numerical investigation of formation of bed topography in a u shape channel bend with lateral intake with ssiim2

نویسندگان

حسین آسیائی

حسین منتصری

چکیده

the mechanism of flow and sediment transport in channel bend is much complex. because of secondary current, the sediment moves away from outer bank toward inner bank and therefore outer bank of the bend is one of best positions for lateral diversion. in this paper, the mechanism of sediment transport was simulated with ssiim software in the u shape channel with lateral intake. in order to verify the numerical model results used in montaseri’s lab studies, the position of injection was upstream of bend and sediment injection rate was approximately is equal to 250 gr/min and frude number is equal to 0.32. the ssiim numerical model solves the navier-stokes equations with the k-ε model on a three-dimensional. the bed load can be calculated van rijn’ formula. the numerical model has been implemented at various times to see how the formation and development of bed forms in the u shape channel with lateral intake. the numerical results show that the prediction of development of bed forms, mechanism of sediment entry to intake, location of intermittent dune and location of sediment accumulation are in fairly good agreement with experimental data and the maximum error occurred in front of intake.

برای دانلود باید عضویت طلایی داشته باشید

برای دانلود متن کامل این مقاله و بیش از 32 میلیون مقاله دیگر ابتدا ثبت نام کنید

اگر عضو سایت هستید لطفا وارد حساب کاربری خود شوید

منابع مشابه

Numerical Investigation of Turbulent Mass Transfer in a 90° Bend

This paper presents a numerical study of local mass transfer coefficients in a 90° bend using the RNG version of k–e model to include the influence of curvature on the turbulent transport. Simulations were performed for flow through a 90°, 3-D bend for Reynolds numbers of 13500, 90000, and 390000, Schmidt numbers of 2.53 and 700 and curvature ratios of 1.5, 2, and 2.5. The differences betwe...

متن کامل

Experimental Investigation of Turbidity Flow in 90 Degree Bend with Mobile Bed

Turbidity currents in the ocean and lakes are driven by suspended sediment. The vertical profiles of velocity and excess density are shaped by interaction between the current and bed as well as between the current and the ambient water. This paper presents 48 series of experiments in which saline gravity currents flow through a laboratory sinuous flume. flume contains three successive bends wit...

متن کامل

Experimental Investigation of Turbidity Flow in 90 Degree Bend with Mobile Bed

Turbidity currents in the ocean and lakes are driven by suspended sediment. The vertical profiles of velocity and excess density are shaped by interaction between the current and bed as well as between the current and the ambient water. This paper presents 48 series of experiments in which saline gravity currents flow through a laboratory sinuous flume. flume contains three successive bends wit...

متن کامل

منابع من

با ذخیره ی این منبع در منابع من، دسترسی به آن را برای استفاده های بعدی آسان تر کنید


عنوان ژورنال:
مهندسی عمران فردوسی

جلد ۲۷، شماره ۱، صفحات ۱۱۵-۰

کلمات کلیدی

میزبانی شده توسط پلتفرم ابری doprax.com

copyright © 2015-2023