asfpm conference, june 11 2013 (b7_jesic)

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    Redwood Basin

    Stormwater Master

    Plan Development

    Employing anIntegrated 1D/2D

    xpswmm Model

    Cedomir Jesic, P.E.

    Water Resource Practice Leader

    ASFPM Conference, June 11 2013

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    Using xpswmm for Master Plan Development

    26/07/2013

    Redwood Basin

    Josephine County, Oregon

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    26/07/2013

    Why was this project completed

    Overview of Project

    1D model development with results and findings

    Basics of 2D modeling

    Elements of this 2D model explained

    2D model results Open Channel

    2D model results Closed System

    Presentation Overview

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    Study performed for Josephine County, Oregon, other stakeholders:

    Grants Pass Irrigation District and City of Grants Pass

    No Intergovernmental Agreements for stormwater managment

    Management and capital improvement projects are completed

    independently The purpose of the master plan was to study the entire catchment to

    establish problem areas, the source of the problems and detail CIP

    projects to alleviate the problem areas.

    Flooding (Roadways)

    Water Quality

    Habitat

    Flooding became the driving factor due to significant capacity

    problems throughout the catchment.

    Master Plan Description

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    Located in south west Oregon

    Wet winters and dry summers

    Redwood Basin is 6,400 acres

    Land use

    Forest

    Agriculture

    Low & medium density residential

    Commercial

    Transportation

    Soils: Clays

    Sand

    Redwood Catchment Study - Area Location

    Study Area

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    Aerial photo shows land use,

    irrigation canals, and creeks

    Canals significantly altered

    drainage characteristics

    NE corner developed, City Of

    Grants Pass

    NW corner agriculture South

    predominantly forest

    Canals

    Sand Creek

    Sparrow Hawk

    Creek

    Jack Creek

    Redwood Catchment Study Area

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    A complete 1D xpswmm model was built initially

    The hydrology was included in the 1D model and all major hydraulic

    elements were included as well. The 1D model was robust.

    At the time a 2D model was not scoped with the client.

    Hydrology was completed utilizing the Runoff and Green Amptmethods

    177 sub-catchments classified with soil type and all Green Ampt

    parameters were input to xpswmm

    Calibration was done with stream gage data collected over the

    2010 winter and rain events occurring in 2010 Historic and Design Storms

    Redwood Catchment Study 1D Model

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    Redwood Catchment Study 1D Model

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    Irrigation canals, Creeks, Open

    channels, pipe 12 inches or

    larger, roadside ditches and

    culverts

    As development increases the

    level of detail of the 1D model

    increases as well

    Redwood Catchment Study 1D Model

    CanalsCanals

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    55 nodes flood 25 year 24 hour design storm

    Volume and location identified with graphical

    encoding tool:

    Flooding occurs only the volume is known

    Spatial extent is unknown Depth is unknown

    Overland velocity is unknown

    Flooded volume is lost

    Where does the flooding go?

    Unable to accurately describe surface floodingwith a 1D tool:

    2D modeling needed

    Redwood Catchment Study 1D Model

    Spill connecting canal with

    Sand Creek

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    A representation of the project areas topography and surface

    characteristics (roughness).

    The project area is split into a grid where each square has an

    associated elevation and roughness for cell center and cell sides.

    Water can move from one grid to another in any direction.

    2D Modeling Summarized

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    Advantages

    More accurate modeling of overland flood flow

    Flood storage, flood fringe & floodway accurately depicted

    Suitable for bridges/structures hydraulic analysis

    Provides spatial extent of flooding, velocity and depth for all

    areas, a nice picture

    Disadvantages

    Large amount of data is required (typically LiDAR)

    More computational power and time required

    High storage requirement as the output files can be large

    Tough to model very large areas with small grid size

    2D Model Advantages/Disadvantages

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    Geo-referenced Aerial

    1D/2D Model Input

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    Surface built from LiDAR

    1D/2D Model Input

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    Grid Extents for the entire model, Boundary conditions, Grid extent optimization,

    and Inactive areas

    1D/2D Model Input

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    Green = Impervious

    Black = Buildings

    Blue = Water

    Red = Open Space

    White = Grass/Pasture

    1D/2D Model Input

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    1D Node (1D water

    level computed)

    1D Link

    Inactive 2D Area

    Polygon

    Active 2D Area

    1D/2D Interface Line

    1D/2D Connection Line

    2D Water level interpolated

    using water levels at 1D nodes

    Inactive cells

    1D/2D Model Input

    Inactive area, Interface and Connection lines

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    1D/2D Interface lines (light blue), 1D/2D Connection lines (purple),

    Inactive area (dark blue hatch)

    The 2D active grid has 998,000 cells, each 100 ft2

    We will examine at the area highlighted with the red circle

    1D/2D Model Schematization

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    Comparison 1D and 1D/2D Results Open Channel

    Flooding of storm and combined sewers

    Flooding due to lack of network capacity or system defects

    1D closed system and 2D overland flow system

    Better description of dual drainage (i.e. intersections, trap lows, flow outside of

    right of way)

    Transfer of flow to and from 1D can include inlet capacity

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    Flooding is captured and properly

    rerouted, flooding is accurately

    described and volume is

    accounted for

    Comparison 1D and 1D/2D Results Open Channel

    Over 50 million ft3 , no accounting for

    flooded volume

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    Movement from 1D to 2D to 1D etc.

    1D and 1D/2D Results Open Channel

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    Flooding exits the closed system

    and is conveyed down the street

    Comparison 1D and 1D/2D Results Closed System

    Flooding volume is lost, model is

    incomplete

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    1D/2D model has a water

    surface level of 888.92 feet for

    last link of Sand Creek.

    This is 1.14 feet higher than the

    1D model

    Comparison 1D and 1D/2D Results Sand

    Creek

    1D model has a water surface level

    of 887.78 feet for last link of Sand

    Creek

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    The cascade effect in one case starts in the South Highline Canal

    and travel in and out of 6 1D elements utilizing the 2D grid in between

    each 1D element

    This could not be modeled in 1D!!!

    The 1D model had 34% volume lost to flooding, while the Integrated

    1D/2D model simulated all this flow to the Rogue River

    Establishment of problem areas, sources and development of Capital

    Improvement Project list for Client was completed with confidence.

    Was able to present a picture to stakeholders.

    Discussion

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    Questions