Observations Regarding Impacts of Tile Drainage in Southern Manitoba - An Engineer's Perspective
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Observations Regarding Impacts of Tile Drainage in Southern Manitoba - An Engineer's Perspective
Observations on Tile Drainage in Southern Manitoba B r u c e S h e w f e l t , M s c . , P. E n g . PBS Water Engineering Ltd. Outline ….. • Brief history of tile in Manitoba and current situation • Design principles • Value added tools for Professionals • Sustainability elements (e.g. BMPs) • Brief case histories in application of tools 2 What is tile drainage? • corrugated HDPE perforated pipe w/wo a filter sock (silt) • installed at 2 to 4 foot depth (typical) • lowers water table 3 Factors that Impact Soil Moisture, GWT and Tile Flow Courtesy of Stantec 4 Self Propelled vs. Pull Type Situation Analysis -Southern Manitoba • Expanding tile drainage activity in Manitoba – 6 commercial tile machines 2013 + self installation – tile plants – 4 in MB and ND – 10,000 – 15,000 + acres per year ? • North Dakota and Minnesota activity – similar rate of growth; • Research – Mainly BMPs oriented – NDSU, SDSU, ISU, U of Minnesota, U of Manitoba • BMP Adoption --- Mainly USA ! – NRCS – USDA funding BMPs – ADMC (Ag Drainage Management Coalition) • Controlled Drainage and Subirrigation • Saturated Buffers • Bioreactors Brief Retrospective 1960s ---- Morden Research Station 1970’s 80’s --- Almassippi Wet Sands Studies 1990’s --- Manitoba Corn Growers Association 2000’s --- Research and Demonstration (BMPs) Morden Research Station - Then and Now 1965 Detailed Soil Survey – Michalyna Water table < 4 feet in spring Saline sub-soils noted Clay Tile installed 1966 Deep (4-5’) and Wide Space 2013 Soils Report - Stantec (1:5000) New Technology (Veris) Saline sub-soils mapped HDPE Tile installed 2013 Shallow (2.5 -3’) and Narrow Space Salinity Reclaim Possible ? Stantec Soil Survey 1:5000 Relationship of Drainage to Soils and Deep Veris Wet Sands Research –ID Engineering (1983) Report • Drainage research targets 300,000 ha • Landscape impacts (i.e. depth to GWT) • Crop water use from shallow groundwater “very important” • Shallow tile 76 cm recommended Project 408: Almassippi Wet Sands Management Project Impact of Drainage Depth and Upflow On Water Table and Water Use Evapotranspiration from shallow ground water by cotton as affected by soil and water table depth (after Grismer and Gates, 1988) North Dakota Research on Shallow Water Table Follett et al. , 1974 – Effect Water Table Depth on Crop Yields 12 Manitoba Corn Growers Association Pilot Project – 1994 to 1997 4 sites (clay loam to sand) evaluated • drainage effectiveness • environmental impact Professional Input geologist pedologist agronomist hydrologist ag engineer tile company (Ontario) geotechnical engineer (filter) SITE A – Random 27 Acres Impacted Loamy Sand over Clay Spacing Random (low areas) Spring vs. Summer ! - 1995 115 acre –inches ¼ “ Drainage Coefficient 15 Producer Results 1990s – Anecdotal Largest Tiled Farm Reported Benefits • BENEFITS SEEN ! – Earlier start – Reduced drown out – Access for spraying and cultivation – Compaction reduced – HOPE for salinity reduction – PROBABLY better fertilizer utilization and timing – Decreased surface runoff Yield gains (verbally reported): • 20% corn • 10-50% potato ! • 20 % wheat NOW growing beans/ potatoes on fields not grown before because of risk of drown out EM 38 Horizontal …. 16 years after tile drainage reduction salinity 17 2009 – 2012 Manitoba Research and Demonstration Hespler Farms and CMCDC Winkler • • • • • Tile Drainage and Irrigation of Potatoes and Corn Published – U of Manitoba Water Balance, Demand and Yield Response DRAINMOD Modelling of Fine Sandy Loam Ongoing Work AT CMCDC (Dr. Ranjan) Kelburn Farms - Heavy Clay • • • • Clay (40-60%) Soils Flow/Soil Moisture Two drain spacings No published data Kroeker Farms – Water Footprint Monitoring • No published data Total Precipitation = 332 mm Total Flow = 71 mm Flow-FDIR-B3-2011 FDIR-B3 Precipitation Irrigation 0 14 Drainage Flow (mm) 12 20 10 30 8 40 ¼ Inch Per Day DC 6 50 4 60 2 70 0 80 6-May-11 5-Jun-11 5-Jul-11 4-Aug-11 3-Sep-11 3-Oct-11 Recharge (mm) 10 2-Nov-11 19 Variation in ETc and Water Table – CMCDC 2012 Monitoring Tools --- Field 747 --- FarmsWater Table and Soil Moisture Monitoring 21 Water Footprint - 2012 22 Drainage (and Irrigation) BMPs – Professional Input Water Recycling Controlled Drainage and Subirrigation Nutrient Management Cover Crops Tillage VRI Irrigation Water Recycling … 200? How to Do it: Control “Zones” – Control Water Table ! Target: 20 acres/structure Water Control Structure 25 Impact of BMP – Nutrient Management Reduced GWT Nitrate = Reduced Tile Nitrate ? CMCDC Groundwater Nitrate-N (ppm) Nitrate N ppm 120.0 100.0 80.0 Fall 2011 60.0 Fall 2012 40.0 June 2013 Fall 2013 20.0 0.0 A1-1 A1-2 A1-3 A1-4 A1-5 A1-6 West SB BIOREACTOR BMP – Nitrate N Reduction in Water • Wood chip bioreactors • Proven Nitrate – N reduction • Potential P reduction being examined • None in Manitoba • Iowa and Illinois are leaders • Concern is impact on drinking water and Gulf of Mexico 27 Design Principles Spacing and Depth vs. Tile Response • • • • • • Hooghoudt Equation - 1963 (steady state) Kirkham Equation - 1957 (preferential flow) Control water table depth (H) Influenced by depth to restrictive layer (D) Spacing of tiles is computed (S) Drainage Coefficient (DC) 28 Design Principles Critical Input to Equations • • • • • • Soil layers, texture and structure Water retention Hydraulic conductivity Depth to impermeable layer (and GWT) Surface storage Downslope and lateral water movement – need additional math Soil Texture Sat Hyd Conductivity (ft./day) Sand 18.9 Loamy sand 4.72 Sandy loam 1.73 (52 cm) Loam 1.02 (31 cm) Silt loam 0.54 Sandy clay loam 0.24 Clay loam 0.16 Silty clay loam 0.16 Sandy clay 0.09 (2.7 cm) Silty clay 0.08 Clay 0.05 Average Saturated Hydraulic Conductivity Values Source: Rawls et al. (1993)[2] Site Variability --- Precision Drainage and Irrigation Site Variability --- Site Investigation and Modelling Photo courtesy of Precision Land Solutions 30 Texture vs. Hydraulic Conductivity Soil Texture Sand 18.9 Loamy sand 4.7 Sandy loam 1.7 Loam 1.0 (1.3 cm/hr) Silt loam 0.54 Sandy clay loam 0.24 Clay loam 0.16 (0.2 cm/hr) Silty clay loam 0.16 Sandy clay 0.09 Silty clay 0.08 Clay 0.05 Hydraulic Conductivity Guelph Permeameter Example - Fine sandy loam 7 sample sites on 100 + acres Guelph Permeameter at 30 and 75 cm Varies 2.3 cm/hour to 4.2 cm/hour at 75 cm Compaction/ infiltration issues, lower readings at shallower depth ? 32 Soil Texture and Structure vs. Tile Depth Example --- Fine Soils ---- Drainage Guide for Ontario Preferential flow in cracks S-1 Fine textured surface and blocky or massive B and C. Hydraulic conductivity low. Relies on soil cracking, deep tillage, mole drainage IF tiled. Surface drainage first solution. S-2 Somewhat coarser than S-1. Finer texture B and C horizons. Extensively drained in Ontario. Drains should not be deep and should be placed in B horizon for best results. Salinity Mapping Saline areas match to soils well and also to yield maps for this quarter Question tile poorest yielding, most saline soils first ? Question install tile shallow to limit salt movement downstream ? Question any upward flow (artesian) conditions ? Depth to Impervious Soils • • • • • EM31 utility deep texture mapping E.g. depth to impervious clay or depth averaged clay Hydrogeologic anomalies (to 12 feet) (silt, sand, etc.) EM34 available Landscape Affects Surface Runoff and Drainage Class and Drainage Coefficient Increase drainage coefficient IF surface drainage admitted directly into the pipe drain Critical to Understand Geology – Use Available Information (e.g. well logs, regional geology maps and studies ) Downslope water movement Artesian conditions require geology/engineering Drainage coefficient ? – Downstream impacts ? Source of salts ? WELL LOG From To Log (ft.) (ft.) 0 6.0 BROWN TILL 6.0 8.0 SAND 8.0 10.0 BROWN SAND 10.0 14.0 GRAVEL 14.0 22.0 BROWN TILL 22.0 40.0 GREY TILL 40.0 55.0 SHALE GRAVEL 55.0 70.0 GREY TILL 70.0 160.0 SHALE AND CLAY No construction data for this well. 37 Sodic Soils Hazard Assessment NDSU Approach is Systematic Case Study --- Homewood Soil surveys 1:20,000 map PME, EBG, RGB, DHO, JOD, GYV Veris comparison to soils surveys depth to sand layer or no sand (auger holes) Variable spacing 30 – 60 feet landscape (top slope vs downslope) texture/hydraulic conductivity VARIES, use 1:20,000 BMPs Controlled drainage/subirrigation (BMP) Monitoring data Adcon (soil moisture, GWT) Soils Investigations… 40 2011 -- Early Adopter Field Scale Controlled Drainage Seven Control Structures ---- 300 acres Producer influenced by test plots at Hespler and CMCDC Contractor interested in value added Producer looking at “long term” Contractor needed technical assistance Monitor performance critical (e.g. does it work) Professional input provided Yield North 150 Acres – 2013 Explain Using Soils Zones and Subirrigation ? Value of models ? Sub Irrigated Corn Manitoba – 25 acre trial 2013 300 acres Controlled Drainage 43 Design Tools - Internet South Dakota State University http://climate.sdstate.edu/water/DrainSpacingCal.html Computer Simulation Models DRAINMOD – North Carolina State University Climate Soils min/max temp precipitation ET crop freeze/thaw soil water characteristics Ksat drainage volume infiltration upflux soil water content Seepage Drainage System Parameters Crop Parameters http://www.bae.ncsu.edu/soil_water/documents/Dr ainmod.Model.Use.Calibration.And.Validation.pdf http://www.bae.ncsu.edu/soil_water/methods_data/Sustai nable_High_Yields_on_Poorly_Drained_SoilsPres_Color.pdf Sands et al., 2013 University of Minnesota Used DRAINMOD Looked at 6 soils, 3 locations 100 years data Averaged impacts and yield (relative) Very similar to MORDEN – 20 inches precip Increase tile drainage coefficient => decrease surface runoff http://www1.extension.umn.edu/agriculture/water/reports/docs/final_report_ _developing_drainage_guidelines_for_rrb_sands.pdf 46 DRAINMOD – Non Tiled – 2010 Weather Data – Clay Loam 0 2010-05-20 2010-07-09 2010-08-28 2010-10-17 50 20 WT Depth (cm) 40 40 60 80 100 120 140 160 Water Table Depth Rainfall Drainage (Total) Surface Runoff (Total) 30 20 10 180 200 0 Rainfall/Drainage/Runoff (cm) 2010-03-31 DRAINMOD - Tiled – 2010 Weather Data – Clay Loam 0 20 40 WT Depth (cm) 60 80 100 120 140 160 2010-05-20 2010-07-09 2010-08-28 Water Table Depth Rainfall 2010-10-17 50 Drainage (Total) Surface Runoff (Total) 40 30 20 10 180 200 0 Rainfall/Drainage/Runoff (cm) 2010-03-31 DRAINMOD Results – Red River Valley Sands, 2011; Sands et al. 2013 http://www.redriverbasincommission.org/Conference/Proceedings/28th_Proceedings/Sands.pdf Increase DC = Closer Tiles Where Can You Add Value