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Sjoerd W. Duiker, PhD, CCA
DEALING WITH POOR SOIL STRUCTURE
AND SOIL COMPACTION
Causes of Soil Compaction
• Tillage compaction
– Moldboard
– Reduced tillage tools
• Compaction by heavy
equipment traffic
– Surface > 35 psi
– Subsoil >10 ton/axle
• Animal trampling
Tillage Compaction
Most
Less
Least
Tillage compaction on dairy farms in
southeast Pennsylvania using chisel plow
Source: Penn State Study
Compaction by Heavy Farm Equipment
Soil Compaction by Animals
Source: Soil Types and Structures Module, DEPI Victoria
Workability
&
trafficability

Germination
and root
growth 
Pests and
diseases 
Runoff 
Nutrient and
water uptake

Effects of
Compaction
Compaction Effects on
Emergence
Young seedlings will
have trouble emerging
Increased likelihood of
seedling disease and
pest attacks
Compaction Restricts Root Growth
Compaction Restricts Nutrient
Uptake
• P and K –
relatively
immobile
nutrients in the
soil
• Restricted root
system limits
uptake
Compaction Restricts Nutrient
Uptake and Increases Losses
Increased nitrogen losses
due to denitrification,
ammonia volatilization,
reduced infiltration
N-rate (lbs / A)
0 50 100 150
Drymatteryield(tons/A)
0.0
0.5
1.0
1.5
2.0
2.5
3.0
1.30
1.55
bulk density (g / cm3)
Twice N-rate needed to get same yield in compacted soil!
Compaction Limits Plant Growth
• Due to restricted
emergence and root
growth
Compacted with 30-ton truck w. road tires
in spring (10 ton axle load), chisel plowed
Compacted Control
Note drought-stressed
corn
Compaction Increases Runoff
• Due to decreased
macroporosity and
soil structure
destruction
Understand causes of surface vs subsoil compaction
Understand how continuous no-till impacts
soil resilience to compaction
Long-
Term
No-Till
2 yrs old
No-Till
1 yr old
No-Till
Strip-Till
% water
Bulk
density
(g/cm3)
1.65
1.40 No-Till – high OM
Conventional Till – low OM
Top 5 cm, proctor, Thomas et al., 1996
Continuous No-Till Increases
Soil Resistance to Compaction
Soil Structure – ‘Ped’ scale
The arrangement of sand, silt, and clay particles to form larger
aggregates or peds.
• Macropores (large pores) between
aggregates are filled with air in a
moist soil (>0.003 in)
• Mesopores (intermediate pores) are
filled with water in a moist soil and
with air in a dry soil (0.001 – 0.003
in).
• Micropores (very small pores)
between particles that make up soil
aggregates are filled with water in
all but the driest soil (<0.001 in).1/10 inch
Undesirable Desirable
Depth(“)
0
2
4
6
8
10
12
14
16
18
20
22
24
Plow pan,
Massive,
platy
structure
Crust - platy
Pulverized
soil
aggregates
Crop
Residue
High OM,
crumb
Platy
structure
(not desired)
Bio pores
Firm, blocky
Aggregates
Middens
Soil Structure – Profile Scale
Organic matter decreases bulk density
Hudson, B.D. 1994. Soil organic matter and available water capacity. J. Soil& Water Cons 49:189-194.
SOM
(wt %)
Bulk
Density
(g cm-3)
0 1.56
1 1.50
2 1.44
3 1.38
4 1.32
5 1.26
Texture = silt loam
0
5
10
15
20
25
30
35
Jan Feb Mar Apr May Jun Jul Aug Sep Oct Nov Dec
Trafficabledays(#/month)
Well-structured pasture without
plow-pan
Arable land with plowpan
Continuous No-Till Decreases the
Risks of Soil Compaction
Long-term undisturbed soil with active root system has good trafficability
Yield decrease due to Compaction
in continuous no-till
27%
14%
10%
Wet summersDry summer
Compaction every spring
when soil was wet with 30 T
manure truck, road tires.
Several passes to cover
every square inch of field
Compaction Study in No-Till
Benefit of flotation tires
600 Bu. 20 tons/axle
Covering the plot twice
The benefits of subsoiling tend to
be less on continuous no-till –
lessons from NW Ohio
Corn-soybean rotation w/o cover crop. Ohio State Study on Hoytville silty clay loam, tile drained. Study was started
in 1987 – chisel plowing until 2002, then converted to no-till. Compaction (2 times repeated, every inch) was done
with 600 bu graincart. Subsoiling done annually with low-disturbance subsoiler after compaction treatment.
Compaction Compaction Compaction
1.35
1.4
1.45
1.5
1.55
1.6
1.65
w/o Rye with Rye
Early
Late
a a a
b
0-4” depth
Rye effect on bulk density (g/cm3)
in following corn crop in July
Early = early killed cover crop
Late = late killed cover crop
With Rye w/o Rye
Both samples under manure spreader tracks on dairy farm operation
Make Soil Resist Compaction Better with Cover Crops
Alfalfa roots – taproots penetrate subsoil
Annual Ryegrass established in
standing corn with interseeder
Make Soil Resist Compaction Better with Cover Crops
and Perennial Deep-Rooted Crops in Rotation
Canola roots
penetrate plow pan
in winter when soil
is soft
Soybean roots
follow root
channels created by
canola
Williams and Weil, 2004
Repair Compaction with Cover Crops
Alleviate Compaction using Living
Root System 24/7/365
16” deep after 40 days
Courtesy Randall Reeder, OSU
‘Zone-till’ using cover crop
mixtures – radish and legume
Cover crop roots to alleviate compaction
1st
year
2nd
year
High Compaction Medium Compaction No Compaction
Tap-rooted species seem to be more effective to alleviate
compaction
• less friction with soil
* Less ‘buckling’
Chen, G., and R.R. Weil. 2010. Penetration of cover crop roots through compacted soil. Plant Soil 331:31-43.
Alleviate Compaction by Stimulating
Biological Activity
Worm holes covered with
organic matter
Feed the soil and it will feed you!
Nightcrawler burrow
Fresh Cast
Removed midden
Conclusions
• Soil Structure critical for
healthy soil
• Soil compaction avoidance is
key – respect soil moisture,
reduce axle load and contact
pressure
• Soil compaction – work with
nature to increase SOM
content, improve soil structure
and stimulate biological
activity, through no-till,
permanent living root system,
deep-rooted crops
• Soil compaction – use tillage
only as a help to let nature
Additional Resources
Penn State Fact sheets :
• Avoiding Soil Compaction
• Effects of Soil Compaction
• Diagnosing Soil Compaction using a Penetrometer
• Quick & Easy Worksheet for Assessing Traffic-Induced Soil Compaction Risk
• And more …….

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Dr. Sjoerd Duiker - Dealing with Poor Soil Structure and Soil Compaction

  • 1. Sjoerd W. Duiker, PhD, CCA DEALING WITH POOR SOIL STRUCTURE AND SOIL COMPACTION
  • 2. Causes of Soil Compaction • Tillage compaction – Moldboard – Reduced tillage tools • Compaction by heavy equipment traffic – Surface > 35 psi – Subsoil >10 ton/axle • Animal trampling
  • 4. Tillage compaction on dairy farms in southeast Pennsylvania using chisel plow Source: Penn State Study
  • 5. Compaction by Heavy Farm Equipment
  • 6. Soil Compaction by Animals Source: Soil Types and Structures Module, DEPI Victoria
  • 7. Workability & trafficability  Germination and root growth  Pests and diseases  Runoff  Nutrient and water uptake  Effects of Compaction
  • 8. Compaction Effects on Emergence Young seedlings will have trouble emerging Increased likelihood of seedling disease and pest attacks
  • 10. Compaction Restricts Nutrient Uptake • P and K – relatively immobile nutrients in the soil • Restricted root system limits uptake
  • 11. Compaction Restricts Nutrient Uptake and Increases Losses Increased nitrogen losses due to denitrification, ammonia volatilization, reduced infiltration N-rate (lbs / A) 0 50 100 150 Drymatteryield(tons/A) 0.0 0.5 1.0 1.5 2.0 2.5 3.0 1.30 1.55 bulk density (g / cm3) Twice N-rate needed to get same yield in compacted soil!
  • 12. Compaction Limits Plant Growth • Due to restricted emergence and root growth Compacted with 30-ton truck w. road tires in spring (10 ton axle load), chisel plowed Compacted Control Note drought-stressed corn
  • 13. Compaction Increases Runoff • Due to decreased macroporosity and soil structure destruction
  • 14. Understand causes of surface vs subsoil compaction
  • 15. Understand how continuous no-till impacts soil resilience to compaction Long- Term No-Till 2 yrs old No-Till 1 yr old No-Till Strip-Till
  • 16. % water Bulk density (g/cm3) 1.65 1.40 No-Till – high OM Conventional Till – low OM Top 5 cm, proctor, Thomas et al., 1996 Continuous No-Till Increases Soil Resistance to Compaction
  • 17. Soil Structure – ‘Ped’ scale The arrangement of sand, silt, and clay particles to form larger aggregates or peds. • Macropores (large pores) between aggregates are filled with air in a moist soil (>0.003 in) • Mesopores (intermediate pores) are filled with water in a moist soil and with air in a dry soil (0.001 – 0.003 in). • Micropores (very small pores) between particles that make up soil aggregates are filled with water in all but the driest soil (<0.001 in).1/10 inch
  • 18. Undesirable Desirable Depth(“) 0 2 4 6 8 10 12 14 16 18 20 22 24 Plow pan, Massive, platy structure Crust - platy Pulverized soil aggregates Crop Residue High OM, crumb Platy structure (not desired) Bio pores Firm, blocky Aggregates Middens Soil Structure – Profile Scale
  • 19. Organic matter decreases bulk density Hudson, B.D. 1994. Soil organic matter and available water capacity. J. Soil& Water Cons 49:189-194. SOM (wt %) Bulk Density (g cm-3) 0 1.56 1 1.50 2 1.44 3 1.38 4 1.32 5 1.26 Texture = silt loam
  • 20. 0 5 10 15 20 25 30 35 Jan Feb Mar Apr May Jun Jul Aug Sep Oct Nov Dec Trafficabledays(#/month) Well-structured pasture without plow-pan Arable land with plowpan Continuous No-Till Decreases the Risks of Soil Compaction Long-term undisturbed soil with active root system has good trafficability
  • 21. Yield decrease due to Compaction in continuous no-till 27% 14% 10% Wet summersDry summer Compaction every spring when soil was wet with 30 T manure truck, road tires. Several passes to cover every square inch of field
  • 22. Compaction Study in No-Till Benefit of flotation tires
  • 23.
  • 24. 600 Bu. 20 tons/axle Covering the plot twice The benefits of subsoiling tend to be less on continuous no-till – lessons from NW Ohio
  • 25. Corn-soybean rotation w/o cover crop. Ohio State Study on Hoytville silty clay loam, tile drained. Study was started in 1987 – chisel plowing until 2002, then converted to no-till. Compaction (2 times repeated, every inch) was done with 600 bu graincart. Subsoiling done annually with low-disturbance subsoiler after compaction treatment. Compaction Compaction Compaction
  • 26. 1.35 1.4 1.45 1.5 1.55 1.6 1.65 w/o Rye with Rye Early Late a a a b 0-4” depth Rye effect on bulk density (g/cm3) in following corn crop in July Early = early killed cover crop Late = late killed cover crop With Rye w/o Rye Both samples under manure spreader tracks on dairy farm operation Make Soil Resist Compaction Better with Cover Crops
  • 27. Alfalfa roots – taproots penetrate subsoil Annual Ryegrass established in standing corn with interseeder Make Soil Resist Compaction Better with Cover Crops and Perennial Deep-Rooted Crops in Rotation
  • 28. Canola roots penetrate plow pan in winter when soil is soft Soybean roots follow root channels created by canola Williams and Weil, 2004 Repair Compaction with Cover Crops
  • 29. Alleviate Compaction using Living Root System 24/7/365 16” deep after 40 days Courtesy Randall Reeder, OSU ‘Zone-till’ using cover crop mixtures – radish and legume
  • 30. Cover crop roots to alleviate compaction 1st year 2nd year High Compaction Medium Compaction No Compaction Tap-rooted species seem to be more effective to alleviate compaction • less friction with soil * Less ‘buckling’ Chen, G., and R.R. Weil. 2010. Penetration of cover crop roots through compacted soil. Plant Soil 331:31-43.
  • 31. Alleviate Compaction by Stimulating Biological Activity Worm holes covered with organic matter Feed the soil and it will feed you!
  • 33. Conclusions • Soil Structure critical for healthy soil • Soil compaction avoidance is key – respect soil moisture, reduce axle load and contact pressure • Soil compaction – work with nature to increase SOM content, improve soil structure and stimulate biological activity, through no-till, permanent living root system, deep-rooted crops • Soil compaction – use tillage only as a help to let nature
  • 34. Additional Resources Penn State Fact sheets : • Avoiding Soil Compaction • Effects of Soil Compaction • Diagnosing Soil Compaction using a Penetrometer • Quick & Easy Worksheet for Assessing Traffic-Induced Soil Compaction Risk • And more …….