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Mathematical modeling -- heat conduction of subgrade on Permafrost
2022-07-29 02:03:00 【abcwsp】
The problem of subgrade heat conduction on permafrost
Problem description
Pave roads on permafrost 、 Foundation of aircraft runway and some structures . Analyze the structure of this kind of foundation , There is an asphalt layer 、 Concrete layer 、 Dry sand layer 、 Gravel layer 、 Insulating material layer , Below is the wet sandy soil layer and frozen soil layer ( See chart 1). It is known that , The outside temperature is a function of time , The temperature of the frozen soil layer is constant below zero . Please answer the following questions :
- problem 1: Analyze the law of air temperature entering the subgrade , Temperature distribution of each material layer ;
- problem 2: Because the supports of some equipment cannot be fixed on the thawed soil , It must be fixed in permafrost , Therefore, it is very important to determine the thawing location of the underground soil , Please give the dividing line between thawed sand and frozen sand ;
- problem 3: Please give the best thickness of each layer ( Combined with temperature distribution 、 Cost and durability );
- problem 4: Please simulate the permafrost foundation of Qinghai Tibet Railway in China , And give reasonable suggestions to the construction unit .
Model solving
Analysis of problem 1
For question 1 , Considering that the curvature at each point on the frozen soil surface is large enough , Treat the foundation layer as a plane layer parallel to each other , A one-dimensional parabolic partial differential equation model based on Fourier law is established , Because the outside temperature is a function of time , Therefore, we can collect the daily temperature data of the four seasons in Lhasa , Sine function fitting , Thus, the fitting function of the external temperature changing with time is obtained . Take it as the boundary condition of the heat conduction equation , According to the reference, the temperature of frozen soil layer is 0℃ And the following , Selected by this group T 0 = 0 T_0=0 T0=0 ℃ As the right boundary of the heat conduction equation , Given an initial value , By finite difference method , Give a high precision Crank-Nicolson The difference scheme , The discrete system of linear equations is obtained by replacing differential with derivative , Solving linear equations by catch-up method , Get the temperature distribution in time and one-dimensional space dimension , And the stability analysis and error test of the results .
One dimensional coupled parabolic partial differential equation module
Heat conduction equation
According to Fourier heat conduction law , The differential equation of the conductor acquiring heat :
d Q = − λ ∇ u ⋅ d S → d t dQ=-\lambda \nabla u\cdot d\overrightarrow{S}dt dQ=−λ∇u⋅dSdt
Consider that the problem is studied in one dimension , After simplification by integral and Gauss formula t 1 t_1 t1~ t 2 t_2 t2 The heat flowing into the conductor during the time period is :
Q 1 = ∫ t 1 t 2 [ ∫ x 1 x 2 k ∂ 2 u ∂ x 2 d x ] d t Q_1=\int_{t_1}^{t_2}{\left[ \int_{x_1}^{x_2}{k \frac{\partial ^2u}{\partial x^2}dx} \right] dt} Q1=∫t1t2[∫x1x2k∂x2∂2udx]dt
Due to the increase of temperature in the conductor, the absorbed heat is :
Q 2 = ∫ x 1 x 2 c ρ [ ∫ t 1 t 2 ∂ u ∂ t d t ] d x = ∫ t 1 t 2 [ ∫ t 1 t 2 c ρ ∂ u ∂ x d x ] d t Q_2=\int_{x_1}^{x_2}{c\rho \left[ \int_{t_1}^{t_2}{\frac{\partial u}{\partial t}dt} \right] dx}=\int_{t_1}^{t_2}{\left[ \int_{t_1}^{t_2}{c\rho \frac{\partial u}{\partial x}dx} \right] dt} Q2=∫x1x2cρ[∫t1t2∂t∂udt]dx=∫t1t2[∫t1t2cρ∂x∂udx]dt
According to the conservation of energy, the energy relationship equation :
Q 1 = Q 2 Q_1 =Q_2 Q1=Q2
To get :
∂ u ( x , t ) ∂ t = k c ρ ∂ 2 u i ( x , t ) ∂ x 2 \displaystyle \frac{\partial u\left( x,t \right)}{\partial t} = \displaystyle \frac{k}{c\rho } \displaystyle \frac{\partial ^2u_i\left( x,t \right)}{\partial x^2} ∂t∂u(x,t)=cρk∂x2∂2ui(x,t)
among : k k k Is the thermal conductivity , c c c Is the specific heat of conductor , ρ \rho ρ Is the dry density of the conductor .
The schematic diagram of microelement method is shown in Figure 2.
Coupled Parabolic Partial Differential Equations
in consideration of 5 Thermal conductivity of different foundation structures 、 Differences in specific heat and dry density , Establish five one-dimensional heat conduction equations :
∂ u i ( x , t ) ∂ t = k i c i ρ i ∂ 2 u i ( x , t ) ∂ x 2 , i = 1 ⋯ 5 , \begin{align} \displaystyle \frac{\partial u_i\left( x,t \right)}{\partial t} = \displaystyle \frac{k_i}{c_i\rho _i} \displaystyle \frac{\partial ^2u_i\left( x,t \right)}{\partial x^2},i=1 \cdots 5, \end{align} ∂t∂ui(x,t)=ciρiki∂x2∂2ui(x,t),i=1⋯5,
according to Fourier Law of heat conduction , In the process of heat conduction , Heat flux density at the critical interface of two adjacent foundation materials q ⃗ \vec{q} q identical , The coupling condition of heat flux density is obtained :
k i ∂ u i ( x , t ) ∂ n i ∣ Γ i = k i + 1 ∂ u i + 1 ( x , t ) ∂ n i + 1 ∣ Γ i , i = 1 ⋯ 4 , \begin{align} k_i \displaystyle \frac{\partial u_i\left( x,t \right)}{\partial n_i}|_{\varGamma _i} = k_{i+1} \displaystyle \frac{\partial u_{i+1}\left( x,t \right)}{\partial n_{i+1}}|_{\varGamma _i},i=1 \cdots 4, \end{align} ki∂ni∂ui(x,t)∣Γi=ki+1∂ni+1∂ui+1(x,t)∣Γi,i=1⋯4,
The temperature at the critical interface of adjacent conductors is equal at any time , Thus, the critical interface temperature coupling condition of conductor heat transfer is obtained :
u i ( x , t ) ∣ Γ i = u i + 1 ( x , t ) ∣ Γ i , \begin{align} u_i\left( x,t \right) |_{\varGamma _i}=u_{i+1}\left( x,t \right) |_{\varGamma _i}, \end{align} ui(x,t)∣Γi=ui+1(x,t)∣Γi,
Through the sine function second-order fitting of the searched temperature data of the four seasons in Lhasa :
a ( t ) = α i sin ( w 1 t + φ i ) + β i sin ( w 2 t + θ i ) , i = 1 ⋯ 4 , \begin{align} a(t)=\alpha _i\sin \left( w_1 t+\varphi _i \right) +\beta _i\sin \left( w_2 t+\theta _i \right) ,i=1 \cdots 4, \end{align} a(t)=αisin(w1t+φi)+βisin(w2t+θi),i=1⋯4,
Therefore, the fitting function is used as the change function of the external temperature as the boundary condition of the heat conduction equation :
u 0 ( 0 , t ) = a ( t ) , \begin{align} u_0\left( 0,t \right) =a\left( t \right), \end{align} u0(0,t)=a(t),
According to the review, the temperature of frozen soil layer is 0℃ And the following , Selected by this group T 0 = 0 T_0 =0 T0=0, As the right boundary condition :
u 5 ( L 5 , t ) = T 0 , \begin{align} u_5\left( L_5,t \right) =T_0, \end{align} u5(L5,t)=T0,
Finally, the heat conduction equation of the initial boundary value problem is obtained by sorting out the above formula :
{ ∂ u i ( x , t ) ∂ t = k i c i ρ i ∂ 2 u i ( x , t ) ∂ x 2 , x ∈ ( L i − 1 , L i ) , k i ∂ u i ( x , t ) ∂ n i ∣ Γ i = k i + 1 ∂ u i + 1 ( x , t ) ∂ n i + 1 ∣ Γ i , u i ( x , t ) ∣ Γ i = u i + 1 ( x , t ) ∣ Γ i , u 0 ( 0 , t ) = a ( t ) , u 5 ( L 5 , t ) = T 0 , \begin{align} \begin{cases} \displaystyle \frac{\partial u_i\left( x,t \right)}{\partial t} = \displaystyle \frac{k_i}{c_i\rho _i} \displaystyle \frac{\partial ^2u_i\left( x,t \right)}{\partial x^2},x\in \left( L_{i-1},L_i \right),\\ k_i \displaystyle \frac{\partial u_i\left( x,t \right)}{\partial n_i}|_{\varGamma _i} = k_{i+1} \displaystyle \frac{\partial u_{i+1}\left( x,t \right)}{\partial n_{i+1}}|_{\varGamma _i},\\ u_i\left( x,t \right) |_{\varGamma _i}=u_{i+1}\left( x,t \right) |_{\varGamma _i},\\ u_0\left( 0,t \right) =a\left( t \right),\\ u_5\left( L_5,t \right) =T_0,\\ \end{cases} \end{align} ⎩⎨⎧∂t∂ui(x,t)=ciρiki∂x2∂2ui(x,t),x∈(Li−1,Li),ki∂ni∂ui(x,t)∣Γi=ki+1∂ni+1∂ui+1(x,t)∣Γi,ui(x,t)∣Γi=ui+1(x,t)∣Γi,u0(0,t)=a(t),u5(L5,t)=T0,
use CN Format processing
{ u j n + 1 − u j n τ = k i c i ρ i ⋅ [ ( u j + 1 n + 1 − 2 u j n + 1 + u j − 1 n + 1 ) + ( u j + 1 n − 2 u j n + u j − 1 n ) ] 2 h 2 k i u J n − u J − 1 n h = k i + 1 u J + 1 n − u J n h u i ( J , t ) = u i + 1 ( J , t ) u 1 ( 0 , t ) = a ( t ) u 5 ( N , t ) = T 0 J = L i L N \begin{align} \begin{cases} \displaystyle \frac{u_{j}^{n+1}-u_{j}^{n}}{\tau}=\displaystyle \frac{k_i}{c_i\rho _i}\cdot \displaystyle \frac{\left[ \left( u_{j+1}^{n+1}-2u_{j}^{n+1}+u_{j-1}^{n+1} \right) +\left( u_{j+1}^{n}-2u_{j}^{n}+u_{j-1}^{n} \right) \right]}{2h^2}\\ k_i\frac{u_{J}^{n}-u_{J-1}^{n}}{h}=k_{i+1}\frac{u_{J+1}^{n}-u_{J}^{n}}{h}\\ u_i\left( J,t \right) =u_{i+1}\left( J,t \right)\\ u_1\left( 0,t \right) =a\left( t \right)\\ u_5\left( N,t \right) =T_0\\ J=\frac{L_i}{L}N\\ \end{cases} \end{align} ⎩⎨⎧τujn+1−ujn=ciρiki⋅2h2[(uj+1n+1−2ujn+1+uj−1n+1)+(uj+1n−2ujn+uj−1n)]kihuJn−uJ−1n=ki+1huJ+1n−uJnui(J,t)=ui+1(J,t)u1(0,t)=a(t)u5(N,t)=T0J=LLiN
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