Bed-load measurements on large, sand-bed rivers in the United States
The movement of bed forms (sand dunes) in large sand-bed rivers is being used to determine the transport rate of bed load. The ISSDOTv2 (Integrated Section Surface Difference Over Time version 2) methodology uses time sequenced differences of measured ...
Abraham David +2 more
doaj +1 more source
Parameter Optimization of a Bed Load Transport Formula for Nestos River, Greece
In the Second EWaS International Conference (June 2016, Chania, Crete, Greece), the bed load transport formula of Meyer-Peter and Müller (1948) was calibrated with respect to the bed roughness coefficient for Nestos River.
Epameinondas Sidiropoulos +2 more
doaj +1 more source
A Formula for The Maximum Rate of Bed-load Transport on Smooth and Fixed Bed
This paper describes a new formula for the calculation of the maximum rate of bed-load transport on smooth and fixed beds. The transport rate in unit width is expressed as the product of the volume of the moving particles on unit area of bed surface and their mean advancing velocity.
OKABE, Takeshi +2 more
openaire +2 more sources
Correction to “A general power equation for predicting bed load transport rates in gravel bed rivers” [PDF]
[1] In the paper ‘‘A general power equation for predicting bed load transport rates in gravel bed rivers’’ by Jeffrey J. Barry et al. (Water Resources Research, 40, W10401, doi:10.1029/2004WR003190, 2004), the y axis for Figures 5 and 10 was incorrectly labeled and should have read ‘‘log10 (predicted transport) – log10 (observed transport).’’ In ...
Jeffrey J. Barry +2 more
openaire +1 more source
Effect of sampling time on measured gravel bed load transport rates in a coarse‐bedded stream [PDF]
This study empirically quantified the effect of sampling time on measured transport rates and fitted rating curves based on results obtained from bed load traps deployed for 2, 10, and 60 min in a coarse‐bedded stream. As expected for a skewed distribution of transport rates, 2 min deployment underpredicted transport rates obtained from 10 and 60 min ...
Kristin Bunte, Steven R. Abt
openaire +1 more source
Influence of Suspended Sediment Load on Roughness Coefficient and Intensity of Flow Turbulence (Case study: Haraz, Rostamabad and Beheshtabad Rivers) [PDF]
Estimating the effect of sediment transport, especially suspended load, is important in river planning and management. The aim of this study was to investigate the effect of suspended sediment load on the roughness coefficient and the intensity of flow ...
Hossein Afzalimehr +3 more
doaj +1 more source
ABSTRACT Background Sickle cell disease (SCD) has undergone major changes in the last decades. Its prevalence has been steadily increasing and numerous advances have been made in the management of the disease. However, the effect in real‐life setting of these major changes is unknown, particularly in a Canadian environment. Procedure We aimed to assess
Maude Cigna +16 more
wiley +1 more source
Improving a multi-grain-size total sediment load model through a new standardized reference shear stress for incipient motion and an adjusted saltation height description [PDF]
Modelling sediment transport is important to understand how fluvial systems respond to climatic change or other transient conditions such as catastrophic sediment release.
M. Le Minor +4 more
doaj +1 more source
Experimental Study on Uniform and Mixed Bed-Load Sediment Transport under Unsteady Flow
The scouring and deposition of sediment caused by unsteady flows (e.g., storm waves and floods) produces many secondary disasters. The resultant bed-load movement exhibits different transport laws compared with that by steady flow.
Zihao Duan +4 more
doaj +1 more source
ABSTRACT Background Establishing a comprehensive apheresis medicine program in a resource‐constrained setting presents significant structural, financial, and logistical challenges. Despite the growing clinical importance of apheresis services globally, published experience from sub‐Saharan Africa remains sparse.
Folasade Adelekan‐Popoola +4 more
wiley +1 more source

