© Office of Water Programs — 2010 The Office of Water Programs Christian Carleton, P.H., CPSWQ, CPESC Brian Currier, P.E. David Alderete LID Implementation.

Slides:



Advertisements
Similar presentations
Peatscapes: Monitoring of Hydrology and Water Quality at Geltsdale and Priorsdale Report of Phase 1: Nov 2007 – Mar 2009 Dr Jennine Jonczyk, Dr Mark Wilkinson,
Advertisements

Transport of nitrogen and phosphorus from Rhode River watersheds during storm events David Correll, Thomas Jordan, and Donald Weller Water Resources Research,
Permeable Heavy Use Area for Livestock Farms Presentation for Kitsap County DCD, September 28 th, 2006, Lab Test Findings and Calculated Storm Water Performance.
Cascade Charter Township
LID Site Design and Drainage Dan Cloak Environmental Consulting May 23, 2011.
UW LID Workshop Bioretention Flow Control Modeling May 2008
INLAND EMPIRE ASCE & APWA LOW IMPACT DEVELOPMENT (LID) SEMINAR INLAND EMPIRE ASCE & APWA LOW IMPACT DEVELOPMENT (LID) SEMINAR LID FACILITY DESIGN Prepared.
Field Hydrologic Cycle Chapter 6. Radiant energy drives it and a lot of water is moved about annually.
Soil Conservation Service Runoff Equation
Monitoring and Analytical Issues For BMP Performance Evaluation Hong Lin, Ph.D. Gary Lippner, P.E. CDS Technologies May 9, 2006 NWQMC San Jose, CA.
CLIMATE ADAPTATION, INNOVATIVE SUDS AND PROTECTION OF HARRESTRUP Å By Sille Lyster Larsen, Grontmij & Vinni Rønde, MSc Hydrology, Wageningen UR Retrofitting.
Hydrologic Abstractions
Infiltration Infiltration is the process by which water penetrates from ground surface into the soil. Infiltration rate is governed by: rainfall rate hydraulic.
Hydrologic Cycle and Watersheds. Hydrologic Cycle Components Precipitation Infiltration Percolation Runoff Evapotranspiration.
School of Civil and Environmental Engineering Life Impact The University of Adelaide Water Balance and the Influence of Soil Structural Changes on Final.
Chapter 3 -Hydrology Hwk#3 - pp ,4,7,11 Hydrologic Cycle Runoff - Ground Surface Water Infiltration - Ground Penetration (percolation) Transpiration.
Quantitative Assessment – SMEX 02/03/04 Digital Elevation Model (DEM) of Iowa Drainage Network across catchments Aircraft based soil moisture (PSR C-Band)
UVM-AWRA CHARRETTE: designing an alternative stormwater treatment technique W h a t I s a C h a r r e t t e? A Charrette is a cross-disciplinary workshop.
Low Impact Development Training Module 4: Bioretention Design Exercise Neil Weinstein.
For Stormwater Treatment and Flow Control Dan Cloak Environmental Consulting December 14, 2010 Contra Costa Clean Water Program.
B.S. Engineering Science, Humboldt State University, Arcata, CA MSCE, San Jose State University, San Jose, CA Ph.D., Environmental Engineering,
Sustainable Development: Practical Solutions to Real World Problems Fishkill, NY November 7, 2012 Low Impact Development and Rainwater Harvesting Solutions.
Role Of Catchment Drain For Earth Slope Stability
Modeling Green Infrastructure Components in a Combined Sewer Area Robert Pitt, Ph.D., P.E., D.WRE, BCEE Department of Civil, Construction, and Environmental.
FNR 402 – Forest Watershed Management
Infiltration Rainwater that soaks into the ground and may reach the groundwater table.
COUNTRY PAPER ON REUSE OF LOW QUALITY WATER IN EGYPT.
How do Wetlands Factor into New Infiltration Policies?
Bill Eyring – CNT Senior Engineer Illinois Sustainable Technology Center September 29, 2010 Monitoring and Documenting Green Stormwater Best Management.
Upper Brushy Creek Water Control & Improvement District
RAIN GARDEN DESIGN CONTEST 2013 MARCH 11 TH – 27 TH.
Rush River Assessment Project Hydrologic Flow Study Sibley County SWCD Presentation to the Minnesota River Research Forum March 10, 2005.
Project Our group collaborated with students at the University of Zacatecas (UAZ) to accomplish the following: 1- Create an accurate hydrologic model which.
Urban Storm Drain Design: Rainfall-Runoff relations.
Discussion of Proposed MS4 Permit Design Standards Language.
Presented by George Doubleday 1. What is The Woodlands Purpose of this Research Build and Calibrate Vflo TM model for The Woodlands Compare storms with.
Basic Hydrology Water Quality: Sediment production and transport.
Seifu A Tilahun School of Civil & Water Resources Engineering,BDU Storm Runoff and soil erosion processes on the Ethiopian highland.
Why are we here today? To discuss the challenges we face in meeting NPDES Phase II minimum requirements for stormwater control. The NPDES program requires.
Underground Systems: Hydraulic Design
Stormwater Water Quality Treatment Options Alvin Shoblom, P.E. Hydraulics Engineer.
Term Project Presentation CE 394K.2 Hydrology Presented by Chelsea Cohen Thursday, April 24, 2008.
Why Single-Event Modeling Doesn’t Work for LIDs presented at Stormcon 2009 Anaheim, CA August 2009 Doug Beyerlein, P.E. Clear Creek Solutions, Inc.
Group IV Project – The Rain Garden 2009 – 2010 School Year by Merritt Perry, Ted Parker, Jordan Gwyn, Marc Fleischhauer.
Central Valley Flood Protection Board Update Presented by: Michael Mierzwa, P.E. Lead Flood Management Planner California.
State Board Modeling Needs and Interests Eric Berntsen, PH, CPESC, CPSWQ State Water Resources Control Board CWEMF Hydrology and Watershed Modeling Workshop.
Hydrological Study of a stream catchment in Palau Pacific HYCOS - SOPAC 39 th STAR Session - Nadi 18 th October 2010.
Photo Placeholder Bloedel Donovan Park Stormwater Retrofit Alternatives and Analysis May 31 st 2013.
STORM WATER STORAGE AND TREATMENT
Surface Water Surface runoff - Precipitation or snowmelt which moves across the land surface ultimately channelizing into streams or rivers or discharging.
Andrea Ryan April 22,2010. Increased imperviousness on the Texas A&M West Campus is damaging the watershed.
Clear Creek Solutions, Inc. LID Hydrology and Hydraulics Doug Beyerlein, P.E. Clear Creek Solutions, Inc.
ASCE LID Conference LID Analysis Considerations in Western Washington November 17, 2008 Doug Beyerlein, P.E. Clear Creek Solutions, Inc.
Surface Water Applied Hydrology. Surface Water Source of Streamflow Streamflow Characteristics Travel Time and Stream Networks.
HOW MUCH WATER ENTERS THE SOIL? Infiltration. PrecipitationEvaporation Runoff Infiltration.
Irrigation Management Practices Cropping A*Syst Katie L. Droscha 01/14/ /15/2013.
MIDS Calculator Fundamentals
Cudworth Professor of Urban Water Systems
Hydrologic Analysis (Bedient chapter 2)
RUNOFF.
Continuous Surrogate Monitoring for Pollutant Load Estimation in Urban Water Systems Anthony A. Melcher, USU Civil and Environmental.
Basic Hydrology & Hydraulics: DES 601
Case Study: Evaluating Retrofit Urban Best Management Practice Performance and Lessons Learned Nick Muenks, Marc Leisenring, Mark Willobee – Geosyntec.
Infiltration and unsaturated flow (Mays p )
John Murnane, Mark Healy, Owen Fenton
Green and Ampt Infiltration
Northern California LID Hydrology and Hydraulics
Preciptation.
Love Field Modernization Program
Preciptation.
Presentation transcript:

© Office of Water Programs — 2010 The Office of Water Programs Christian Carleton, P.H., CPSWQ, CPESC Brian Currier, P.E. David Alderete LID Implementation Challenges: Monitoring and Measuring Results Select OWP Experiences

© Field monitoring guidance Results of testing at Sacramento State

Field Monitoring Guidance Flow Monitoring Issues –Accurate rain gauges and drainage areas –Influent flume sizing We know large storms bypass, so why size flumes to monitor what we already know? Size flumes up to the design storm for water quality purposes 0.16 in/hr is a common water quality design intensity, so 0.5 in/hr may be reasonable for a good range of storms. –Effluent flume sizing Smaller flumes should be used for flows from filter media or orifice- controlled outlets

Do not ignore small events –Monitor flow on the small events and consider a few water quality events as bonus data –There is far more uncertainty in the hydraulic performance than there is in the quality of filtered water, so focus on the flow! Small storms are avoided to minimize ‘false-starts’ for water quality samples due to insufficient volume to collect a minimum number of aliquots. Field Monitoring Guidance

80/20 Sand/Compost Initial hydraulic capacity can be very high and depends on drying Maximum was nearly 500 in/hr Mostly-saturated hydraulic capacity ranged from 40 to 60 in/hr, though as low as 17 in/hr was observed. Results of Testing at Sacramento State

Dry-weather flow negatively impact LID systems –Soil doesn’t have a chance to dry out –How does it happen: Raised-landscaping runoff Irrigation overspray Vehicle/street/sidewalk/driveway washing Results of Testing at Sacramento State

Treatment is governed by hydraulics Instantaneous and short-term treatment tests are very misleading Filtered vs. bypass depends on: –Media type, depth, area, and ponding depth –Local hydrology –Catchment size and shape Results of Testing at Sacramento State