arXiv:1805.09172v1 [math.AP] 23 May 2018 inldrvtv nteCpt es forder of restrictio sense a Caputo when the obtained, in is derivative face tional fixed t the initial at constant condition with flux material semi–infinite a for problem o ucin o h lsia w-hs Lamé-Clapeyron- Neu two-phase classical classical the the and for data Sc function, on ror charac restriction Math. which the recover Adv. coefficient also Roscani–Tarzia, We the in for obtained inequality interface the change an at fracti condition obtain this temperature we between constant fact, a relationship with c a one the another find of and we one in Furthermore, and equations ary. heat governing two in considered Abstract: ue ftetotmeaue orsodn otesldand solid the to corresponding temperatures two velocity the wh the freezing, of connecting and interface fluxes solid-liquid melting one–dimensional the of at the processes tion the for to problems linked boundary problems free that Recall tfnpolmwt etflxcniinat condition flux heat a with problem Stefan rbe a tde yuigtefatoa eiaieo or of derivative fractional derivat th the [14], using fractional by in fractiona a studied particular, was In on where problem works 34–36]. problems 24–26, 13, 6, some 3, [2, boundary bee years lished has free recent equation the is, diffusion in (that fractional and the 29] 21–23, decades 19, last the In Introduction 1 bound temperature condition, boundary flux heat Solutions, Keywords: xlctslto o w–hs fractional two–phase a for solution Explicit eeaie emn ouinfrtetopaefractiona two-phase the for solution Neumann generalized A auoFatoa eiaie aéCaernSea Pro Lamé–Clapeyron–Stefan Derivative, Fractional Caputo OIE et.Mtmtc,FE nv Austral, Univ. FCE, Matemática, Depto. - CONICET [email protected],[email protected]) ([email protected], arn .RsaiadDmnoA Tarzia A. Domingo and Roscani D. Sabrina aauy15,S00Z oai,Argentina Rosario, S2000FZF 1950, Paraguay h xdface fixed the 1 α ∈ (0 , 1) lsia Lamé–Clapeyron–Stefan classical e epc ntetmoa aibeis variable temporal the on respect ftefe onayadteheat the and boundary free the of tfnpolmfrtecase the for problem Stefan meaueadapriua heat particular a and emperature ndt sstse.Tefrac- The satisfied. is data on n der anslto,truhteer- the through solution, mann r condition. ary c aealtn etcondi- heat latent a have ich .Ap. 4(04,237-249. (2014), 24 Appl., i. nlfe onayproblem boundary free onal bound- free the for onditions xesvl tde 8 17, [8, studied extensively n eie h rcinlphase- fractional the terizes v sivle) eepub- were involved), is ive xdfc n ae nthat on based and face fixed lsia eteuto are equation heat classical 2 1 rebudr problems boundary free l Lamé–Clapeyron–Stefan l iudpae.Ti kind This phases. liquid . lm Neumann blem, α 1 = . of problems are known in the literature as Stefan problems or, more precisely, as Lamé– Clapeyron–Stefan problems. We remark that the first work on phase–change problems was done by G. Lamé and B.P. Clapeyron in 1831 [16] by studying the solidification of the Earth planet, which has been missing in the scientific literature for more than a century. Next, sixty years later, the phase–change problem was continued by J. Stefan through sev- eral works around year 1890 [30] by studying the melting of the polar ice. For this reason, we call these kind of problems as Lamé–Clapeyron–Stefan problems or simply by Stefan problems. Nowadays, there exist thousands of papers on the classical Lamé–Clapeyron–Stefan prob- lem, for example the books [1, 4, 7, 9, 10, 12, 18, 28] and the large bibliography given in [32]. Especially, a review on explicit solutions with moving boundaries was given in [33].
In this paper, a generalized Neumann solution for the two–phase fractional Lamé– Clapeyron–Stefan problem for a semi–infinite domain is obtained when a constant initial data and a Neumann boundary condition at the fixed face are considered. Recently, a generalized Neumann solution for the two–phase fractional Lamé-Clapeyron-Stefan problem for a semi–infinite domain with constant initial data and a Dirichlet condition at the fixed face was given in [26]. So, the classical time derivative will be replaced by a fractional derivative in the sense of Caputo of order 0 <α< 1, which is present in the two governing heat equations and in one of the governing conditions for the free boundary. The fractional Caputo derivative is defined in [5] as:
t 1 α α Γ(1 α) (t τ)− f ′(τ)dτ, 0 <α< 1 D f(t)= − Z0 − (1) f ′(t), α = 1. where Γ is the Gamma function defined in R+ by the following expression:
∞ x 1 t Γ(x)= t − e− dt. Z0 It is known that the fractional Caputo derivative verifies that [15]: For every b R+, ∈ α 1 1 1 D is a linear operator in W (0, b)= f (0, b] : f ′ L (0, b) , (2) ∈ C ∈
Dα(C) = 0 for every constant C R (3) ∈ and α β Γ(β + 1) β α D (t )= t − for every constant β > 1. (4) Γ(β α + 1) − −
2 Now we define the two functions (Wright and Mainardi functions) which are very im- portant in order to obtain the explicit solution given in the following Sections.
The Wright function is defined in [37] as:
∞ xn W (x; ρ; β)= , x R, ρ> 1, β R (5) n!Γ(ρn + β) ∈ − ∈ Xn=0 and the Mainardi function, which is a particular case of the Wright functions, is defined in [11] as:
∞ ( x)n M (x)= W ( x, ρ, 1 ρ)= − , x R, 0 <ρ< 1. (6) ρ − − − n!Γ ( ρn + 1 ρ) ∈ nX=0 − − Proposition 1. Some basic properties of the Wright function are the following:
1. [15] The Wright function (5) is a differentiable function for every ρ > 1, β R − ∈ such that ∂W (x; ρ; β)= W (x; ρ; β + ρ) . ∂x α 1 x 2. [25] lim W x; ; 1 = W x; ; 1 = erfc , and α 1− − − 2 − −2 2 → α 1 x lim 1 W x; ; 1 = 1 W x; ; 1 = erf . α 1− − − − 2 − − −2 2 → 3. [22] For all α, c R+, ρ (0, 1), β R we have ∈ ∈ ∈ α β 1 ρ β α 1 ρ D x − W ( cx− , ρ, β) = x − − W ( cx− , ρ, β α). − − − − −
4. [25] For every α (0, 1), W x, α , 1 is a positive and strictly decreasing function ∈ − − 2 in R+ such that 0