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Record 1 of 1Title: THE MICROSCOPIC-MACROSCOPIC SCALE TRANSFORMATION THROUGH A CHAOS SCENARIO IN THE FRACTAL SPACE-TIME THEORY Author(s): Munceleanu, GV (Munceleanu, G. V.); Paun, VP (Paun, V. -P.); Casian-Botez, I (Casian-Botez, I.); Agop, M (Agop, M.)Source: INTERNATIONAL JOURNAL OF BIFURCATION AND CHAOS Volume: 21 Issue: 2 Pages: 603-618 DOI: 10.1142/S021812741102888X Published: FEB 2011 Times Cited in Web of Science: 1 Total Times Cited: 1 Cited Reference Count: 29 Abstract: Considering that the particle movement takes place on fractal curves, the mathematical and physical aspects in fractal space-time theory are analyzed. In such context, the harmonic oscillator problem implies that the microscopic-macroscopic scale transition could be associated with an evolution scenario towards chaos. The splitting of the plasma plume, generated by laser ablation, into two patterns, has been successfully reproduced through a numerical simulation using the fractal hydrodynamic model. For the free time-dependent particle in a fractal space-time, the uniform movement is naturally obtained by a specific mechanism of vacuum polarization.Accession Number: WOS:000289468300018 Language: EnglishDocument Type: ArticleAuthor Keywords: Fractal space-time theory; microscopic-macroscopic scale transitionKeyWords Plus: HYDRODYNAMIC MODEL; LASER-ABLATION; RELATIVITYAddresses: [Munceleanu, G. V.] Alexandru Ioan Cuza Univ, Fac Phys, Iasi 700506, Romania [Paun, V. -P.] Univ Politehn Bucuresti, Fac Sci Appl, Dept Phys 1, Bucharest 060042, Romania [Casian-Botez, I.] Gh Asachi Tech Univ, Fac Elect Telecommun & Informat Technol, Iasi 700050, Romania [Agop, M.] Univ Sci & Technol Lille, Lab Phys Lasers Atomes & Mol, UMR 8523, F-59655 Villeneuve Dascq, France [Agop, M.] Gh Asachi Tech Univ, Dept Phys, Iasi 700050, RomaniaReprint Address: Munceleanu, GV (reprint author), Alexandru Ioan Cuza Univ, Fac Phys, Blvd Carol 1,11, Iasi 700506, RomaniaPublisher: WORLD SCIENTIFIC PUBL CO PTE LTD Publisher Address: 5 TOH TUCK LINK, SINGAPORE 596224, SINGAPORE Web of Science Category: Mathematics, Interdisciplinary Applications; Multidisciplinary SciencesSubject Area: Mathematics; Science & Technology - Other TopicsIDS Number: 749LL ISSN: 0218-1274 29-char Source Abbrev.: INT J BIFURCAT CHAOS ISO Source Abbrev.: Int. J. Bifurcation Chaos Source Item Page Count: 16
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International Journal of Bifurcation and Chaos, Vol. 21 , No. 2 (2011) 603- 618 © World Scientific Publishing Company DOI: 10.1142/ S021812741102888X
THE MICROSCOPIC-MACROSCOPIC SCALE TRANSFORMATION THROUGH A CHAOS
SCENARIO IN THE FRACTAL SPACE-TIME THEORY
G. V. MUNCELEANU Faculty of Physics, "Al. I. Cuza " University, Blvd. Carol I No. 11, Iasi 700506, Romania
V.-P. PAUN Physics Department I,
Faculty of Applied Sciences, ~
Politehnica University of Bucharest, Bucharest 060042, Romania
paun@physics. pub. ro
I. CASIAN-BOTEZ Faculty of Electronics,
Telecommunication and Information Technology, "Gh. Asachi" Technical University,
Iasi 700050, Romania
M.AGOP Laboratoire de Physique des Lasers, Atomes et Molecules (UMR 8523) ,
Universite des Sciences et Technologies de Lille, Villeneuve d 'Ascq cedex 59655, France
Department of Physics, "Gh. Asachi" Technical University,
Iasi 700050, Romania
Received May 24, 2010
Considering that the particle movement t akes place on fractal curves, the mathematical and physical aspects in fractal space-time theory are analyzed. In such context , the harmonic oscillator problem implies that the microscopic-macroscopic scale transition could be associated with an evolution scenario towards chaos. The splitting of the plasma plume, generated by laser ablation, into two patterns, has been successfully reproduced through a numerical simulation using the fr act al hydrodynamic model. For the free time-dependent particle in a fractal space-time, the uniform movement is naturally obtained by a specific mechanism of vacuum polarization.
Keywords : Fractal space-time theory; microscopic-macroscopic scale transit ion.
603
604 G. V. Munceleanu et al.
1. Introduction
The complex dynamical systems which display chaotic behavior are recognized to acquire selfsimilarity and manifest strong fluctuations at all possible scales [Mandelbrot, 1982; Gouyet, 1992; Nottale, 1993]. Since the fractality appears as an universal property of the complex systems, it is necessary to construct a new physics, entitled fractal physics maybe, either through the nondifferentiability property or through the transfinite sets, in the same manner as the Cantor set and its physical implications, in El Naschie's model [El Naschie et al., 1995; Weibel et al., 2005], for example. The mathematical procedures are in agreement with similar items [Olteanu et al., 2005; Cresson, 2005] and the support of relevant physical processes is based on the references [N ottale et al., 2006; Celerier & Nottale, 2004]. Thus, both the scale relativity (SR) and the transfinite physics were developed. In the following, let us refer only to the SR Nottale's model i.e. to a continuous but nondifferentiable physical model. The SR uses the word "nondifferentiability" in its general meaning, denoting a set that shows structures at all scales and is, thus, explicitly resolutiondependent.
The SR model is based both on the fractal space-time concept and on a generalization of Einstein's principle of relativity to scale transformations. In other words, the SR model is built by completing the standard laws of classical physics (motion in space-time) by new scale laws. We can state that "the space-time resolutions are used as intrinsic variables, playing for the scale transformation the same role as played by velocities for motion transformation" [Nottale, 1993; Nottale et al., 2006; Celerier & Nottale, 2004]. Also, in the present work, the harmonic oscillator problem is analyzed using a generalized Nottale 's model in its hydrodynamic version.
In fact, three scales of interaction of SR were developed:
(i) a "Galilean" version corresponding to the standard fractals with constant fractal dimensions [Mandelbrot, 1982; Gouyet, 1992] and which involves quantum mechanics [Nottale, 1993; Nottale et al., 2006; Celerier & Nottale, 2004; Gottlieb et al., 2006; Agop et al., 2005; Agop et al., 2008b];
(ii) a special scale-relativistic version which implies the high energy physics [Nottale, 1993];
(iii) a "general scale-relativistic" version which implies the cosmology [Nottale, 1993, 1997; Agop et al. , 2007; Agop et al., 2008c].
In the accepted vision, the microscopic-macroscopic scale transition could be associated with an evolution scenario towards chaos.
This paper is structured in eight sections, with the introduction as the first. In the second, the mathematical and physical aspects in fractal spacetime are presented. The geodesics concept is the subject of Sec. 3 and, in Sec. 4, the hydrodynamic version in the fractal space-time is developed. In Sec. 5, the harmonic oscillator in fractal space-time is offered as an example and the hydrodynamic behavior of laser ablation plasma will be established in Sec. 6. Section 7 is devoted to the free particle in the fractal space-tim~ category and, finally, the conclusions are included in Sec. 8.
2. Mathematical and Physical Aspects in Fractal Space-Time
Let us suppose that the motion of particles takes place on continuous but nondifferentiable curves (fractal curves) with an arbitrary and constant fractal dimension, Dp. There is a diversity of fractal dimensions type, but Kolmogorov dimension and Hausdorff dimension are most frequently used. For example, we present below the current definition of Hausdorff dimension [Olteanu~et al., 2005]. Let A C rytn and let C1, C2, ... be an open cover of it. More precisely, an open cover of A is defined by covers Ci such that A C LJ~1 Ci. Then, for every positive number s and E, let h~(A) = inf{Li diam(Ci) 8 I (Ci)i2'.0 is an open cover of A, diam (Ci)< E}, so that the s-dimensional Hausdorff measure of A is h8 (A) = limc:-.o h~(A).
It can be proved that there is a number DH(A) such that h8 (A) = oo if s < DH(A) and h8 = 0, ifs > DH(A). The number DH(A), the Hausdorff dimension of A, can be zero, infinite or a positive real number.
For the fixed fractal dimension type, we shall operate with it up to the end. In this paper, the Hausdorff's dimension is used.
The nondifferentiability, according with Cresson's mathematical procedures [Cresson, 2005] and Nottale's physical principles [Nottale, 1993; Nottale et al., 2006; Celerier & Nottale, 2004], implies the following:
(i) a continuous and a nondifferentiable curve (or almost nowhere differentiable) is explicitly
The Microscopic-Macroscopic Scale Transformation Through a Chaos Scenario 605
scale dependent, and its length tends to infinity, when the scale interval tends to zero. In other words, a continuous and nondifferentiable space is fractal, in the general meaning given by Mandelbrot to this concept [Mandelbrot, 1982];
(ii) there is an infinity of fractal curves (geodesics) related to any couple of points (or starting from any point), and this is valid for all scales;
(iii) the breaking of local differential time reflection invariance. The time-derivative of a function F can be written two-fold:
(iv)
dF = lim F(t + dt) - F(t) dt dt---+D dt
= lim F(t) - F(t - dt). dt-->D dt
(1)
Both definitions are equal in the differentiable case. In the nondifferentiable situation, these definitions fail, since the limits are no longer defined. "In the framework of scale relativity, the physics is related to the behavior of the function during the "zoom" operation on time resolution 8t , here identified with the differential element dt ( "substitution principle"), which is considered as an independent variable. The standard function F(t) is therefore replaced by a fractal function F(t, dt) (for details see [Cresson, 2005]) explicitly dependent on the time resolution interval, whose derivative is undefined only at the unobservable limit dt ---t 0 [Nottale, 1993]. As a consequence, this leads us to define the two derivatives of the fractal function as explicit functions of the two variables t and dt
d+F = lim F(t + dt , dt) - F(t) dt dt-->D+ dt
(2a)
d_ F = lim F(t , dt) - F(t - dt, dt). dt dt---+D- dt
(2b)
The sign, +, corresponds to the forward process and, -, to the backward process; the differential of a fractal function F(t, dt) can be expressed as the sum of two differentials, one which is not scale-dependent , dF'(t) , and the other dependent on it , dF"(t) , therefore [Cresson, 2005]
dF ( t , dt) = dF' ( t) + dF" ( t, dt) . ( 3)
Particularly, the differential of the generalized coordinates, d±X(t, dt), can be decomposed as follows
where d±x(t) is the "classical part" and d±~(t , dt) is the "fractal part". Starting from here, multiplying by dt.__ 1 and using the substitutions
V _ d±X ± - dt )
d±X V± = dt '
d±~ li± =--
;:;o dt
we obtain the velocity field
(5a)
(5b)
(5c)
(6a,b)
( v) the fractal part of F, i.e. F", satisfies the relation [Cresson, 2005]
IF"(t) - F"(t') I ~it - t' l6 (7)
where 8 depends on the fractal dimension Dp (for details see [Notta'le, 1993; Cresson, 2005]). Particularly, the differential of the "fractal part" of d±X, becomes
~(8a ,b)
or more, as an equality relation:
( d~~i) = ( ~) D1
F • (9a,b)
Written as
A ( dt ) ( D1
p ) - l d±~i = - - dt.
T T (lOa,b)
Equations (9a,b) imply the temporal scales 8t and T, and the length scale ,\, respectively. The significance of time dt and T results from Random Walk (Brownian motion) or its generalization, Levy motion [Nottale, 1993]. The differential time dt is identified by the resolution time ("substitution principle" [Nottale, 1993; Nottale et al., 2006; Celerier & Nottale, 2004]) , 8t = dt , while T
corresponds to the fractal-nonfractal transition time. ,\ is a characteristic length, for example, of Planck's or de Broglie's type (for details see [Nottale, 1993]) ;
606 G. V. Munceleanu et al.
(vi) by the relation (10a,b) the velocity field becomes
. . . . ,\ ( T )1-(:tf-) V± = v± + u± = v± + -:; dt F .
(lla,b)
The transition scale T yields two distinct behaviors of the speed, depending on the resolution at which it is considered, since V± ___, v~ when dt » T, and Vi___, u~ , when dt « T .
Obviously, the fractal dimension Dp also plays an important role in relations ( lla, b), but we shall consider this problem later on;
(vii) the local differential time reflection invariance is recovered by combining the two derivatives, d+/dt and d_ /dt, in the complex operator [Nottale, 1993; Nottale et al., 2006; Celerier & Nottale, 2004]
We call this procedure "an extension by differentiability" (Cresson's extension - for details see [Cresson, 2005; Gottlieb et al., 2006]). Applying this operator to the "position vector" yields a complex speed
A dX V=
dt
= ! (d+X + d_X) _ !_ (d+X - d_ X) 2 dt 2 dt
V + +V_ .V +- V -2 - i 2
i - 2 [ ( v + - v _) + ( u+ - u_)]
= V-iU (13)
with
V ++ V_ 1 V =
2 = 2 [ ( V + + V _) + ( U+ + U_) ]
(14a) V+-V- 1
U = 2
= 2 [ ( V + - V - ) + ( U+ - U_ )]
(14b)
(viii)
(ix)
The real part , V, of the complex speed V, represents the standard classical speed, which is differentiable and independent of resolution, while the imaginary part, U, is a new quantity arising from fractality, which is nondifferentiable and resolution-dependent. In the usual classical limit , dt » T,
V+ =V_ =V,
U+ = U_ = 0
so that
V=v, U = O.
In the limit, dt « T ,
and
V+ =v-= 0,
u+~ u_ = u
V = u, U = O;
(15a)
(15b)
(16)
(17a)
(17b)
(18)
in order to t ake into consideration for the infinity of geodesics in the bundle, for their fractality and for the two valuedness of the derivative which all come from the nondifferentiable geometry of the space-time continuum, one therefore adopts a generalized statistical fluid like description, where instead of a classical deterministic speed or of a classical fluid speed field, one uses a doublet of frac-
·:-.. tal functions of space coordinates anJ time which are also explicit functions of "resolution time" [Nottale, 1993; Nottale et al., 2006; Celerier & Nottale, 2004]. Thus, the average values of the quantities must be considered in the previously mentioned sense [Nottale, 1993; Nottale et al., 2006; Celerier & Nottale, 2004]. Particularly, the average of d±X is
\d±X} = d±x (19)
with
(20a,b)
in such an interpretation, the "particles", are identified with the geodesics themselves. As a consequence, any measurement is interpreted as a sorting out (or selection) of the geodesics by the measuring device [Nottale, 1993].
Let us now assume that the movement curves (continuous, but nondifferentiable) are immersed in a three-dimensional space, and that x of components xi ( i = 1,"3) is the position vector of a point on the curve. Let us also consider a function f (X, t) and the
The Microscopic-Macroscopic Scale Transformation Through a Chaos Scenario 607
following Taylor series expansion, up to the second order:
of d± J = at dt + v f . d± x
1 82 f . . + 2 ()Xi()XJ d±Xid±X1
. (21a,b)
The relations (21a,b) are valid in any point of the space-time manifold and also for the points "X" on the fractal curve which we have selected in relations (21a,b). From here, the forward and backward average values of this relation, take the form:
(22a,b)
We make the following stipulations: the mean values of the function f and its derivates coincide with themselves and the differentials d±Xi and dt are independent. Therefore, the averages of their products coincide with the product of average. Thus, Eqs. (22a,b) become:
of d±f = 8t dt + "V f (d±X )
1 321 . . + 2 8Xi8XJ (d±Xid±XJ) (23a,b)
or more, using Eqs. ( 4a, b) with the properties (20a,b),
of d±f = at dt + '\1 j d±X
1 32 f (d id j (dci dcJ ) ) + 2 ()Xi()XJ ±X ±X + '>± '> ± .
(24a,b)
Even the average value of the fractal coordinate, d~~ , is null [see ( 20a, b)], for the higher order of the fractal coordinate average, the situation can be different. Let us focus on the mean (d~±d~~ ). If ii= j , t his average is zero due to the independence of de and d~j. So, using (lOa,b) we can write (see also [Cresson , 2005; Agop et al., 2008a, 2008b, 2008c]):
(25a,b)
with
. . { 1 if i = j 5i1 =
0 ifi-=/=j
and we had considered that
(d~~d~~) > 0 and dt > 0
(d~i_d~~ ) > 0 and dt < 0.
Then, Eqs. (24a,b) may be written under the form:
02 f .. A 2 ( dt) ( D2F ) - 1 ± . .JiJ _ - dt. ()Xi()XJ 2T T
(26a,b)
If we divide by dt, and neglect the terms which contain differential factors (for details on the method see [Gottlieb et al., 2006]) , Eqs. (26a,b) are reduced to:
d±f = of v VJ± >.2 (dt)(dF)-1 ~f
dt Ot + ± 2T T
~(27a,b)
with "V2 = 2=i 82 I 8X'f. These relations also allow us to define the operator,
d± 0 A 2 ( dt) ( D2
F ) - l -=-+V±"V± - - ~ dt Ot 2T T
(28a,b)
(see also [Agop et al., 2008b]). Under t hese circumstances, let us calculate dj / dt. Taking into account Eqs. (12), (13) and (28a,b), we obtain:
df = ~ [(d+f d_f) - i (d+f - d_f)] dt 2 dt + dt dt dt
= - - + v + "V f + - - ~f 1 [ ( 0 j A 2
( dt ) ( D2
F ) - l )
2 Ot 2T T
( 0 j ). 2 ( dt ) ( D
2
F ) - l ) l + Ot + V - '\1 j - 2T -; ~j
608 G. V. Munceleanu et al.
i [ (a j ,\ 2
( dt ) ( D2
F )- l ) - - - + v + \7 f + - - b.f 2 at 2T 7
- ( ~~ + v - \7 f -~: ( ~) ( ,;F )- 1 1'f) l =af (V++V _ _ iV+-V- )v1
dt + 2 2
A2 (dt) (dF )-l -i- - b.f
27 7
a f A • >-2 ( dt ) ( D
2
F ) -1
= - + v . \7 f - i - - b.f. dt 27 7
(29)
This relation also allows us to define the fractal operator:
d a A >-2 ( dt ) ( D
2
F ) -1
dt = at + V . \7 - i 27 --; 6_. (30)
We now apply the principle of scale covariance (for details see [Nottale, 1993; Nottale et al. , 2006; Celerier & Nottale, 2004]), and postulate that the passage from classical (differentiable) mechanics to the "fractal" mechanics, which is considered here, can be implemented by replacing the standard timederivative, d/ dt, by the complex operator dj dt (this result is the principle of scale covariance given by Nottale in [Nottale, 1993; Nottale et al., 2006; Celerier & Nottale, 2004]).
3. Geodesics in Fractal Space-Time
The inertial principle in its strong covariance form (Nottale 's principle [Nottale, 1993; Nottale et al., 2006; Celerier & Nottale, 2004]) is reduced to an equation of the N avier- Stokes type (geodesics equation) ,
AA A 2 ( 2 ) 1 dV av A A >- ( dt) D F - A
- = - + V · \7V - i - - b. V = 0 dt at 27 7
(31)
with an imaginary viscosity coefficient v
v = i A 2 ( dt) ( D2F )-1 27 7
(32)
This means that the local complex acceleration field , av/ at, the convective term , v . vv, and the dissipative one, b. V, reciprocally compensate at any point of the fractal curve. Moreover , the behavior of the fractal fluid is visco-elastic type or hysteretic type. Such results are in agreement with the opinions given in the books [Agop et al. , 2008a; Ferry & Goodnick, 1997]: the fractal fluid can be described by Kelvin- Voight or Maxwell rheological model with imaginary structure coefficient v. In the case of the irrotational motions:
\7 xV =O (33)
so that the speed field (13) can be expressed through the gradient of a scalar function <I>
(34)
named the scalar potential of the complex speed field: <I> = Re <I> + ilm <I>. Substituting Eq. (34) in Eq. (31) , we see
[ a<I> 1 2 . ,\
2 ( dt ) ( D
2
F ) - l l \7 - + -(\7¢) - i- - b.<I> = 0 at 2 27 7
(35)
and by an integration, a Bernoulli type equation
a.'f.. \ 2 ( d ) ( -2 )- 1
_'±' + ~(\7<I>) 2 - i~ _..!_ DF b.<I> = F(t'}' (36) at 2 27 7
with F(t) being a function which depends only on time. Particularly, for <I> of the form [Nottale, 1993]
. A 2 ( dt ) ( D
2F ) - l
<I> = -i- - ln w 27 7
(37)
where W is a new complex scalar function. For this condition, Eq. (36) takes the form
,\4 (dt) ( D~ ) - 2 ,\
2 (dt) (D2F )-l aw
- - b.w+ - - -472 7 2T 7 at
(38)
From here, "Schrodinger" type geodesics result for F(t) = 0, i.e.
~ (dt) (D~)-2 b.w + >-2 (dt) (D2
F)-1 aw = o. 472 7 27 7 at
(39)
The Microscopic-Macroscopic Scale Transformation Through a Chaos Scenario 609
Particularly, for the movement on fractal curves of the Peano's type, i.e. in the fractal dimension Dp = 2, and Compton's length and temporal scales,
.\=-n-2m0c '
n T=-moc2'
(40a)
(40b)
Equation (55) takes the Schrodinger standard form
n2 aw - t::..w + in- =O. 2mo at ( 41)
4. Hydrodynamic Model in Fractal Space-Time
Replacing the complex speed field (34) in Eq. (31), and separating the real and imaginary parts, we obtain
8V mo at +mo V · \7V = -\7(Q) (42a)
oU .\ 2 ( dt) ( D2
F ) - l at + \7 (V . U) + 2T --:;- \7V = 0
(42b)
where Q is the fractal potential,
Q = - moU2 - mo .\2 (dt) (dF) -1 \7. U. (43) 2 2T T
The explicit form of the complex speed field is given by the expression
(44)
with p being the amplitude and S the phase. Then Eq. (34) with
,2 (d ) (-2 )- 1 . /\ t DF iS
<I>= -i- - ln(fae ) 2T T
( 45)
involves the complex velocity field components
.\2 (dt) (D2F)-l
V=- - \7S 2T T '
(46a)
.\2 (dt) (dF)-l U= - - \7lnp
2T T (46b)
while the fractal potential ( 43), is given by the simple expression
Q = - mo(dt)(D2F) -1 !:::.fa. T VP (47)
For other details see [Halbwachs, 1960; Wilhelm, 1970]. With Eqs. (46a,b) , Eq. (42b) takes the form:
(48)
or, by integration with p =/= 0
~ + \7 · (pV) = T(t) (49)
with T(t) a function which depends only on time. Equation (42a) corresponds to the momentum
conservation law, while~Eq. (49), with T(t) = 0, to the probability density conservation law. So equations:
mo ( 8
8~ + V · \7V) = -\7(Q) (50a)
~~ + \7 · (pV) = 0 (50b)
with Q given by ( 4 7) form the fractal hydrodynamic equations in the fractal dimension Dp. The fractal potential ( 4 7) is induced by the nondifferentiable space-time (for more details see [Agop et al., 2007]). Our results are more general ~ those of Nottale (the movements take place on fractal curves of Peano's type at Compton's space-time scale - i.e. the hydrodynamic model of quantum mechanics [Nottale, 1993; Nottale et al., 2006; Celerier & Nottale, 2004]).
The synchronization of the movements at the differentiable and non-differentiable scales implies V = - U. In such context , Eq. (50b) , through Eqs. ( 46a, b) , become a well-known differential equation for diffusion:
\7p = D!:::.. . Vt P
This equation becomes an important issue in the analysis of Brownian motion at any scale .
In an external potential U, the fractal hydrodynamic equations become
mo ( 0
8~ + V · \7V) = - \7(Q + U) (51a)
~~ + \7 · (pV) = 0. (51b)
610 G. V. Munceleanu et al.
Two types of stationary states are distinguished:
(i) Dynamic states. For a/at= 0 and V-/= 0, i.e. at the differentiable scale, Eqs. (51a,b) give
V (mot - mo2U' - mo;: (~)(,JP) -\· U + U) ~ 0 (52a)
'V·(pV) = O (52b)
namely,
mo V 2 mo U 2 ,\
2 ( dt) ( v2
F )-1
------mo- - \7-U+U=E 2 2 2T T
(53a)
Consequently, the non-fractal inertia, mo V · 'VV, external force, -'VU and the fractal force, - \7 Q, are in balance at every field point -Eq. (52a). The sum of the nonfractal kinetic energy, m V 2 /2, external potential, U and fractal potential, Q, is invariant, i.e. equal to the integration constant E -/= E(r) - Eq. (53a).
pV = \7 x F. (53b)
E = (E) representQ. the total energy of the dynamic system. The probability fl.ow density pV has no sources - Eq. (52b), i.e. its streamlines are closed - Eq. (53b).
(ii) Static states. For a/at = 0 and V = 0, i.e. at the nondifferentiable scale, Eqs. (10a,b) give
n ( mo U2
,\ 2
( dt) ( v2
p ) -1
) v ----mo- - \7-U+U =0 2 2T T
(54a)
i.e.
mo U 2 ,\ 2 ( dt) ( D2
F ) - l ----mo- - 'V·U+U=E.
2 2T T ~(54b)
Thus, the fractal force, - \7 Q and external force - 'VU are in balance at every field point -Eq. (54a). The sum of the external potential, U and fractal potential, Q, is invariant, i.e. equal to the integration constant E -/= E ( r) -Eq. (54b). E = (E) represents the total energy of the static system. Equation ( 51 b) is identically satisfied.
As an illustration of the fractal hydrodynamic formalism, a static fractal system is further analyzed.
5. Harmonic Oscillator in Fractal -Space-Time
This model describes a particle of rest mass mo in a field of the form:
In a stationary state, the one-dimensional current density is constant through Eq. (52b ).
j(x) = p(x)V(x) = C = const. (56)
From here, by imposing the boundary conditions:
p(x = -oo) = p(x = +oo) = 0 (57)
we get C = 0, meaning that the velocity field V(x) is
V(x) = 0. (58)
From ( 58) and ( 46a) , we see that S is constant , i.e. the fluid particles are in phase. Therefore, at the macroscopic (differentiable) scale, we have a coherent fluid with a behavior of either suprafiuidic or supraconductor type. Moreover, a momentum transfer does not exist on the velocity field
The Microscopic-Macroscopic Scale Transformation Through a Chaos Scenario 611
V(x). For a static state, the momentum conservation law, with the restrictions (54b), becomes:
d\fi5 [ E ( fl )2
2] dx2 + 2moD2 - 2D x VP = O,
p(x = - oo) = p(x = +oo) = 0
D = A 2 ( dt) ( D2p )-1 2T T
(59a)
(59b)
(59c)
or further, by introducing the dimensional variable:
(60)
d\fi5 ( E 2) d( 2 + moDO - ( VP = O,
-oo ~ ( ~ +oo, p(( = -oo) = p(( = + oo) = 0.
(61a- c)
A solution p(() = Pn(() exists if and only if the total energy is quantified:
E = 2moDO ( n +}), n = 0, 1, 2,... (62)
The following probability density is found :
( ) - /fl_l_H2 (C)e- e Pn ( - V 2;[j 2nn! n <,, (63)
with the Hermite's polynomials of degree n [Nikiforov & Ouvarov, 1974].
For movement on fractal curves of the Peano's type, i.e. in the fractal dimension DF = 2, and Compton's length and temporal scales, i.e. for D = n/2m0 , from (62) and (63), the usual results of quantum mechanics are obtained. For DF < 2, from (59c), we get dt « T, i.e. the time resolution is much smaller than the fractal-nonfractal transition time, while for DF > 2, from (59c), we get dt » T, i.e. the time resolution is much greater than the fractalnonfractal transition time. Now, using (63), we can build the one-dimensional fractal velocities field:
d ~[ Hn-1(() ] Ux = D dx(lnp) = vDO 2n Hn(() - ( (64)
respectively the fractal potential:
Q = _ 2m0D2
d2
(VP)=_ mou~ _ m Ddux n VP dx2 p 2 ° dx
= moD0(2n + 1 - e) (65)
where we used the relations [Nikiforov & Ouvarov, 1974]:
dH;((() = 2nHn-1(() (66a)
Hn(() - 2(Hn-1(() + 2(n - l)Hn-2(() = 0.
(66b)
Therefore:
(i) There is a nonzero velocity field, (64), generated through a fractal process and hence a transfer of momentum.
(ii) The velocity field (64) "controls", through the fractal potential (65), "the flow regimes" of a fractal fluid.
(iii) The "observable" ~from the clasical quantum mechanics given Jnder the form of quantified energy:
En = Qn + U = 2moDO ( n + 1) (67)
allows the implementation of Reynold's criterium:
n = 0, 1, 2, ...
through the notations
1 2 En = 2m0Ve '
Ve= 4Rerl,
v=D
~
(68a,b)
(69a)
(69b)
(69c)
where Ve is a critical flow velocity, Re is a critical length through which the flow takes place, and v is a "viscosity" coefficient specific to the fractal fluid. There is a minimum value of the Reynolds number, n = 0, and which, through the notations:
6'.px = mo Ve,
~x=Re
(70a)
(70b)
introduces, for Peano's movements at Compton ' scale, i.e. for DF = 2 and D = n/2mo, a Heisenberg's "egalitarian" relationship [Ballentine, 1998; Phillips, 2003]:
n ~Px~X = 2· (71)
For big Reynold's numbers, n < +oo, the flow regime of the fractal fluid becomes turbulent. In other words, the microscopic-macroscopic scale transition could be associated with an evolution
612 G. V. Munceleanu et al.
scenario towards chaos (equivalent to the RuelleTakens mechanism [Cristescu, 2008; Jackson, 1991]), through which a coherent fractal fluid, at microscopic scale, becomes turbulent (incoherent, normal) at macroscopic scale.
6 . The Hydrodynamic Behavior of Laser Ablation Plasma
In the usual theories of plasma physics, in which the charged particle movements take place on continuous and differentiable curves (kinetic or bi-fluid type theories [Goldston & Rutherford, 1995]) , it is difficult to determine either the collision terms or source terms in connection with the elementary plasma processes (excitations, ionizations, recombinations, etc.). A new way to analyze the plasma dynamics is to consider that the charged particle movements take place on continuous but nondifferentiable curves, i.e. on fractals [Mandelbrot, 1982; Gouyet, 1992; Nottale, 1993; Nottale et al., 2006; Celerier & Nottale, 2004]. Then, the complexity of these dynamics is substituted by fractality. There are some fundamental arguments which can justify such hypothesis:
(i) by collision, the trajectory is no longer everywhere differentiable. The "uncertainty" in tracking the particle is eliminated by means of the fractal approximation of motion;
(ii) the complex dynamical systems as plasma, which display chaotic behavior, are recognized to acquire self-similarity and manifest strong fluctuations at all possible scales [Nottale, 1993; El Naschie et al., 1995; Weibel et al., 2005].
For example, in laser ablation plasma [Gurlui et al. , 2008], the conductive behavior manifests at µs time scale, while the convective behavior, at ns time scale. In such context, every type of elementary process from plasma induces both spatial-temporal scales and the associated fractals. Moreover, the movement complexity is directly related to the fractal dimension: the fractal dimension increases as the movement becomes more complex [Mandelbrot, 1982; Gouyet, 1992]. Different definitions were given for the fractal dimension (Kolmogorov dimension, Hausdorff dimension, etc. [Gouyet , 1992]), but once we choose the fractal-type dimension in the study of motion we must work with it until the end. Therefore, considering that the complexity of the physical
processes from plasma is replaced by fractality (situation in which the particle movements take place on fractal curves) then, it is no longer necessary to use notions as collision time, mean free path, etc., i.e. the whole classical "arsenal" of quantities from plasma physics [Goldston & Rutherford, 1995]. Then plasma will behave as a special collision-less fluid through geodesics in a fractal space-time [see Eqs. (50a,b)]. In the following, we shall analyze the dynamics of a laser plasma ablation. Let us rewrite the hydrodynamic equations of the scale relativity, Eqs . (50a,b), for the two-dimensional case and Cartesian coordinates, in the following form:
on 0 0 ot + ox (nvx) + oy (nvy) = 0
"' o o 2 o op ot (nvx) + ox (nvx) + oy (nvxvy) = - ox
o o o 2 op ot (nvy) + ox (nvxvy) + oy (nvy) = - oy
(72a)
(72b)
(72c)
where we considered that the fractal potential ( 4 7) plays the role of the internal pressure p such that
1 VQ = -Vp,
p
p=nm.
(73a)
(73b)
The assumption is not singular, it was also used in [Gurlui et al., 2008]. By introducing th~ nondimensional coordinates:
wt= t , (74a)
kx = x, (74b)
ky = y (74c)
Vxk (74d) - =Vx,
w Vyk _ - =Vy, w
(74e)
n (74f) n= -
no
and by admitting that the pressure variation is only due to concentration variation (we consider that the expansion process of the ablation plasma is isotherm) , that is:
(75)
with kB the Boltzmann constant and T the charge carriers temperature, Eqs. (72a)-(72c) become:
on o o ot + ox (nvx) + oy (nvy) = 0 (76a)
The Microscopic-Macroscopic Scale Transformation Through a Chaos Scenario 613
In expressions (76b) and (76c), we considered the scaling relation for the unit mass, (m= 1), kBTk2/w 2 := 1.
The plasma expansion is analyzed in a system of plane and normalized coordinates (see relations (74a)- (74f)), in the region above the target, Fig. 1. The Oy axis coincides with the symmetry axes of the laser pulse, and the Ox axis is considered along the target surface. The evolution of the ablation plasma satisfies the following hypothesis:
(i) plasma is in a local thermodynamically equilibrium and satisfies the quasi-neutrality condition;
(ii) the expansion is described in the approximation of a nonviscous and non-thermoconductive gas by the system of Eqs. (76a)(76c);
(iii) the energy dissipated by thermal radiation is negligible such that we can consider the ideal gas law;
(iv) the source term is introduced by means of boundary conditions.
For numerical integration we shall impose the initial conditions:
vx(O, x, y) = 0, vy(O, x, y) = 0, 1
n(O,x,y) = 4 T =To= const. 0:::; xx y:::; 1 x 1
(77a-c)
1 ...... ·· ·· ····· ....... ····•··· 1 UOOisturbed gas
• •
!/"~""~ 0 \'-~~--------... ~~~-1-;;._+
Fig. 1. The integration domain used for the numerical simulation of the laser-produced plasma expansion.
and the boundary conditions:
Vx(t, 0, y) = 0, Vx(t, 1, y) = 0,
vy(t, 0, y) = 0, vy(t, 1, y) = 0,
n(t, o, y) = l' n(t, 1, y) = l vx(t ,x,0) = 0, vx(t,x, 1) = 0,
vy(t , x, 0) = 0, vy(t, x, 1) = 0,
n(i , x,o)~=[-(tj~)']cxp[-(xi~)'] n(t, x, 1) = l·
(78a-l)
Let us observe that the laser pulse which "hits" the target induces a plasma source that is assumed to have a spatial-temporal Gaussian profile [the boundary conditions (78k)]. The system (76a- c) with the initial conditions (77a-c) and the boundary conditions (78a- l) was numerically integrated using finite differences [Zienkievicz & Taylor, 1991].
·)\
In Figs. 2(a)-(d), 3(a)-(d) and 4(a)-(81), the two-dimensional contour curves of the normalized density and normalized velocities Vx and Vy for normalized time spans t = 4/10 (a), t = 6/10 (b), t = 8/10 (c), t = 10/10 (d), are presented. It results in the following:
(i) the generation of two plasma structures [see Figs. 2(a)- (d)];
(ii) the symmetry of the normalized speed field Vx against the symmetry axis of the spatialtemporal Gaussian [see Figs. 3(a)-(d)];
(iii) shock waves and vertices of the normalized speed field Vy [see Figs. 4(a)- (d)]. These numerical results are in good agreement with the theoretical [Paun & Paun, 2009] and experimental results, [Gurlui et al., 2008; Bulgakov & Bulgakova, 1998].
We mention that similar processes, as that modeled above, take place at different space-time scales, imposed by the elementary processes in plasma [Bulgakov & Bulgakova, 1998].
614 G. V. Munceleanu et al.
(a) t = 4/10
IL B
0 0. 2 0 - i£ O . .S (L B
(c) t = 8/10
0
0 . .:3 0 .6
(b)t=6/10
1J.6 0.8
(d) t = 10/ 10
:1
Fig. 2. Two-dimensional contour curves of the normalized density, at various normalized times.
7. Free Particle in the Fractal Space-Time
In the one-dimensional case, the fractal hydrodynamic Eqs. (50a,b) and (47) take the form
mo ( [)z; + l/ av) = - !!__ [-2moD2 _1 32 VP] ' at ax at VP ax2
op a at + at (pv) = 0·
(79a,b)
The initial state of the particle in a fractal spacetime is specified by the speed
v(x, t = 0) = c (80)
and a Gaussian position distribution (distribut ion parameter a)
1 ( x )2 p(x , t = 0) = r,;; e- o: = po(x) . (81) y7ra
This means that at t = 0, the center of the distribution p(x) is at (x)o = 0 and has the speed (v)o = c. The boundary conditions are
v(x = ct, t) = c, (82a)
p(x = +oo, t) = p(x = - oo, t) = 0. (82b)
According to the method given in [Wilhelm, 1970] the solutions of the system (79a,b) with the restrictions (80)- (82a), (82b) are:
(83)
The Microscopic-Macroscopic Scale Transformation Through a Chaos Scenario 615
(L Ei
(LB
!L 15
JJ - ~
o_ ~ 0_6 Q_B
(a) t = 4/10
(L ':'2 1L6
(c) t = 8/10
0 - :.:!
l o _~ Q _':'2 0. 6 O.B
(b) t = 6/10
(d) t = 10/10
Fig. 3. Two-dimensional contour curves of the normalized velocity !ix for various normalized times.
and
(84)
Equations (83) and (84) represent the fractalhydrodynamic solution of the free motion of a particle at the differentiable scale. At the nondifferentiable scale, the speed field of the particle
u(x t) = D8lnp = -2D x - ct (85)
' ox a 2 + ( 2: t y gets "felt" through the fractal potential
mou2 ou Q = --2- -moD ox
1 + 2m0 D 2 2 (86)
a2 + (2: t)
and the fractal force
F = - oQ = ox
4moD2(x - ct)
[ a2 + ( 2: t) r . (87)
While the observable motion of the particle is uniform, (v) = c, the associated motions both at the differentiable scale - see Eq. (84) and at the nondifferentiable one - see Eq. (85) are inhomogeneous
616 G. V. Munceleanu et al.
1L B
0 .6
0 - ·~
0 O. if· O.B
(a) t = 4/10
!L 8.
(d) t = 10/10
Fig. 4. Two-dimensional contour curves of the normalized velocity Dy for various normalized times.
in x and t fractal space, owing to the action of a fractal force ( 87) . The fractal forces on the semi-spaces -oo S x S (x/ and (x/ s x s oo, with (x/ = const. compensate each other,
\
dv )(x) _ \ dv )x=+= mo - - mo-
dt x=- = dt (x) (88)
This means that the particle in free motion in the fractal space-time polarizes the "vacuum" behind itself, x S ct, and ahead of itself, x ;::: ct, in such a form that the resulting fractal forces are distributed symmetrically with respect to the plane through the observable particle position (x/ = ct at any time t. Therefore, in the fractal hydrodynamic model, the free time-dependent particle in a fractal space-time is equivalent to an incoherent
fractal fluid. Both the differentiable and the fractal components of the complex speed field are inhomogeneous in fractal coordinates due to the action of a fractal force. A momentum transfer on both speed components exists, and the "observable" movement , i.e. the uniform movement, is naturally given by a specific mechanism of vacuum polarization (the fractal components of the complex speed field and the fractal force become simultaneously zero). In such context , the brownian motion can get a new meaning: between two succesive collisions, when the motion is an uniform one, the vacuum polarization [Wilhelm, 1970; Cristescu, 2008; Jackson, 1991] is absent, while in the presence of particle collision, the vacuum polarization begins. In this last case, the trajectory of the particle is modified to become a fractal one.
The Micrnscopic-Macrnscopic Scale Transformation Thrnugh a Chaos Scenario 617
8. Conclusions
The main conclusions of the present paper are the fol owing:
(i) Considering that the motion of the particles takes place on continuous but nondifferentiable curves, i.e. on fractals with constant arbitrary fractal dimension Dp, mathematical and physical aspects are presented.
(ii) It results in a Navier- Stokes-type equation with an imaginary viscosity coefficient, and from here, in the particular case of irrotational movement , a Schrodinger-type equation. The standard Schrodinger equation is obtained as a particular case of irrotational movement at Compton scale, with the constant fractal dimension Dp = 2.
(iii) Fractal hydrodynamic model results from a Navier-Stokes-type equation by separating the real and the imaginary parts of the complex speed field. The model is described through a momentum transport equation and a conservation law of the probability density.
(iv) Using the SR model in its hydrodynamic version, the harmonic oscillator is analyzed. The complex speed field of the fractal fluid proves to be essential: the zero value of the real (differentiable) part specifies the fractal fluid coherence (superconductor or super-fluid type behavior), while the nonzero value of the imaginary (nondifferentiable or fractal) part selects, through the energy quantification condition, the stationary trajectory of the fractal fluid particles. Moreover, the momentum transfer is achieved only through the fractal component of the complex speed field of the fractal fluid and, the same fractal component , imposes totally the "observable" in the form of energy which is quantified. The "observable" from the clasical quantum mechanics given under the form of quantified energy allows the implementation of Reynold's criterium. In such a context, for a minimum value of the Reynolds number and Peano's movements at Compton scale, a Heisenberg's "egalitarian" relationship results. Moreover, for big Reynold's numbers, the flow regime of the fractal fluid becomes turbulent. In other words, the microscopic-macroscopic scale transition could be associated with an evolution scenario towards chaos (equivalent to the Ruelle- Takens mechanism), through
which a coherent fractal fluid , at microscopic scale, becomes turbulent (incoherent, normal) at macroscopic scale.
( v) The hydrodynamic behavior of a laser plasma ablation has been numerically simulated through the momentum and particle number conservation laws. In these conditions, the splitting of the plasma plume into two patterns has been successfully reproduced.
(vi) For the free time-dependent particle in a fractal space-time, both the differentiable and the fractal components of the complex speed field are inhomogeneous in fractal coordinates due to the action of a fractal force. There exists a momentum transfer on both speed components and, the "observable" movement , i.e. the uniform movement, it' naturally given by means of a specific mechanism of vacuum polarization. More precisely, the particle in free motion in the fractal space-time polarizes the "vacuum" behind itself and ahead of itself. The resulting fractal force field is distributed symmetrically with respect to the plane through the observable particle position. On this plane, the fractal speed field and the fractal force are null for any time. In such a context, a new interpretation on the Brownian motion is possible.
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