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Integrated Soil TillageIntegrated Soil Tillage
Force PredictionForce Prediction
ModelsModels
Richard GodwinRichard Godwin
andand
MichaelMichael O’DoghertyO’Dogherty
Engineering GroupEngineering Group
National Soil Resources InstituteNational Soil Resources Institute
Soil implement forcesSoil implement forces
Sugar cane fields – Iran Land preparation – South Australia
Autumn cultivations - Cambridge
Soil failure patternsSoil failure patterns
After: Godwin and Spoor, 1977
MohrMohr –– Coulomb RelationshipsCoulomb Relationships
Coulomb Equation
τ
σ
φ
c
τ = c + σ tan φ
σ3
σ1
σ1
σ3
C = cohesion
Ø = internal friction
σ3 σ1
General Soil Mechanics EquationGeneral Soil Mechanics Equation
2 dimensional passive soil failure2 dimensional passive soil failure
Direction of travel
( )( )[ ] )sin(2
δαγ γ +++= wqdNcdNNdH qcat
Ht
Vt
α
P
Normal
δ
Blade or tine face
Soil
surface
( )( )[ ] )cos(2
δαγ γ +++−= wqdNcdNNdV qcat
+ vertical forces act
After: Hettiaratchi , Witney and Reece,1966
Dimensionless N Factor’sDimensionless N Factor’s
Nγ
α
φ
δ = 0
δ = φ
δ = 0
δ = 0
δ = φ
δ = φ
Nγ
Nc
Nc
Nq
Nq
20
10
1
0
Nγδ = Nγδ = 0 Nγδ = φ Nγδ = 0
δ /φ
After: Hettiaratchi, Witney and Reece, 1966
Narrow Tine EquationsNarrow Tine Equations
3 dimensional soil failure3 dimensional soil failure
After: Godwin and Spoor, 1977
Tine width (w) + crescent
effects
( ){ }13
1
−− mmdw +
Inertia termsInertia terms
wdN
g
v
a
2
γ
Inertia term =
where
( )
( ) ( ) ( )( )( )αβφβδαβα
φββ
cottan1cotsincos
cottan
+++++
++
=aN
After :McKyes, 1985
General Soil Mechanics EquationGeneral Soil Mechanics Equation
for blades and narrow tinesfor blades and narrow tines
Including velocity effectsIncluding velocity effects
Horizontal
( ) ( )( ) ( ) )sin(6.0)1(3
1
δαγγ γ +++−−+++= dwdNvmmdwqdNcdNNdH aqcat [ ]22
Force = [( Soil factors )(Implement size) + Inertia term ]Direction
Vertical
( ) ( )( ) ( )[ ] )(cos6.0)1( 2
3
12
δαγγ γ +++−−+++−= dwdNvmmdwqdNcdNNdV aqcat
After: Hettiaratchi et al.,1966; Godwin and Spoor, 1977; Godwin et al.,1984; McKyes,1985 and
Wheeler and Godwin, 1996
Deep or Very Narrow TinesDeep or Very Narrow Tines
–– Lateral failureLateral failure
Deep tine failureDeep tine failure
After: Godwin and Spoor, 1977
Critical depth, dc
Lateral Force (Q) is based
on Meyerhof (1951)
Bearing Capacity Equation
and N factors
Additional component for very narrow tinesAdditional component for very narrow tines
( ) ( ) ( )22
sin15.0 cqcc ddwNddwcNQ −
′
−+−
′
= γφ
( )
( )( ) ⎥
⎦
⎤
⎢
⎣
⎡
−
+−
+
=
′
1
2sinsin1
sin1
cot
tan2
φηφ
φ
φ
φθ
e
Nc
( )
( )( )φηφ
φ φθ
+−
+
=
′
2sinsin1
sin1 tan2
e
Nq
Hence the total horizontal force is
HT
Q
dc
d
D = HT + Q
Lateral failure under plate glass After: Godwin and Spoor ,1977
Laboratory studiesLaboratory studies
Controlled conditions for soil
disturbance and implement
force measurement
Effect of tine widthEffect of tine width
-0.5
0
0.5
1
1.5
2
3
0 10 20 30 40 50 60
Tine width, mm
Force,kN
After: Godwin and Spoor, 1977
Vertical force
Predicted
2.5
Horizontal forceMeasured▀
Effect of tine depthEffect of tine depth
0
0.5
1
1.5
2
2.5
100 120 140 160 180 200 220 240
Tine depth, mm
Force,kN
After: Godwin and Spoor, 1977
Vertical force
3
3.5
Horizontal force
▀
Predicted
Measured
Effect of rake angleEffect of rake angle
-1
-0.5
0
0.5
1
1.5
2
2.5
3
3.5
30 40 50 60 70 80 90 100
Tine rake angle, degrees
Force,kN
After: Godwin and Spoor, 1977
Horizontal force
Vertical force
▀
Predicted
Measured
Effect of speedEffect of speed
0
1
2
3
4
5
0 2.5 5 7.5 10 12.5 15 17.5 20
Speed, km/h
Force,kN
After: Wheeler and Godwin, 1996
√ 5gw* √ 5g(w+0.6d)
*After: Schuring and Emori, 1964
Horizontal force
Vertical force
Measured
Predicted
Multiple tinesMultiple tines
After: Godwin, Spoor and Soomro, 1984
MultipleMultiple --interacting tine modelinteracting tine model
Imaginary tines Real tine
di
d
d
D =ns HTs + nd HTd – ni HiT
( ) ( )}{[ ] ( )δαγ γ +−−++−+= sin13
12
mmdNqdNcdNdnHnHnD iqicaiiiTddTss
After: Godwin, Spoor and Soomoro, 1984
Effects of tine spacingEffects of tine spacing
Spacing
Too close
Optimum
Too wide
After: Godwin, Spoor and Soomro, 1984
Effect of tine spacingEffect of tine spacing
▲ Predicted
● Measured
After: Godwin, Spoor and Soomro, 1984
Anchor performanceAnchor performance
Mg
Ht
Vt
Vt+ Mg
Pa
( ) ( )( )[ ] )sin()1(3
12
δαγ γ +−−+++= mmdwqdNcdNNdH qcat
( ) tta HMgVP ++= δtan
( ) ( )( )[ ] )(cos)1(3
12
δαγ γ +−−+++−= mmdwqdNcdNNdV qcat
where
After: Godwin and Wheeler, 1996
Anchor forcesAnchor forces
0
10
20
30
40
50
60
0 0.2 0.4 0.6 0.8 1
Anchor depth, m
Anchorforce,kN
After: Godwin and Wheeler, 1996
Compact sandy loam: field
Loose sandy loam: laboratory
Compact sandy loam: laboratory
Predicted ■ Measured
Disc forcesDisc forces
Disc harrow modelDisc harrow model
( )( ) θθγγ γ sin22sin 22
dRddNdRcdNNdP qfcai −−++=
Passive reaction
Passive soil crescent
reaction
Direction of travel Bearing capacity/
scrubbing reaction
Plan of disc
λ = clearance angle
θ
θ = sweep angle
λ
Surcharge effects Effective width
Vs =cNc’A
Nc’ Bearing Capacity Number
Scrubbing reaction
A Area
After. Godwin, Sieg and Allott, 1987
Disc forcesDisc forces
( ) θδα sinsin += PDp
( )δα +−= cosPVp
( ) θδα cossin += PSp
( ) ( )θλδα −−= sintanss VD
( )
λ
θλπ
2
sin
−
′= AqVs
( ) ( )θλδα −−= costanss VS
sp DDD +=
sp VVV +=
sp SSS −=
PassivePassive
TotalTotal
DraughtDraught
VerticalVertical
Lateral
ScrubbingScrubbing
Lateral
After. Godwin, Sieg and Allott, 1987
Effect of sweep angle on draught forceEffect of sweep angle on draught force
0
0.5
1
1.5
2
2.5
3
3.5
0 20 40 60 80 100
Disc sweep angle, deg
Draughtforce,kN
Measured
Predicted
▀
After. Godwin, Sieg and Allott, 1987
Effect of sweep angle on lateral forceEffect of sweep angle on lateral force
-2.5
-2
-1.5
-1
-0.5
0
0.5
1
1.5
0 20 40 60 80 100
Disc sweep angle, deg
Lateralforce,kN
After. Godwin, Sieg and Allott, 1987
Measured
Predicted
▀
Effect of sweep angle on disc forcesEffect of sweep angle on disc forces
Sweep angle (θ), degrees
Force,kN
Horizontal
Vertical
Lateral
Predicted
Measured
After: Godwin et al, 1987 and Gill et al, 1979
Mouldboard plough forcesMouldboard plough forces
Mouldboard plough forcesMouldboard plough forces
Landside
Mouldboard
Point
Share
Ht
Hp
Hs
Hmc
He
HcsHms Hfs
βθ
Direction of travelDirection of travel
Landside frictional drag force
Lifting energy force
Momentum change force
Passive share force
Passive point force
After: Saunders, Godwin and O’Dogherty , 2000
Mouldboard plough draught forceMouldboard plough draught force
Ht = Hp + Hs + Hmc + He + Hcs + Hms + Hfs
( ) ( ) βδαγγ γ sinsin/22
+++= sssacasss wgdNvNcdNdH
Total forceTotal force
WhereWhere
( ) ( ){( )θδθγ costansin11)/ 2
−−+= vdwdwgH ssppmc
( ) sssppe ddwdwH += γ2
( ) ( ) δβδαγγ γ tancossin/22
+++= sssasscs wgdNvNcdNdH ca
( )( ) ( ) δδθθγ tantansin1sin/ 2
−+= vdwdwgH ssppms
( ) δδγ tantan95.0 sssppfs dwdwH +=
After: Saunders, Godwin and O’Dogherty , 2000
Effect of velocity on plough draught forceEffect of velocity on plough draught force
0
0.5
1
1.5
2
2.5
3
3.5
0 1 2 3 4 5
Speed (m/s)
DraughtForce(kN)
225mm deep, measured, predicted
125mm deep, measured, predicted
After : Balafoutis,2003
Laboratory studies : Sandy loam soilLaboratory studies : Sandy loam soil
0
1
2
3
4
5
6
7
0 0.5 1 1.5 2 2.5
Speed (m/s)
DraughtForce(kN)
Effect of velocity on plough draught forceEffect of velocity on plough draught force
225mm deep, measured, predicted
180 mm deep, measured, predicted
After : Balafoutis,2003
Field studies : Sandy clay soilField studies : Sandy clay soil
ShallowShallow -- high speed mouldboard ploughhigh speed mouldboard plough
Because depth has a greater effect on draught
force than forward speed, shallow high speed
ploughs are becoming a popular alternative
Soil parameters Tine parameters
Force prediction spreadsheet modelsForce prediction spreadsheet models
Predicted v measured tinePredicted v measured tine and disc forcesand disc forces
HorizontalHorizontal
0
1
2
3
4
0 1 2 3 4
Measured draught force, kN
Predictedforce,kN
1:1
-20%
After: Godwin and O’Dogherty, 2003
Average error -3%
5 +20%
-1
-0.5
0
0.5
1
1.5
2
2.5
-0.5 0 0.5 1 1.5 2
Measured vertical force, kN
Predictedverticalforce,kN
1:1
+50%
-50%
After: Godwin and O’Dogherty, 2003
Average error + 33%
VerticalVertical
Predicted v measured tinePredicted v measured tine and disc forcesand disc forces
0
1
2
3
4
5
6
0 1 2 3 4 5
Total Measured Force (kN)
TotalPredictedForce(kN)
-20%
+20%
1:1
125 mm
225 mm
Laboratory studies : Sandy loam soilLaboratory studies : Sandy loam soil
Predicted v measured plough draught forcesPredicted v measured plough draught forces
After : Balafoutis,2003
0
2
4
6
8
10
12
0 1 2 3 4 5 6 7 8
Total Measured Force (kN)
TotalPredictedForce(kN)
1:1
+20%
+20%
180 mm
225 mm
Predicted v measured plough draught forcesPredicted v measured plough draught forces
Field studies : Sandy clay soilField studies : Sandy clay soil
After : Balafoutis,2003
ConclusionsConclusions
The general soil mechanics equation has been
developed to enable the draught and vertical forces
to be calculated for a wide range of implements.
The use of the equations has:
1. predicted the magnitude of the horizontal soil
force with an average error of -3%, with the
majority of comparisons within ±20%,
2. predicted the magnitude of the vertical soil force
with an average error of +33%, with the majority
of comparisons within ±50%, and
3. provided a good basis for designers of
cultivation equipment for optimal design of
cultivating tools.
The spreadsheet model will be freely available.
AcknowledgementsAcknowledgements
Gordon Spoor,Gordon Spoor,
Tony Reynolds,Tony Reynolds,
DanDan HettiaratchiHettiaratchi
andand
The DouglasThe Douglas BomfordBomford TrustTrust

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Istvs2003 godwin presentation

  • 1. Integrated Soil TillageIntegrated Soil Tillage Force PredictionForce Prediction ModelsModels Richard GodwinRichard Godwin andand MichaelMichael O’DoghertyO’Dogherty Engineering GroupEngineering Group National Soil Resources InstituteNational Soil Resources Institute
  • 2. Soil implement forcesSoil implement forces Sugar cane fields – Iran Land preparation – South Australia Autumn cultivations - Cambridge
  • 3. Soil failure patternsSoil failure patterns After: Godwin and Spoor, 1977
  • 4. MohrMohr –– Coulomb RelationshipsCoulomb Relationships Coulomb Equation τ σ φ c τ = c + σ tan φ σ3 σ1 σ1 σ3 C = cohesion Ø = internal friction σ3 σ1
  • 5. General Soil Mechanics EquationGeneral Soil Mechanics Equation 2 dimensional passive soil failure2 dimensional passive soil failure Direction of travel ( )( )[ ] )sin(2 δαγ γ +++= wqdNcdNNdH qcat Ht Vt α P Normal δ Blade or tine face Soil surface ( )( )[ ] )cos(2 δαγ γ +++−= wqdNcdNNdV qcat + vertical forces act After: Hettiaratchi , Witney and Reece,1966
  • 6. Dimensionless N Factor’sDimensionless N Factor’s Nγ α φ δ = 0 δ = φ δ = 0 δ = 0 δ = φ δ = φ Nγ Nc Nc Nq Nq 20 10 1 0 Nγδ = Nγδ = 0 Nγδ = φ Nγδ = 0 δ /φ After: Hettiaratchi, Witney and Reece, 1966
  • 7. Narrow Tine EquationsNarrow Tine Equations 3 dimensional soil failure3 dimensional soil failure After: Godwin and Spoor, 1977 Tine width (w) + crescent effects ( ){ }13 1 −− mmdw +
  • 8. Inertia termsInertia terms wdN g v a 2 γ Inertia term = where ( ) ( ) ( ) ( )( )( )αβφβδαβα φββ cottan1cotsincos cottan +++++ ++ =aN After :McKyes, 1985
  • 9. General Soil Mechanics EquationGeneral Soil Mechanics Equation for blades and narrow tinesfor blades and narrow tines Including velocity effectsIncluding velocity effects Horizontal ( ) ( )( ) ( ) )sin(6.0)1(3 1 δαγγ γ +++−−+++= dwdNvmmdwqdNcdNNdH aqcat [ ]22 Force = [( Soil factors )(Implement size) + Inertia term ]Direction Vertical ( ) ( )( ) ( )[ ] )(cos6.0)1( 2 3 12 δαγγ γ +++−−+++−= dwdNvmmdwqdNcdNNdV aqcat After: Hettiaratchi et al.,1966; Godwin and Spoor, 1977; Godwin et al.,1984; McKyes,1985 and Wheeler and Godwin, 1996
  • 10. Deep or Very Narrow TinesDeep or Very Narrow Tines –– Lateral failureLateral failure
  • 11. Deep tine failureDeep tine failure After: Godwin and Spoor, 1977 Critical depth, dc Lateral Force (Q) is based on Meyerhof (1951) Bearing Capacity Equation and N factors
  • 12. Additional component for very narrow tinesAdditional component for very narrow tines ( ) ( ) ( )22 sin15.0 cqcc ddwNddwcNQ − ′ −+− ′ = γφ ( ) ( )( ) ⎥ ⎦ ⎤ ⎢ ⎣ ⎡ − +− + = ′ 1 2sinsin1 sin1 cot tan2 φηφ φ φ φθ e Nc ( ) ( )( )φηφ φ φθ +− + = ′ 2sinsin1 sin1 tan2 e Nq Hence the total horizontal force is HT Q dc d D = HT + Q Lateral failure under plate glass After: Godwin and Spoor ,1977
  • 13. Laboratory studiesLaboratory studies Controlled conditions for soil disturbance and implement force measurement
  • 14. Effect of tine widthEffect of tine width -0.5 0 0.5 1 1.5 2 3 0 10 20 30 40 50 60 Tine width, mm Force,kN After: Godwin and Spoor, 1977 Vertical force Predicted 2.5 Horizontal forceMeasured▀
  • 15. Effect of tine depthEffect of tine depth 0 0.5 1 1.5 2 2.5 100 120 140 160 180 200 220 240 Tine depth, mm Force,kN After: Godwin and Spoor, 1977 Vertical force 3 3.5 Horizontal force ▀ Predicted Measured
  • 16. Effect of rake angleEffect of rake angle -1 -0.5 0 0.5 1 1.5 2 2.5 3 3.5 30 40 50 60 70 80 90 100 Tine rake angle, degrees Force,kN After: Godwin and Spoor, 1977 Horizontal force Vertical force ▀ Predicted Measured
  • 17. Effect of speedEffect of speed 0 1 2 3 4 5 0 2.5 5 7.5 10 12.5 15 17.5 20 Speed, km/h Force,kN After: Wheeler and Godwin, 1996 √ 5gw* √ 5g(w+0.6d) *After: Schuring and Emori, 1964 Horizontal force Vertical force Measured Predicted
  • 18. Multiple tinesMultiple tines After: Godwin, Spoor and Soomro, 1984
  • 19. MultipleMultiple --interacting tine modelinteracting tine model Imaginary tines Real tine di d d D =ns HTs + nd HTd – ni HiT ( ) ( )}{[ ] ( )δαγ γ +−−++−+= sin13 12 mmdNqdNcdNdnHnHnD iqicaiiiTddTss After: Godwin, Spoor and Soomoro, 1984
  • 20. Effects of tine spacingEffects of tine spacing Spacing Too close Optimum Too wide After: Godwin, Spoor and Soomro, 1984
  • 21. Effect of tine spacingEffect of tine spacing ▲ Predicted ● Measured After: Godwin, Spoor and Soomro, 1984
  • 22. Anchor performanceAnchor performance Mg Ht Vt Vt+ Mg Pa ( ) ( )( )[ ] )sin()1(3 12 δαγ γ +−−+++= mmdwqdNcdNNdH qcat ( ) tta HMgVP ++= δtan ( ) ( )( )[ ] )(cos)1(3 12 δαγ γ +−−+++−= mmdwqdNcdNNdV qcat where After: Godwin and Wheeler, 1996
  • 23. Anchor forcesAnchor forces 0 10 20 30 40 50 60 0 0.2 0.4 0.6 0.8 1 Anchor depth, m Anchorforce,kN After: Godwin and Wheeler, 1996 Compact sandy loam: field Loose sandy loam: laboratory Compact sandy loam: laboratory Predicted ■ Measured
  • 25. Disc harrow modelDisc harrow model ( )( ) θθγγ γ sin22sin 22 dRddNdRcdNNdP qfcai −−++= Passive reaction Passive soil crescent reaction Direction of travel Bearing capacity/ scrubbing reaction Plan of disc λ = clearance angle θ θ = sweep angle λ Surcharge effects Effective width Vs =cNc’A Nc’ Bearing Capacity Number Scrubbing reaction A Area After. Godwin, Sieg and Allott, 1987
  • 26. Disc forcesDisc forces ( ) θδα sinsin += PDp ( )δα +−= cosPVp ( ) θδα cossin += PSp ( ) ( )θλδα −−= sintanss VD ( ) λ θλπ 2 sin − ′= AqVs ( ) ( )θλδα −−= costanss VS sp DDD += sp VVV += sp SSS −= PassivePassive TotalTotal DraughtDraught VerticalVertical Lateral ScrubbingScrubbing Lateral After. Godwin, Sieg and Allott, 1987
  • 27. Effect of sweep angle on draught forceEffect of sweep angle on draught force 0 0.5 1 1.5 2 2.5 3 3.5 0 20 40 60 80 100 Disc sweep angle, deg Draughtforce,kN Measured Predicted ▀ After. Godwin, Sieg and Allott, 1987
  • 28. Effect of sweep angle on lateral forceEffect of sweep angle on lateral force -2.5 -2 -1.5 -1 -0.5 0 0.5 1 1.5 0 20 40 60 80 100 Disc sweep angle, deg Lateralforce,kN After. Godwin, Sieg and Allott, 1987 Measured Predicted ▀
  • 29. Effect of sweep angle on disc forcesEffect of sweep angle on disc forces Sweep angle (θ), degrees Force,kN Horizontal Vertical Lateral Predicted Measured After: Godwin et al, 1987 and Gill et al, 1979
  • 31. Mouldboard plough forcesMouldboard plough forces Landside Mouldboard Point Share Ht Hp Hs Hmc He HcsHms Hfs βθ Direction of travelDirection of travel Landside frictional drag force Lifting energy force Momentum change force Passive share force Passive point force After: Saunders, Godwin and O’Dogherty , 2000
  • 32. Mouldboard plough draught forceMouldboard plough draught force Ht = Hp + Hs + Hmc + He + Hcs + Hms + Hfs ( ) ( ) βδαγγ γ sinsin/22 +++= sssacasss wgdNvNcdNdH Total forceTotal force WhereWhere ( ) ( ){( )θδθγ costansin11)/ 2 −−+= vdwdwgH ssppmc ( ) sssppe ddwdwH += γ2 ( ) ( ) δβδαγγ γ tancossin/22 +++= sssasscs wgdNvNcdNdH ca ( )( ) ( ) δδθθγ tantansin1sin/ 2 −+= vdwdwgH ssppms ( ) δδγ tantan95.0 sssppfs dwdwH += After: Saunders, Godwin and O’Dogherty , 2000
  • 33. Effect of velocity on plough draught forceEffect of velocity on plough draught force 0 0.5 1 1.5 2 2.5 3 3.5 0 1 2 3 4 5 Speed (m/s) DraughtForce(kN) 225mm deep, measured, predicted 125mm deep, measured, predicted After : Balafoutis,2003 Laboratory studies : Sandy loam soilLaboratory studies : Sandy loam soil
  • 34. 0 1 2 3 4 5 6 7 0 0.5 1 1.5 2 2.5 Speed (m/s) DraughtForce(kN) Effect of velocity on plough draught forceEffect of velocity on plough draught force 225mm deep, measured, predicted 180 mm deep, measured, predicted After : Balafoutis,2003 Field studies : Sandy clay soilField studies : Sandy clay soil
  • 35. ShallowShallow -- high speed mouldboard ploughhigh speed mouldboard plough Because depth has a greater effect on draught force than forward speed, shallow high speed ploughs are becoming a popular alternative
  • 36. Soil parameters Tine parameters Force prediction spreadsheet modelsForce prediction spreadsheet models
  • 37. Predicted v measured tinePredicted v measured tine and disc forcesand disc forces HorizontalHorizontal 0 1 2 3 4 0 1 2 3 4 Measured draught force, kN Predictedforce,kN 1:1 -20% After: Godwin and O’Dogherty, 2003 Average error -3% 5 +20%
  • 38. -1 -0.5 0 0.5 1 1.5 2 2.5 -0.5 0 0.5 1 1.5 2 Measured vertical force, kN Predictedverticalforce,kN 1:1 +50% -50% After: Godwin and O’Dogherty, 2003 Average error + 33% VerticalVertical Predicted v measured tinePredicted v measured tine and disc forcesand disc forces
  • 39. 0 1 2 3 4 5 6 0 1 2 3 4 5 Total Measured Force (kN) TotalPredictedForce(kN) -20% +20% 1:1 125 mm 225 mm Laboratory studies : Sandy loam soilLaboratory studies : Sandy loam soil Predicted v measured plough draught forcesPredicted v measured plough draught forces After : Balafoutis,2003
  • 40. 0 2 4 6 8 10 12 0 1 2 3 4 5 6 7 8 Total Measured Force (kN) TotalPredictedForce(kN) 1:1 +20% +20% 180 mm 225 mm Predicted v measured plough draught forcesPredicted v measured plough draught forces Field studies : Sandy clay soilField studies : Sandy clay soil After : Balafoutis,2003
  • 41. ConclusionsConclusions The general soil mechanics equation has been developed to enable the draught and vertical forces to be calculated for a wide range of implements. The use of the equations has: 1. predicted the magnitude of the horizontal soil force with an average error of -3%, with the majority of comparisons within ±20%, 2. predicted the magnitude of the vertical soil force with an average error of +33%, with the majority of comparisons within ±50%, and 3. provided a good basis for designers of cultivation equipment for optimal design of cultivating tools. The spreadsheet model will be freely available.
  • 42. AcknowledgementsAcknowledgements Gordon Spoor,Gordon Spoor, Tony Reynolds,Tony Reynolds, DanDan HettiaratchiHettiaratchi andand The DouglasThe Douglas BomfordBomford TrustTrust