the assessment of soil variability is one of the most on-the...

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1 On On- the the- Go Proximal Soil Go Proximal Soil Sensing for Agriculture Sensing for Agriculture Viacheslav I. Adamchuk Viacheslav I. Adamchuk Department of Department of Bioresource Bioresource Engineering Engineering McGill University McGill University February 21, 2011 February 21, 2011 AGRI AGRI- SENSING 2011 (Haifa, Israel) SENSING 2011 (Haifa, Israel) Problem Statement Problem Statement The assessment of soil variability is one of the most important steps in site-specific management Conventional means to attain soil variability data are incapable of accurately identifying spatial inconsistency within a production field at an economically feasible cost There is a need to develop equipment for mapping soil attributes on-the-go Sensor Use Approaches Sensor Use Approaches Map-Based Approach Integrated Approach (Real-Time with Supplemental Base Maps) Real-Time Application Nature of Sensing Nature of Sensing Listen Taste Smell Touch Look On On- the the- go Proximal Soil Sensors go Proximal Soil Sensors Electrical and Electromagnetic Acoustic Mechanical Electrochemical Pneumatic Optical and Radiometric Electrical end Electromagnetic Sensors Electrical end Electromagnetic Sensors Electrical Conductivity/Resistivity Sensors EC a EC1 EC2 EC3 EC4 EC5 Soil Soil Galvanic Contact Resistivity Method Electromagnetic Induction Method Capacitively-Coupled Resistivity Method Soil type/texture Salinity Water content Organic matter content Depth variability Soil pH / nitrate content Volumetric water content Soil type/structure Salinity Dielectric Sensors Magnetic Sensors Subsurface soil impurities Iron

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Page 1: The assessment of soil variability is one of the most On-the ...adamchukpa.mcgill.ca/presentations/Agri-Sensing_2011.pdf1 On-the-Go Proximal Soil Sensing for Agriculture Viacheslav

1

OnOn--thethe--Go Proximal Soil Go Proximal Soil Sensing for AgricultureSensing for Agriculture

Viacheslav I. AdamchukViacheslav I. AdamchukDepartment of Department of BioresourceBioresource EngineeringEngineering

McGill UniversityMcGill University

February 21, 2011February 21, 2011

AGRIAGRI--SENSING 2011 (Haifa, Israel)SENSING 2011 (Haifa, Israel) Problem Statement Problem Statement

• The assessment of soil variability is one of the most important steps in site-specific management

• Conventional means to attain soil variability data are incapable of accurately identifying spatial inconsistency within a production field at an economically feasible cost

• There is a need to develop equipment for mapping soil attributes on-the-go

Sensor Use ApproachesSensor Use Approaches

Map-Based Approach

Integrated Approach (Real-Time with Supplemental Base Maps)

Real-Time Application

Nature of SensingNature of Sensing

Listen

Taste

SmellTouch

Look

OnOn--thethe--go Proximal Soil Sensorsgo Proximal Soil Sensors

Electrical and Electromagnetic

Acoustic

Mechanical Electrochemical

H+

H+ H+H+

H+

Pneumatic

Optical and Radiometric

Electrical end Electromagnetic SensorsElectrical end Electromagnetic Sensors

Electrical Conductivity/Resistivity Sensors

ECa

EC1

EC2

EC3

EC4

EC5

Soil Soil

Galvanic Contact Resistivity Method

Electromagnetic Induction Method

Capacitively-Coupled Resistivity Method

• Soil type/texture• Salinity• Water content• Organic matter content• Depth variability• Soil pH / nitrate content

• Volumetric water content• Soil type/structure• Salinity

Dielectric Sensors

Magnetic Sensors

• Subsurfacesoil impurities • Iron

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Galvanic Contact Resistivity MethodGalvanic Contact Resistivity Method

I

UA

BN

M

Current flow

Equipotentials

Veris Technologies, Inc. (Salina, Kansas)

http://www.veristech.com

Veris® 3100 and MSP(0.3 and 0.9 m)

Geocarta (Paris, France)

http://www.geocarta.netGeocarta ARP

(0.5, 1, and 2 m)

Crop Tehchnologies, Inc. (Spring, Texas)

http://www.soildoctor.com

Soil Doctor® System (real-time approach)

Electromagnetic Induction MethodElectromagnetic Induction Method

Receiver

Primary field

SoilEddy currents

Transmitter

Secondary field

Geonics Limited (Mississauga, Ontario)

http://www.geonics.com

Geonics EM-38

horizontal – 0.75 m vertical – 1.5 m

Dualem, Inc.(Milton, Ontario)

http://www.dualem.com

DUALEM – 1S

co-planar – 0.4 m perpendicular – 0.95 m

CapacitivelyCapacitively--Coupled Resistivity Coupled Resistivity MethodMethod

Capacitoranalogue Metal shield as a

capacitor plate

Soil as a capacitor plate

Insulation as dielectric material

Coaxialcable

Soil

Transmitter

Inner wire

Geometrics, Inc.(San Jose, California)

http://www.geometrics.com

Geometrix OhmMapper TR1

Pneumatic Angular Scanning Pneumatic Angular Scanning System (PASS)System (PASS)

UNL (Lincoln, Nebraska)2008-2009

Dielectric SensorDielectric SensorUNL (Lincoln, Nebraska) –

Retrokool (Berkeley, California)2001-2003

• Silty clay loam soil• Triple replicates• Two tests

2.0

2.2

2.4

2.6

2.8

3.0

3.2

0.00 0.05 0.10 0.15 0.20 0.25 0.30 0.35

Gravimetric Soil Moisture, g/g

Sens

or O

utpu

t, V

Test 1Test 2Average

Dielectric Sensor MapDielectric Sensor Map

Page 3: The assessment of soil variability is one of the most On-the ...adamchukpa.mcgill.ca/presentations/Agri-Sensing_2011.pdf1 On-the-Go Proximal Soil Sensing for Agriculture Viacheslav

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Soil Water ContentSoil Water ContentGravimetric soil moisture

R2 = 0.85SE = 2.7%

0%

5%

10%

15%

20%

25%

30%

0% 5% 10% 15% 20% 25% 30%

Sensor measurement

Labo

rato

ry m

easu

rem

ent

Volumetric soil moisture

R2 = 0.85SE = 3.9%

0%

5%

10%

15%

20%

25%

30%

35%

40%

0% 10% 20% 30% 40%

Sensor measurement

Labo

rato

ry m

easu

rem

ent

Optical and Radiometric SensorsOptical and Radiometric Sensors

Subsurface Soil Reflectance Sensors

Visual

Near-infrared

Mid-infrared

Image analysis

Polarized light

• Organic matter (carbon) content• Soil texture• Cation exchange capacity (CEC)• Soil water content• Soil pH• Mineral nitrogen and phosphorous

• Water content• Geophysical soil structure

Ground Penetrating Radar

Gamma Radiometer

• Potassium• Uranium • Thorium

Microwave Sensors

• Water content

Small Scale Topography

Shank

660 nm LEDs

Photodiode

Purdue University (West Lafayette, Indiana)

Subsurface Soil Reflectance SensorsSubsurface Soil Reflectance Sensors

UNL (Lincoln, Nebraska)

0.50

0.55

0.60

0.65

0.70

0.75

0.80

0.85

0.90

0.95

1.00

900 1000 1100 1200 1300 1400 1500 1600 1700

Wavelength, nm

Refle

ctan

ce, %

15 Nebraska soils

Individual WavelengthsIndividual Wavelengths

Spectroradiometer

Shank

DGPS Antenna

Notebook Computer

Coulter

Light Source

HyperspectralHyperspectral ResponseResponse

VIS/NIR SpectrophotometerVIS/NIR Spectrophotometer

Predicted Carbon Measured CarbonSapphire Window

Veris Technologies, Inc. (Salina, Kansas)

http://www.veristech.com

Integrate Soil Mapping System Integrate Soil Mapping System (ISMS)(ISMS)

UNL and Holland Scientific(Lincoln, Nebraska)

Retrokool (Berkeley, California) 2008-2010

Load Cell Sensor

Optical Sensor

Dielectric Sensor

Mechanical SensorsMechanical Sensors

Cantilever beam sensors

Direct load sensors

Single-tip horizontal sensors

Multiple-tip horizontal sensors

Verticallyoscillating sensors

Vertically-operated cone penetrometers

Soil profile sensors

Tine-based sensors

Tip-based sensors

Soil strength sensors

• Soil mechanical resistance • Soil compaction• Water content• Soil types• Depth of hard (plow) pan

Vertically actuated sensors

Bulk soil strength sensors

Draft and vertical force sensors

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Strain Gauges

Soil Mechanical Resistance MappingSoil Mechanical Resistance Mapping

Tool Bar

Travel Direction

Purdue University (West Lafayette, Indiana)

Discrete Depth Profiling ToolsDiscrete Depth Profiling Tools

UC-Davis(Davis, California)

Three Cutting Three Cutting BladesBlades

UNL(Lincoln, Nebraska)

University of Missouri(Columbia, Missouri)

Load Cell Load Cell ArrayArray

ExampleExampleSoil Mechanical Resistance Map Soil Mechanical Resistance Map

Soil Mechanical Resistance Map (20-30 cm)

Yield Map

Compacted area Old roads

Integrated Soil Physical Properties Integrated Soil Physical Properties Mapping System (ISPPMS)Mapping System (ISPPMS)

Two wavelengths soil reflectance sensor

Soil mechanical resistance profiler with an array of

strain gage bridgesCapacitor-based

sensor

UNL (Lincoln, Nebraska)

Bulk Density PredictionBulk Density Prediction

Moisture R2 = 0.50

Soil Mechanical Resistance R2 = 0.19

&

Bulk Density

R2 = 0.69

1.2

1.4

1.6

1.8

1.2 1.4 1.6 1.8

Measured Bulk Density, g/mL

Pre

dic

ted

Bul

k D

ensi

ty, g

/mL

Disc Coulter SensorDisc Coulter Sensor

Rotational Potentiometer

Ultrasound Depth Sensor

GPS Antennae

DAQ

UNL (Lincoln, Nebraska)

Page 5: The assessment of soil variability is one of the most On-the ...adamchukpa.mcgill.ca/presentations/Agri-Sensing_2011.pdf1 On-the-Go Proximal Soil Sensing for Agriculture Viacheslav

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Instrumented Tillage ImplementInstrumented Tillage Implement

Load Cells

Custom Protective

Shin

Custom Point

Depth Sensor

Strain Gauges

GPS Antenna

Laptop with DAQ Card

Signal Conditioning

Unit

Straight Standard

Variable Depth Tillage ConceptVariable Depth Tillage Concept

Soil StrengthSoil StrengthSoil Soil SurfaceSurface

Dep

thD

epth

Load Load CellsCells

Strain Strain GaugesGauges

US Patent No. 7,028,554

Acoustic and Pneumatic SensorsAcoustic and Pneumatic SensorsSoil Penetration Noise Sensors

University of Illinois(Urbana-Champaign, Illinois)

University of Kentucky(Lexington, Kentucky)

Air Permeability Sensor

• Soil structure/tilth• Water content• Soil type

• Soil clay content (type)• Soil compaction• Depth of hard (plow) pan

Electrochemical SensorsElectrochemical SensorsIon-Selective Field Effect

Transistors (ISFETs)

Agitated Soil Measurement

Direct Soil Measurement

Soil Solution Measurement

Activity of selected ions• Soil pH (H+)• Potassium content (K+)• Residual nitrogen (NO3

--N)• Sodium content (Na+)

Ion-Selective Electrodes (ISEs)

Conventional Laboratory

Analysis

Sample collectionfor calibration

Cleaning

ISFET Electrode

Water jet

~50 g soil core

Mixing

Add 20 ml DI H2O

Automated Soil TestingAutomated Soil Testing

Shank

Soil cutters

Coring tube

Purdue University (West Lafayette, Indiana)

Automated Soil pH Mapping SystemsAutomated Soil pH Mapping Systems

US Patent No. 6,356,830Purdue University

(West Lafayette, Indiana)

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Mobil Sensor Platform (MSP)Mobil Sensor Platform (MSP)

Veris Technologies, Inc.(Salina, Kansas)

http://www.veristech.com

EC Surveyor 3150

Soil pH Manager

Direct Soil MeasurementDirect Soil MeasurementPurdue University

(West Lafayette, Indiana)Veris Technologies, Inc.

(Salina, Kansas)UNL (Lincoln, Nebraska)

Water Nozzle

Soil Sampler

Ion-selective Electrodes

ExampleExampleSoil pH MappingSoil pH Mapping

Soil pH Maps of a Kansas Field

On-the-Go Mapping Conventional 1 ha Grid Sampling

Directed Soil Sampling

Mapping AlternativesMapping Alternatives

pHMSPSlopeInterceptpHMSPUniversal UniversalUniversal ⋅+=

pHMSPSlopeInterceptpHMSPAdjusted specificFieldspecificField ⋅+= −−

pHMSPShiftpHMSPShifted specificField += −

Soil SamplingOn-the-Go Sensing

MSP pH

Universal MSP pH

Directed Sampling

Adjusted MSP pH

Shifted MSP pH

Field Average

Interpolated Grid Map

Soil pH Maps EvaluationSoil pH Maps Evaluation

4

5

6

7

8

9

4 5 6 7 8 9

Grid Sampling pH

Lab

pH

IA1IL1IL2KS1KS2NE1OK1WI11:1 lineReg

4

5

6

7

8

9

4 5 6 7 8 9

Field Average pH

Lab

pH

IA1IL1IL2KS1KS2NE1OK1WI11:1 lineReg

4

5

6

7

8

9

4 5 6 7 8 9

Shifted MSP pH

Lab

pH

IA1IL1IL2KS1KS2NE1OK1WI11:1 lineReg

4

5

6

7

8

9

4 5 6 7 8 9

Adjusted MSP pH

Lab

pH

IA1IL1IL2KS1KS2NE1OK1WI11:1 lineReg

4

5

6

7

8

9

4 5 6 7 8 9

Unprocessed MSP pH

Lab

pH

IA1IL1IL2KS1KS2NE1OK1WI11:1 lineReg

4

5

6

7

8

9

4 5 6 7 8 9

Universal MSP pH

Lab

pH

IA1IL1IL2KS1KS2NE1OK1WI11:1 lineReg

R2 = 0.47 R2 = 0.25

R2 = 0.60 R2 = 0.60

R2 = 0.81 R2 = 0.81

2.5 Acre Grid

Raw MSP Universal MSP

Shifted MSPAdjusted MSP

Field Average

R2 = 0.99SE = 0.23

4.0

4.5

5.0

5.5

6.0

6.5

7.0

4.0 4.5 5.0 5.5 6.0 6.5 7.0

Soil pH Glass Electrodes

Soil

pH A

ntim

ony

Ele

ctro

des

Antimony ElectrodeAntimony ElectrodeSandy and stony soils

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Portable ProbePortable Probe OnOn--thethe--Spot Measurement of Soil pHSpot Measurement of Soil pH

3.0

3.5

4.0

4.5

5.0

5.5

6.0

6.5

7.0

7.5

8.0

0 10 20 30 40 50

Depth, cm

Soi

l pH

Plot APlot BPlot CAverage Plot AAverage Plot BAverage Plot C

10 – 20 ~ 8 ~ 18 ~28

Portable Probe Reference Lab

Integrated Direct Soil Measurement Integrated Direct Soil Measurement

15 Nebraska soils with fixed field water content

UNL(Lincoln, Nebraska)

4.0

4.5

5.0

5.5

6.0

6.5

7.0

7.5

4.0 4.5 5.0 5.5 6.0 6.5 7.0 7.5

Reference pH

Mea

sure

d pH

R2 = 0.93 (0.96 means)RMSE (Precision) = 0.12 pH

Reg. SE (Accuracy) = 0.16 pH

pH

10

100

1000

1 10 100

Reference nitrate-nitrogen (CR), mg/kg

Mea

sure

d ni

trate

-nitr

ogen

, mg/

kg R2 = 0.35 (0.61 means)RMSE (Precision) = 0.19 pNO3

Reg. SE (Accuracy) = 0.12 pNO3

pNO31

10

100

10 100 1000

Reference soluble potassium (AAS), mg/kg

Mea

sure

d so

lubl

e po

tass

ium

, mg/

kg

R2 = 0.52 (0.62 means)RMSE (Precision) = 0.13 pK

Reg. SE (Accuracy) = 0.15 pK

pK

VRT PrescriptionVRT Prescription

4.0

4.5

5.0

5.5

6.0

6.5

7.0

7.5

8.0

6.0 6.5 7.0 7.5

Measured buffer pH

Mea

sure

d so

il pH

and

pre

dict

ed b

uffe

r pH Predicted buffer pH

Measured soil pH1:1 line

( )

LR = f (buffer pH)

Buffer pH = f (soil pH, CEC)R2 = 0.91

R2 = 0.68

0

200

400

600

0 200 400 600

Measured exchangeble K, mg kg-1

Mea

sure

d so

lubl

e K

and

pre

dict

ed

exch

ange

ble

K, m

g kg

-1

Predicted exchangable KMeasured soluble K1:1 line

K rate = f (exchangeable K)

Exchangeable K = f (soluble K, CEC)

R2 = 0.94

R2 = 0.65

Integrated Multiple Data LayersIntegrated Multiple Data Layers

Maps produced by Veris Technologies, Inc. (Salina, Kansas)

Soil pH & Clay & OM

= Lime Recommendation

Applicability of OnApplicability of On--thethe--Go Soil SensorsGo Soil Sensors

OKSomeSomeResidual nitrate (total nitrogen)

OKOKCEC (other buffer indicators)

OKSomeOther nutrients (potassium)

GoodSomeSoil pH

SomeOKSomeDepth variability (hard pan)

SomeGoodSoil compaction (bulk density)

SomeOKSoil salinity (sodium)

GoodGoodSoil water (moisture)

GoodSomeSoil organic matter or total carbon

SomeOKGoodSoil texture (clay, silt and sand)

Soil property H+

H+ H+H+

H+

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Targeted Soil SamplingTargeted Soil Sampling

• Directed sampling should be used to calibrate and/or validate sensor data

• Directed samples should be collected from relatively homogeneous field areas away from the boundary and other transitional areas

• Directed samples should cover the entire range of sensor-based measurements, especially toward low and high ends

• Directed samples should be physically spread across the entire field

• It should be possible to process multiple sensor-based data layers

Objective FunctionObjective Function

5ECcrpHcrECoptpHoptopt HHDDSOF −−−− ⋅⋅⋅⋅=

• S-optimality• D-optimality (soil pH)• D-optimality (soil EC)• H-criteria (soil pH)• H-criteria (soil EC)

SummarySummary

• On-the-go soil sensors can provide high density information about soil properties

• Many sensor approaches are past initial commercialization stage

• Sensor fusion provides the ability to separate various agronomic effects

• Site-specific sensor calibration and validation are essential steps of the mapping process

• Laboratory soil analysis remains a required supplementary practice http://bse.unl.edu/adamchuk

E:mail: [email protected]