Chapter 3 : Reservoir models - KU Leuven
Chapter 3 : Reservoir models - KU Leuven
Chapter 3 : Reservoir models - KU Leuven
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Other more detailed runoff <strong>models</strong> could be used, but the calibration of the parameters<br />
requires large amounts of high quality data. Although a detailed runoff model for the<br />
pervious areas might be necessary for the modelling of runoff to brooks and rivers<br />
(e.g. [Clarke, 1994; DHI, 1993]), the influence of pervious areas and certainly<br />
the influence of the detail of the infiltration description will be small for urban<br />
drainage. If it is necessary to incorporate the infiltration, in most cases the rough<br />
description by Horton (equation 3.5) will suffice.<br />
Next to the losses, also the smoothing by the overland flow should be considered.<br />
Many complex <strong>models</strong> can be used for this, as was described in paragraph 1.3.3.<br />
However, if this is already taken into account in the single storm simulations that are<br />
used for the calibration of the routing model, the smoothing is already incorporated in<br />
the routing part of the simplified model.<br />
3.2.5 Complex systems<br />
In the previous paragraphs, the sewer system characterisation was applied to simple<br />
sewer systems with one overflow. In reality, sewer systems are more complex, but it<br />
is not always necessary to incorporate this complexity into the model. Before a model<br />
is built, the modeller has to decide which output he wants to obtain. Then, the model<br />
has to be built in such a way that the required output is achieved with the desired<br />
accuracy.<br />
The first step in the transformation of a combined sewer system into a reservoir model<br />
is to separate the hydraulically independent subcatchments. This can be done<br />
e.g. at pumping stations, internal weirs, places where the critical water depth always<br />
occurs, ... The number of places where these conditions occur may be limited.<br />
However, other places can be used to disconnect different subcatchments as long as no<br />
significant backwater effects occur at these places. Whether a certain place is suitable<br />
for disconnecting subcatchments, can be seen in the storage/throughflow-relationships.<br />
If the storage volume in the subcatchment cannot be linked unambiguously to the<br />
inflow and outflow, the place is not suitable for disconnection of subcatchments. In all<br />
other cases the disconnection can be applied at that place.<br />
As a reservoir model is a conceptual model, the outflows of the reservoir do not<br />
necessarily have to agree with the flow in a single pipe or at a single overflow.<br />
The throughflow can be the sum of different pipes which connect two<br />
subcatchments and the overflow can be the sum of two overflows which spill into<br />
the same brook or river. This gives more possibilities to separate subcatchments,<br />
but also to simplify the <strong>models</strong>.<br />
<strong>Chapter</strong> 3 : <strong>Reservoir</strong> <strong>models</strong> 3.25