Version 2 (modified by 12 years ago) ( diff ) | ,
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Sub Sampling
Cell centered quantities
- AstroBEAR stores most fluid quantities as volume averages in the array
Info%q(i,j,k,:)
- Each cell is a cube with a side
dx=levels(Info%level)%dx
- The 'lower' corner of the cube is located at
Info%xbounds(:,1) + ((/i,j,k/)-1)*dx
- The 'upper' corner of the cube is located at
Info%xbounds(:,1) + ((/i,j,k/))*dx
- The 'center' of the cube is located at
Info%xbounds(:,1) + (REAL(/i,j,k/)-.5)*dx
Sub-sampling
- If we break each cube into NxNxN sub-pieces, and set
ddx=dx/N
then the center of the [ii,jj,kk] sub piece will be atInfo%xBounds(:,1)+(/i-1,j-1,k-1/)*dx + (REAL(/ii,jj,kk/)-.5)*ddx
- So we could use the following routine to initialize cell centered quantities in q. Here is a routine for density.
dx=levels(Info%level)%dx ddx=dx/N DO i=1,Info%mX(1) DO j=1,Info%mx(2) DO k=1,Info%mx(3) new_rho=0d0 DO ii=1,N DO jj=1,N DO kk=1,N pos=Info%xBounds(:,1)+(/i-1,j-1,k-1/)*dx + (REAL(/ii,jj,kk/)-.5)*ddx new_rho=new_rho+rho_func(pos) END DO END DO END DO Info%q(i,j,k,1)=new_rho/N**nDim END DO END DO END DO
or we could try to speed it up by reducing some repeated computations.
dx=levels(Info%level)%dx ddx=dx/N DO i=1,Info%mX(1) pos(1)=Info%xBbounds(1,1)+(i-1)*dx DO j=1,Info%mx(2) pos(2)=Info%xBbounds(1,1)+(i-1)*dx DO k=1,Info%mx(3) pos(3)=Info%xBbounds(1,1)+(i-1)*dx new_rho=0d0 DO ii=1,N ppos(1)=pos(1)+(REAL(ii)-.5)*ddx DO jj=1,N ppos(2)=pos(2)+(REAL(jj)-.5)*ddx DO kk=1,N ppos(3)=pos(3)+(REAL(kk)-.5)*ddx new_rho=new_rho+rho_func(pos) END DO END DO END DO Info%q(i,j,k,1)=new_rho/N**nDim END DO END DO END DO
and sometimes we may be implementing a function that is only defined for a certain region (like a clump object etc…) where the value for q outside of a given radius is unknown. In that case, we just want to add up changes to q for subcells within the region. So for example to calculate the x component of the potential along a given edge we would
dx=levels(Info%level)%dx ddx=dx/N DO i=1,Info%mX(1)+1 pos(1)=Info%xBbounds(1,1)+(i-1)*dx DO j=1,Info%mx(2)+1 pos(2)=Info%xBbounds(1,1)+(i-1)*dx DO k=1,Info%mx(3)+1 pos(3)=Info%xBbounds(1,1)+(i-1)*dx drho=0d0 DO ii=1,N ppos(1)=pos(1)+(REAL(ii)-.5)*ddx DO jj=1,N ppos(2)=pos(2)+(REAL(jj)-.5)*ddx DO kk=1,N ppos(3)=pos(3)+(REAL(kk)-.5)*ddx drho=(rho_func(ppos)-Info%q(i,j,k,1)) END DO END DO END DO Info%q(i,j,k,1)=Info%q(i,j,k,1)+drho/N**nDim END DO END DO END DO
For face centered fields we could also subsample, but their is the divergence criterion to consider for B-fields. We could calculate the potential on a subgrid, and then take a bunch of curls on each face and add them up, but Stoke's theorem lets us just do the integral around the outside. So we really just need to subsample along the appropriate edge for each component of the vector potential.
dx=levels(Info%level)%dx ddx=dx/N DO i=1,Info%mX(1) pos(1)=Info%xBbounds(1,1)+(i-1)*dx DO j=1,Info%mx(2) pos(2)=Info%xBbounds(1,1)+(i-1)*dx DO k=1,Info%mx(3) pos(3)=Info%xBbounds(1,1)+(i-1)*dx drho=0d0 DO ii=1,N ppos(1)=pos(1)+(REAL(ii)-.5)*ddx DO jj=1,N ppos(2)=pos(2)+(REAL(jj)-.5)*ddx DO kk=1,N ppos(3)=pos(3)+(REAL(kk)-.5)*ddx drho=(rho_func(ppos)-Info%q(i,j,k,1)) END DO END DO END DO Info%q(i,j,k,1)=Info%q(i,j,k,1)+drho/N**nDim END DO END DO END DO