2013 NUE Conference Des Moines, Iowa August 5-7 Jacob T. Bushong.

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Presentation transcript:

2013 NUE Conference Des Moines, Iowa August 5-7 Jacob T. Bushong

 Current OSU winter wheat midseason N rate recommendations are determined using: ◦ Grain Yield Potential ◦ Response index (RI), N-Rich strip and the farmer practice ◦ Assumed maximum grain yield for the region ◦ Economic factors (grain price & fertilizer price) Farmer Practice N-Rich Strip

 Based upon NDVI and GDD  In-season estimate of yield (INSEY)=NDVI/GDD

 Aids in stand establishment and early vegetative growth  Increases nutrient uptake of mobile nutrients  Yields can be maximized if consistent available water is present throughout the growing season

 To improve the current method for estimating in-season grain yield potential by utilizing soil moisture data. Photo courtesy of Oklahoma State University + =

 Oklahoma Mesonet ◦ Collaboration with Oklahoma State & University of Oklahoma ◦ 120 automated weather monitoring stations statewide ◦ Measures air temperature, wind speed, soil temperature, soil moisture ◦ Soil moisture data, since 1996

 Soil Moisture ◦ Heat dissipation sensors ◦ Depths of 5, 25, 60, 75 cm ◦ Data reported as Fractional Water Index (FWI)  Range from 0.00 to 1.00  Soil Temperature ◦ Recorded at 1.5 m above the surface

 Downloaded from website ◦  Average daily values  SQL queries designed to retrieve desired data

 Normalized Difference Vegetation Index (NDVI)  Growing Degree Days (GDD’s)  Soil Moisture Factor (SMF)

 Collected with Trimble Greenseeker Optical Sensor NDVI RED = ρ ρ 670 ρ ρ 670

 Current: Days from planting to sensing where the average daily temperature > 4.4 °C  Proposed: Days from planting to sensing where the average daily temperature > 4.4 °C and FWI > 0.30

NDVI FWI GDD Data sources: USGS Earth Explorer and Mesonet.org

 Proportion of 0-80cm PAW at sensing to the daily water use (ET) of the growing crop from sensing to harvest ◦ Assumed harvest date of June 10 ◦ Assumed daily water use 5 mm day -1  FWI index converted to PAW utilizing soil water content values (PWP, FC, SAT) from USDA-NRCS soil survey  Value cannot exceed 1.0

 Lahoma: Grant silt loam (fine-silty, mixed, superactive, thermic Udic Argiustolls)  Stillwater: Kirkland silt loam (fine, mixed, superactive, thermic Udertic Paleustolls)  Perkins: Konawa fine sandy loam (fine-loamy, mixed, active, thermic Ultic Haplustalfs)  Data collected from 2003 to 2011  22 total site-years of data  Plots had a wide range of pre-plant N rates  Data collected over a range of growth stages (Feekes 3 to 10)

 Lahoma: Grant silt loam (fine-silty, mixed, superactive, thermic Udic Argiustolls)  Stillwater: Kirkland silt loam (fine, mixed, superactive, thermic Udertic Paleustolls)  Perkins: Konawa fine sandy loam (fine-loamy, mixed, active, thermic Ultic Haplustalfs)  Hennessey: Bethany silt loam (fine, mixed, superactive, thermic Pachic Paluestolls)  LCB: Port silt loam (fine-silty, mixed, superactive, thermic Cumulic Haplustolls)  LCB: Konawa fine sandy loam (fine-loamy, mixed, active, thermic Ultic Haplustalfs)  Data collected from 2012 and 2013  11 total site-years of data  Plots had a wide range of pre-plant N rates  Data collected over a range of growth stages (Feekes 3 to 10)

 Stepwise regression was utilized ◦ Maximize the adjusted R 2  Three models developed ◦ All Calibration Sites (Lahoma, Stillwater, Perkins) ◦ Loamy Calibration Sites (Lahoma, Stillwater) ◦ Coarse Calibration Site (Perkins)

All SitesLoamy SitesCoarse Sites Parameter Est.Pr > |t|Est.Pr > |t|Est.Pr > |t| Intercept GDD -0.09< SMF < < NDVI < GDD*SMF 0.11< GDD*NDVI 0.22< NDVI*SMF 25.80< < NDVI*GDD*SMF -0.28< <

R2R2

R2R2

R2R2

R2R2

R2R2

R2R2

R2R2

R2R2

R2R2

Actual Yield (Mg/ha) Predicted Yield (Mg/ha) Actual Yield (Mg/ha) New INSEY Current INSEY RMSE = 0.92 RMSE = 0.95 X X

 Soil moisture at the time of sensing had a significant effect on final wheat grain yield for all locations  Models that included soil moisture parameters typically outperformed current models at most locations  One model developed from loamy and coarse textures sites is sufficient to use compared to having different models based on soil type.

 Investigate the GDD adjustment for soil moisture ◦ What depth? ◦ Soil moisture threshold?  Evaluate which estimate of grain yield provides the most accurate mid-season N rate recommendation  Evaluate if Vertisol soils can use the new model or if they need their own model