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92 PRACTICAL METHODS FOR DETERMINING STORMWATER RUNOFF RATES AND QUANTITIES AT INDUSTRIAL SITES George D. Biemel, Director, Environmental Studies Section, Burgess & Niple, Limited Columbus, Ohio 43220 INTRODUCTION Determining stormwater runoff rates and quantities is a necessary step in several phases of industrial plant operations. First, flow rate estimates are needed for initial design of stormwater runoff collection and conveyance system. Secondly, runoff rates and quantities are required for design and installation of stormwater detention/retention facility design and stormwater runoff treatment plant design. Finally, runoff rates must be reported as a part of the stormwater permit application requirements as established by the United States Environmental Protection Agency (U.S. EPA). DEFINITION OF TERMS Drainage Area The drainage area or tributary area is the area, including ground surfaces, buildings, and paved areas, that contribute stormwater runoff to the point of interest. Drainage areas are developed by determining drainage boundaries from topographic maps, grading and site drainage plans, and field inspections. From this information, drainage boundaries are marked on the site map and the drainage area (in acres or square miles) is determined by planimetering around the drainage boundary on the map. Time of Concentration The time of concentration is the time in minutes or hours that is required for runoff to reach the point of interest from the most distant point in the drainage area. This represents the time at which the entire drainage area is contributing runoff to the point of interest. The time of concentration is composed of two parts: first, the travel time of overland flow and, second, the travel time as pipe or channel flow. Overland flow travel time is a function of the ground slope and the ground cover, such as forested, grassed, or paved land. Pipe and channel flow is related to the bed slope and the cover or material of construction. Cover and materials of construction affect the pipe or channel friction forces which may slow down the speed with which runoff leaves the drainage area. Flow Hydrograph A typical flow hydrograph is illustrated on Figure I, The hydrograph represents the flow rate, usually in cubic feet per second (cfs) or gallons per minute (gpm), as a function of time at the point of interest for a given storm event. Several pieces of information are shown on a hydrograph. First, the peak flow can be read directly from the hydrograph. The time to peak can be read, representing the time from the beginning of runoff to the time when the peak flow occurs. The area beneath the hydrograph represents the total runoff volume from the tributary area. This volume is the total storm rainfall less interception by plants, infiltration into the soil, evaporation, and storage in local ponds and depressions. The rainfall that caused the runoff may also be shown in the upper left hand corner on the plot. 46th Purdue Industrial Waste Conference Proceedings, 1992 Lewis Publishers, Inc., Chelsea, Michigan 48118. Printed in U.S.A. 893
Object Description
Purdue Identification Number | ETRIWC199192 |
Title | Practical methods for determining stormwater runoff rates and quantities at industrial sites |
Author | Biemel, George D. |
Date of Original | 1991 |
Conference Title | Proceedings of the 46th Industrial Waste Conference |
Conference Front Matter (copy and paste) | http://e-archives.lib.purdue.edu/u?/engext,42649 |
Extent of Original | p. 893-902 |
Collection Title | Engineering Technical Reports Collection, Purdue University |
Repository | Purdue University Libraries |
Rights Statement | Digital object copyright Purdue University. All rights reserved. |
Language | eng |
Type (DCMI) | text |
Format | JP2 |
Date Digitized | 2009-11-24 |
Capture Device | Fujitsu fi-5650C |
Capture Details | ScandAll 21 |
Resolution | 300 ppi |
Color Depth | 8 bit |
Description
Title | page 893 |
Collection Title | Engineering Technical Reports Collection, Purdue University |
Repository | Purdue University Libraries |
Rights Statement | Digital copyright Purdue University. All rights reserved. |
Language | eng |
Type (DCMI) | text |
Format | JP2 |
Capture Device | Fujitsu fi-5650C |
Capture Details | ScandAll 21 |
Transcript | 92 PRACTICAL METHODS FOR DETERMINING STORMWATER RUNOFF RATES AND QUANTITIES AT INDUSTRIAL SITES George D. Biemel, Director, Environmental Studies Section, Burgess & Niple, Limited Columbus, Ohio 43220 INTRODUCTION Determining stormwater runoff rates and quantities is a necessary step in several phases of industrial plant operations. First, flow rate estimates are needed for initial design of stormwater runoff collection and conveyance system. Secondly, runoff rates and quantities are required for design and installation of stormwater detention/retention facility design and stormwater runoff treatment plant design. Finally, runoff rates must be reported as a part of the stormwater permit application requirements as established by the United States Environmental Protection Agency (U.S. EPA). DEFINITION OF TERMS Drainage Area The drainage area or tributary area is the area, including ground surfaces, buildings, and paved areas, that contribute stormwater runoff to the point of interest. Drainage areas are developed by determining drainage boundaries from topographic maps, grading and site drainage plans, and field inspections. From this information, drainage boundaries are marked on the site map and the drainage area (in acres or square miles) is determined by planimetering around the drainage boundary on the map. Time of Concentration The time of concentration is the time in minutes or hours that is required for runoff to reach the point of interest from the most distant point in the drainage area. This represents the time at which the entire drainage area is contributing runoff to the point of interest. The time of concentration is composed of two parts: first, the travel time of overland flow and, second, the travel time as pipe or channel flow. Overland flow travel time is a function of the ground slope and the ground cover, such as forested, grassed, or paved land. Pipe and channel flow is related to the bed slope and the cover or material of construction. Cover and materials of construction affect the pipe or channel friction forces which may slow down the speed with which runoff leaves the drainage area. Flow Hydrograph A typical flow hydrograph is illustrated on Figure I, The hydrograph represents the flow rate, usually in cubic feet per second (cfs) or gallons per minute (gpm), as a function of time at the point of interest for a given storm event. Several pieces of information are shown on a hydrograph. First, the peak flow can be read directly from the hydrograph. The time to peak can be read, representing the time from the beginning of runoff to the time when the peak flow occurs. The area beneath the hydrograph represents the total runoff volume from the tributary area. This volume is the total storm rainfall less interception by plants, infiltration into the soil, evaporation, and storage in local ponds and depressions. The rainfall that caused the runoff may also be shown in the upper left hand corner on the plot. 46th Purdue Industrial Waste Conference Proceedings, 1992 Lewis Publishers, Inc., Chelsea, Michigan 48118. Printed in U.S.A. 893 |
Resolution | 300 ppi |
Color Depth | 8 bit |
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