International Journal of Engineering Science 37 (1999) 1985±2005
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Thermo-elastic-plastic porous material undergoing thermal loading Andrzej Søu_zalec
*
Technical University of Czestochowa, 42-201 Czestochowa, Poland Received 8 August 1997; received in revised form 2 December 1998
Abstract A model for predicting elastic±plastic stresses within a surface-heated porous structure has been developed. The relevant phenomena for the moisture, pressure, temperature and displacement ®elds in thermoelastic-plastic porous material are analysed. Considering mass and energy transfer processes, a set of governing dierential equations is presented. The solution of the problem has been obtained with a ®nite dierence scheme. The results demonstrate the in¯uence of the evaporation mechanism on pressure and thermal stresses within the porous material. Ó 1999 Elsevier Science Ltd. All rights reserved.
1. Introduction Transport phenomena and elastic±plastic stresses in porous media have recently received growing attention in light of the common usage of such media in various applications in the ®elds of energy technology. The physical phenomena of moisture transfer in porous media are usually explained by the following theories: diusion theory [1]; capillary ¯ow theory [2]; and evaporation condensation theory [3]. Diusion theory, which has been used extensively in the past does not give results in agreement with experimental data. Capillary ¯ow theory, in which the diusivity depends on the pore water content, has been employed [4,5] to predict the drying rate in concrete slabs. However, the coecient of diusivity is a complex function of pore moisture, temperature and other variables of the porous system. It cannot be de®ned as a simple function of pore moisture as done in Refs. [4,5]. Later, drying experiments at elevated temperatures revealed high pore pressure as a consequence of intense water vaporization [6]. The measured pore pressure, determined under equilibrium heating conditions, correspond well to the sum of the calculated
*
Corresponding author. Tel.: +48-34-3-250-966; fax: +48-34-3-250-920. E-mail address:
[email protected] (A. Søu_zalec)
0020-7225/99/$ ± see front matter Ó 1999 Elsevier Science Ltd. All rights reserved. PII: S 0 0 2 0 - 7 2 2 5 ( 9 9 ) 0 0 0 1 1 - 7
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saturated water vapor pressure and ambient air pressure. As a consequence of the above models, in a previous work the evaporation mechanism was assumed with concentration and pressure gradient terms [7]. An analysis of poroelastic stresses was developed and improved by Biot [8±10]. In 1976 Rice and Cleary [11] gave a rational reformulation of the Biot theory, and their rationalised version has proved more convenient for solving relevent problems and in interpreting the solutions obtained (e.g. [12±15]). Modern theories of mixtures, taking into account ®nite deformations and thermal eects, for most cases have been developed by Crochet and Naghdi [16] and Bowen [17]. In 1971 Schiman [18] developed an extended Biot theory including thermal eects. The present paper describes equations of heat and mass transfer in a thermo-elasto-plastic material. This theory shows that the displacement ®eld is, in general, completely coupled with the pore pressure and temperature ®elds.
2. Assumptions and equation 2.1. Theoretical assumptions and simpli®cations 1. 2. 3. 4. 5.
The following assumptions are made for the theoretical model: Heat transfer between the ¯uid and the solid is neglected. The response time for local heat transfer between the ¯uid and the solid is several orders of magnitude smaller than the times of interest. Liquid vapor equilibrium exists in the presence of free water, which makes the partial pressure of the vapor equal to the saturation pressure. Movement of the liquid is neglected. Darcy's law with a variable coecient holds for the gases. Air and water vapor are treated as ideal gases.
2.2. Conservation equations for mass The conservation equations for mass can be written as q_ i ÿr
qi wi Wi ;
1
where qi is the density of species i, wi is the velocity of species i and Wi is the production rate of species i. Since no movement of the liquid (subscript c) is assumed wc 0. Also, W ÿWV ÿWm (v vapor, m air±vapor mixture), since the rate of liquid evaporation is the same as the rate of vapor production, and since the air does not change phase, the rate of mixture production equals the rate of vapor production. The above equation thus simpli®es to q_ c ÿWm :
2
The continuity equation for the air (subscript a) takes the form q_ a ÿr
qa wa
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and for the vapor, q_ v ÿr
qv wv Wv :
4
The conservation of gas phase mass gives q_ m ÿr
qm wm Wm :
5
Fick's law allows the ¯uxes to be presented in the forms of Eqs. (6) and (7): ja qa
wa ÿ wm ÿqm Drqba ;
6
where qbi qi =qm is the mass fraction of species i with respect to the density of the air±vapor mixture, and D is the diusion coecient for Fick's law for the air±vapor mixture; and jv qv
wv ÿ wm ÿqm Drqbv :
7
Finally, we get the following species equations: qmba qm wm rqba r
qm Drqba ÿ qba Wm
8
qmbv qm wm rqbv r
qm Drqbv
1 ÿ qbv Wm :
9
and
2.3. Thermal equations The ¯uxes of heat q and ¯owing gases r can be expressed as q ÿkrh
10
r qa wa ha qv wv hv ;
11
and
where k is the thermal conductivity, h is the temperature and hi is the enthalpy of component i per unit mass of component i. Eq. (11) can be transformed [19] to the form r qm wm hm ÿ qm Dha rqba ÿ qm Dhv rqbv
12
r qm wm hm qm D
hv ÿ ha rqba :
13
or
Assuming that qe qs hs qc hc qm hm ÿ qm Rm h;
14
where e is the thermal energy and R is the gas constant, the thermal equations can be expressed as
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qcp h_ rkrh ÿ qm wm cpm D
cpv ÿ cpa rqba rh ÿ
hv ÿ ha Wm ÿ qm rm_ h;
15
where cp is the speci®c heat at constant pressure. 2.4. Darcy's law The velocity of the air±vapor mixture is given by wm ÿkD rp ;
16
where kD is Darcy's coecient and p is the pressure. 2.5. Thermodynamic relations Assuming that the vapor and air are ideal gases we have the following relations. 2.5.1. Ideal gas equation for the vapor pv V v qv Rv h;
17
where V i qi =qai represents the volume occupied by component i per unit total volume. 2.5.2. Ideal gas equation for the air pa V a qa Ra h:
18
2.6. Clausius±Clapeyron equation Since the liquid and vapor are assumed to be in equilibrium, pv psat
h in the presence of liquid water. An analytic expression for psat is A ÿ
B=Rv exp ÿ : psat
h Ch Rv T
19
20
2.7. State equation Using the notations qbi and V i , the state equation can be presented as pv
/ ÿ V c qm qbv Rv h
1 ÿ qba qm Rv h and
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pa
/ ÿ V c qm qba Ra h;
1989
22
where V v V a
/ ÿ V c and / is the porosity. Combining the above equations we get p
/ ÿ V c qm Rm h;
23
where Rm qbv Rv qba Ra :
24
2.8. Porosity In a linearized approach, the current porosity / depends on the current values of ¯uid mass density, strain and increase in ¯uid mass content according to relation qc ÿ qc;o m tr e
25 ÿ /o / /o qc;o qc;o where m is the ¯uid mass content, qc;o is the ¯uid mass density in the reference state, /o is the porosity in the reference state. In in®nitesimal transformation, the trace tr e eii of the linearized stress tensor e represents the volume change per unit volume in the deformation. It is called volume dilatation. 2.9. Thermo-elastic-plastic constitutive equations 2.9.1. Isotropic hardening The basic hypothesis of isotropic hardening is the assumption that the shape of the yield surface is unchanging, and its growth can be described by one scalar parameter which is a function of plastic deformation. We can describe the plastic potential function F of the porous material by the porous material by the equation [24] F F
rij ; K; h; p
26
where rij is the stress tensor, and K is the work ± hardening parameter. According to the Quinney±Taylor (QT) hypothesis [23] K_ rij e_ pij :
27
If we dierentiate F by using the chain rule for partial dierentiation we obtain oF oF _ oF _ oF _ F_ r_ ij p: K h orij oK oh op
28
Using the QT hypothesis, it is seen that the second term in the right-hand side of Eq. (28) can be expressed in terms of plastic strains rates e_ pij as
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oF _ oF oK p e_ : K oK oK oepij ij
29
Combining Eqs. (28) and (29) gives oF oF oK p oF _ oF _ F_ r_ ij e_ h p: orij oK oepij ij oh op
30
Equilibrium conditions require that variation of the plastic energy be stationary oF oF oK p oF _ oF F_ r_ ij e_ h p_ 0: orij oK oepij ij oh op
31
In the approach presented we assume the small strain thermo-elastic-plasticity theory in which the total small strain rate is a sum of elastic, thermal, plastic and strain rate due to pressure changes. By this assumption strain rate tensor in a thermo-elasto-plastic process in a solid body is of the form e_ ij e_ eij e_ Tij e_ bij e_ pij ;
32
where e_ ij ; e_ eij ; e_ Tij ; e_ bij ; e_ pij are the rates of the total, elastic, thermal, pressure and plastic strain tensor, respectively. After rearranging Eq. (32) we can obtain the components of the elastic strain rate tensor e_ eij e_ ij ÿ e_ Tij ÿ e_ bij ÿ e_ pij :
33
Making use of Hooke's law the rates of change of the total stress are given as e
_eekl ÿ e_ Tkl ÿ e_ bkl ÿ e_ pkl ; r_ ij Cijkl e where Cijkl are components of the elasticity tensor 1 2 e Cijkl dik djl dil djk ÿ dij dkl ; 4G 1m
34
35
and G is the shear modulus, m is Poisson's ratio, dij is the Kronecker delta. Combining Eqs. (31), (33) and (34) and considering the ¯ow rule e_ pij k
oF ; orij
36
we get oF e oF oK oF oF _ oF _ Cijkl
_ekl ÿ e_ Tkl ÿ e_ bkl ÿ e_ pkl k h p: p orij oK oeij orij oh op
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After some calculations we obtain the relation for the proportionality factor k T b oF oF _ oF e _ _ _ h p C
_ e ÿ e ÿ e kl kl orij ijkl kl oh op k : oF oF oF oK oF e C ÿ p orpq pqrs orrs oK oe opq
1991
38
pq
Introduce the notations S
oF e oF oF oK oF C ÿ ; orpq pqrs orrs oK oeppq orpq
39
_ e_ Tij aij h;
40
aij ah dij
41
_ e_ bij Bij p;
42
Bij
3
mu ÿ m dij ; 2GBu
1 m
1 mu
43
where mu is the undrained Poisson ratio, ah is the thermal expansion coecient and Bu is the induced pore pressure parameter. In general, 0 < Bu 6 1;
1 0 < m < mu 6 : 2
From Eqs. (38)±(42) we get 1 oF e oF _ oF _ _ C
_ekl ÿ akl h ÿ Bkl p k h p_ : S orij ijkl oh op
44
45
Next combining Eqs. (34) and (45) we have e Cijkl oF e e _ _ekl ÿ Cijkl _rij Cijkl _
akl h Bkl p S orkl oF e oF _ oF _ _ C
_ekl ÿ akl h ÿ Bkl p h p_ : orij ijkl oh op
46
After rearranging the terms
1 e oF oF e e e _ ÿ Cijkl
akl h_ Bkl p C e_ kl e_ kl ÿ Cijkl r_ ij Cijkl S orkl orij ijkl 1 e oF oF e 1 e oF oF _ oF _ _ ÿ Cijkl Cijkl C
akl h Bkl p h p_ : S orkl orij ijkl S orkl oh op
47
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Assuming the Huber±Mises (HM) condition and making use of the fact oF sij orij
48
we can de®ne the so-called plasticity tensor 1 e oF oF e 1 p e Cijkl C C e skl sij Cijkl Cijkl S orkl orij ijkl S ijkl
49
where sij are components of the deviatoric stress tensor. 1 sij rij ÿ rkk dij : 3
50
By substituting Eq. (49) into Eq. (47) we get p e e e _ ÿ Cijkl _ r_ ij Cijkl
akl h_ Bkl p
akl h_ Bkl p e_ kl ÿ Cijkl e_ kl Cijkl 1 e oF oF _ oF ÿ Cijkl h p_ : S orkl oh op
51
De®ning the so-called elasto-plasticity tensor ep p e Cijkl ÿ Cijkl Cijkl
52
the thermo-elasto-plastic constitutive equation can be expressed as r_ ij
ep Cijkl e_ kl
ÿ
ep Cijkl
akl h_
e Cijkl skl _ ÿ Bkl p S
oF _ oF h p_ : oh op
53
One may ®nd that during plastic deformation of a solid e skl 2Gsij Cijkl
54
due to the fact that the ®rst deviatoric strain invariant vanishes. It leads to the following relation p on Cijkl : e e Cijkl skl sij Cijkl 2G sij skl 2G 4G2 sij skl :
55
e srs 2Gspq the ®rst term in Eq. (39) can be Now we evaluate the S given by Eq. (39). Since Cpqrs expressed as
oF e oF 2 r2 4 2 e Cpqrs spq Cpqrs srs spq 2Gspq 2G G r; 3 orpq orrs 3
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where 1 2 1 spq spq : r 3 2
57
By Eq. (27) and Eq. (36) we have oF K_ krij : orij
58
From Eq. (27) we get rij
K_ : e_ pij
59
During plastic deformation of work-hardening materials, the yield strength increases with load. The de®nitions of the HM plastic potential function can be used to derive the following useful relation: oF o 1 2 2 o r ÿ r J2s ÿ r ; oK oK 3 3 oK
60
where J2s is the second invariant of the devatoric stress. If we refer to a typical ¯ow curve, we have dep ; dK r
61
dep 1 : dK r
62
or
Since o r o r dep 1 H0 H0 ; p r oK oe dK r
63
where H 0 is the plastic modulus of the material in a multiaxial stress state (see Fig. 1) H0
o r : oep
Eq. (60) will have the form 0 oF 2 H 2H 0 ; ÿ r 3 r oK 3 which leads to the following relation:
64
65
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Fig. 1. Slope H 0 as a plastic modulus of the material during plastic deformation.
oF oK oF 2H 0 2 2 2 4 2 0 ÿ r H: ÿ rpq ssq ÿ H 0 r p 3 oK oepq orpq 3 3 9
66
Then S can be expressed in terms of the material properties and the state of stress as follows: 4 4 2 0 4 2 2 H ÿ r
3G H 0 :
67 r ÿ ÿ r S G 3 9 9 2.9.2. Kinematic hardening In processes of kinematic hardening, in order to describe the motion of the initial yield surface, one introduces the translation tensor aij , whose components determine a new position of the yield surface centre. Ziegler [20] assumes a motion of the surface in the direction of the dierence of r and a: _ ij ÿ aij ; a_ ij l
r
68
where l_ is the multiplier. Melan [21] has proposed de®nition of the tensor aij as a_ ij C e_ pij :
69
This de®nition was also used by Prager [22]. Considering the modi®cation of the yield surface with respect to temperature and pressure we assume C C
h; p:
70
The plastic potential function F can be expressed as F F
rij ; aij ; h; p:
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The total dierential of F is oF oF oF _ oF F_ r_ ij a_ ij h p_ 0: orij oaij oh op
72
The condition, Eq. (72), is sometimes called the compatibility equation for the plastic yielding condition. On the basic of Eq. (68) we can obtain the following relations: oF oF ÿ ; oaij orij orij ÿ1: oaij
73
74
If one substitutes the above expressions into Eq. (72) the following relations is obtained: oF oF _ oF
r_ ij ÿ a_ ij h p_ 0 orij oh op
75
oF oF oF _ oF _ a_ ij r_ ij h p: orij orij oh op
76
or
Further substitution of Eq. (68) into the above expression yields oF oF _ oF _ _ h p r ij orij oh op : l_ oF
rkl ÿ akl orkl
77
In kinematic hardening theory we de®ne the so-called translated stress tensor rij rij ÿ aij ;
78
and translated stress deviators 1 sij rij ÿ rkk dij : 3
79
The yield function becomes 2 F sij sij ; 3
80
which leads to the expression osij oF 3sij 6sij : orij orij
81
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By substituting Eq. (81) into Eqs. (77) and (78) we get u_
k
h_ oF p_ 6sij r_ ij oF oh op 6rpq spq
;
82
h_ oF p_ 6sij r_ ij oF 1 oh op ; 36spq spq C
h; p
83
e_ pij 6sij k:
84
Assuming the decomposition (32) e_ ij e_ eij e_ Tij e_ bij e_ pij ;
85
and using Hooke's law one obtains e r_ ij Cijkl
_ekl ÿ e_ Tkl ÿ e_ bkl ÿ e_ pkl
86
e e r_ ij Cijkl
akl h_ Bkl p_ 6skl k: e_ kl ÿ Cijkl
87
or
Substituting Eq. (69) and Eq. (81) into Eq. (36) gives a_ ij 6C
h; psij k:
88
The above expression, after substituting into Eq. (72), gives oF oF _ oF F_
r_ ij ÿ 6C
h; psij k h p_ 0: orij oh op
89
By Eqs. (89) and (83) we get oF oF _ dF e e _
Cijkl
akl h_ Bkl p e_ kl ÿ Cijkl h p_ orij oh op : k oF e s 6
C
h; pspq Cpqrs rs orpq
90
Substituting Eq. (90) into Eq. (87) we get e e _ e_ kl ÿ Cijkl
akl h_ Bkl p r_ ij Cijkl
ÿ
oF e orij Cijkl skl
e e _ oF h_ oF p_
Cijkl
akl h_ Bkl p e_ kl ÿ Cijkl oh op s oF 6
C
h; pspq Cpqrs rs orpq
:
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Let e srs S
C
h; pspq Cpqrs
oF e 6spq spq C
h; p 6spq Cpqrs srs : orpq
92
With the aid of Eq. (92) the relation Eq. (91) becomes oF 1 e e e e _ ÿ Cijkl _
akl h_ Bkl p skl e_ kl ÿ Cijkl
C e_ kl
akl h_ Bkl p r_ ij Cijkl orij S ijkl 1 e oF _ oF 1 e e oF e ÿ Cijkl skl e_ kl C h p_ Cijkl ÿ Cijkl skl S oh op S orij ijkl 1 1 e oF _ oF e e oF e _ _ ÿ Cijkl skl
akl h Bkl p ÿ Cijkl ÿ C Cijkl skl h p_ : S orij ijkl S oh op
93
Assuming that 1 1 p e oF e e e Cijkl
6Cijkl skl sij Cijkl Cijkl Cijkl skl s orij S
94
and ep p e Cijkl Cijkl ÿ Cijkl ;
95
the constitutive equation for kinematic hardening material subject to thermo-elasto-plastic deformation takes the form r_ ij
ep Cijkl e_ kl
ÿ
ep Cijkl
akl h_
1 e oF _ oF _ ÿ Cijkl skl Bkl p h p_ : S oh op
96
2.10. Momentum balance If no body force exists, the momentum balance in the quasi-static nonisothermal context is rij;j 0:
97
2.11. Strain±displacement relation The deformation of the material is described by the strain tensor eij , which is de®ned in terms of the displacement ui of the solid constituent as follows: 1 eij
ui;j uj;i : 2
98
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3. Example 3.1. Simpli®ed equations for a 1D axisymmetrical problem One of the simple examples of the thermo-poro-elasticity theory presented in this paper is 1D axisymmetrical problem. In such a case the set of governing equations and suitable boundary conditions in a cylindrical coordinate system take the form as follows. 3.1.1. Thermal equations
qcp
oh o2 h 1 o D
cpr ÿ cpa oqba oh k 2 r ÿ qm cpm wm or or ot or r or cpm o ÿ
hv ÿ ha Wm ÿ
qm Rm h ; ot
99
h
r; 0 h0
r;
100
oh
0; t 0; or
101
and ÿk
oh
R; t hh
R; t ÿ hf
t f rh4
R; t ÿ h4f
t; or
102
where R is the radius of the element, hf is the environmental temperature, h is the convective heat transfer coecient, f is the eective shape factor for radiation and r is the Stefan±Boltzman constant. 3.1.2. Species equations oqba o2 qba oqba qba Wm 1 o D ÿ ;
rqm D ÿ wm 2 ot or or qm qm r or
103
qba
r; 0 qba;0
r;
104
oqba
0; t 0: or
105
and
A. Søu_zalec / International Journal of Engineering Science 37 (1999) 1985±2005
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3.1.3. Continuity equations oqm 1 o
rqm wm Wm ; ot r or
106
wm
0; t 0;
107
oqc ÿWm ; ot
108
qc
r; 0 qc;0
t:
109
and
3.1.4. Field equations (
drrr
)
" 2G
drhh
1ÿm 1ÿ2m
m 1ÿ2m
m 1ÿ2m
1ÿm 1ÿ2m
err ehh
derr
) ÿ
3
ml ÿ m dp Bl
1 ml
1 ÿ 2m #( ) d 2rr srr shh
dehh " 2 2G
1 m 2G srr ÿ adh ÿ 1 ÿ 2m So srr shh s2hh d 2hh " 2 # srr shh 2G srr 3
ml ÿ m adh dp So srr s2hh s2hh 2GBl
1 m
1 ml " 1ÿm #( ) m srr 2G 1ÿ2m 1ÿ2m oF oF dh dp ÿ m 1ÿm So oh op shh 1ÿ2m
#(
110
1ÿ2m
ou r
or ur r
111
where 2 2 H0 1 So r : 3G 3
112
The plastic potential function is assumed in the form r 1 2 F
rrr ÿ rhh
Bp ch ÿ k 0 2 where b; c and k are material parameters.
113
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The thermodynamics relations are given by Eq. (17) and Eq. (18), the Clausius±Clapeyron equation by Eq. (20) and Darcy's law by Eq. (16). 3.2. The solution The solution is obtained by an implicit ®nite dierence technique with a constant grid and variable time step sizes. Since the equations describing heat and mass transfer in porous materials are partial dierential equations of parabolic type, the solutions of such equations are well known and can be found in many textbooks on numerical analysis. These data do not provide any special information regarding this paper and have been omitted. For most heating situations with rapid heating a time step size of 1 s is found to be satisfactory for the calculations. A mesh size of slightly less than 2 10ÿ3 m was found to be adequate for the example. 3.3. Temperature, pressure and stresses in a 1D axisymmetrical element The speci®c case of a 1D axisymmetrical structural element with a uniform initial temperature is considered to illustrate the results of the analysis (Fig. 2). The radius of the considered cylindrical element is 0.12 m. The initial moisture content is from 0 to 0.108 m and the remaining 0.108 to 0.12 m is supposed to be dry. The assumption of the existence of a dry region close to the surface is often validated. The thermal and mechanical parameters used are presented in Table 1. Fig. 3 presents the temperature in the porous element as a function of time for the assumed heating curve for a 10 J=s m2 K, kD 10ÿ11 m3 s=kg and qc;o 70 kg=m3 . In Fig. 4 one can observe maximum pressures for various values of kD and in Fig. 5 changes of pressure with time.
Fig. 2. Cylinder under consideration.
A. Søu_zalec / International Journal of Engineering Science 37 (1999) 1985±2005
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Table 1 Thermal and mechanical parameters used in this study cp 1040 J=kg K
kD 5 10ÿ12 to 1 m3 s=kg
D 2:142 10ÿ5 m2 =s f 0:9 a 0 to A aD 1 A 3:18 106 J=kg B 2470J=kg K C 6:05 1026 N=m2 ah 10 10ÿ6 1=K b 0:1 c 0:1 K 5 106 N=m2
qba1 1:0 a 5:22 10ÿ7 m2 =s / 0:2 q 2400 kg=m3 qc;o 0:200 kg=m3 Bu 0:7 m 0:16 mu 0:17 E 2 1010 N=m2
Fig. 6 shows the distribution of stresses for maximum pressures (kD 10ÿ12 m3 s=kg and t 3 103 s). Figs. 4 and 5 show the pressure pro®les and pressure histories respectively for the several values of Darcy's coecient. Fig. 4 indicates that for lower values of Darcy's coecients pressures in elements increases. So for very porous material such as sand the pressures are very low and we do not observe signi®cant deformations due to pressure eect during heating. Increasing of Darcy's coecient shifts the point of maximum pressure toward the inside. This is consistent with the preceding argument since to have reasonable ¯ow resistance the point should
Fig. 3. Temperatures in the structural element for a 10 =sm2 K, kD 10ÿ11 m3 s=kg and qc;0 70 kg=m3 : (a) r 120 mm; (b) r 100 mm; (c) r 80 mm; (d) r 60 mm.
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Fig. 4. Maximum pressures as a function of the distance from the heating surface for various kD values: (a) kD 10ÿ12 m3 s=kg; (b) kD 10ÿ10 m3 s=kg.
Fig. 5. Changes of pressure as a function of time for various kD values: (a) kD 10ÿ12 m3 s=kg; (b) kD 10ÿ10 m3 s=kg.
A. Søu_zalec / International Journal of Engineering Science 37 (1999) 1985±2005
Fig. 6. Radial (a) and circumferential (b) stresses in an element for kD 10ÿ12 m3 s=kg and t 3 103 s.
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be farther inside the medium for a higher value of Darcy's coecient. The pressure term in¯uences on the stresses pro®les in the element.
4. Concluding remarks An analysis is developed for heat and mass transfer in a wet porous medium subject to unsteady, nonlinear boundary conditions. The simpli®ed equations have been solved simultaneously by an implicit ®nite dierence technique. The assumption of no liquid movement was made in the development of the present theory. This assumption is probably valid for low and medium pressures. However, for high pressures it is questionable.
References [1] V.K. Sherwood, Application of the theoretical diusion equations to the drying of solids, Trans Am. Inst. Mech. Eng. 27 (1931) 190±202. [2] R. Buckingham, Studies in the movement of soil moisture, US Department Agr. Bur. Soils Bull. 38 (1907) 29±61. [3] C.G. Gurr, T.J. Marshall, J.T. Hutton, Movement of water in soil due to a temperature gradient, Soil Science 74 (1952) 335±345. [4] S.E. Pihlajavaara, Introductory bibliography for research on drying of concrete. The state Institute for Technical Research, Helsinki, 1964. [5] Z.P. Bazant, L.J. Najjar, Nonlinear water diusion in nonsaturated concrete, Materials Constructions 5 (25) (1972) 3±20. [6] S. Whitaker, A theory of drying in porous media, Adr. Heat Transfer 12 (1977) 34. [7] Z.P. Bazant, Constitutive equation for concrete and shrinkage based on thermodynamics of multiphase systems, Materials Constructions 3 (1970) 13. [8] M.A. Biot, General theory of three-dimensional consolidation, J. Appl. Phys. 12 (1941) 155. [9] M.A. Biot, Theory of elasticity and consolidation for a porous anisotropic solid, J. Appl. Phys. 26 (1955) 182. [10] M.A. Biot, General solutions of the equations of elasticity and consolidation for a porous material, J. Appl. Phys. 78 (1956) 91. [11] J.R. Rice, M.P. Cleary, Some basic stress diusion solutions for ¯uid-saturated elastic porous media with compressible constituents, Rev. Geophys. Space Phys. 14 (1976) 227. [12] M.P. Cleary, Fundamental solutions for ¯uid-saturated porous media and application to localized rupture phenomena, Ph.D. thesis, Univ. Micro®lms Int., Ann Arbor, MI, 1976. [13] M.P. Cleary, Fundamental solutions for a ¯uid-saturated porous solid, Int. J. Sol. Struc. 13 (1977) 785. [14] M.P. Cleary, Moving singularities in elasto-diusive solids with applications to fracture propagation, Int. J. Sol. Struc. 14 (1978) 81. [15] J.W. Rudnicki, Plane strain dislocations in linear elastic diusive solids, J. Appl. Mech. 54 (1987) 545. [16] M.J. Crochet, P.M. Naghdi, On constitutive equations for ¯ow of ¯uid through an elastic solid, Int. J. Eng. Sci. 4 (1966) 383. [17] R.M. Bowen, Incompressible porous media models by use of the theory of mixtures, Int. J. Eng. Sci. 18 (1980) 1129. [18] R.L. Schiman, A thermoelastic theory of consolidation, Envir. Geophys. Heat Transfer 4 (1971) 78. [19] A. Søu_zalec, J. Paluszy nski, Thermal and moisture phenomena in heat-resisting concrete, Archiv of Thermodynamics 11 (3/4) (1990) 135±157. [20] H. Ziegler, A modi®cation of Prager's hardening rule, Q. Appl. Math 17 (1) (1959) 55±56. [21] E. Melan, Zur Plastizit at der r aumliichen Kontinuums, Ing. Archiv 9 (1938) 116±126.
A. Søu_zalec / International Journal of Engineering Science 37 (1999) 1985±2005
2005
[22] Prager, W. The general theory of limit design, Proceedings of the Eighth International Congress on Appl. Mech, Istanbul, 2 (1955) 65±72. [23] Taylor, G., Quinney, H., The plastic distortion of metals, Phil. Trans. R. Soc. Ser. A 230 (1931) 323±362. [24] A. Søu_zalec, Introduction to Nonlinear Thermomechanics, Springer, Berlin, 1992.