FLOW OVER A SHARP CRESTED WEIR. Chittagong University of Engineering and Technology Dept. of Civil Engineering GROUP-B1(4 ) ID:

Slides:



Advertisements
Similar presentations
Introduction to Long-Throated Flumes and Broad-Crested Weirs
Advertisements

Plotting scales This concludes the discussion of this agenda topic. Please return to the Agenda and choose the next topic for study.
Weirs and Canal Intakes By: Nell Kolden and Taylor Barnett Thursday April 12, 2012 CIVE 717.
Erik Strandskov and Joshua C. Galster Dept. of Earth & Environmental Studies, Montclair.
Streamflow and Runoff The character, amount, and timing of discharge from a basin tells a lot about flow paths within the basin Therefore, important to.
53:071 Principles of Hydraulics Laboratory Experiment #2 Local Losses in Pipe Flows Li-Chuan Chen, Marian Muste, and Larry Weber.
Experiment (6) Flow over weirs
All critical-flow devices determine flow rate by measuring one or more water levels and computing flow from a calibration equation. Water Level Sensors.
Notes on river discharge measurements
Control Structures.
Long Term Storage Long term storage means to store water during high inflows years for the benefit of low inflows years. Long term storage means to store.
Hydraulic Jump.
Monroe L. Weber-Shirk S chool of Civil and Environmental Engineering Prelim 1 Review.
The Centrifugal Pump.
Hydrology and Water Resources RG744 Institute of Space Technology December 11, 2013.
MEASURING FLUMES By CH. VENKATARAMAIAH.
Procedure Writing Basics Mr. Richard Crisler Spring-2006.
Overview of Open Channel Flow Definition: Any flow with a free surface at atmospheric pressure Driven entirely by gravity Cross-section can vary with location.
INTRODUCTION TO ENGINEERING TECHNOLOGY SEVENTH EDITION ROBERT J. POND & JEFFERY L. RANKINEN Chapter 7 The Technical Laboratory.
Microhydro Flow, nozzles. Site Assessment: Flow 5-gallon bucket –Small stream, small waterfall Float –Larger, flat, uniform stream V-notch Weir Rectangular.
1 Experiment No.1 & 2 Orifice and free jet flow Hydraulics CE-331 Lab.
CE 210Dr SaMeH1 Soil Mechanics & Foundation 1 (CE 210) [8] Associate Professor of Environmental Eng. Civil Engineering Department Engineering College Majma’ah.
Lab Write-ups. Grading Lab reports are graded with a maximum of 30 points. The report is broken down into 6 sections Each section is worth a different.
Basic Hydraulics: Rating curve. Definition & terminology Rating curve, also known as stage–discharge curve, is a graph showing the relation between the.
Hydrology and Water Resources RG744 Institute of Space Technology November 13, 2015.
Energy Equation The expanded Bernoulli's equation
Wave Research Experiential Science 11 Ben Snow, Stephen Horton, Bob Sharp.
Compressible Flow in Nozzles Thermal Engineering Lab ME-4111 Professor: Eduardo Cabrera Damian Luna Yetziel Sandoval – Alberto Gonzales –
Prepared By:- Divyesh Shingala ( )
Lesson 2 – page 1.  To learn what is a flood hydrograph  To learn how to read a flood hydrograph  To learn what is:  Lag time  Peak discharge  Rising.
Compressive Flow in Nozzles
PUMPS Thermal Systems Laboratory Samuel A. Santiago Pérez Modesto González David Alvarado.
General Information Worksheet and Spreadsheets due Thursday PM Lab Reports due Tuesday by 4.00 pm Lab 2 - Flow Calculations Objectives To measure.
FUNDAMENTALS OF CONTROLLING DHANYA ASOKAN M120005MS.
Pump Characteristic Curves & Selection of centrifugal pumps
PREPARE BY : ENROLLMENT NO.
Components Pumps.
Stormwater Conveyance Design 2
EXPT. 2 STUDY OF DIFFERENT TYPES OF ERRORS IN ANY ONE MEASUREMENT SYSTEM. ERRORS HUMAN ERROR OR GROSS ERRORS SYSTEMATIC ERROR RANDOM ERROR INSTRUMENTAL.
FLUID MECHANICS.
Storm Hydrographs Storm hydrographs are used to measure a river’s flow and show the change in river discharge over a short period of time after a storm.
RUNOFF.
DISCHARGE OVER A BROAD-CRESTED WEIR
Water and the Atmosphere - Chapter 1 Lesson 3
Basic Hydrology & Hydraulics: DES 601
Maniks High Quality Regulating Valve
EXPERIMENTAL DESIGN Science answers questions with experiments.
Presented by Arne van der Hout Tom O’Mahoney Tommaso Boschetti
Pipe Components, Piping System.
Frese DPRV Introduction Introduction 2017.
IE-432 Design Of Industrial Experiments
Open Channel Storm water Irrigation Waste water collection and treatment.
Lab Write-ups.
Lab Write-ups.
Your gon’na need to know it eventually.
Cavitation Demonstration Unit (Font: Arial Font Size: 32 )
Li-Chuan Chen, Marian Muste, and Larry Weber
Graphing with Uncertainties
The shapes of stream channels
Groundwater hydraulics – lecture 8
Marine Biotechnology Lab
Flood Routing.
Hydraulic Structures HYDRAULIC STRUCTURES.
Preciptation.
Module 3 Irrigation Engineering Principles Version 2 CE IIT, Kharagpur.
Chapter Four RUNOFF When a storm occurs, a portion of rainfall infiltrates into the ground and some portion may evaporate. The rest flows as a thin sheet.
Hydraulic Pump Power Power = rate of conversion of energy.
Multiple Regression Berlin Chen
Lab Write-ups.
Hydraulic Flow Control • Metering Fluid Flow
Presentation transcript:

FLOW OVER A SHARP CRESTED WEIR

Chittagong University of Engineering and Technology Dept. of Civil Engineering GROUP-B1(4 ) ID:

TABLE OF CONTENTS 1.Introduction2.Theory3.Procedure4.Calculation5.Result6.Discussion7.Application

Introduction  A weir with a sharp upstream corner or edge such that the water springs clear of the crest is a sharp-crested weir. It is commonly used in large scale situations. For small scale applications, weirs are often referred to as notches and invariably are sharp edged.

THEORY

PROCEDURE At first, the pump was started & to get the uniform flow 4-5 minutes were needed. Then the bench was adjusted regulating the valve to give the first required head level of approximately 10mm. The pressure head was observed after that. Depth of water level was fixed. Time was counted through a stop watch till water reaches the required level. Collected data was used to plot graphs.

CALCULATION

RESULT  The co-efficient of discharge from graph, C d = 0.62  The co-efficient of discharge from calculation, C d = 0.61  The exponent of H = 1.45

DISCUSSION  The experiment has been done very carefully. We have found the Cd 0.62 and the exponent of H 1.45 where the standard value of these are 0.65 and 1.50 respectively. Though maximum precautions were maintained, some errors have been occurred. The meniscus reading was not found accurately as it was not hold in a stable position. There was some shakings and vibrations which might have affected the value. The apparatus is old, so there may have some mechanical errors and the fluid flow was not fully uniform. Also there was some inaccuracy in recording time in the stopwatch (human error) and plotting the points in the log paper was also not hundred percent accurate. All these factors together contributed to the error for which the ideal value could not be found rather a value quite near to the ideal value was calculated.

APPLICATION The data gained from flow rate calculations over a rectangular sharp-crested weir can be used in a number of ways:  Flood control and general water management policies are often designed on the basis of such data.  The data can be used to determine if a hydroelectric project would be possible or profitable.  It can also be useful for environmental impact studies, specifically in determining how the weir would affect the ecosystem of a stream or river.  Irrigation is also benefited from this kind of data.

THANK YOU