English (United Kingdom)

https://curated-unify.zendy.io/wp-json/zendy-region/v1/featured_content/oa?rat=en

https://curated-unify.zendy.io/wp-json/zendy-region/v1/highlighted_journal/

Global: Zendy Plus annual

Presents the access of premium content as premium feature

Premium Content

Presents the keyphrase highlighting as premium feature

Keyphrase Highlighting

Presents the summarisation as premium feature

Summarisation

Insights

Presents the pdf analysis as premium feature

PDF Analysis

Presents the zaia usage as premium feature

ZAIA

Global: Zendy Tools annual

Global: Zendy Free Plan

Global: Zendy Tools monthly

Global: Zendy Plus monthly

Stream-bed porosity has received substantial interest of research in the field of fluvial hydraulics since few decades and the focus of our present study has been on the respond of gravel-bed porosity on form-induced shear stresses and pressure energy diffusion rates in open channel flows. An inherent parameter called roughness geometry function is introduced to further broaden the aforementioned issues within the frameworks of near-bed turbulent flow characteristics. Laboratory experiments were conducted over three rough beds: (a) uniformly poised gravel bed (b) water-worked bed and (c) uniformly poised sphere bed. The roughness geometry functions of the channel beds are compared to those obtained by water displacement method. An acoustic Doppler velocimeter is used to measure the instantaneous velocity components and double-averaging methodology is applied for data interpretation. Most significantly, the form-induced shear stresses were predicted 30–42% of the double averaged Reynolds shear stresses in case of water-worked bed. The extreme upper limits of the form-induced shear stress distributions in all the three beds corroborated the effects of gravel bed porosity. Furthermore, the negative pressure energy diffusion rates with increasing turbulent production provided additional support offering overwhelming evidence of the effects of gravel bed porosity within the interfacial sub-layer.

Role of roughness geometry function on spatially averaged form induced shear stresses and pressure energy diffusion rates in gravel-bed stream