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Diego Saez-Gomez

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ere right lethand us remind side (r.h.s.). that T Thus, = T it µ = may ρ −lead 3p. toThe violations last equation of the usual differs evolution from theofusual different continuity species equation in theon th<br />

,-null T Nevertheless, ) mean rightdifferentiation hand in side the next (r.h.s.). with section Thus, respect<br />

F(R,T)<br />

we it focus may to Rour lead orattention T to , and violations<br />

gravity<br />

the on atensor model of theΘ that usual keeps evolution the usual of the continuity differentequation<br />

species in th<br />

µν is<br />

iverse. d. Nevertheless, in the next section we focus our attention on a model that keeps the usual continuity equatio<br />

hanged.<br />

δT αβ<br />

δg µν = −2T µν − g µν L m +2g αβ δL m<br />

. (4)<br />

III. δg µν<br />

f 1 g(R)+f αβ 2 (T ) TYPE THEORIES<br />

III. f 1 (R)+f 2 (T ) TYPE THEORIES<br />

section, absencewe of any choose kind the ofalgebraic matter, the function corresponding f(R, T ) to f(R) be agravity sum ofequations<br />

two independent functions<br />

nonding thisA section, particular properties wecase,<br />

choose and the thewell-known algebraic function solutionsf(R, for f(R) T ) togravity be a sum areof also two independent functions<br />

acuum (for a review on f(R) theories, f(R, T see )=f [1]). 1 (R)+f Moreover, 2 (T ) here we are<br />

d of theories for spatially flat FLRW spacetimes, f(R, T )=f which 1 (R)+f are expressed 2 (T ) in<br />

(12)<br />

(12<br />

(R) and f 2 (T ), respectively depend on the curvature R and the trace T . The generalized Einstein equations<br />

ere rgy<br />

yield fdensity, Friedmann<br />

1 (R) andwith f<br />

equations,<br />

2 (T ), respectively depend on the curvature R and the trace T . The generalized Einstein equation<br />

(8) ds 2 yield = a 2 (η) f 10 ≡ f 1 (R 0 ), f 1R0 ≡ df 1 (R 0 )/dR 0 , f 20 ≡ f 2 (T 0 ), f 2T0 ≡ df 2 (T 0 )/dT 0 and c 2<br />

dη 2 − dx 2 s = p 0 /ρ 0 . Th<br />

tinuity equation (11) for Lagrangians given by (12) yields<br />

(5)<br />

<br />

− 3Hf 1R +3H f 1R0 − a2<br />

2 f <br />

<br />

10 = −κ 2 a 2 ρ 0 +(1+c 2 s)ρ 0 a 2 f 2T0 + a2<br />

l time η. Then, the main ∇ 2 f 20 , (13)<br />

− 3Hf 1R 0<br />

+3H f 1R0 − a2<br />

f <br />

1R 0<br />

+ Hf 1R 0<br />

− (H +2H 2 )f 1R0 + a2<br />

2 f 2 f 10 = −κ 2 a 2 ρ 0 +(1+c 2 s)ρ 0 a 2 f 2T0 + a2<br />

µ T µ issue arises on the content of the Universe is<br />

0 ν = 1<br />

1<br />

10 = −κ 2 2 c 2 sρ 0 − a2<br />

2 f 2 f 20 , (13<br />

ensor, defined in (2). Since we are κ 2 δ ν µ ∂ µ<br />

−interested f 2T0 on flat 2 f 20 + c 2 sρ 0 f 2T0 + T µ<br />

0 ν ∂ µf 2T0 , (15<br />

FLRW cosmologies,<br />

less matter, radiation,... ) can be well described 20 . (14)<br />

f <br />

1R 0<br />

+ Hf 1R 0<br />

− (H +2H 2 )f 1R0 + a2 by<br />

2 f perfect fluids, whose<br />

wing explicitly that the energy-momentum tensor is not<br />

10 = a priori −κ 2 a 2 covariantly c 2 sρ 0 − a2<br />

2 f conserved<br />

20 . in f(R, T ) theories. Thus (14<br />

these theories, the test particles moving in a gravitational<br />

e prime holds for the derivative with respect to η, H ≡ a field do not follow geodesic lines. By exploring th<br />

ation /a and the subscript 0 holds for unperturbed<br />

ere ndT (15)<br />

quantities: the prime Rholds 0 denotes for the thederivative scalar curvature with respect corresponding to η, Hto ≡the a µν =(ρ<br />

for<br />

+ p)u<br />

ν =<br />

µ u<br />

0 component,<br />

ν − pg µν .<br />

one gets<br />

Continuity equation,<br />

/a unperturbed and (6) the subscript metric, ρ0 holds the unperturbed for unperturbe<br />

kground quantities: R 0 denotes the scalar curvature corresponding to the unperturbed metric, ρ 0 the unperturbe<br />

ρ 0 +3Hρ 0 (1 + c 2 1<br />

s)=<br />

κ 2 (1 + c 2<br />

− f<br />

s)ρ 0 f2T 0<br />

+ c 2 sρ 0f 2T0 + 1 <br />

2T0<br />

2 f 20<br />

. (16<br />

e that The whether usual continuity f 2 vanishes equation (i.e., is f(R) recovered theories) when, or characterizes a non-running cosmological constant, both f 2T<br />

vanish, and then the continuity equation in these scenarios becomes<br />

f 2T0<br />

f<br />

ρ 0 +3H 2 (T )=α √ 1+c 2 T + β<br />

s<br />

ρ0 =0 . (17<br />

n order to Lagrangians such as (12) consistent with the standard conservation equation, the r.h.s. of (15) has t<br />

ish leading to the differential equation<br />

1 <br />

F. Alvarenga, A. Cruz-Dombriz, S. Houndjo, M. Rodrigues, DSG, to appear in PRD, ArXiv:1302.1866

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