Vegetative Treatment Area Performance and Design Recommendations Joshua W. Faulkner Biological and Environmental Engineering Cornell University.

Slides:



Advertisements
Similar presentations
The Drainage Basin System
Advertisements

Estrogen reduction in a coupled wetland and ground water flow-through system Laura Hanna Eric Peterson Illinois State University.
Ecological Engineering - Maleny Effluent Irrigated Rainforest and Wetland Irrigation Australia Conference 2-6 June 2014.
Northern Ecohydrology Jessica M. Cable and W. Robert Bolton International Arctic Research Center (Fairbanks) Environment and Natural Resources Institute.
Relationship between size of vegetative buffers and transport of fecal coliform bacteria from pasturelands treated with dairy cow manure T. Sullivan,
Permeable Heavy Use Area for Livestock Farms Presentation for Kitsap County DCD, September 28 th, 2006, Lab Test Findings and Calculated Storm Water Performance.
Overland Flow n Once rainfall exceeds infiltration, water begins to flow. –Clay is hard to pick up due to cohesion. –Sand is hard to pick up due to size.
Oak Hill Case Soil Physical Problems. Poor Drainage Surface Drainage Reflects the ease with which water can move downslope. Reflects access to catch.
Bruno Basso Dept. Crop, Forest and Environmental Sciences University of Basilicata, Italy Contacts Joe T Ritchie: Bruno Basso :
Field Hydrologic Cycle Chapter 6. Radiant energy drives it and a lot of water is moved about annually.
Runoff Processes Slides from Venkatesh Merwade and Suzanne Anderson Reading: Applied Hydrology Sections 5.1 and 5.2.
Runoff Processes Reading: Applied Hydrology Sections 5.6 to 5.8 and Chapter 6 for Tuesday of next week.
Additional Questions, Resources, and Moving Forward Science questions raised in the development of a science assessment Effect of Conservation Tillage.
Lecture 22 Runoff (2) Event-based Hydrographs
The Hillslope-Stream Continuum Wed 4/22/2009. "The El Nino-Southern Oscillation and Global Precipitation Patterns: A View from Space" Dr. Scott Curtis.
Re-conceptualizing SWAT for Variable Source Area Hydrology
The Effect of Soil Hydraulic Properties and Deep Seepage Losses on Drainage Flow using DRAINMOD Debjani Deb 26 th April, 2004.
Unit: Soil Science Lesson 1
SWAT – Land Phase of the Hydrologic Cycle Kristina Schneider Kristi Shaw.
Kristie J. Franz Department of Geological & Atmospheric Sciences Iowa State University
Conservation Drainage: Drainage for the 21st Century
Building risk indicators of surface water contamination by pesticides at the small catchment scale. Taking into account spatial and temporal dimensions.
Modeling Variable Source Area Hydrology With WEPP
Run-Off Characteristics of Streams
Virtual Tour of a Vegetative Treatment System at the USDA Meat Animal Research Center Feedlot.
Digital Terrain Analysis and Simulation Modeling to Assess Spatial Variability of Soil Water Balance B. Basso J.T. Ritchie J.C. Gallant Dipartimento di.
Routing GenRiver 1.0 Distributed process-based model spatial scale: ha,temporal scale: daily Can be used as a tool to explore our understanding.
Rural, Community & Onsite Wastewater & Waste Management Role of Soil in Biological Treatment.
MODELING THE IMPACT OF IRRIGATION ON NUTRIENT EXPORT FROM AGRICULTURAL FIELDS IN THE SOUTHEASTERN UNITED STATES W. Lee Ellenburg Graduate Research Assistant.
Seifu A Tilahun School of Civil & Water Resources Engineering,BDU Storm Runoff and soil erosion processes on the Ethiopian highland.
Created by The North Carolina School of Science and Math.The North Carolina School of Science and Math Copyright North Carolina Department of Public.
Sources of streamflow from hillslopes Baseflow streamflow maintained by groundwater contributions Stormflow Augmented by direct precipitation on saturated.
Water Movement Below Surface
Created by: Mildred $100 Ground Water Climate Water Stuff Vocabulary Assorted Killer Questions $200 $300 $400 $500 $100 $200 $300 $400 $500 $100 $200.
1 Groundwater Pollution Week 1 – 0306 Introduction to Groundwater.
Ground Water. Makes up 0.397% of Earth’s Water. - song.
Drainage Management for Water Quality and Crop Production Benefits Don Pitts Agricultural Engineer NRCS USDA Champaign, IL.
DRAINMOD APPLICATION ABE 527 Computer Models in Environmental and Natural Resources.
Drainage Basin. Mississippi River Basin Drainage Basin.
Watershed Modeling Approaches Distributed: CASC-2D (CSU, U Conn, WMS) overland flow: 2-D diffusion wave with explicit FD channel flow: 1-D diffusion wave.
An Overview of the Safe Drinking Water Act. Objectives Explain threats to drinking water Describe the hydrologic cycle and pathways of contamination Understand.
Fire Effects on Water. The Watershed Concept What is a watershed? Area of land that drains into a common outlet Watershed condition- health or status.
Photo Placeholder Bloedel Donovan Park Stormwater Retrofit Alternatives and Analysis May 31 st 2013.
Fig. 16-CO, p Study Guide Chapter Explain how the groundwater system operates. 2.Describe the zones of aeration and saturation. 3.Locate the.
INVESTIGATING CONSERVATION AGRICULTURE SYSTEMS IN ZAMBIA AND ZIMBABWE TO MITIGATE FUTURE EFFECTS OF CLIMATE CHANGE By Christian Thierfelder and Patrick.
Kristina Schneider Kristi Shaw
Jefferson High School Compton Creek Research Project UCLA and Los Angeles Waterkeeper Funded by the Environmental Protection Agency.
EHST 3370 Wastewater Management Spring 2016 Unit 1:Introduction to On-site Wastewater Treatment and Disposal Systems.
Aquifer A body of rock or sediment that stores groundwater and allows the flow of groundwater.
6. Drainage basins and runoff mechanisms Drainage basins Drainage basins The vegetation factor The vegetation factor Sources of runoff Sources of runoff.
Hydrology for Nutrient Management Joshua W. Faulkner, PhD WVU-Extension Fundamentals of Nutrient Management Training Course December 16-17, 2009 *Portions.
RACC High School Training June 26, 2012 Jody Stryker University of Vermont Introduction to Watershed Hydrology.
Will Weiss Spring #7: Candler sand, 0-5% slope #8: Candler sand, 5-12% slope Mean rain fall: 48 in Mean temperature: 74 degrees F Elevation: 80ft.
Sanitary Engineering Lecture 4
Infiltration February __, Infiltration Most _____________ that reaches Earth’s surface ____________ the ground. Infiltration can occur if the ground.
Riparian Buffers for Water Resource Protection Michael R. Burchell II Associate Professor and Extension Specialist Department of Biological and Agricultural.
Hydrosphere Notes Parts 6 - Groundwater. Where is most of Earth’s useable freshwater found? ~97% is Groundwater.
R.A. Chavez | G.O. Brown LRGV Stormwater– South Padre Island May 18, 2016 The Impact of Variable Hydraulic Conductivity on Bioretention Cell Performance.
Establishing a Soil Chemical Baseline for the Catskills
General Road Construction Information
AIM AIM point-scale plot-scale hillslope-scale
Terrain Analysis for Water Quality Modeling
Civil & Chemical Engineering Department Graduation Project 2
Storm Water Storage and Treatment
Reading: Applied Hydrology Sections 5.1 and 5.2
Streamflow Processes Watershed – area of land draining into a stream at a given location Streamflow – gravity movement of water in channels Surface and.
The diagram shows a coastal region in which the land slopes toward the ocean. Point X is near the top of the hill, point Y is at the base of the hill,
Quiz 7 Answers 1. Soil A has a Ksat value of 8 cm/h, Soil B has a Ksat value of cm/h, and Soil C is shallow and rocky and has a Ksat value of.
Connections between groundwater flow and transpiration partitioning
Environmental Modelling with RASTER DEMs: Hydrologic Features
Presentation transcript:

Vegetative Treatment Area Performance and Design Recommendations Joshua W. Faulkner Biological and Environmental Engineering Cornell University

Vegetative Treatment Area (VTA) Function N Transformations, Sorption, Vegetative Uptake Surface Processes: Deposition, Infiltration, Volatilization NO -3 –N < 10 mg/L Zero Discharge

Shallow: 0.33 mg/L Deep: 0.06 mg/L

VTA with Restrictive Layer FRAGIPAN

WTD: 6 cm WTD: 26 cm

Surface of West VTA – lower water table Surface of East VTA – higher water table 7.5 hr11.5 hr19.5 hr9.5 hr13.5 hr17.5 hr 25.5 hr43 hr66 hr From: Faulkner, 2009

West VTA ShallowEast VTA Shallow 7.5 hr11.5 hr15.5 hr 19.5 hr23.5 hr41 hr 9.5 hr13.5 hr17.5 hr 21.5 hr25.5 hr43 hr From: Faulkner, 2009

Kim et al., 2006

Conclusions Elevated water table = increased concentrated flow paths = pollutant discharge A VTA design approach is needed in humid climates and soils containing a restrictive layer that accounts for likelihood of complete soil saturation

VTA Model FRAGIPAN ROOTZONE SUB-ROOTZONE Field 1 - Upslope Field 3 – Middle of VTA Field 2 – Wastewater Infiltration Field 4 – Downslope edge of VTA

Design Recommendations Based on Simulations Increased Ksat and slope increase subsurface lateral flow rates – effectively lowering water table Deeper soils – increases available storage Locate VTAs toward the top of a slope – two effects

Lastly…