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eISSN: 2576-4543

Physics & Astronomy International Journal

Review Article Volume 1 Issue 4

Exact solutions of the newton-schrödinger equation, infinite derivative gravity and schwarzschild atoms

Carlos Castro Perelman

Center for Theoretical Studies of Physical Systems, Clark Atlanta University, Georgia

Correspondence: Carlos Castro Perelman, Center for Theoretical Studies of Physical Systems, Clark Atlanta University, Atlanta, GA 30314, Georgia,

Received: October 07, 2017 | Published: November 13, 2017

Citation: Perelman CC. Exact solutions of the Newton-Schrödinger equation, infinite derivative gravity and Schwarzschild atoms. Phys Astron Int J.2017;1(4):131-137. DOI: 10.15406/paij.2017.01.00024

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Abstract

Exact solutions to the stationary spherically symmetric Newton-Schrödinger equation are proposed in terms of integrals involving generalized Gaussians. The energy eigenvalues are also obtained in terms of these integrals which agree with the numerical results in the literature. A discussion of infinite derivative-gravity follows which allows generalizing the Newton-Schrödinger equation by replacing the ordinary Poisson equation with a modified non-local Poisson equation associated with infinite-derivative gravity. We proceed to replace the nonlinear Newton-Schrödinger equation for a non-linear quantum-like Bohm-Poisson equation involving Bohm’s quantum potential, and where the fundamental quantity is no longer the wave-function Ψ but the real-valued probability density ρ . Finally, we discuss how the latter equations reflect a nonlinear feeding loop mechanism between matter and geometry which allows us to envisage a “Schwarzschild atom” as a spherically symmetric probability cloud of matter which curves the geometry, and in turn, the geometry back-reacts on this matter cloud perturbing its initial distribution over the space, which in turn will affect the geometry, and so forth until static equilibrium is reached.

Keywords: quantum mechanics, Newton-Schrödinger equation, infinite derivative gravity, de Broglie-Bohm theory, Schwarzschild metric

Introduction

The Newton-Schrödinger equation

Various arguments have been put forward from time to time to support the view that quantum state reduction is a phenomenon that occurs objectively, because of some gravitational influence.16 According to a particular argument put forward by Penrose,1 a superposition of two quantum states, each of which would be stationary on its own, but for which there is a significant mass displacement between the two states, ought to be unstable and reduce to one state or the other within a certain characteristic average timescale TG . This argument is motivated by a conflict between the basic principles of quantum mechanics and those of general relativity. It is accordingly proposed that TG  can be calculated in situations for which velocities and gravitational potentials are small in relativistic units, so that a Newtonian approximation is appropriate, and TG is the reciprocal, in Planckian units, of the gravitational self-energy EG  of the difference between the mass distributions of the two states.

There is of course a substantial literature on the problem of wave-function collapse and the related measurement problem. See, for example46 and references therein. For a different idea about gravitationally-induced wave-function collapse see.3 It has been pointed out by Penrose R et al.1,2 that one can regard the basic stationary states, into which a superposition of such states is to decay into (on a timescale of order /EG ), as stationary solutions of the Schrödinger equation where there is an additional term provided by a certain gravitational potential. The appropriate gravitational potential is the one which arises from the mass density given by the expectation value of the mass distribution in the state determined by the wave-function. In the practical situations under consideration in1 (such as with the proposed class of experiments put forward there), it would be sufficient to consider Newtonian gravity. This leads us to consider what Penrose termed the Schrödinger-Newton equation. This equation has had a long history since the 1950"s.717 It is the name given to the system coupling the Schrödinger equation to the Poisson equation. In the case of a single particle, this coupling is effected as follows: for the potential energy term in the Schrödinger equation take the gravitational potential energy determined by the Poisson equation from a matter density proportional to the probability density obtained from the wave-function. For a single particle of mass m the system consists of the following pair of partial differential equations:

The Newton-Schrödinger equation is nonlinear and nonlocal modification of the Schrödinger equation given by

iΨ(r,t)t=22m2Ψ(r,t)+V(r,t)Ψ(r,t)+mVG(r,t)Ψ(r,t)   (1)

Where V(r,t)  is the external potential acting on the particle and mVG(r,t)  is the self- gravitational potential energy arising due a mass density obtained from the wave function of the particle itself. Given the Poisson equation sourced by a mass density ρ=m|Ψ(r,t)|2

2VG(r,t)=4πGm|Ψ(r,t)|2     (2)

It leads to a self-gravitational potential

VG(r,t)=Gm|Ψ(r,t)|2|rr|d3r     (3)

Inserting equation (3) into equation (1) leads to the integro differential form of the nonlinear and

nonlocal Newton-Schrödinger equation

iΨ(r,t)t=22m2Ψ(r,t)+V(r,t)Ψ(r,t)(Gm2m|Ψ(r,t)|2|rr|d3r)Ψ(r,t)   (4)

Relevant work pertaining pseudo differential and hyper differential operators, nonlinear partial differential equations and their applications can be found in.1820

This equation is based on the assumption that the point-particle is smeared over space such that its mass is distributed according to its wave function. Namely, there is a mass cloud over space whose net mass m=m|Ψ(r,t)|2d3r. coincides with the mass of the point-particle. The mass cloud is self-gravitating and experiences a gravitational potential energy given by equation (3).1

More recently, the authors21 showed that nonlinear Schrödinger equations (NSEs) for individual particles do not follow from general relativity (GR) plus quantum field theory (QFT). Contrary to what is commonly assumed, the NSEs are not the weak-field, non-relativistic limit of the semi-classical Einstein equation. The wave-function in the NSEs makes sense only as that for a mean field describing a system of N particles as N   , not that of a single or finite many particles. They concluded that the origins and consequences of NSEs are very different, and should be clearly demarcated from those of the semi-classical Einstein equation, the only legitimate representative of semi classical gravity, based on GR+QFT. Bearing this in mind, we proceed to find solutions to the NSE’s.

Solutions to the Newton-Schrödinger equation

Let us set the external potential to zero and look for stationary solutions Ψ(r,t)=e-iEt/Φ(r) such that the gravitational potential becomes time independent. Φ(r) obeys the equation

EΦ(r)=22m2Φ(r)(Gm2|Φ(r)|2|rr|d3r)Φ(r)   (5)

The authors2226 found numerical spherically-symmetric solutions to equation (5). Variational forms of the stationary Newton-Schrödinger equation to find a lower bound for the ground state energy have been studied by several authors, see references in27 and co,mpared to numerical values in the literature.

1This may be in conflict with Born’s rule of interpreting |Ψ(r,t)|2 as the probability density of finding a particle at the point r if one has abandoned the notion of point-particles. At the moment we shall not be concerned with this.

If one replaces a delta function point-mass source distribution mδ3(r)=mδ(r)/4πr2  for a normalized Gaussian mass distribution of width

ρ(r)=mπ3/2er2/σ2σ3m=0ρ(r)4πr2dr                     (6)   (6)

The solution to Poisson's equation

2VG(r)=4πGρ(r)   (7)

Is given in terms of the error function Erf(r)2 as follows

VG(r)=GmrErf(rσ)=Gmr1πr/σr/σet2dt   (8)

In the asymptotic regime r,Erf()1. , the potential recovers the Newtonian form Gm2r . Because the error function Erf(r)  admits a series expansion around r=0 as

Erf(r)2rπr3π+11r520π241r7840π+...      (9)

The potential VG(r) is no longer singular at the origin r=0 , but it behaves as

VG(r)2Gmπσ[1r22σ2+11r440σ4+...]       (10)

The normalized Gaussian wave function

Φ(r)1π3/4er2/2σ2σ3/2   (11)

Satisfies

0|Φ(r)|24πr2dr=1    (12)

Let us minimize the energy functional

E=22m0(Φ(r)2Φ(r))4πr2dr + 0mVG[Φ(r)]|Φ(r)|24πr2dr   (13)

Using this Gaussian as a trial function, and which generates the regular potential at the origin VG[Φ(r)]=GmrErf(rσ)  given by equation (8) after solving Poisson's equation (7).2 The integrals to be evaluated in equation (13) are of the form

0(x43x2) ex2dx=38πErf(x)14ex2x(2x23)    (14)

2Which is also related to the incomplete gamma function γ(12;r)=πErf(r)

0xErf(x)ex2dx=14(2Erf(2x)2ex2Erf(x))    (15)

After performing the definite integrals we find that

E(σ)=3π42mσ22πGm2σ     (16)

σmin=3π222Gm3    (17)

And inserting this value of σ  into E(σ)  gives

Emin=23π3/2G2m52=0.119 G2m52     (18)

Which is a satisfactory value since it is above the lower energy bound

Ebound=329π2G2m52=0.360G2m52   (19)

Derived by.27 and it is also close to the value 0.163(G2m5/2)  obtained numerically by.2226 We can also verify that the value of σmin  given by equation (17) is consistent with the virial theorem |U |= 2T, stating that the absolute value of the potential energy is twice the kinetic energy. It is also worth mentioning that a trial exponential ψ(r)=(k3/π)1/2ekr  leads to an upper energy bound for the ground state of27

E0   75512  G2m52 = 0.146  G2m52       (20)

Which is close to the value found numerically by.2226 However the series expansion of ekr  involves even and odd powers of r  which is not the case of the numerical solutions provided by.2226 The spherically-symmetric solutions of the stationary Schrödinger-Newton equations have been solved numerically by many authors.2226 They have demonstrated numerically the existence of a discrete set of “bound-state” solutions which are everywhere finite and smooth (and which are associated with finite energy eigenvalues), but which separate ever decreasing intervals of partial solutions which diverge alternately to plus or minus infinity.

The value found for the ground state energy turned out to be

E0 =  0.163  G2m52 = 0.163 (mMplanck)5Mplanck c2   (21)

These numerical values for the energy are very small for masses much smaller than the Planck mass.

 

The width (spread) σ of the Gaussian wave-function is measured in units of (2/G2m5) , which translated into Planckian units is (LP /LS)3(2LP) , where LP is the Planck length (2G/c3)1/2 , and LS = 2Gm/c2 is the Schwarzschild radius. It was argued by the authors22 that for a nucleon mass m the value of σ  is vast and is of order of 1024 cm . The corresponding time Δt = /ΔE  for the largest (in magnitude) energy is about of 1053 seconds for the mass of the nucleon, and is of the order of 1 second for 1011 nucleon masses. This is perfectly satisfactory for the state vector reduction of,1 because it tells us that the state of a single nucleon will not self-reduce on a timescale of relevance to any actual particle, in agreement with observation. For large collections of particles, on the other hand, the reduction time can become important.

The coupled system of differential equations (1,2) can be recast after integrating twice, and using dimensionless variables S, V , as22

S(r) = S0 1l2 r0x (1  xr) S(x) V(x) dx   (22)

V(r) = V0 1l2 r0x (1  xr) S2(x) dx     (23)

The value of V0  must be V0 > 0  to ensure convergence of S(r) and V(r)  at r   . Scaling arguments allow one to choose V0 = 1 . The numerical solutions to equations (22,23) foundby,22 when V0 = 1 , are

S(r) = S0 (1 16 r2l2 + (S20 + 1)120 r4l4 + ....   )   (24)

V(r) =  (1 S206 r2l2 + S20 60 r4l4 + ....   )     (25)

The wave-functions are Ψ(r) =αl2S(r)  , and where α,β are defined by

α   [28πGm2]1/2, β   22m    (26)

And l is a physical length parameter (the gravitational analog of the Bohr’s radius) given by l = 2/ Gm3 , such that β / l2= 12 (G2m5/ 2), .

The energy eigenvalues are E = U(r) + βl2 V(r) .Because U(r= 0)  is of the form  × 0  which is undefined, it is more convenient to evaluate the energy at r =  where  U() vanishes, as follows2226,28

E = U(r = )  +  βl2 V(r = ) = βl2  (V0  1l2  0x S2(x) dx),  V0 =  1   (27)

The values of S0  are fine-tuned such that the ground state wave-function has no zeros, it is bounded at the origin and vanishes at infinity. By demanding that Ψ and U are finite and smooth everywhere, the authors showed that the n-th eigen function has n zeros and the wave-functions are normalizable. The corresponding energy eigenvalues are negative, converging monotonically to zero as n increases. Each bound-state is unstable in the sense that infinite precision is required in the initial value of S (r= 0) = S0  to ensure that the solutions do not diverge to infinity as r increases. For the ground state, the numerical value of S0 fell in the range given by 1.088< S0 <1.090  and it led to the ground state energy E0 =  0.163  G2m52 .

For further details of how to obtain other energy eigen values and eigen functions by choosing different values for S0 we refer to.2336 The study of the Newton-Schrödinger equations in D dimensions other than D= 3 can be found in.28

A careful inspection of the work by2226,28 inspired us to find the remarkable numerical coincidence provided by the definite integral

0e(y2+y4)y2dy=0.1600.163=12(11l20xS2(x)dx)    (28)

(We set Vo=1 ). The normalization of the wave function Ψ=αl2S(r)

α2l404πr2S2dr=1   (29a)

Allows to recast the right-hand side of (28) as

α22l404πr2S2dr12l20xS2(x)dx     (29b)

After relabeling the variable r  for x  in the above expression, equation (28) becomes

0.160=0e(y2+y4)y2dy12  0(4πα2ly1)yS2(y)dy=0.163   (30)

Which allows to identify the variables yxl=rl , and basically equate the dimensionless integrals. However this does not mean that the integrands are the same. The integral in the right-hand side of equation (30) is evaluated after inserting the value of 4πα2/l=12 . The expression for S2(r) corresponding to the ground state is derived from equation (24) after inserting a value of So1.088 (lying in the interval [1.088,1.090] ). The other “bound" states require different values of So,n  yielding different expressions for Sn(r)  (Sn(r=0)=So,n), and which have n  nodes (zeros). Next we shall present the novel and most salient results of this section. To our knowledge these findings below are new. The following remarkable numerical coincidences for the values of the remaining (negative) energy eigenvalues E1,E2,E3,..... have also been found. To obtain the values for the first excited state we replace the integral in the left-hand side of (28) for:

n=1:1220e(y2+y4+y6)y2dy=0.03020.0308   (31)

To get the second one

n=2:1320e(y2+y4+y6+y8)y2dy=0.01200.0125   (32)

The third one

n=3:1420e(y2+y4+y6+y8+y10)y2dy = 0.00641  0.00675        (33)

The fourth one

n=4:1520e(y2+y4+y6+y8+y10+y12)y2dy=0.003990.00421   (34)

And so forth..... The pre-factors in front of the integrals for the n -th energy eigenvalue are (n+1)2 , which are “reminiscent” of the Balmer series for the Hydrogen atom, and the arguments of the negative exponentials are y2+y4++y2(y+2) . The authors22 plotted the ten energy eigenvalues as functions of n and found that the slope of log(n)  versus log(E(n)) was not 2 .22 However, the slope is asymptotically close to 2 .35 which would be the exact value for the Hydrogen atom as previously note by Bernstein et al.2326

Using these expressions in equation (28), and equations (31-34), we find that energy values are remarkably close to the numerical results obtained in,35 and given by the numbers in the right-hand side of equations (28, 31-34). We don"t believe this is a numerical coincidence and could point to the fact that integrability may underlie the solutions of the stationary spherically symmetric Newton-Schrödinger equations. It was emphasized by2226,28 that one would need to know the values of Sn(r=0)=So,n  with infinite precision in order to ensure that Sn(r)  does not shoot off to ±  at a finite value of r . All the numerical results appearing in the right-hand side of equations (28, 31-34) are obtained by narrowing in the values of So,n  within certain domains. For this reason we find the analytical results in the left-hand side of equations (28,31-34) very appealing.

To conclude this section we shall recur to the virial theorem <U>=2<Τ>  E=<T+U>=<T>  to write the most general expression for the energy after integration by parts, in the form

En=<T>n=22m(Ψn(r))*2Ψn(r)d3r=22m|(Ψn(r))|2d3r1(n+1)2G2m520e(y2+y4+y6++y2(n+2))y2dy   (35)

The wave-functions must be normalized and vanish at ± . One must emphasize that one is comparing (roughly equating) the values of the integrals in (35) and not the integrands.

It is clear that one cannot equate the integrands in equation (35). By a simple inspection one can see that there are zeros (besides r=0 ) in the left hand side, while in the right hand side one has zeros only at r=0 . If one were to equate the integrands one would arrive at another contradiction. In the spherically symmetric case, for real-valued wave-functions, and after setting y=r/l , it gives

2l2myΨny2πy21n+2G2m52ey2+y4+y6++yn+y21n+212πl3ey2+y4+y6++yn+   (36)

Given Ψn an even, or an odd function, for n= even, odd, respectively, the left hand side is always even due to the squaring of the derivatives, as it should, since the right hand side of (36) is an even functions.3 For this reason, if one is going to take the square root of equation (36) we must choose n=odd Ψ= even. Hence

yΨn(y)1(n+1)12πl3e12(y2+y4+y6++y2(n+2)),n=oddyΨn(y)1(n+1)12πl3e12(y2+y4+y6++y2(n+2)),n=odd   (37)

Integrating (37) between 0 and y we arrive finally

Ψn(y)Ψn(0)1(n+1)12πl3y0e12(y2+y4+y6++y2(n+2))dy,n=odd   (38)

We still need to check that vanishes at , and include normalization constant to enforce. |Ψ|2d3r=1 .When n=odd, Ψ(0)=0  because anti symmetric functions must vanish at the origin. 3This assumes that one can extend to extend r  to negative values r<0 , which is not unreasonable because r=±x2+y2+z2 . Black-hole solutions can be extended to r<0 . The Schwarzschild metric solution is invariant under rr,mm .

Here is where the contradiction arises. The integral in the right-hand side is not zero when y= . It is given by a finite number. This would force Ψn()=0  since Ψn(0)=0 , for n = odd. Since the wave-functions do not vanish at  these solutions are unphysical. For this reason one cannot equate the integrands in equation (35) only the integrals which can be equated.

To conclude this section, based on the numerical results by2226,28 we have arrived at the integrals.

y0(yΨn(y))2y2dy1(n+1)212πl3y0e(y2+y4+y6++y2(n+2))y2dy,n=0,1,2,  (39)

Which furnish implicitly the stationary spherically symmetric wave-function solutions to the Newton-Schrödinger equation in terms of integrals involving generalized Gaussians. The energy eigen values are provided by the left hand side of equations (28,31-34). Equations (39) must be supplemented by the normalization condition of the wave-function. The time-dependent evolution of the Schrödinger-Newton equations has been studied by many authors, in particular.3639 The experimental tests of the validity of the nonlinear Newton-Schrödinger equation pose a technologically formidable challenge due to the weakness of gravity and the difficulty of controlling quantum coherence.39

Infinite derivative gravity, modified Newton-Schrödinger equation and Schwarzschild atoms

Since Quantum Mechanics is notoriously non-local, it is not farfetched that a theory of Quantum Gravity may require modifying Einstein’s theory of gravity (and other local theories of gravitation) to include a modified gravitational theory involving infinite derivatives, which by construction, is non-local. It turned out that the infinite derivative gravity (IDG) can resolve the problem of massive ghosts as well as it may avoid the singularity of the Newtonian potential at the origin, when one chooses the exponential of an entire function. This model is also named super-renormalizable quantum gravity.4042 However, one does not understand fully how this non-local gravity could provide a regular potential. It was argued that the cancellation of the singularity at the origin is an effect of an infinite amount of hidden ghost-like complex poles.42,43

A regular potential at the origin of the form (8) has been studied by several authors44 in connection to infinite derivative gravity42,43 which is ghost-free and renormalizable when one chooses the exponential of an entire function in the construction of the infinite-derivative gravitational (IDG) action SIDG .42,43 For this IDG case, the corresponding Newtonian potential generated from the delta function is non-singular at the origin. However, the authors44 explicitly showed that the source generating this non-singular potential is given not by the delta-function due to the point-like source of mass, but by the Gaussian mass distribution. This explains clearly why the IDG with the exponential of an entire function yields the finite potential at the origin. The infinite-derivative (non-local) modified Poisson equation associated to a point-mass particle at r=0 is given by4244

(eσ2422)V=4πGmδ3(r)=Gmδ(r)r2

σ  Is a length scale which can be taken to be equal to the Planck-scale. Such equation (40) leads to identical solutions for the potential V  as the solutions for the potential in the ordinary Poisson equation sourced by a Gaussian mass distribution,44 and which is a smeared version of the delta function mass distribution. This can be shown by taking the 3D  Fourier transform of equation (40)

eσ24k2k2˜V(k)=Gm˜V(k)=Gmeσ24k2k2 

And then performing the inverse 3D  Fourier transform it yields VG(r)=GmrErf(rσ) , see44 for further details. One can generalize the Newton-Schrödinger coupled system of equations (1,2) by replacing the ordinary Poisson equation with the modified non-local Poisson equation associated with infinite-derivative gravity (IDG)

(eσ2422)VIDG(r)=4πGρ=4πGm|Φ(r)|2    (42)

In this case

VIDG(r)=Gm|Φ(r')|2|rr'|d3r   

Therefore to find (numerical) solutions of the highly nonlinear and nonlocal modified Newton-Schrödinger equation

EΦ(r)=22m2Φ(r)+mVIDG[Φ(r)]Φ(r)  

Becomes more problematic. However, solutions to the infinite-derivative modified Poisson equation are not that difficult to find. For example, in the case when ρ(r)  is given by a Gaussian profile, after performing the Fourier transform procedure it gives VIDG=Gm2rErf(r2σ) , which is almost identical to Gm2rErf(rσ) , the main difference being that Erf(rσ)=Erf(r2σ) .

Bohm’s quantum potential VQ=22m(2ρ/ρ)  has a geometrical description as the Weyl scalar curvature produced by an ensemble density of paths associated with one, and only one particle45,46 This geometrization process of quantum mechanics allowed to derive the Schrödinger, Klein-Gordon45,46 and Dirac equations.47,48 M.ost recently, a related geometrization of quantum mechanics was proposed49 that describe the time evolution of particles as geodesic lines in a curved space, whose curvature is induced by the quantum potential. This formulation allows therefore the incorporation of all quantum effects into the geometry of space-time, as it is the case for gravitation in the general relativity. Based on these results we propose the following nonlinear quantum-like Bohm-Poisson equation for static solutions ρ=ρ(r) .

2VQ=4πGmρ22m2(2ρρ)=4πGmρ   (45)

Such that one could replace the nonlinear Newton-Schrödinger equation for the above non-linear quantum-like Bohm-Poisson equation (45) where the fundamental quantity is no longer the wave-function Ψ  (complex-valued in general) but the real-valued probability density ρ=Ψ*Ψ .

It has been proposed by2931 to give up the description of physical states in terms of ensembles of state vectors with various probabilities, relying instead solely on the density matrix as the description of reality. The time evolution of ρ  is governed by the Lindblad equation.4 The authors31 also investigated a number of unexplored features of quantum theory, including an interesting geometrical structure- which they called subsystem space-that they believed merits further study.

The infinite-derivative-gravity generalization of equation (45) is

22m(eσ2422)(2ρρ)=4πGmρ

The above equation is nonlinear and nonlocal. If one wishes to introduce a temporal evolution to ρ  via a Linblad-like equation, for instance, this would lead to an over determined system of differential equations for ρ(r,t) . This problem might be another manifestation of the problem of time in Quantum Gravity. Naively replacing 2  in equations (45-46) for the D’Alambertian operator μμ,μ=0,1,2,3 has the caveat that in QFT ρ(xμ) no longer has the interpretation of a probability density (it is now related to the particle number current). For the time being we shall just focus on static solutions ρ(r) . Integrating (45) gives the integral-differential equation for ρ(r)

22m(2ρρ)=Gmρ(r)|rr|d3r

4To be more precise it is the Gorini-Kossakowski-Sudarshan-Lindblad equation

The right hand side of (47) can be written as

GmMeff(r)r,Meff(r)=rρ(r)|rr|d3r

Where extreme caution must be taken because Meff(r)  is not the same as the enclosed mass inside a spherical region of radius r  encircling the origin. It is convenient to write (47) in this form (48) because it reminds us of a “Schwarzschild atom" analog in the spherically symmetric case, where the g00 metric component for signature (+,,,) , and c=1 , is

g00(r)=(12GMeff(r)r),grr=1g00(r),Meff(r)=Meff(r),c=1   (49)

See33,34 for many references related to the solutions (49). In the weak field limit, for slowing moving masses, one has g00η00+h00=1+2V,(c=1) , and from equations (47-49) one arrives at the relation between the temporal components of hμν  and the matter/probability distribution

h00(r)=2m2(2ρ(r)ρ(r))=2GMeff(r)r,c=1  (50)

The equations (45-50) reflect the back-reaction that the geometry has no matter, and in turn, the effect that this matter has on the geometry. Such equations (45-50) reflect a nonlinear feeding loop mechanism between matter and geometry. The probability distribution ρ cannot be arbitrary due to the restrictions imposed by equations (45,46). One may envisage the “Schwarzschild atom" as a spherically symmetric probability cloud of matter which curves the geometry, and in turn, the geometry back-reacts on this matter cloud perturbing its initial distribution over the space, which in turn will affect the geometry, and so forth until static equilibrium is reached. The author32 described the gravitational degrees of freedom of the Schwarzschild black hole by one free variable and introduced a “Schrödinger equation” for the Schwarzschild black hole corresponding to this model. The mass spectrum of the black hole was obtained as such as it can be observed by an observer very far away and at rest relative to the black hole. Such “Schrödinger equation” implied that there is no singularity inside the Schwarzschild black hole, and that the black hole has a certain ground state in which its mass is non-zero. A modern treatment of this approach can be found in.33,34 We believe the picture of this “Schwarzschild atom" model will cast some light into Quantum Gravity.

Conclusion

Exact solutions to the stationary spherically symmetric Newton-Schrödinger equation were proposed in terms of integrals involving generalized Gaussians. The energy eigenvalues were also obtained in terms of these integrals which agree with the numerical results in the literature. A discussion of infinite-derivative-gravity followed which allows generalizing the Newton-Schrödinger equation by replacing the ordinary Poisson equation with a modified non-local Poisson equation associated with infinite-derivative gravity. Finally we proceeded to replace the nonlinear Newton-Schrödinger equation for a non-linear quantum-like Bohm-Poisson equation involving Bohm’s quantum potential, and where the fundamental quantity is no longer the wave-function Ψ  but the real-valued probability density ρ .

Recently, solutions to the nonlinear Bohm-Poisson equation were found50 with cosmological applications. We envisioned the present Universe’s matter density distribution as being proportional to the probability density, in the same vain that one can view an electron orbiting the Hydrogen nucleus as an “electron probability cloud" surrounding the nucleus, and whose mass density distribution is ρ=meΨ*Ψ , where Ψ(r) the stationary wave-function solutions to the Schrödinger equation are. In doing so we were able to obtain the observed vacuum energy density after introducing an ultraviolet (very close to the Planck scale) and an infrared (Hubble radius) scale, and explained the origins of its repulsive gravitational nature. By inspection one can see that if ρ(r)  is a solution to the Bohm-Poisson equation (45) with G>0 , and then ρ is a solution with . A negative gravitational constant is tantamount to repulsive gravity. For this reason, we believe that the Bohm-Poisson equation (45), and its relativistic generalization, deserves further investigations.

Acknowledgments

We thank M. Bowers for her assistance and to the referee for providing important references.

Conflicts of interest

Author Declare there is no conflict of interest.

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