Determination of critical shear stress of non‐cohesive soils using submerged jet test and turbulent kinetic energy

Laboratory tests using Jet Erosion Testing (JET) apparatus, impinging normally on a horizontal boundary, were conducted to determine the critical shear stress ( τ c ) of non‐cohesive soil samples. A three‐dimensional (3D) SonTek/YSI 16 MHz Micro‐Acoustic Doppler Velocimeter (MicroADV) was used to measure turbulent kinetic energy (TKE) at a radial limit of entrainment in the wall jet zone and the measurements were used to calculate τ c of the samples. The results showed that TKE increases exponentially with increasing particle size. The τ c from this study were comparable ( R 2  = 0.8) to the theoretical τ c from Shields diagram after bed roughness scale ratio ( D / k s ), due to the non‐uniform bed conditions, was accounted for. This study demonstrated that JET and TKE can be used to determine τ c of non‐cohesive soils. The use of JET and TKE was found to be faster and easier when compared to the conventional approach of using flumes. A relationship of TKE at the onset of incipient motion (TKE c ) and samples’ D 50 developed in this study can be used to predict τ c of non‐cohesive soils under similar non‐uniform conditions. Copyright © 2015 John Wiley & Sons, Ltd.