Highway Drainage: Determining Flow Rates

Slides:



Advertisements
Similar presentations
Hydrology Rainfall Analysis (1)
Advertisements

Storm Water Runoff. Where Does Storm Water Go? Site Development Watershed Characteristics Storm Water Management The Rational Method Storm Characteristics.
Flood and Runoff estimation methods
1 Urban Drainage System Analysis & Design CEVE 512 Hydrologic Design Lab Spring 2011.
Using HEC-1 for Subdivision Runoff Detention Pond Design Stacie Kato April 26, 2004.
1 Determining Peak Flows. 2 Several Methods Statistical Analysis of Streamflow Records Transfer Methods (using gaged data to estimate an ungaged location)
Soil Conservation Service Runoff Equation
Rainfall-Runoff Modeling
Surface Water. WATER SEDIMENT The Lane Diagram I. Events During Precipitation A. Interception B. Stem Flow C. Depression Storage D. Hortonian Overland.
CE 515 Railroad Engineering
Watershed Management Runoff models
Hyetographs & Hydrographs
1 Time of Concentration. 2 Objectives Know how to calculate time of concentration Know how to calculate time of concentration Know why it’s important.
Ch  Know how to determine peak flow using the rational method 2.
The Objectives of storm water drainage To prevent erosion in hillside areas (paved roads and terracing are needed) To prevent land-slides To improve the.
Ch  Know what design frequency means  Know how to delineate a drainage area on a topographic map 2.
1 Highway Drainage: Determining Flow Rates Ch. 8.
Reading: Applied Hydrology, Sec 15-1 to 15-5
Wes Marshall, P.E. University of Connecticut May 2007 CE 276 Site Design Final Exam Outline.
ABE 527 Computer Models in Environmental and Natural Resources Engineering Presented by Ibrahim M M Aly Final Project.
Lecture ERS 482/682 (Fall 2002) Rainfall-runoff modeling ERS 482/682 Small Watershed Hydrology.
1 CTC 450 Review Distributing flow in a pipe network Hardy-Cross Method At any node: Flows in = flows out Head losses around a loop = 0.
Surface Drainage CE 453 Lecture 25.
CE 3372 – Lecture 10. Outline  Hydrology Review  Rational Method  Regression Equations  Hydrographs.
Estimating Qmax Using the Rational Method
TR-55 Urban Hydrology for Small Watersheds
Siti Kamariah Md Sa’at PPK Bioprocess..2010
HEC-HMS Runoff Computation.
Urban Storm Drain Design: Rainfall-Runoff relations.
Review of SWRCB Water Availability Analysis Emphasis on Dry Creek Water Availability Analysis.
STORMWATER MANAGEMENT
Description of WMS Watershed Modeling System. What Model Does Integrates GIS and hydrologic models Uses digital terrain data to define watershed and sub.
CE 3354 Engineering Hydrology
Basic Hydrology: Rainfall-Runoff – I
1 TR-55 Urban Hydrology for Small Watersheds. 2 Simplified methods for estimating runoff and peak discharge for small urban/urbanizing watersheds Ch 1.
Glenn E. Moglen Department of Civil & Environmental Engineering Virginia Tech Introduction to NRCS/SCS Methods (continued) CEE 5734 – Urban Hydrology and.
Sanitary Engineering Lecture 4
Detention Basics
HYDROLOGY Lecture 10 Unit Hydrograph
Modified Rational Method
HEC-HMS Simulation Adding a detention pond at the outlet
Hydrologic Analysis (Bedient chapter 2)
TR-55 Urban Hydrology for Small Watersheds
Basic Hydrology & Hydraulics: DES 601
Basic Hydrology: Rainfall-runoff based methods – II
Cristina Nelson, Term Project, CEE 6440, Fall 2007
CE 3372 Water Systems Design
Modified Rational Method
Rainfall-Runoff Modeling
Highway Drainage-Hydrology
CTC 450 Review Distributing flow in a pipe network Hardy-Cross Method
CEVE 412/512 Dr. Phil Bedient Jan 2016
Hydrology.
Storm Water Runoff Storm Water Runoff
Where Does Storm Water Go?
Time of Concentration.
Hydrograph Computation
Storm Water Runoff Storm Water Runoff
Determining Peak Flows
Hyetographs & Hydrographs
Find: Qp [cfs] tc Area C [acre] [min] Area Area B A
Floods and Flood Routing
Find: Qp [cfs] shed area tc C 1,050 1,200 1,300 1,450 A B C Q [acre]
Preciptation.
Love Field Modernization Program
WRE-1 BY MOHD ABDUL AQUIL CIVIL ENGINEERING.
Preciptation.
Preciptation.
HEC-HMS Runoff Computation Modeling Direct Runoff with HEC-HMS Empirical models Empirical models - traditional UH models - traditional UH models - a.
WinTR-20 Project Formulation Hydrology Using WinTR-20 for Small Watersheds What is Small ?? Some individuals are using WinTR-20 for subdivision planning.
Presentation transcript:

Highway Drainage: Determining Flow Rates HDM Ch. 8

Objectives Ability to determine the peak flow using the rational method

Design Flow Methods Rational method TR-55 Regression Equations Historical Data TR-20 HEC-RAS

Methods-Smaller drainage areas Rational Method Drainage areas<200 acres TR-55 (Technical Release-55) Drainage areas < 2,000 acres

Methods-Larger drainage areas TR-20 Large drainage areas broken into subareas HEC-RAS (Hydraulic Engineering Circular-River Analysis System)

Rational Method (metric) Q=kCIA Q – peak discharge (m3/sec) K- conversion factor= .00278 (cms-hr/ha-mm) C-runoff coefficient (unitless) I-rainfall intensity (mm/hr) A-drainage area (hectares--100 square meters)

Rational Method (english) Q=kCIA Q – peak discharge (cfs) K (conversion factor)=1 (cfs-hr / in-acre) C-runoff coefficient (unitless) I-rainfall intensity (in/hr) A-drainage area (acres)

Rational Method Rational Coefficient-C (Tables) Rainfall intensity-I Time of concentration (need for I) Drainage area-A (previous lecture)

Basic Steps to Estimate Peak Flow Rational Method Determine Drainage Area (previous lecture) Choose a value of C Estimate time of concentration Overland (sheet) flow Shallow concentrated flow Open channel flow Select a frequency (return period) Determine the average storm intensity from IDF Curve Use rational method equation to estimate peak flow

Rational Coefficient C

Example of Runoff Coefficient Table

Weighted Rational Coefficient Must be weighted if you have different area types within the drainage area Drainage area = 8 acres: 2 acres; C=0.35 (residential suburban) 6 acres; C=0.2 (undeveloped-unimproved) Weighted C=[(2)(.35)+(6)(.2)]/8 = 0.24

Intensity I (“/hr)

To determine intensity: Find the time of concentration Set the storm duration equal to the time of concentration Determine frequency Use an IDF curve to determine the intensity

Time of Concentration Time required for water to flow from the most distant part of a drainage area to the drainage structure

Water can move through a watershed as: Sheet flow (max of 300’; usually 100’) Shallow concentrated flow Open channel flow Gutter Ditch Swale Creek Some combination of above

Design Frequencies Not economically feasible to design for all floods for every structure for any type of road

Design Storm Frequencies Highway class Culverts Storm Drainage Ditches Interstates 50 (check 100) 10 (check 50 if sag) 25 Princ. Arterials (Check 100) Minor arterials & other 5 (check 25 if sag)

IDF Curve Rainfall Intensity Storm Duration, Rainfall Frequency

http://www.mathworks.com/matlabcentral/fileexchange/9740-intensity-duration-frequency-curves

http://www. pub. gov. sg/general/code/Pages/SurfaceDrainagePart2-7 http://www.pub.gov.sg/general/code/Pages/SurfaceDrainagePart2-7.aspx

IDF Curve: Oneida County, NY

Example: Determine the peak flow for a 100-acre watershed in central NY (mostly forested). Assume the intensity is 3” per hour. What is the peak flow if the watershed is developed into light industrial usage? Assume the intensity is 3” per hour.

Example-undeveloped: C=0.13 (reference table) I=3” per hour (given) A=100 acres Q=CIA = 39 cfs

Example-developed: C=0.65 (0.5+0.8)/2 I=3” per hour (given) A=100 acres Q=CIA = 195 cfs In reality, the peak could be higher, since the time of concentration would likely decrease (which would increase the intensity)

Gaged Stations – New York http://waterdata.usgs.gov/ny/nwis/rt

Detention Structures Stores runoff temporarily and then releases it in a controlled manner to limit the peak flow leaving a site Mitigates destructive effects of increased runoff May improve water quality May increase recharge http://www.tleng.net/Dentention_Pond.html#anchor_70

Detention Structures Basically a tank or pond Complex because water coming in (inflow hydrograph) is not constant Water going out is not constant (single or multistaged outlet structure where Qout varies based on water elevation in the structure) Water elevation in the structure is not constant

Quiz What is the difference between a hydrograph and a peak flow? What is the Rational Method equation? Q=? What are the units of the rational coefficient? What are the units of intensity? What are the units of area? What words to the letters IDF stand for? What is the “time of concentration”? What does frequency refer to? How do you determine the storm duration? What is the function of a detention structure?