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TOPIC: RIGID BED AT UPSTREAM BOUNDARY

RIGID BED AT UPSTREAM BOUNDARY 9 years 7 months ago #16521

  • kipkos
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We wanted to specify the rigid boundary (non erodible) at upstream to be the same as bottom elevation and the following sub routine (noerod.f)

! RIGID BEDS POSITION
!
!
! DEFAULT VALUE: ZR=ZF-100.D0
!
CALL OV('X=Y+C ',ZR,ZF,ZF,-100.D0,NPOIN)

DO I=1,NPOIN
IF(BOUNDARY_COLOUR%I(I).GE.77 .AND.
& BOUNDARY_COLOUR%I(I).LE.97) THEN
ZR(I)=ZF(I)
ENDIF
ENDDO
!

We still have erosion at upstream boundry. Can somebody assist me here!
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RIGID BED AT UPSTREAM BOUNDARY 9 years 7 months ago #16522

  • qilong
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Hi,

Use the different type of boundary for sediment as described in the SISYPHE manual and it can solve this problem:

The following thirteen variables for each edge point are first read out of the boundary conditions file:
X1, X2, X3, X4, X5, X6, X7, LIEBOR, EBOR, X10, X11, N, K.

LIEBOR is an integer providing the type of boundary conditions along the edges :
= KENT (numerical value 5): bottom evolution imposed to EBOR value at a liquid boundary,
= KSORT (numerical value 4): free evolution at a liquid boundary,
= KLOG or KADH (numerical value 2 or 0) : solid boundary.
EBOR provides the values of sedimentary evolutions when they are imposed.

A fixed bottom depth is usually imposed at the boundaries with an inflow (EBOR = 0; LIEBOR = KENT),
whereas a free evolution is imposed at the boundaries with an outflow (LIEBOR = KSORT).

Kind regards,
Qilong
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RIGID BED AT UPSTREAM BOUNDARY 9 years 7 months ago #16524

  • kipkos
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Thanks so much Qilong
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