Stochastic processes via the pathway model
After collecting data from observations or experiments, the next step is to build an appropriate mathematical or stochastic model to describe the data so that further studies can be done with the help of the models. In this article, the input-output …
Authors: A.M. Mathai, H.J. Haubold
STOCHASTIC PR OCESSES VIA THE P A THW A Y MODEL Arak M. Mathai Cen tre for Mathematical and Sta tistical Sciences, Pe ec hi Campus, KF RI P eec hi-680653 , Kerala, India directorcms458@gmail.com and Departmen t of Mathematics and Statistics, McGill Univ ersit y 805 Sherbro oke Street W est, Mon treal, Queb ec, Canada , H3A2K6 Hans J. Haub old Cen tre for Mathematical and Sta tistical Sciences, Pe ec hi Campus, KF RI P eec hi-680653 , Kerala, India hans.haub old@gmail.com and Office for Outer Space Affair s, United Nations P .O. Box 500, Vienna In t ernat io nal Center, A-1400 Vienna, Austria Abstract After collecting data from observ ations or exp erimen t s, the next step is to build an appropriate mathematical or s to c hastic mo del to describ e the data so that further studies can b e done with the help of the mo dels. In this article, the input-output type mec hanism is considered first, where reaction, diffus ion, reaction-diffusion, a nd pro duction-destruction ty p e phys ical situations can fit in. Then tec hniques ar e des crib ed to pro duce thic k er or thinner tails (p o w er law b eha vior) in sto c hastic mo dels. Then the pathw a y idea is describ ed where one can switc h to differen t functional forms of the probabilit y densit y function) through a parameter called the path wa y parameter. Keyw ords Data analys is, mo del building, input- output t yp e sto c hastic mo dels, thic ker or thinner-tailed mo dels, path w ay idea, pathw a y mo dels. 2000 Mathematics Sub ject Classific ation: 44A3 5 , 26A33, 47G10 1. In tro duction After collecting da ta from exp erimen ts or from observ ations, the next step is 1 to study the data and mak e inference out o f the da ta. This can b e ac hieve d b y using mathematical metho ds and mo dels if the ph ysical situation is deterministic in nature, otherwise create sto c hastic mo dels if the ph ysical situation is no n- deterministic in nature. If the underlying phenomenon, whic h created the data, is unkno wn, p ossibly deterministic but the underlying factors and the wa y in whic h these fa ctors act are unkno wn, thereb y t he situation b ecomes random in nature. Then w e go for sto c hastic mo dels o r non-deterministic type mo dels. One has to kno w or sp eculate ab out the underlying factors as w ell as the w ay in which these factors a ct so that one can decide whic h category of mo dels are appropriate. If the observ ations are a v ailable ov er time then a time series type of mo del ma y b e appropriate. If the time series sho ws p erio dicities then eac h cycle can b e analyzed b y using sp ecific types of sto c ha stic mo dels. Here w e will consider mo dels to describ e short-term b ehavior of data or b eha v- ior within one cycle if a cyclic b ehavior is noted. When monitoring solar neutrinos it is seen that there is lik ely to b e an elev en y ear cycle and within eac h cycle the b eha vior of the graph is something lik e slo w increase with sev eral lo cal p eaks to a maxim um p eak and slo w decrease with hum ps bac k to normal le v el. In such situ- ations, what is observ ed is not really what is actually pro duced. What is observ ed is the residual part of what is pro duced min us w hat is consumed or con v erted and th us the a ctual observ ation is made on the residual part only . Man y of na t ural phenomena belong to this t ype of behavior of the form u = x − y where x is the input or pro duction v aria ble and y is the o ut put or consumption or destruction v ariable and u r epresen ts the residual part whic h is o bserv ed. A general analysis of input-output situation ma y b e s een from [21]. In man y situations one can assume that x and y are statistically indep enden tly distributed and that u ≥ 0 means pro duction dominates ov er destruction or input dominates o v er the output. In reaction- rate theory , when particles react with each other pro ducing new particles or pro ducing neutrinos w e ma y ha v e the f o llo wing t ype of situations. Certain particles may react with eac h other in short-span o r short-time p erio ds and pro duce small n um b er of particles, others ma y tak e medium time in t erv als and pro duce larger num b ers of particles and y et o thers ma y react ov er a long span and pro duce larger n um b er of part icles. F o r desc ribing suc h types of situations in the pro duction of solar neutrinos the presen t authors considered creating mathe- matical mo dels b y erecting triangles whose ares are prop ortiona l to the neutrinos pro duced, see [5],[6 ],[7 ],[8]. Another approach that w a s adopted w as to assume x and y as independen tly distributed ra ndom v ariables, then w ork out the densit y of the residual v ariable under the assumption that x − y ≥ 0. The simplest suc h situation is an exp onen tial 2 t ype input a nd an exp onen tial ty p e output. T hen w e can lo ok at sum of suc h indep enden tly distributed residual t ype v ariables. This is a reasonable type of assumption. Then input-output mo del has the Laplace dens it y , when x and y are iden tically and indep enden tly distributed and the densit y is g iv en b y , f 1 ( u ) = β 1 2 e − β 1 | u − α 1 | , 0 ≤ u < ∞ , β 1 > 0 , (1 . 1) and f 1 ( u ) = 0 elsewhere, where α 1 is a lo cation para meter. Note that β 1 can act as a scale para meter or as a dispersion or scatter parameter. Supp ose tha t this situation is rep eated at successiv e lo cations and with the scale parameter β = β 1 , β 2 , ... . Then the nature of t he graph will b e that of a sum o f Laplace densities. If the lo cation para meters are sufficien tly fa rther apart then the graph will lo ok lik e that in Figure 1(b). If suc h blips are o ccurring sufficien tly close together then we hav e a graph of the t ype in Figure 1(a). In these graphs w e ha v e tak en only fiv e to six lo cations f or simplic it y . But b y taking successiv e lo cations w e can generate many of the phenomena that are seen in nature, esp ecially in t ime series data. When the lo cations are sufficien tly closer w e get the graph with sev eral lo cal maxima/spike s and a con tin uous curv e. This is the t yp e of b eha vior seen in solar neutrino pro duction. Cyclic patterns can also a r ise dep ending up on t he lo cation and scale parameters. Here β 1 measures the in tensit y of t he blip and α 1 the lo cat io n where it happ ens, and eac h blip is the residual effect of an exp onen tial t ype input and an independen t exp onen tial t yp e output o f the same strength. If α 1 , α 2 , ... are farther apart then the con tributions coming from other blips will b e negligible and if α 1 , α 2 , ... a r e close tog ether then there will b e contributions from other blips. The function will b e of the follo wing form: f ( u ) = k X j =1 β j 2 e − β j | u − α j | , 0 ≤ u < ∞ , β j > 0 , j = 1 , ..., k < ∞ (1 . 2) If one requires f ( u ) to b e a densit y within a n um b er of spik es then divide the sum b y k so that w e ha v e a conv ex com bination of Laplace densities, whic h will again b e a densit y . The mo del do es not require that w e create a densit y out of the pattern. I f the arriv al of the lo cation p oints ( α j ) is go v erned b y a P oisson pro cess then we will ha v e a P oisson mixture of Laplace densities. 3 (a) (b) Figure 1 (a) (b) A symmetric Laplace densit y will b e of the following form: f 2 ( u ) = 1 2 β e − | u | β , − ∞ < u < ∞ (1 . 3) and the graph is of the follo wing form: Figure 2 Symmetric Laplace densit y This is the symmetric case where u < 0 b ehav es t he same w a y as u ≥ 0. If the b eha vior of u is differen t fo r u < 0 and u ≥ 0 then we get the asymmetric La pla ce case whic h can b e written a s g ( u ) = ( 1 ( β 1 + β 2 ) e u β 1 , − ∞ < u < 0 1 ( β 1 + β 2 ) e − u β 2 , 0 ≤ u < ∞ (1 . 4) 4 Figure 3 Asymmetric Laplace case When α 1 > 1 , α 2 > 1 , α 1 = α 2 = α , β 1 = β 2 = β w e hav e indep endently and iden tically distributed gamma random v ariables for x and y and u = x − y is the difference b etw een them. Then g 1 ( u ) can b e seen t o be the follo wing: g 1 ( u ) = u 2 α − 1 e − u β β 2 α Γ 2 ( α ) Z ∞ z =0 (1 + z ) α − 1 z α − 1 e − 1 β (2 uz ) d z (1 . 5) for u ≥ 0, α > 0 , β > 0. This b eha v es lik e a gamma density and prov ides a symmetric mo del for u ≥ 0 and u < 0. The following is the nature of the gra ph. Figure 4 g 1 ( u ) in the symmetric gamma t ype input-output v aria bles 2. Mo dels with Thic k er and Thinner T ails 5 F or a large num b er of situations a gamma type mo del ma y be appropriate. A t w o parameter gamma densit y is of the type f ( x ) = 1 β α Γ( α ) x α − 1 e − x β , x ≥ 0 , α > 0 , β > 0 . (2 . 1) Sometimes a member from this parametric family of functions ma y b e a ppro priate to de scrib e a data set. Sometimes the data require a sligh tly thic ke r-tailed mo del due to chances of higher probabilities or more area under the curv e in the tail. Tw o of suc h mo dels dev eloped b y t he authors’ groups will be describ ed here. One t ype is where the mo del in (2.1 ) is app ended with a Mittag-Leffler series and another t ype is where (2.1) is app ended with a Bessel series, see also [25]. 2.1. Gamma mo del with app ended Mittag-Leffler function Consider a gamma densit y o f t he t yp e g 3 ( x ) = c 1 x γ − 1 e − x δ , δ > 0 , γ > 0 , x ≥ 0 . Supp ose that w e a pp end this g 3 ( x ) with Mittag- L effler function E β α,γ ( − x α ) where E β α,γ ( − ax α ) = ∞ X k =0 ( β ) k k ! ( − a ) k x α k Γ( γ + αk ) , α > 0 , γ > 0 . Consider the function f ∗ ( x ) = c ∞ X k =0 ( β ) k k ! ( − a ) k x αk + γ − 1 e − x δ Γ( γ + αk ) , x ≥ 0 where c is the normalizing constan t. Let us ev aluate c . Since the total in tegra l is 1, 1 = Z ∞ 0 f ∗ ( x )d x = c ∞ X k =0 ( β ) k k ! ( − a ) k Z ∞ 0 x αk + γ − 1 e − x δ Γ( γ + αk ) d x = c ∞ X k =0 ( β ) k k ! ( − a ) k δ αk + γ = c δ γ (1 + aδ α ) − β , | aδ α | < 1 for β > 0 , α > 0 , δ > 0 , aβ δ α < 1 , | aδ α | < 1 . Therefore the densit y is f ∗ ( x ) = (1 + aδ α ) β δ γ x γ − 1 e − x δ ∞ X k =0 ( β ) k k ! ( − a ) k δ αk Γ( γ + αk ) 6 for 0 ≤ x < ∞ , α > 0 , γ > 0 , δ > 0 , β > 0, | aδ α | < 1 , aβ δ α < 1. That is, f ∗ ( x ) = (1 + aδ α ) β δ γ x γ − 1 e − x δ [ 1 Γ( γ ) + ∞ X k =1 ( β ) k k ! ( − 1) k δ αk Γ( γ + α k ) ] . Note that a = 0 corresp onds to the original gamma densit y . The follow ing are some gra phs of the app ended Mittag-Leffler-gamma densit y . When a < 0 w e hav e thinner tail and when a > 0 we ha v e thic k er tails compared to the gamma tail. Figure 5 Gamma densit y with Mittag-Leffler function app ended 2.2. Bessel app ended gamma densit y Consider the mo del o f the t yp e of a basic g a mma densit y app ended with a Bessel function, see also [25]. ˜ f ( x ) = c x γ − 1 e − x δ ∞ X k =0 x k ( − a ) k k !Γ( γ + k ) , δ > 0 , γ > 0 , x ≥ 0 , where c is the normalizing constan t. The app ended function is o f the form 1 Γ( γ ) 0 F 1 ( ; γ : − ax ) whic h is a Bessel function. Let us ev aluate c . 1 = c ∞ X k =0 ( − a ) k k ! Z ∞ 0 x γ + k − 1 Γ( γ + k ) e − x δ d x = c δ γ ∞ X k =0 ( − a ) k δ k k ! = c δ γ e − aδ . 7 Hence the densit y is of the f orm ˜ f ( x ) = e aδ δ γ x γ − 1 e − x δ ∞ X k =0 x k ( − a ) k k !Γ( γ + k ) , x ≥ 0 , γ > 0 , δ > 0 . Figure 6 Gamma app ended with Besse l function Note : Instead of app ending with Bessel function one could hav e app ended with a general h ypergeometric series. But a general h yp ergeometric series do es not simplify in t o a con v enien t form. W e ha v e chose n sp ecialized parameters as w ell as suitable functions so that the normalizing constan ts simplify to con venie n t fo r ms thereb y general computations will b e m uc h easier and simpler. 3. Pa th w ay Idea Here w e cons ider a mo del whic h can switc h to three functional for ms co v ering almost all statistical densities in curren t use, see [23]. Let f ∗ 1 ( x ) = c ∗ 1 | x | γ [1 − a (1 − α ) | x | δ ) η 1 − α , α < 1 , η > 0 , a > 0 , δ > 0 , (3 . 1) and 1 − a (1 − α | x | δ > 0, where c ∗ 1 is the normalizing constan t. When α < 1 the mo del in (3.1) sta ys as the generalized t ype-1 b eta family , extended o v er the real line. When α > 1 write 1 − α = − ( α − 1) with α > 1. Then the functional form in (3.1) changes to f ∗ 2 ( x ) = c ∗ 2 | x | γ [1 + a ( α − 1) | x | δ ] − η α − 1 (3 . 2) for α > 1 , a > 0 , η > 0 , −∞ < x < ∞ . Note that (3.2) is the extended generalized t ype-2 b eta family of functions. When α → 1 then b o th (3.1) and (3.2 ) g o to 8 f ∗ 3 ( x ) = c ∗ 3 | x | γ e − aη | x | δ , a > 0 , η > 0 , δ > 0 , −∞ < x < ∞ . (3 . 3) Eq. (3.3) is the extended generalized gamma family of functions. Th us (3.1) is capable of switc hing to three families of functions. This is the pathw a y idea and α is the path w ay parameter. Through this parameter α one can reac h the three families of functions in (3 .1 ),(3.2), and (3 .3 ). The pathw a y idea was in tro duced b y Mathai [23]. The normalizing constan t s can b e seen to b e the following: c ∗ 1 = δ 2 [ a (1 − α )] γ +1 δ Γ( γ +1 δ + η 1 − α + 1) Γ( γ +1 δ )Γ( η 1 − α + 1) (3 . 4) for a > 0 , α < 1 , δ > 0 , γ > − 1 , η > 0, c ∗ 2 = δ 2 [ a ( α − 1)] γ +1 δ Γ( η α − 1 ) Γ( γ +1 δ )Γ( η α − 1 − γ +1 δ ) (3 . 5) for α > 1 , a > 0 , δ > 0 , η > 0 , δ > 0 , η α − 1 − γ +1 δ > 0, c ∗ 3 = δ 2 ( aη ) γ +1 δ Γ( γ +1 δ ) , a > 0 , δ > 0 , η > 0 , γ > − 1 . (3 . 6) Note that (3.1) is a finite rang e mo del, suitable to describe situations where the tails are cut off. When α comes closer and closer to 1 then the cut-off p oint mov es a w ay from the origin and ev entually go es to ±∞ . When α → 1 then mo del (3.1) go es to mo del (3.3) whic h is an extended generalized gamma mo del. The mo del in (3.2) is type-2 b eta form, spreads out ov er t he whole real line and the shap e will b e closer to that of a gamma t ype mo del when α approache s 1. Th us the pat hw ay mo dels in (3.1),(3.2), and (3.3) co v er all t ypes of situations where the tails are cut off, tails are made thinner or thic k er compared to a gamma t ype mo del. The extended ga mma type mo del in (3.3) also contains the Gaussian mo del, Brow nian motion, Maxw ell-Bo ltzmann density etc. If Gaussian or Maxw ell-Boltzmann is the stable or ideal f o rm in a ph ysical situation then the unstable neigh b orho o ds are co v ered by (3 .1) and (3.2) or the paths leading to t his s table form is describ ed b y (3.1) and (3.2). It is w orth noting that (3.1) for x > 0 , γ = 0 , a = 1 , δ = 1 , η = 1 is the Tsallis statistics for non-extensiv e statistical mec hanics. Also note that (3.2) for a = 1 , δ = 1 , η = 1 is sup erstatistics. This sup erstatistics can also b e deriv ed as the unconditional densit y when both the conditional dens it y of x giv en a parameter θ 9 and the margina l density of θ are gamma densities or exponential t yp e densities, the details may b e seen from Mathai and Haubo ld ([15], [26], [27 ], [29], [30]). V arious t yp es of mo dels whic h are applicable in a v ariety of situatio ns ma y b e seen from Mathai [2 5]. 4. Reaction Rate P robabilit y I n t egral Mo del Starting from 1980’s the presen t authors had pursued mathematical mo dels for reaction-rate theory in v arious situations suc h as non-resonant reactions and resonan t reactions under v arious cases suc h as depletion, high energy tail cut off etc, see [2],[3 ],[4], [5], [9], [11]. Th e basic mo del is a n inte gral o f the following form: I (1) = Z ∞ 0 x γ − 1 e − ax δ − z x − ρ , a > 0 , z > 0 , ρ > 0 , δ > 0 . (4 . 1) F or ρ = 1 2 , δ = 1 one has the basic probabilit y in tegral in the non-resonan t case, see [4]. F or γ = 0 , ρ = 1 one has Kr¨ atzel in t egra l [24]. F or γ = 0 , δ = 1 , ρ = 1 one has inv erse Gaussian densit y . Computational asp ect of (4.1) is discuss ed in [1] and related materia l ma y b e seen f rom [20]. Since the integral in (4.1) is a pro duct of integrable functions one can ev aluate the integral in (4.1) with the help of Mellin conv olution of a pro duct b ecause the in tegra nd can b e written as Z ∞ 0 1 v f 1 ( v ) f 2 ( u v )d v , f 1 ( x ) = x γ e − ax δ , f 2 ( y ) = e − y ρ (4 . 2) for u = z 1 ρ , u = xy . Then the Mellin conv olution of the integral in (4.1), denoting the Mellin transform of a function f with Mellin para meter s as M f ( s ), w e ha v e from (4.1) M I (1) ( s ) = M f 1 ( s ) M f 2 ( s ) , (4 . 3) where M f 1 ( s ) = Z ∞ 0 x s − 1 f 1 ( x )d x = Z ∞ 0 x γ + s − 1 e − ax δ d x = 1 δ Γ( s + γ δ ) a s + γ δ , ℜ ( s + γ ) > 0 and M f 2 ( s ) = Z ∞ 0 y s − 1 e − y ρ d y = 1 ρ Γ( s ρ ) , ℜ ( s ) > 0 . 10 Hence M I (1) ( s ) = M f 1 ( s ) M f 2 ( s ) = 1 ρδ a γ δ Γ( s + γ δ )Γ( s ρ ) a s δ . Therefore the in tegral in (4.1 ) is the in v erse Mellin transform of (4.3). That is, I (1) = 1 2 π i Z c + i ∞ c − i ∞ 1 ρδ a γ δ Γ( s + γ δ )Γ( s ρ )( ua 1 δ ) − s d s, u = z 1 ρ , i = √ − 1 = 1 ρδ a γ δ H 2 , 0 0 , 2 [ z 1 ρ a 1 δ (0 , 1 ρ ) , ( γ δ , 1 δ ) ] (4 . 4) where H ( · ) is the H-function, see [28],[32]. F rom the basic result in (4.4) w e can ev aluate the reaction-rate probabilit y integrals in the other cases of non-r elativistic reactions. 4.1. Generalization of reaction-rate mo dels A companion integral corresp o nding to ( 4.1) is the integral I (2) = Z ∞ 0 x γ e − ax δ − z x ρ d x, a > 0 , δ > 0 , ρ > 0 , z > 0 . (4 . 5) In ( 4.1) we had x − ρ with ρ > 0 whereas in (4.5) w e hav e x ρ with ρ > 0. F or δ = 1, (4.5) corresp onds to the L a place transfor m or momen t generating function o f a generalized gamma de nsit y in statistical distribution theory . The in tegral in (4.5) can b e ev aluated. Note that (4.5) can b e written in the form of an in tegral of the form Z ∞ 0 v f 1 ( v ) f 2 ( uv )d v , f 1 ( x ) = x γ − 1 e − ax δ , f 2 ( y ) = e − y ρ (4 . 6) for u = z 1 ρ . The inte gral in (4.6) is in the structure of a Mellin transform of a ratio u = y x , so that the Mellin transform of I (2) is then M I (2) ( s ) = M f 2 ( s ) M f 1 (2 − s ) . (4 . 7) The in v erse Mellin transform in (4.7) giv es the in tegral I (2) . The pair of integrals I (1) and I (2) b elong to a par t icular case of a general vers atile mo del considered b y the authors earlier [33]. A generalization of I (1) and I (2) is the pathw a y generalized mo del, whic h results in the v ersatile in tegral. The pathw a y generalization is done b y r eplacing the t w o exp o nen tia l functions b y the corresp onding path w ay form. Consider the in tegrals of the following t yp es: 11 I p = Z ∞ 0 x γ [1 + a ( q 1 − 1) x δ ] − 1 q 1 − 1 [1 + b ( q 2 − 1) x ρ ] − 1 q 2 − 1 d x, (4 . 8) where q 1 > 1 , q 2 > 1 , a > 0 , b > 0 , . W e will ke ep ρ free, could b e negat iv e or p ositiv e. Note that lim q 1 → 1 [1 + a ( q 1 − 1) x δ ] − 1 q 1 − 1 = e − ax δ and lim q 2 → 1 [1 + b ( q 2 − 1) x ρ ] − 1 q 2 − 1 = e − bx ρ . Hence lim q 1 → 1 ,q 2 → 1 I p = Z ∞ 0 x γ e − ax δ − bx ρ d x whic h is t he integral in (4.5 ) a nd if ρ < 0 then it is the in tegra l in (4.1). The general in tegral in (4.8) b elongs to the general family of v ersatile inte grals. The factors in the integrand in (4.8) ar e of the generalize d t yp e-2 b eta form. W e could hav e taken eac h factor in type-1 b eta o r t yp e-2 b eta form, th us pro viding 6 differen t com binations. F or eac h case, w e could ha v e the situation of ρ > 0 or ρ < 0. The whole collection of suc h mo dels is kno wn as the v ersatile integrals. In t egr a l transforms, k no wn as P -transforms, a re also asso ciated with the integrals in (4.8), see for example [18],[19]. 4.3. F ractional c alculus mo dels In a series of pa p ers the authors ([12], [13], [14], [15], [17 ], [22], [28]) hav e show n recen tly that fra ctional in tegrals can b e classified into the forms in (4.2) and (4.6) or fr actional in tegral op erators o f the second kind or righ t-sided fractional integral op erators can b e considered as Mellin con volution of a pro duct as in (4.2 ) and left-sided or fractional integral op erators of the first kind can b e considered as Mellin con v olution of a ratio where the functions f 1 and f 2 are of the follow ing forms: f 1 ( x ) = φ 1 ( x )(1 − x ) α − 1 , 0 ≤ x ≤ 1 , f 2 ( y ) = φ 2 ( y ) f ( y ) (4 . 9) where φ 1 and φ 2 are pre-fixed functions, f ( y ) is arbitrary and f 1 ( x ) = 0 outside the in terv al 0 ≤ x ≤ 1. Th us, essen tially , all fractional in tegr a l op erator s b elong to the categories o f Mellin con v olution of a pro duct or ratio where one function is a m ultiple of type-1 b eta form and the other is arbitrary . The righ t-sided or t ype-2 fractional in tegral of order α is denoted b y D − α 2 ,u f and defined as D − α 2 ,u f = Z v 1 v f 1 ( u v ) f 2 ( v )d v (4 . 10) 12 and the left-sided o r type-1 fractional in tegral of order α is giv en b y D − α 1 ,u f = Z v v u 2 f 1 ( v u ) f 2 ( v )d v (4 . 11) where f 1 and f 2 are a s giv en in (4.9). Let n be a p ositive in teger suc h that ℜ ( n − α ) > 0. The smallest suc h n is [ ℜ ( α )] + 1 = m where [ ℜ ( α )] denotes the in teger part of ℜ ( α ). Here D − α 2 ,u f and D − α 1 ,u f are defined as in (4.10) and (4.11) resp ectiv ely . Let D = d d u the ordinar y deriv ativ e with resp ect to u and D n b e the n -th order deriv ativ e. Then the fractional deriv ativ e of order α is defined as D α f = D n [ D − ( n − α ) i,u f ] in the Riemann-Liouville sense and D α f = [ D − ( n − α ) i,u D n f ] in the Caputo sense (4 . 12 ) for i = 1 , 2, see also [31]. The input-o utput mo del t hat we started with, when applied to reaction- diffusion problems can result in fractional order r eactio n- diffusion differen tial equations. Suc h fractio na l o rder differen tial equations are seen t o pro vide so- lutions whic h are more relev ant to practical situations compared to the solutions coming from differen tial equations in the con v entional sense o r inv olving in teger- order deriv at iv es. Some of the relev ant papers in this direction ma y b e seen from [12], [13], [16], [17]. Ac kno wledgemen t The authors w ould lik e to thank the D epart ment of Science and T ec hnology , Go v ernmen t of India, for the financial assis tance for this w ork under Pro j ect Num b er SR/S4/MS:287 /05 and t he Cen tre for Mathematical Sciences India for facilities. References [1] W.J. Anderson, H.J. Haub old and A.M. Mathai (1994): Astroph ysical ther- mon uclear functions, Astr ophysics and Sp ac e Scienc e , 214(1-2) , 4 9 -70. [2] H.J. Haub old and A.M. Mathai (1984): On the nuclear energy generation rate in a simple analytic stellar mo del, Annalen der Physik , 41 , 372-379. [3] H.J. Haubo ld and A.M. Mathai (1984): On n uclear reaction rate theory , A nnalen der Physik , 41 , 380-396. [4] H.J. Haub old a nd A.M. Mathai (1988): Mo dern Pr oblems in Nucle ar and Neutrino Astr ophysics , Ak ademie-V erlag, Berlin. 13 [5] K. Sakurai (2014): So lar Neutrino Pr oblems - How They Wer e Solve d , TER- RAPUB, T oky o. [6] H.J. Ha ub old a nd A.M. Mathai (1995): A heuristic remark on the p erio dic v ariation in the num b er of solar neutrinos detected o n Eart h, Astr ophysics and Sp ac e scienc e , 228 , 113- 134. [7] H.J. Haub old, A.M. Mathai, and R.K. Sa xena (201 4 ) Analysis of solar neutrino data from Sup er-Kamiok a nde I and I I, Entr opy , 16 , 1414. [8] A.M. Mathai a nd H.J. Haub old (2013) On a generalized en trop y measure leading to the pat hw ay mo del with a preliminary application to solar neutrino data, Entr opy , 15 , 4011. [9] H.J. Haub old and A.M. Mathai (1998): On thermonuclear reaction rat es, Astr ophysics and Sp ac e scienc e , 258 , 185-18 9. [11] H.J. Haub old and A.M. Mathai (19 9 8): An in tegral arising frequen tly in astronom y and ph ysics, SIAM R eview , 40(4) , 995-997 . [12] H.J. Haub old and A.M. Mathai (2000): The fractio na l kinetic equation and thermon uclear functions, Astr ophysic s an d Sp ac e Scienc e , 273(1-4) , 53- 63. [13] H.J. Haub old and A.M. Mathai ( 2 002): On f r actional kinetic eq uations, Astr ophysics and Sp ac e Scienc e , 282 , 281-28 7. [14] H.J. Haub old and A.M. Mathai ( 2 006): A certain class of Laplace transform with a pplicatio n to reaction and reaction- diffusion equations, Astr ophysics and Sp ac e Scienc e , 305 , 283- 288. [15] H.J. Haub old and A.M. Mathai (2007): Path w a y mo del, sup erstatistics, Tsallis statistics and a measure of en trop y , Physic a A , 375 , 110 - 122. [16] H.J. Haub o ld, A.M. Mathai and R.K. Sa xena (2010): Solution of certain fractional kinetic equations and a fractio na l diffusion equation, Journal of Math- ematic al Physics , 51 , 10350 6 -1,10350 6-8. [17] H.J. Haub old, A.M. Mathai and R.K. Saxena (2011): F urther solutions of fractional reaction-diffusion equations in tems of the H-function, Journal o f Computational and Appli e d Mathematics , 235 , 1311-13 16. [18] D . Kumar and A.A. Kilbas (2010): F ractional calculus of P- t ransform, ] F r ac- tional Calculus and Applie d Analysis , 13(3) , 317-328. [19] D. Kumar (2011): P-transform, Inte gr al T r a nsforms and Sp e cial F unctions , 22(8) , 603- 3 611. 14 [20] A.M. 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Mathai (2012) : Sto c hastic mo dels under p o w er transfor ma t io ns and exp o nen tia t ion, Journal of the Indian So ciety fo r Pr ob ability and Statistics , 13 , 1-19. [26] A.M. Mathai a nd H.J. Haub o ld (2 0 07): On generalized en tro p y measure and path w ays , Physic a A , 385 , 493-500 . [27] A.M. Mathai and H.J. Haub old (20 08): Path w a y parameter and t hermonu- clear functions, Physic a A , 387 , 2462-2470 . [28] A.M. Mathai a nd H.J. Haub old (2 008): Sp e cial F unctions for Applie d Sci- entists , Springer, New Y o rk. [29] A.M. Mathai a nd H.J. Haubold (2011): Mittag-Leffler functions to path wa y mo del to Tsallis statistics, Inte gr al T r ansforms and Sp e cial F unctions , 21(11) , 867-875 . [30] A.M. Mathai and H.J. Haub old (201 1 ): A path w ay for Ba y esian statistical analysis to sup erstatistics, Appli e d Mathema tics and Computations , 218 , 799-804 . [31] A.M. Mathai and H.J. Haub old (20 13): Erdelyi-Kob er fractional in tegral op erators from a statistical p ersp ectiv e I-IV, arXiv:13 03.3978-3981 . [32] A.M. Mathai, R.K. Saxe na and H.J. Haub o ld (2010) : The H-function: The- ory and Applic ations , Springer, New Y or k. [33] A.M. Mathai and H.J. Haub old (201 1): A v ersatile in tegral in ph ysics and astronom y , . 15
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