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Transients between free-surface and pressurized conduit flow are handled by changing the capacity term of the conduit flow equation.
This chapter concerns two types of flow open-surface channel flow open-surfaceonduit flow.
Detailed hydraulic head profiles also show no influence of conduit flow.
This formula is based on a 1-dimensional steady conduit flow model that considers vertical gas escape from magma.
During the rainy season strong rain events induce point recharge from surface water through fast conduit flow.
The numerical analysis also helped us to estimate the proportion of the disconnected karstic conduit flow to the overall flow.
Similar(19)
A detailed parametric analysis allowed the re-calibration of two of these laws, which are now specifically tailored for the case of highly concentrated conduit flows that feed collapsing columns, and dilute flows that feed convective plumes.
The spatio-temporal variability of the observed exchanges was explored using a 2D coupled continuum-conduit flow model under saturated conditions (Feflow®).
However, the steady conduit-flow model in the present study assumes a vertical geometry.
In contrast, some karst springs reported in literature display a discharge maximum, attributed to reaching the finite discharge capacity of the conduit system (flow threshold).
Conclusions: The findings indicate that fenoldopam, 0.1 μg/kg/min, did not influence coronary conduit blood flow to a clinically significant extent.
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