Results 1 to 10 of about 66 (62)
Controls on Erosion and Cyclic Step-Formation Upstream of Waterfalls. [PDF]
Abstract Waterfall retreat transmits base‐level perturbations upstream, thereby providing markers of changing climate and tectonics. In homogeneous rock, waterfalls often retreat either by direct waterfall‐face erosion or incision from repeating (‘cyclic’) steps formed above waterfalls.
Inoue T +4 more
europepmc +2 more sources
Hydraulics of free overfall in smooth triangular channels
The present study deals with the hydraulic behavior of smooth triangular channels with free overfall in order to obtain useful relationships for the estimation of end depth discharge (EDD) in terms of brink depth (yb), channel side slopes (m) and channel
Karzan Abdullah Muhsin +1 more
doaj +3 more sources
Power-law free overfall in subcritical flow regime
Free overfall can be used as a discharge measuring structure by a single measurement of end flow depth. Many theoretical and experimental studies carried out on free overfalls with different cross-section shape, different slope (mild and steep), and ...
Ali R. Vatankhah
doaj +3 more sources
Numerical modeling of laminar free overfall in triangular channels
Design of open channel transport and flow measurement systems for highly viscous liquids requires accurate modelling of laminar free overfall. In this study, a computational fluid dynamics model was developed to investigate subcritical laminar free ...
Primož Drešar +3 more
doaj +3 more sources
Using the Brink Depth in Discharge Measurement for Inverted Semicircular Open Channels [PDF]
A free overfall at the end of an open channel provides a simple means for measuring flow discharge. The semicircular open channel plays a significant role in various applications, and it is of interest to calculate its discharge.
Reham Zeidan +2 more
doaj +1 more source
Estimating the scour depth of slope control structures with sharp-crested weir using artificial intelligence models [PDF]
Introduction: In free overfall spillways, waterfalls over the crown of the spillway almost vertically and impacts the downstream bed of the dams. Due to the high velocity and energy of the flow which impacts the erodible downstream bed, it may cause ...
Shahram Mousavi
doaj +1 more source
Different shaped catastrophic palaeoflood hydrographs result in different giant flood bar morphologies and stratification styles. Distinctive morphologies and stratigraphic motifs are associated with, and discriminate, surge wave floods from protracted recessions and prolonged discharges.
Dingzhu Liu +7 more
wiley +1 more source
Abstract Debris flows are among the most dangerous phenomena in mountain environment. Recently the use of seismic and infrasonic recordings has proven to be a powerful tool for studying and monitoring debris flows. However, open questions remain about how signal characteristics refllect flow parameters and fluid dynamic processes.
Giacomo Belli +4 more
wiley +1 more source
One of the significant problems facing the water resource engineer is calculating the coefficient of roughness for subsequent design calculations of the discharge amount of a channel or river. In this study, experiments were conducted in a semi-circular,
Raad Hoobi Irzooki, Ayad Saoud Najem
doaj +1 more source
Little River Experimental Watershed, a keystone in understanding of coastal plain watersheds
Long‐term (52 years) of streamflow data are currently available for nine flow measurement sites in the US EPA Level III Southeastern Plains ecoregion. Hydrologic comparisons across several regional watersheds indicated few differences. Differences found for a smaller nested watershed indicate significant changes in crop and forest coverage can alter ...
David D. Bosch +5 more
wiley +1 more source

