter, based on a force comparison (the gravitational force is counter-balanced by an electromagnetic force maintaining the test mass at rest). While superconducting gravimeters nowadays reach the best sensitivity on Earth, force comparison gravimeters intrinsically suffer from drifts of their calibration factor (with e.g., aging of the system). Development of other types of gravimeters has evaded this drawback: free fall gravimeters. Monitoring the motion of a freely falling test mass, they provide an absolute measurement of g. State-of-the art free fall gravimeters use light to monitor the mass free fall. Beyond classical gravimeters that drop a corner cube, the development of atom cooling and trapping techniques and atom interferometry has led to a new generation of free fall gravimeters, based on a quantum measurement: atomic gravimeters.
Atomic gravimeters use atoms in gaseous phase as a test mass. The atoms are initially trapped with magneto-optical fields in vacuum, and laser cooled (down to 100 nK) in order to control their initial velocity (down to a few mm/s). The resulting cold atom gas, containing typically a million atoms, is then launched or dropped for a free fall measurement. Manipulating the electronic and motional state of the atoms with two counterpropagating lasers, it is possible to measure, using atom interferometry, their free fall acceleration with respect to the local frame defined by the two lasers [
90]. This sensitive direction is aligned to be along the local gravitational acceleration noted
; the atom interferometer then measures the phase
, where
T is half the interrogation time,
with
λ the laser wavelength, and
is the free fall acceleration along the laser direction. The free fall time is typically on the order of 500 ms, corresponding to a free fall distance of about a meter. A new “atom preparation—free fall—detection” cycle is repeated every few seconds. Each measurement is affected by white noise, but averaging leads to a typical sensitivity on the order of or below
g [
91,
92,
93].
Such an interferometer has been used by H. Müller et al. in [
47] and K. Y. Chung et al. in [
48] for testing Lorentz invariance in the gravitational sector with Caesium atoms, leading to the best terrestrial constraints on the
coefficients. The analysis uses three data sets of respectively 2.5 days for the first two and 10 days for the third, stretched over 4 years, which allows one to observe sidereal and annual LIV signatures. The gravitational SME model used for this analysis can be found in [
39,
47,
48]; its derivation will be summarized hereunder. Since the atoms in free fall are sensitive to the local phase of the lasers, LIV in the interferometer observable could also come from the pure electromagnetic sector. This contribution has been included in the experimental analysis in [
48]. Focusing here on the gravitational part of SME, we ignore it in the following.
The gravitational LIV model adjusted in this test restricts to modifications of the Earth-atom two-body gravitational interaction. The Lagrangian describing the dynamics of a test particle at a point on the Earth’s surface can be approximated by a post-Newtonian series as developed in [
39]. At the Newtonian approximation, the two bodies Lagrangian is given by
where
and
are the position and velocity expressed in the standard SME Sun-centered frame and
with
. In addition, we have introduced
the observed Newton constant measured by considering the orbital motion of bodies and defined by (see also [
39,
50] or Section IV of [
52])
and the 3-dimensional traceless tensor
From this Lagrangian one can derive the equations of motion of the free fall mass in a laboratory frame (see the procedure in Section V.C.1. from [
39]). It leads to the modified local acceleration in the presence of LIV [
39] given by
where
,
is the Earth’s angular velocity,
is the Earth’s boost,
is the Earth radius,
is the Earth mass and
χ the colatitude of the lab whose reference frame’s
direction is the sensitive axis of the instrument as previously defined here. This model includes the shape of the Earth through its spherical moment of inertia
which appears in
,
and
. In [
48], Earth has been approximated as spherical and homogeneous leading to
,
and
.
The sensing direction of the experiment precesses around the Earth rotation axis with sidereal period, and the lab velocity varies with sidereal period and annual period. At first order in
and
and as a function of the SME coefficients, the LIV signal takes the form of a harmonic series with sidereal and annual base frequencies (denoted resp.
and Ω) together with first harmonics. The time dependence of the measured acceleration
from Equation (7) arises from the terms involving the
indices. It can be decomposed in frequency according to [
39]
The model contains seven frequencies
. The 14 amplitudes
and
are linear combinations of 7
components:
,
and
which can be found in Table 1 of [
48] or Table IV from [
39].
In order to look for tiny departures from the constant Earth-atom gravitational interaction, a tidal model for
variations due to celestial bodies is removed from the data before fitting to Equation (8). This tidal model consists of two parts. One part is based on a numerical calculation of the Newtonian tide-generating potential from the Moon and the Sun at Earth’s surface based on ephemerides. It uses here the Tamura tidal catalog [
94] which gives the frequency, amplitude and phase of 1200 harmonics of the tidal potential. These arguments are used by a software (ETGTAB) that calculates the time variation of the local acceleration in the lab and includes the elastic response of Earth’s shape to the tides, called “solid Earth tides”, also described analytically e.g., by the DDW model [
95]. A previous SME analysis of the atom gravimeter data using only this analytical tidal correction had been done, but it led to a degraded sensitivity of the SME test [
47]. Indeed, a non-negligible contribution to
is not covered by this non-empirical tidal model: oceanic tide effects such as ocean loading, for which good global analytical models do not exist. They consequently need to be adjusted from measurements. For the second analysis, reported here, additional local tidal corrections fitted on altimetric data have been removed [
96] allowing to improve the statistical uncertainty of the SME test by one order of magnitude.
After tidal subtraction, signal components are extracted from the data using a numerical Fourier transform (NFT). Due to the finite data length, Fourier components overlap, but the linear combinations of spectral lines that the NFT estimates can be expressed analytically. Since the annual component
has not been included in this analysis, the fit provides 12 measurements. From there, individual constraints on the 7 SME coefficients and their associated correlation coefficients can be estimated by a least square adjustment. The results obtained are presented in
Table 1.
All results obtained are compatible with null Lorentz violation. As expected from boost suppressions in Equation (7) and from the measurement uncertainty, on the order of a few
[
97], typical limits obtained are in the
range for purely spatial
components and 4 orders of magnitude weaker for the spatio-temporal components
. It can be seen e.g., with the purely spatial components that these constraints do not reach the intrinsic limit of acceleration resolution of the instrument (which has a short term stability of
) because the coefficients are still correlated. Their marginalized uncertainty is broadened by their correlation.
Consequently, improving the uncertainty could be reached through a better decorrelation, by analyzing longer data series. In parallel, the resolution of these instruments keeps increasing and has nowadays improved by about a factor 10 since this experiment. However, increasing the instrument’s resolution brings back to the question of possible accidental cancelling in treating “postfit” data. Indeed, it should be recalled here that local tidal corrections subtracted prior to analysis are based on adjusting a model of ocean surface from altimetry data. In principle, this observable would as well be affected by gravity LIV; fitting to these observations thus might remove part of SME signatures from the atom gravimeter data. This was mentioned in the first atom gravimeter SME analysis [
47]. The adjustment process used to assess local corrections in gravimeters is not made directly on the instrument itself, but it always involves a form of tidal measurement (here altimetry data, or gravimetry data from another instrument in [
98]). All LIV frequencies match to the main tidal frequencies. Further progress on SME analysis with atom gravimeters would thus benefit from addressing in more details the question of possible signal cancelling.
4.2. Very Long Baseline Interferometry
VLBI is a geometric technique measuring the time difference in the arrival of a radio wavefront, emitted by a distant quasar, between at least two Earth-based radio-telescopes. VLBI observations are done daily since 1979 and the database contains nowadays almost 6000 24 h sessions, corresponding to 10 millions group-delay observations, with a present precision of a few picoseconds. One of the principal goals of VLBI observations is the kinematical monitoring of Earth rotation with respect to a global inertial frame realized by a set of defining quasars, the International Celestial Reference Frame [
99], as defined by the International Astronomical Union [
100]. The International VLBI Service for Geodesy and Astrometry (IVS) organizes sessions of observation, storage of data and distribution of products, in particular the Earth Orientation parameters. Because of this precision, VLBI is also a very interesting tool to test gravitation in the Solar System. Indeed, the gravitational fields of the Sun and the planets are responsible of relativistic effects on the quasar light beam through the propagation of the signal to the observing station and VLBI is able to detect these effects very accurately. By using the complete VLBI observations database, it was possible to obtain a constraint on the
γ PPN parameter at the level of
[
101,
102]. In its minimal gravitational sector, SME can also be investigated with VLBI and obtaining a constrain on the
coefficient is possible.
Indeed, the propagation time of a photon emitted at the event
and received at the position
can be computed in the SME formalism using the time transfer function formalism [
103,
104,
105,
106,
107] and is given by [
39,
80]
where the terms
and
from [
80] are taken as unity (which corresponds to using the harmonic gauge, which is the one used for VLBI data reduction),
,
,
with the central body located at the origin and where we introduce the following vectors
and where
is the observed Newton constant measured by considering the orbital motion of bodies and is defined in Equation (5). This equation is the generalization of the well-known Shapiro time delay including Lorentz violation. The VLBI is actually measuring the difference of the time of arrival of a signal received by two different stations. This observable is therefore sensitive to a differential time delay (see [
108] for a calculation in GR). Assuming a radio-signal emitted by a quasar at event
and received by two different VLBI stations at events
and
(all quantities being expressed in a barycentric reference frame), respectively, the VLBI group-delay
in SME formalism can be written [
55]
where we only kept the
contribution (see Equation (7) from [
55] for the full expression) and we use the same notations as in [
108] by introducing three unit vectors
Ten million VLBI delay observations between August 1979 and mid-2015 have been used to estimate the
coefficient. First, VLBI observations are corrected from delay due to the radio wave crossing of dispersive media by using 2 GHz and 8 GHz recordings. Then, we used only the 8 GHz delays and the Calc/Solve geodetic VLBI analysis software, developed at NASA Goddard Space Flight Center and coherent with the latest standards of the International Earth Rotation and Reference Systems Service [
109]. We added the partial derivative of the VLBI delay with respect to
from Equation (11) to the software package using the USERPART module of Calc/Solve. We turned to a global solution in which we estimated
as a global parameter together with radio source coordinates. We obtained
with a postfit root mean square of 28 picoseconds and a
per degree of freedom of 1.15. Correlations between radio source coordinates and
are lower than 0.02, the global estimate being consistent with the mean value obtained with the session-wise solution with a slightly lower error.
In conclusion, VLBI is an incredible tool to test Lorentz symmetry, especially the
coefficient. This coefficient has an isotropic impact on the propagation speed of gravitational waves as can be noticed from Equation (27) below (or see Equation (9) from [
56] or Equation (11) from [
60]). The analysis performed in [
55] includes the SME contribution in the modeling of VLBI observations and includes the
parameter in the global fit with other parameters. It is therefore a robust analysis that produces the current best estimate on the
parameter. In the future, the accumulation of VLBI data in the framework of the permanent geodetic monitoring program leads us expect improvement of this constraint.
4.3. Lunar Laser Ranging
On 20 August 1969, after ranging to the lunar retro-reflector placed during the Apollo 11 mission, the first LLR echo was detected at the McDonald Observatory in Texas. Currently, there are five stations spread over the world which have realized laser shots on five lunar retro-reflectors. Among these stations four are still operating: Mc Donald Observatory in Texas, Observatoire de la Côte d’Azur in France, Apache point Observatory in New Mexico and Matera in Italy while one on Maui, Hawaii has stopped lunar ranging since 1990. Concerning the lunar retro-reflectors three are located at sites of the Apollo missions 11, 14 and 15 and two are French-built array operating on the Soviet roving vehicle Lunakhod 1 and 2.
LLR is used to conduct high precision measurements of the light travel time of short laser pulses emitted at time
by a LLR station, reflected at time
by a lunar retro-reflector and finally received at time
at a station receiver. The data are presented as normal points which combine time series of measured light travel time of photons, averaged over several minutes to achieve a higher signal-to-noise ratio measurement of the lunar range at some characteristic epoch. Each normal-point is characterized by one emission time (
in universal time coordinate—UTC), one time delay (
in international atomic time—TAI) and some additional observational parameters as laser wavelength, atmospheric temperature and pressure
etc. According to [
110], the theoretical pendent of the observed time delay (
in TAI) is defined as
where
is the emission time expressed in barycentric dynamical time (TDB) and
is a relativistic correction between the TDB and the terrestrial time (TT) at the level of the station. The reception time
expressed in TDB is defined by the following two relations
with
the time in TDB at the reflection point
and
are respectively the barycentric position vector at the emitter and the reception point,
is the barycentric position vector at the reflection point,
is the one way gravitational time delay correction and
is the one way tropospheric correction.
LLR measurements are used to produce the Lunar ephemeris but also provide a unique opportunity to study the Moon’s rotation, the Moon’s tidal acceleration, the lunar rotational dissipation, etc. [
111]. In addition, LLR measurements have turn the Earth-Moon system into a laboratory to study fundamental physics and to conduct tests of the gravitation theory. Nordtvedt was the first to suggest that LLR can be used to test GR by testing one of its pillar: the Strong Equivalence Principle [
112,
113,
114]. He showed that precise laser ranging to the Moon would be capable of measuring precisely the ratio of gravitational mass to inertial mass of the Earth to an accuracy sufficient to constrain a hypothetical dependence of this ratio on the gravitational self-energy. He concluded that such a measurement could be used to test Einstein’s theory of gravity and others alternative theories as scalar tensor theories. The best current test of the Strong Equivalence Principle is provided by a combination of torsion balance measurements with LLR analysis and is given by [
115,
116,
117]
where
η is the Nordtvedt parameter that is defined as
with
the gravitational mass,
the inertial mass and
U the gravitational self-energy of the body. Using the Cassini constraint on the
γ PPN parameter [
118] and the relation
leads to a constraint on
β PPN parameter at the level
[
116].
In addition to tests of the Strong Equivalence Principle, many other tests of fundamental physics were performed with LLR analysis. For instance, LLR data can be used to search for a temporal evolution of the gravitational constant
[
115] and to constrain the fifth force parameters [
119]. In addition, LLR has been used to constrain violation of the Lorentz symmetry in the PPN framework. Müller et al. [
119] deduced from LLR data analysis constraints on the preferred frame parameters
and
at the level
and
.
Considering all the successful GR tests performed with LLR observations, it is quite natural to use them to search for Lorentz violations in the gravitation sector. In the SME framework, Battat et al. [
45] used the lunar orbit to provide estimates on the SME coefficients. Using a perturbative approach, the main signatures produced by SME on the lunar orbit have analytically been computed in [
39]. These computations give a first idea of the amplitude of the signatures produced by a breaking of Lorentz symmetry. Nevertheless, these analytical signatures have been computed assuming the lunar orbit to be circular and fixed (i.e., neglecting the precession of the nodes for example). These analytical signatures have been fitted to LLR residuals obtained from a data reduction performed in pure GR [
45]. They determined a “
realistic” error on their estimates from a similar postfit analysis performed in the PPN framework. The results obtained by this analysis are presented in
Table 2. It is important to note that this analysis uses projections of the SME coefficients into the lunar orbital plane
(see Section V.B.2 of [
39]) while the standard SME analyses uses coefficients defined in a Sun-centered equatorial frame (and denoted by capital letter
).
However, as discussed in
Section 3 and in [
46,
55], a postfit search for SME signatures into residuals of a data reduction previously performed in pure GR is not fully satisfactory. First of all, the uncertainties obtained by a postfit analysis based on a GR data reduction can be underestimated by up to two orders of magnitude. This is mainly due to correlations between SME coefficients and others global parameters (masses, positions and velocities,
…) that are neglected in this kind of approach. In addition, in the case of LLR data analysis, the oscillating signatures derived in [
39] and used in [
45] to determine pseudo-constraints are computed only accounting for short periodic oscillations, typically at the order of magnitude of the mean motion of the Moon around the Earth. Therefore, this analytic solution remains only valid for few years while LLR data spans over 45 years (see also the discussions in footnote 2 from [
50] and page 22 from [
39]).
Regarding LLR data analysis, a more robust strategy consists in including the SME modeling in the complete data analysis and to estimate the SME coefficients in a global fit along with others parameters by taking into account short and long period terms and also correlations (see [
46]). In order to perform such an analysis, a new numerical lunar ephemeris named “Éphéméride Lunaire Parisienne Numérique” (ELPN) has been developed within the SME framework. The dynamical model of ELPN is similar to the DE430 one [
120] but includes the Lorentz symmetry breaking effects arising on the orbital motion of the Moon. The SME contribution to the lunar equation of motion has been derived in [
39] and is given by
where
is the observed Newtonian constant defined by Equation (5),
M is the mass of the Earth-Moon barycenter,
is the difference between the Earth and the lunar masses;
being the unit position vector of the Moon with respect to the Earth;
with
being the relative velocity vector of the Moon with respect to the Earth;
with
being the Heliocentric velocity vector of the Earth-Moon barycenter and the 3-dimensional traceless tensor defined by Equation (6). These equations of motion as well as their partial derivatives are integrated numerically in ELPN.
In addition to the orbital motion, effects of a violation of Lorentz symmetry on the light travel time of photons is also considered. More precisely, the gravitational time delay
appearing in Equation (14) is given by the gravitational part of Equation (9) [
80].
Estimates on the SME coefficients are obtained by a standard chi-squared minimization: the LLR residuals are minimized by an iterative weighted least squares fit using partial derivatives previously computed from variational equations in ELPN. After an adjustment of 82 parameters including the SME coefficients a careful analysis of the covariance matrix shows that LLR data does not allow to estimate independently all the SME coefficients but that they are sensitive to the following three linear combinations:
The estimations on the 6 SME coefficients derived in [
46] is summarized in
Table 3. In particular, it is worth emphasizing that the quoted uncertainties are the sum of the statistical uncertainties obtained from the least-square fit with estimations of systematics uncertainties obtained with a Jackknife resampling method [
121,
122].
In summary, LLR is a powerful experiment to constrain gravitation theory and in particular hypothetical violation of the Lorentz symmetry. A first analysis based on a postfit estimations of the SME coefficients have been performed [
45] which is not satisfactory regarding the neglected correlations with other global parameters as explained in
Section 3. A full analysis including the integration of the SME equations of motion and the SME contribution to the gravitational time delay has been done in [
46]. The resulting estimates on some SME coefficients are presented in
Table 3. In addition, some SME coefficients are still correlated with parameters appearing in the rotational motion of the Moon as the principal moment of inertia, the quadrupole moment, the potential Stockes coefficient
and the polar component of the velocity vector of the fluid core [
46]. A very interesting improvement regarding this analysis would be to produce a joint GRAIL (Gravity Recovery And Interior Laboratory) [
123,
124,
125] and LLR data analysis that would help in decorrelating the SME parameters from the lunar potential Stockes coefficients of degree 2 and therefore improve marginalized estimations of the SME coefficients. Finally, in [
45,
46], the effects of SME on the translational lunar equations of motion are considered and used to derive constraints on the SME coefficients. It would be also interesting to extend these analyses by considering the modifications due to SME on the rotation of the Moon. A first attempt has been proposed in Section V. A. 2. of [
39] but needs to be extended.
4.4. Planetary Ephemerides
The analysis of the motion of the planet Mercury around the Sun was historically the first evidence in favor of GR with the explanation of the famous advance of the perihelion in 1915. From there, planetary ephemerides have always been a very powerful tool to constrain GR and alternative theories of gravitation. Currently, three groups in the world are producing planetary ephemerides: the NASA Jet Propulsion Laboratory with the DE ephemerides [
120,
126,
127,
128,
129,
130,
131], the French INPOP (Intégrateur Numérique Planétaire de l’Observatoire de Paris) ephemerides [
132,
133,
134,
135,
136,
137] and the Russian EPM ephemerides [
138,
139,
140,
141,
142]. These analyses use an impressive number of different observations to produce high accurate planetary and asteroid trajectories. The observations used to produce ephemerides comprise radioscience observations of spacecraft that orbited around Mercury, Venus, Mars and Saturn, flyby tracking of spacecraft close to Mercury, Jupiter, Uranus and Neptune and optical observations of all planets. This huge set of observations have been used to constrain the
γ and
β post-Newtonian parameter at the level of
[
136,
137,
141,
142,
143], the fifth force interaction (see [
32] and Figure 31 from [
143]), the quantity of Dark Matter in our Solar System [
144], the Modified Newtonian Dynamics [
131,
145,
146,
147], …
A violation of Lorentz symmetry within the gravity sector of SME induces different types of effects that can have implications on planetary ephemerides analysis: effects on the orbital dynamics and effects on the light propagation. Simulations using the Time Transfer Formalism [
104,
106,
107] based on the software presented in [
148] have shown that only the
coefficients produce a non-negligible effect on the light propagation (while it has impact only at the next post-Newtonian level on the orbital dynamics [
29,
39]). On the other hand, the other coefficients produce non-negligible effects on the orbital dynamics [
39] and can therefore be constrained using planetary ephemerides data. In the linearized gravity limit, the contribution from SME to the 2-body equations of motion within the gravitational sector of SME are given by the first line of Equation (17) (i.e., for a vanishing
). The coefficient
is completely unobservable in this context since absorbed in a rescaling of the gravitational constant (see the discussion in [
39,
52]).
Ideally, in order to perform a solid estimation of the SME coefficients using planetary ephemerides, one should include the full SME equations in the integration of the planets motion and fit them simultaneously with the other estimated parameters (positions and velocities of planets, of the Sun, …). This solid analysis within the SME formalism has not been performed so far.
As a first step, a postfit analysis has been performed [
49,
50]. The idea of this analysis is to derive the analytical expression for the secular evolution of the orbital elements produced by the SME contribution to the equations of motion. Using the Gauss equations, secular perturbations induced by SME on the orbital elements have been computed in [
39] (see also [
49] for a similar calculations done for the
coefficients only). In particular, the secular evolution of the longitude of the ascending node Ω and the argument of the perihelion
ω is given by
where
a is the semimajor axis,
e the eccentricity,
i the orbit inclination (with respect to the ecliptic),
is the mean motion,
,
the difference between the two masses and
M their sum (in the cases of planets orbiting the Sun, one has
). In all these expressions, the coefficients for Lorentz violation with subscripts
P,
Q, and
k are understood to be appropriate projections of
along the unit vectors
P,
Q, and
k, respectively. For example,
,
. The unit vectors
P,
Q and
k define the orbital plane (see [
39] or Equation (8) from [
50]).
Instead of including the SME equations of motion in planetary ephemerides, the postfit analysis uses estimations of supplementary advances of perihelia and nodes derived from ephemerides analysis [
135,
140,
144] to fit the SME coefficients through Equation (19). In [
50], estimations of supplementary advances of perihelia and longitude of nodes from INPOP (see Table 5 from [
135]) are used to fit a posteriori the SME coefficients. This analysis suffers from large correlations due to the fact that the planetary orbits are very similar to each other: nearly eccentric orbit and very low inclination orbital planes. In order to deal properly with these correlations a Bayesian Monte Carlo inference has been used [
50]. The posterior probability distribution function can be found on Figure 1 from [
50]. The intervals corresponding to the 68% Bayesian confidence levels are given in
Table 4 as well as the correlation matrix. It is interesting to mention that a decomposition of the normal matrix in eigenvectors allows one to find linear combinations of SME coefficients that are uncorrelated with the planetary ephemerides analysis (see Equation (
15) and Table IV from [
50]).
In summary, planetary ephemerides offer a great opportunity to constrain hypothetical violations of Lorentz symmetry. So far, only postfit estimations of the SME coefficients have been performed [
49,
50]. In this analysis, estimations of secular advances of perihelia and longitude of nodes obtained with the INPOP planetary ephemerides [
135] are used to fit a posteriori the SME coefficients using the Equations (19). The 68% marginalized confidence intervals are given in
Table 4. This analysis suffers highly from correlations due to the fact that the planetary orbits are very similar. A very interesting improvement regarding this analysis would be to perform a full analysis by integrating the planetary equations of motion directly within the SME framework and by fitting the SME coefficients simultaneously with the other parameters fitted during the ephemerides data reduction.
4.5. Gravity Probe B
In GR, a gyroscope in orbit around a central body undergoes two relativistic precessions with respect to a distant inertial frame: (i) a geodetic drift in the orbital plane due to the motion of the gyroscope in the curved spacetime [
149]; and (ii) a frame-dragging due to the spin of the central body [
150]. In GR, the spin of a gyroscope is parallel transported, which at the post-Newtonian approximation gives the relativistic drift
where
is the unit vector pointing in the direction of the spin
of the gyroscope,
and
are the position and velocity of the gyroscope,
and
is the angular momentum of the central body. In 1960, it has been suggested to use these two effects to perform a new test of GR [
151,
152]. In April 2004, GPB, a satellite carrying 4 cryogenic gyroscopes was launched in order to measure these two precessions. GPB was orbiting Earth on a polar orbit such that the two relativistic drifts are orthogonal to each other [
153]: the geodetic effect is directed along the NS direction (North-South, i.e., parallel to the satellite motion) while the frame-dragging effect is directed on the WE direction (West-East, see [
52,
153] for further details about the axes conventions in the GPB data reduction). A year of data gives the following measurements of the relativistic drift: (i) the geodetic drift
mas/yr (milliarcsecond per year) to be compared to the GR prediction of −6606.1 mas/yr; and (ii) the frame-dragging drift
mas/yr to be compared with the GR prediction of −39.2 mas/yr. In other word, the GPB results can be written as a measurement of a deviation from GR given by
Within the SME framework, if one considers only the
coefficients, the equation of parallel transport in term of the spacetime metric is not modified (see Equation (143) from [
39]). Nevertheless, the expression of the spacetime metric is modified leading to a modification of the relativistic drift given by Equation (150) from [
39]. In order to focus only on the dominant secular part of the evolution of the spin orientation, the relativistic drift equation has been averaged over a period. The SME contribution to the precession can be written as [
39]
where
is the effective gravitational constant defined by Equation (5), the coefficients
are defined by
,
is a unit vector normal to the gyroscope orbital plane,
r and
v are the norm of the position and velocity of the gyroscope and
is the traceless part of
as defined by Equation (6). Using the geometry of GPB into the last equation and using Equation (20a), one finds that the gyroscope anomalous drift is given by
where the units are mas/yr. These are the SME modifications to the relativistic drift arising from the modification of the equations of evolution of the gyroscope axis (i.e., modification of the parallel transport equation due to the modification of the underlying spacetime metric).
In addition to modifying the evolution of the spin axis, a breaking of Lorentz symmetry will impact the orbital motion of the gyroscope. As a result, the position and velocity of the gyroscope will depend on the SME coefficients and therefore also impact the evolution of the spin axis through the GR contribution given by Equation (20b). The best way to deal with this effect is to use the GPB tracking measurements (GPS) in order to constrain the gyroscope orbital motion and eventually constrain the SME coefficients through the equations of motion. In [
52], these tracking observations are not used and only the gyroscope drift is used in order to constrain the SME contributions coming from both the modification of the parallel transport and from the modification of GPB orbital motion. In order to do this, the contribution of SME on the evolution of the orbital elements given by Equations (19) and (26) are used, averaged over a period and in the low eccentricity approximation. This secular evolution for the osculating elements is introduced in the relativistic drift equation for the gyroscope from Equation (20b) and averaged over the measurement time using Equation (20a). Using the GPB geometry, this contribution to the relativistic drift is given by
with units of mas/yr.
The sum of the two SME contributions to the gyroscope relativistic drift given by Equations (23) and (24) can be compared to the GPB estimations given by Equation (21). The result is given in
Table 5. The main advantage of GPB comes from the fact that it is sensitive to the
coefficient. The constraint on this coefficient is at the level of
, a little bit less good than the one obtained with VLBI or with binary pulsars but relying on a totally different type of observations. The constraints on the spatial part of the SME coefficients (
) are at the level of
and are superseded by the other measurements. The constraints on these coefficients come mainly from the contribution arising from the orbital dynamics of GPB and not from a direct modification of the spin evolution. Constraining the orbital motion from GPB by using the gyroscope observations only is not optimal and tracking observations may help to improve the corresponding constraints (in this case, a dedicated satellite may be more appropriate as discussed in
Section 5.3).
In summary, the GPB measurement of a gyroscope relativistic drifts due to geodetic precession or frame-dragging can be used to search for a breaking of Lorentz symmetry. The main advantage of this technique comes from its sensitivity to
. As already mentioned, this coefficient has an isotropic impact on the propagation velocity of gravitational waves as can be noticed from Equation (27) below (see also Equation (9) from [
56] or Equation (11) from [
60]). A preliminary result based on a post-fit analysis performed after a GR data reduction of GPB measurements gives a constraint on
at the level of
[
52]. This should be investigated further since the Earth’s quadrupole moment has been neglected and Lorentz-violating effects on the aberration terms can also change slightly the results. In addition, impacts from Lorentz violations on frame-dragging arising in other contexts such as satellite laser ranging (see
Section 5.3) or signals from accretion disks around collapsed stars [
154] would also be interesting to consider.
4.6. Binary Pulsars
The discovery of the first binary pulsars PSR 1913+16 by Hulse and Taylor in 1975 [
155] has opened a new window to test the theory of gravitation. Observations of this pulsar have allowed one to measure the relativistic advance of the periastron [
156] and more importantly to measure the rate of orbital decay due to gravitational radiation [
157]. Pulsars are rotating neutron stars that are emitting very strong radiation. The periods of pulsars are very stable which allows us to consider them as “clocks” that are moving in an external gravitational field (typically in the gravitational field generated by a companion). The measurements of the pulse time of arrivals can be used to infer several parameters by fitting an appropriate timing model (see for example Section 6.1 from [
2]): (i) non-orbital parameter such as the pulsar period and its rate of change; (ii) five Keplerian parameters; and (iii) some post-Keplerian parameters [
158]. In GR, the expressions of these post-Keplerian parameters are related to the masses of the two bodies and to the Keplerian parameters. If more than 2 of these post-Keplerian parameters can be determined, they can be used to test GR [
159]. Nowadays, more than 70 binary pulsars have been observed [
160]. A description of the most interesting binary pulsars in order to test the gravitation theory can be found in Section 6.2 from [
2] or in the supplemental material from [
53].
The model fitted to the observations is based on a post-Newtonian analytical solution to the 2 body equations of motion [
161] (see also [
162]) and includes contribution from the Einstein time delay (i.e., the transformation between proper and coordinate time), the Shapiro time delay, the Roemer time delay [
158]. The model also corrects for several systematics like atmospheric delay, Solar system dispersion, interstellar dispersion, motion of the Earth and the Solar System, … (see for example [
163]).
Pulsars observations provide some of the best current constraints on alternative theories of gravitation (for a review, see [
164,
165]). In addition to the Hulse and Taylor pulsar, the double pulsar [
166] now provides the best measurement of the pulsar orbital rate of change [
165]. In addition, the post-Keplerian modeling has been fully derived in tensor-scalar theories [
167,
168,
169] such that pulsars observations have provided some of the best constraints on this class of theory [
165,
170,
171]. It is important to mention that non perturbative strong field effects may arise in binary pulsars system and needs to be taken into account [
169,
172].
In addition, binary pulsars have also been successfully used to test Lorentz symmetry. For example, analyses of the pulses time of arrivals provide a constraint on the
PPN parameters. Since non perturbative strong field effects may arise in binary pulsars system (see for example [
173] for strong field effects in Einstein-Aether theory), the obtained constraints are interpreted as strong field version of the PPN parameters denoted by
. Estimates of these parameters should be compared carefully to the standard weak field constraints since they may depend on the gravitational binding energy of the neutron star. The best current constraint on
is obtained by considering the orbital dynamics of the binary pulsars PSR J1738+0333 [
174,
175]. The best current constraint on
takes advantage from the fact that this parameter produces a precession of the spin axis of massive bodies [
176]. The combination of observations of two solitary pulsars lead to the best current constraints on
[
177]. Finally, the parameter
produces a violation of the momentum conservation in addition to a violation of the Lorentz symmetry. This parameter will induce a self-acceleration for rotating body that can be constrained using binary pulsars [
178]. The best current constraint uses a set of 5 pulsars (4 binary pulsars and one solitary pulsar) and is given by
[
179].
Furthermore, specific Lorentz violating theories have also been constrained with binary pulsars. In [
72,
73], binary pulsars observations are used to constrain Einstein-Aether and khronometric theory. In these theories, the low-energy limit Lorentz violations can be parametrized by four parameters: the
and
PPN parameters and two other parameters. It has been shown [
72,
73,
173] that the orbital period decay depends on these four parameters. Assuming the solar system constraints on
and
[
2], measurements of the rate of change of the orbital period of binary pulsars have been used to constrain the two other parameters (see for example Figure 2 from [
72]). In this work, strong field effects have been taken into account by solving numerically the field equations in order to determine the neutron stars sensitivity [
73].
Finally, binary pulsars have been used in order to derive constraints on the SME coefficients. As in the PPN formalism, constraints obtained from binary pulsars need to be considered as constraints on strong-field version of the SME coefficients that may include non perturbative effects. Two different types of effects have been used to determine estimates on the SME coefficients: (i) tests using the spin precession of solitary pulsars and (ii) tests using effects on the orbital dynamics of binary pulsars [
53]. The SME contribution to the precession rate of an isolated spinning body has been derived in [
39] and is given by
where
P is the spin period and
is the unit vector pointing along the spin direction. The effects from the pulsar spin precession on the pulse width can be found in [
177,
180]. Two solitary pulsars have been used to constrain the SME coefficients with this effect. The second type of tests come from the orbital dynamics of binary pulsars. As mentioned in
Section 4.3 and
Section 4.4, the SME will modify the two-body equations of motion by including the term from Equation (17). At first order in the SME coefficients, this will produce several secular effects that have been computed in [
39]. In particular, an additional advance in the argument of periastron and of the longitude of the nodes has been mentioned in Equation (19) and used to constrain the SME with planetary ephemerides. For binary pulsars, it is possible to constrain a secular evolution of two other orbital elements: the eccentricity and the projected semi-major axis
x. The secular SME contributions to these quantities have been computed in [
39,
53,
54] and are given by
where
is the mass of the pulsar,
is the mass of the companion and all others quantities have been introduced after Eqs. (19). For each binary pulsar, in principle 3 tests can be constructed by using
,
,
. In [
53], 13 pulsars have been used to derive estimates on the SME coefficients. The combination of the observations from the solitary pulsars and from the 13 binary pulsars are reported in
Table 6. Both orbital dynamics and spin precession are completely independent of
whose constraint will be discussed later.
Several comments can be made about this analysis. First of all, it can be considered as a postfit analysis done after an initial fit performed in GR (or within the post-Keplerian formalism). In particular, correlations between the SME coefficients and other parameters (e.g., orbital parameters) are neglected. Secondly, for most of the pulsars,
and
are not directly measured from the pulse time of arrivals but rather estimated from the uncertainties on
x,
ω and
e divided by the time span of the observations. Further, it is important to mention that effects of Lorentz violations have been considered only for the orbital dynamics but never on the Einstein delay or on the Shapiro time delay in this analysis. The full timing model within SME can be found in Section V.E.3 from [
39] (see also [
181] for a similar derivation with the matter-gravity couplings). In addition, some parameters are not measured like for example the longitude of the ascending node Ω or the azimuthal angle of the spin. These parameters have been marginalized by using Monte Carlo simulations. It is unclear what type of prior probability distribution function has been used in this analysis and what is the impact of this choice. Nevertheless, the results obtained by this analysis (which does not include the
parameter) are amongst the best ones currently available demonstrating the power of pulsars observations. The main advantages of using binary pulsars come from the fact that their orbital orientation vary which allows one to disentangle the different SME coefficients and to end up with low correlations. Furthermore, they are so far the only constraints on the strong field version of the SME coefficients.
In addition, a different analysis has been performed to constrain the parameter
alone [
54]. While the orbital dynamics and the spin precession is completely independent of
(i.e., the time component of
in a local frame), the boost between the Solar System and the binary pulsar frame makes appear explicitly the
coefficient. In [
54], the assumption that there exists a preferred frame where the
tensor is isotropic is made, which makes the results specific to that case (although the analysis can be done without this assumption). The analysis requires the knowledge of the pulsar velocity with respect to the preferred frame as well as the velocity of the Solar System with respect to the same frame. Three pulsars have their radial velocity measured, which combined with proper motion in the sky can be used to determine their velocity. The velocity of the Solar System is taken as its velocity with respect to the Cosmic Microwave Background (CMB) frame
(with
km/s). The analysis is completely similar to the ones performed for the other SME coefficients (see the discussion in the previous paragraph). It is known that
has a strong effect on the propagation of the light neglected in [
54], which may impact the result. In addition, all correlations between
and the other SME coefficients are neglected. Finally, two different scenarios have been considered regarding the preferred frame: (i) a scenario where the preferred frame is assumed to be the CMB frame and (ii) a scenario where the orientation of the preferred frame is left free and is marginalized over but the magnitude of the velocity of the Solar System with respect to that frame is still assumed to be the 369 km/s. The general case corresponding to a completely free preferred frame has not been considered. If the CMB frame is assumed to be the preferred frame, the constraint on
is given by
which is a bit better than the one obtained with VLBI (see Equation (13)) although the VLBI analysis does not assume any preferred frame. The scenario where the orientation of the preferred frame is left as a free parameter leads to an upper bound on
.
In summary, observations of binary pulsars are an incredible tool to test the gravitation theory. These tests are of the same order of magnitude (and sometimes better) than the ones performed in the Solar System. Moreover, observations of binary pulsars are sensitive to strong field effects. Observations of the pulse arrival times have been used to search for a breaking of Lorentz violation within the PPN framework by constraining the strong field version of the
parameters. The parameter
is constrained at the level of
,
at the level of
and
at the level of
[
164]. In addition, constraints on Einstein-Aether and khronometric theory have also been done by combining Solar System constraints with binary pulsars observations [
72,
73]. Finally, within the SME framework, a postfit analysis has been done by considering the spin precession of solitary pulsars and the orbital dynamics of binary pulsars. The obtained results are given in
Table 6 and constrain the strong field version of the SME coefficients. The main advantage of using binary pulsars comes from the fact that they proved an estimate of all the SME coefficients with reasonable correlations. It has to be noted that the modification of the orbital period due to gravitational waves emission has not been computed so far in the SME formalism. In addition, the constraint on
suffers from the assumption of the existence of a preferred frame. Moreover, the corresponding analysis has neglected all effects on the timing delay that may also impact the results and has neglected the other SME coefficients that may also impact this constraint.
4.7. Čerenkov Radiation
Gravitational Čerenkov radiation is an effect that occurs when the velocity of a particle exceeds the phase velocity of gravity. In this case, the particle will emit gravitational radiation until the particle loses enough energy to drop below the gravity speed [
56]. In modified theory of gravity, the speed of gravity in a vacuum may be different from the speed of light and Čerenkov radiation may occur and produces energy losses for particles traveling over long distances. Observations of high energy cosmic rays that have not lost all their energy through Čerenkov radiation can be used to put constraints on models of gravitation that predicts gravitational waves that are propagating slower than light. This effect has been used to constrain some alternative gravitation theories [
182,
183]: a class of tensor-vector theories [
184], a class of tensor-scalar theories [
185], extended theories of gravitation [
186] and some ghost-free bigravity [
187].
The propagation of gravitational waves within the SME framework has been derived in [
56,
60] (including nonminimal SME contributions). In particular, in the minimal SME, the dispersion relation for the gravitational waves is given by [
56]
where
is the 4-momentum of the gravitational wave. A similar expression including nonminimal higher order SME terms can be found in [
56,
60]. If the minimal SME produces dispersion-free propagation, the higher order terms lead to dispersion and birefringence [
60]. As can be directly inferred from the last equation, gravitational Čerenkov radiation can arise when the effective refractive index
n is
where
. The expression for the energy loss rate due to Lorentz-violating gravitational Čerenkov emission has been calculated from tree-level graviton emission for photons, fermions and scalar particles and is given by [
56]
where
d is the dimension of the Lorentz violating operator (
for the minimal SME),
is a dimensionless factor depending on the flavor
w of the particle emitting the radiation,
is the particle incoming momentum (with
) and
is a direction-dependent combination of SME coefficients. In the minimal SME,
is decomposed on spherical harmonics as
where we explicitly indicated the
to specify that these coefficients are spherical harmonic decomposition of the SME coefficients. The calculation of the dimensionless factor
for scalar particles, fermions and photons has been done in [
56]. The integration of Equation (29) shows that if a cosmic ray of specie
w is observed on Earth with an energy
after traveling a distance
L along the direction
, this implies the following constraint on the SME coefficients
where
is another dimensionless factor dependent on the matrix element of the tree-level process for graviton emission.
Using data for the energies and angular positions of 299 observed cosmic rays from different collaborations [
188,
189,
190,
191,
192,
193,
194,
195], Kostelecký and Tasson [
56] derived lower and upper constraints on 80 SME coefficients, including the nine coefficients from the minimal SME whose constraints are given by the
Table 7. In their analysis, they consider the coefficients from the different dimensions separately and did not fit all of them simultaneously. In addition, in the minimal SME, they did a fit for the
parameter alone and another fit for the other 8 coefficients. The number of sources and their directional dependence across the sky allow one to disentangle the SME coefficients and to derive two-sided bounds from the Equation (31). The only coefficient that is one sided is
because it produces isotropic effects. The bounds are severe for these coefficients, on the order of
. However, this analysis assumes that the matter sector coefficients vanish. Furthermore, several assumptions have been made in order to derive the bounds from
Table 7. It is assumed that the cosmic ray primaries are nuclei of atomic weight
(iron), that the Čerenkov radiation is emitted by one of the fermionic partons in the nucleus that carries 10 % of the cosmic ray energy and that the travel distance of the cosmic ray is 10 Megaparsec (Mpc) [
56]. Although only conservative assumptions are used for the astrophysical processes involved in the production of high-energy cosmic rays, the observations rely on the sources on the order of 10 Mpc distant, and thus the analysis is of a different nature than a controlled laboratory or even Solar-System test.
For the sake of completeness and to allow an easy comparison with the estimations of the other standard cartesian
coefficients, the following relations give the links between the spherical harmonic decomposition and the standard cartesian decomposition of the SME coefficients:
In summary, observations of cosmic rays allow one to derive some stringent boundaries on the SME coefficients. The idea is that if Lorentz symmetry is broken, these high energy cosmic rays would have lost energy by emitting Čerenkov radiation that has not been observed. The boundaries on the spherical harmonic decomposition of the SME coefficients are given in the
Table 7 (in order to compare these boundaries to other constraints, they have been transformed into boundaries on standard cartesian SME coefficients in
Table 8). For the minimal SME, one can limit the isotropic
(one sided bound) or the other eight other coefficients in
, but not all the nine simultaneously. These boundaries are currently the best available in the literature at the exception of
whose constraint is only one sided. Nevertheless, several assumptions have been made in this analysis and the observations rely on sources located at very high distances. This analysis is therefore of a different nature than the other ones where more control on the measurements is possible.