Geoscience Reference
In-Depth Information
The discretized sediment equations are then directly solved in the following
sequence:
(1) Compute
A b , i + 1 using Eq. (5.146);
(2) Calculate
A bk , i + 1 using Eq. (5.145);
(3) Compute p n + 1
bk , i
1 using Eq. (5.135);
+
(4) Calculate Q n + 1
t
1 using Eq. (5.141);
k , i
+
(5) Compute Q n + 1
tk , i
1 using Eq. (5.142), and
(6) Update the cross-section topography using Eq. (5.134), and calculate the bed-
material gradations in the subsurface layers.
+
However, the coupled sediment calculation is still decoupled from the flow
calculation so that the entire flow and sediment calculation procedure is in a
semi-coupled form.
The above direct solution method can also be used in the bed-load and suspended-
load transport model in Section 5.3.2, by writing Eqs. (5.130)-(5.132) as Eqs. (5.142)
and (5.143) with C k , i + 1 , C
1 , Q bk , i + 1 , and Q b k , i + 1 as unknowns and deriv-
ing an equation similar to Eq. (5.146) to compute the total bed change
k , i
+
A b , i + 1
directly.
5.3.3.3 Stability of Preissmann scheme for sediment
transport equation
Neglecting the influence of the source term, the error in the sediment transport rate
determined using Eq. (5.138) is governed by
n
+
1
n
+
1
n
i
n
i
c 1
δ
=
c 2
δ
+
c 3
δ
+
c 4
δ
(5.147)
i
+
1
i
+
1
n
i
where
δ
is the Fourier component of the error at point i and time level n , defined
n
i
V n e i σ x i , with V n and
as
being its amplitude and wave number, respectively.
Inserting this definition expression into Eq. (5.147) yields the growth factor:
δ
=
σ
V n + 1
V n
c 3 e i σ x
+
c 4
r
=
=
(5.148)
c 1 e i σ x
c 2
The coefficients of Eq. (5.138) satisfy that c 1
0 and c 2
+
c 3
+
c 4
c 1 at the locally
uniform state. Supposing c 2 , c 3 , and c 4
0 yields
=
c 3 e i σ x
c 4 e i σ x
+
c 4
c 3
+
c 3
+
c 4
|
r
|=
c 2
1
(5.149)
c 1 e i σ x
c 2 e i σ x
c 2
c 1
c 1
which means that the von Neumann stability condition is satisfied. At the locally
uniform state, in which U and L t are constant in each element, the constraints c 2 , c 3 ,
and c 4
0 imply
 
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