PEMASUKAN UDARA ALAMIAH DAN BUATAN DI SALURAN CURAM (SELF AND ARTIFICIAL AIR ENTRAINMENT IN STEEP CHANNEL)

High flow velocity causes a low pressure even negative, especially in steep channel bed. Force caused by negative pressure will lift bed surface and side walls of the building hydraulic structures, which can lead to flaking on the bed surface and side walls of the building. In supercritical flow, ai...

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Bibliographic Details
Main Authors: , YERI SUTOPO, , Prof. Dr. Ir. H. Budi Santoso Wignyosukarto, Dipl. H.E.
Format: Thesis
Published: [Yogyakarta] : Universitas Gadjah Mada 2014
Subjects:
ETD
Description
Summary:High flow velocity causes a low pressure even negative, especially in steep channel bed. Force caused by negative pressure will lift bed surface and side walls of the building hydraulic structures, which can lead to flaking on the bed surface and side walls of the building. In supercritical flow, air from the atmosphere enter into the body even reach the bed flow. Air entrainment enter into the body and bed flow can prevent or reduce the phenomenon of cavitation in channels bed. This research focuses on five things, were: (1) concentration distribution of air bubbles in the developing regions of the self air entrainment, (2) location of the initial point of inception, (3) pressure in the bed flow, (4) configuration and dimensions of the aerator to reduce the phenomenon of cavitation, and (5) concentration distribution of air bubbles in the artificial air entrainment. Five research focus were achieved using experimental methods implemented in the Hydraulics Laboratory of the Department of Civil and Environmental Engineering (JTSL), Faculty of Engineering Gadjah Mada University (GMU). In this study, the steep channel having a length of 10 m, width 0.2 m, height 0.4 m with slope varies from 15º, 20º, and 25º, which was fused with the wall of the water tank. Discharge varied from 9.4 l/s, 11.5 l/s and 20.9 l/s. Initial location of air entrainment during the experiment compared with the initial determination of the location of air entrainment on calculations using the four equations, namely (1) Wood, Ackers, and Loveless (1983), (2) Feranndo and Rico (2002), (3) Hager and Blaser (1998), and (4) Bauer (1954). Concentration distribution of air bubbles in condition of self air entrainment experimental results compared with the results of calculations using the equations Chanson (1995) and Straub and Anderson (1958). Concentration distribution of air bubbles in condition of artificial air entrainment experimental results compared with the results of calculations using the equations Chanson (1995). Conclusion of this research were: (1) concentration distribution of air bubbles on the condition of self air entrainment in slope channel bed 25º and discharge=20.9 l/s can be predicted using the results of the calculation equation Straub and Anderson (1958) modification, (2) concentration distribution of air bubbles on the condition of self air entrainment in slope channel bed=25º can be predicted using the results of the calculation equation Chanson (1995) modification, (3) initial location of the air entrainment experimental results closest to the initial location of the air entrainment on calculations using the method of Hager and Blaser (1998) compared to three other methods, (4) concentration distribution of artificial air entrainment on the slope of the channel bed=25º at a point 7.2 m from the inlet flume and in the free surface aeration, was the Gaussian or normal, and (5) on the slope of the channel bed=25°, at a point 7.2 m from the inlet flume on the condition of artificial air entrainment in the down stream flow region after the first aerator installed a new aerator is not required anymore.