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How can I estimate a coefficient of pde connecting pdepe and lsqcurvefit functions?

조회 수: 2 (최근 30일)
I am trying to fit only D coefficient and I am getting a following error:
??? Attempted to access fL(1); index out of bounds because numel(fL)=0.
Error in ==> pdepe>pdeodes at 363 up(j,1) = sL(j) + (m+1) * fL(j) / xi(1);
Error in ==> odearguments at 98 f0 = feval(ode,t0,y0,args{:}); % ODE15I sets args{1} to yp0.
I would be grateful for any help.

답변 (1개)

Zana Taher
Zana Taher 2019년 4월 7일
Using the matlab function lsqnonlin will work better than lsqcurvefit. Below is an example code for using lsqnonlin with pdepe to solev parameters for richard's equation.
global exper
exper=[-0.4,-112,-121,-128,-131,-131.1,-133.2,-133.1,-134.4,-134.7,-135.12,-135.7,-135.8,-135.1,-135.4,-135.8,-135.9,-134,-135.7,-135.1,-135.3,-135.4,-136,-139,-136];
% p=[0.218,0.52,0.0115,2.03,31.6];
% qr f a n ks
p0=[0.218,0.52,0.0115,2.03,31.6];
lb=[0.01,0.4,0,1,15]; %lower bound
ub=[Inf,Inf,10,10,100]; %upper bound
options = optimoptions('lsqnonlin','Algorithm','trust-region-reflective','Display','iter');
[p,resnorm,residual,exitflag,output] = lsqnonlin(@richards1,p0,lb,ub,options)
uu=richards1(p);
global t
plot(t,uu+exper')
hold on
plot(t,exper,'ko')
function uu=richards1(p)
% Solution of the Richards equation
% using MATLAB pdepe
%
% $Ekkehard Holzbecher $Date: 2006/07/13 $
%
% Soil data for Guelph Loam (Hornberger and Wiberg, 2005)
% m-file based partially on a first version by Janek Greskowiak
%--------------------------------------------------------------------------
L = 200; % length [L]
s1 = 0.5; % infiltration velocity [L/T]
s2 = 0; % bottom suction head [L]
T = 4; % maximum time [T]
% qr = 0.218; % residual water content
% f = 0.52; % porosity
% a = 0.0115; % van Genuchten parameter [1/L]
% n = 2.03; % van Genuchten parameter
% ks = 31.6; % saturated conductivity [L/T]
x = linspace(0,L,100);
global t
t = linspace(0,T,25);
options=odeset('RelTol',1e-4,'AbsTol',1e-4,'NormControl','off','InitialStep',1e-7)
u = pdepe(0,@unsatpde,@unsatic,@unsatbc,x,t,options,s1,s2,p);
global exper
uu=u(:,1,1)-exper';
% figure;
% title('Richards Equation Numerical Solution, computed with 100 mesh points');
% subplot (1,3,1);
% plot (x,u(1:length(t),:));
% xlabel('Depth [L]');
% ylabel('Pressure Head [L]');
% subplot (1,3,2);
% plot (x,u(1:length(t),:)-(x'*ones(1,length(t)))');
% xlabel('Depth [L]');
% ylabel('Hydraulic Head [L]');
% for j=1:length(t)
% for i=1:length(x)
% [q(j,i),k(j,i),c(j,i)]=sedprop(u(j,i),p);
% end
% end
%
% subplot (1,3,3);
% plot (x,q(1:length(t),:)*100)
% xlabel('Depth [L]');
% ylabel('Water Content [%]');
% -------------------------------------------------------------------------
function [c,f,s] = unsatpde(x,t,u,DuDx,s1,s2,p)
[q,k,c] = sedprop(u,p);
f = k.*DuDx-k;
s = 0;
end
% -------------------------------------------------------------------------
function u0 = unsatic(x,s1,s2,p)
u0 = -200+x;
if x < 10 u0 = -0.5; end
end
% -------------------------------------------------------------------------
function [pl,ql,pr,qr] = unsatbc(xl,ul,xr,ur,t,s1,s2,p)
pl = s1;
ql = 1;
pr = ur(1)-s2;
qr = 0;
end
%------------------- soil hydraulic properties ----------------------------
function [q,k,c] = sedprop(u,p)
qr = p(1); % residual water content
f = p(2); % porosity
a = p(3); % van Genuchten parameter [1/L]
n = p(4); % van Genuchten parameter
ks = p(5); % saturated conductivity [L/T]
m = 1-1/n;
if u >= 0
c=1e-20;
k=ks;
q=f;
else
q=qr+(f-qr)*(1+(-a*u)^n)^-m;
c=((f-qr)*n*m*a*(-a*u)^(n-1))/((1+(-a*u)^n)^(m+1))+1.e-20;
k=ks*((q-qr)/(f-qr))^0.5*(1-(1-((q-qr)/(f-qr))^(1/m))^m)^2;
end
end
end

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