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SOIL – Your Very Important
Natural Resource
Ross H. McKenzie
McKenzie Ag Consulting
KEPA Conference
Taking Care of the Land
Standoff, AB
Nov 20, 2014
Outline:
• Introduction to Soil
• Soils – How soils have formed and developed
• Discuss important soil and land conservation
issues
• Provide my thoughts and comments
How many soil
micro-organisms
are in a handful
of fertile soil?
Soil is alive
and teeming
with life!
More than
1,000,000,000
Soils have developed as a result of various
soil forming factors :
1. Parent Geologic Material:
2. Climate:
3. Vegetation:
4. Topography:
5. Drainage:
Northern Great Plains – 10,000 years ago!
After that last glacial period – the Prairie landscape
was transformed leaving behind varying types of
parent material and topography.
Glacial
Ice Sheet
Hummocky
Moraine
Ground
Moraine
Outwash
Fluvial
Lacustrine
(Loam-CL)
Lacustrine
(Clay)
Melt Water
Fluvial
LS-SL
Types of Soil Parent Material
Types of Soil Parent Material
1. Glacial Till Deposits
2. Outwash (Gravel and sand deposits)
3. Fluvial (stream deposited; moving water).
4. Lacustrine (Glacial lakes; fine sediments)
5. Fluvial-Lacustrine (slow moving water)
6. Aeolian (Loess) (Wind deposited)
Dark Gray & Gray
Luvisolic Soils in North
Central & Northern AB
Brown Soils in
SE Alberta
Black Soils in
Central Alberta
Dark Brown
Soils in Southern
Central Alberta
Major Zonal Soil or Agro-Ecological Areas of Alberta
Black Soils
Dark Brown Soils
Major Soil Zones of Alberta
Major Agro-ecological Areas
on the Blood Reserve
• F1 - Dark Brown soil,
slopes <5%, medium to
fine texture with 2A
climate class
• J1- Black soil, slopes
<5%, medium to fine
soil texture with 2AH
climatic class
• J3- Black soil, slopes 5 to
15%,medium to fine soil
texture with 4H to 5H
climatic class
My Comment #1.
• Soils on the Blood Reserve have formed and
developed over the past 10,000 years
–Dark Brown soils – in the Northern portion
of the reserve
–Thin Black soils – in the Central & Southern
portion of the reserve
Soil Survey in Alberta
• Initiated in the early 1920’s
with the Report #1 published in
1925 of the Ft MacLeod Sheet by
Wyatt and Newton
• The last report, #56 was
published in 1996 of the
Gleichen Sheet by Walker and
Pettapiece
AGRASID
Agricultural Region of Alberta Soil Inventory
DatabaseAGRICULTURE,FOODAND
RURALDEVELOPMENT
ConservationandDevelopmentBranch
Alberta Land Resource Unit
http://www.agric.gov.ab.ca/asic
Example of Soil Survey Info
Comment #2
• Forward thinking soil scientists ensured that
soil survey’s were conducted across Alberta
including the Blood Reserve.
• Soil classification information is readily
available via the internet using AGRASID!
Agricultural Land Suitability Rating
-Spring seeded small grains
Classification Limitations to Cropping
1 None to slight
2 Slight
3 Moderate
4 Severe
5 Very severe
6 Extremely severe
7 Not suitable
Question:
How much Class 1 Agricultural
land is:
-On the Blood Reserve?
-In Alberta?
Class 1 – No to slight soil or climatic
limitations for agriculture
Comment #3:
• NONE - on the Blood Reserve!!
• NONE - in Alberta!!
• Alberta does not have any “Class 1 Land”
for annual crop production!
Class 2: 478,000 ha
Comment #4
• Much of the land on the Blood Reserve is
Class 2 and 3 which is suitable for annual
crop production!
• Limitations:
–Limited precipitation – more frequently in
the northern part of the reserve.
–Shorter growing season – more frequently
a concern in the southwestern part of the
reserve.
First Nations People
• Lived in harmony with the land for +10,000 years.
• Fur traders began venturing into the western
prairies in the late 1700’s
• By the 1870’s the native way of life was changing
dramatically – the land and the landscape was
undergoing major changes!
Land Development
1880 to 1900
Cattle ranching &
grazing dominated the
landscape
1900 to 1920
Dramatic Shift – to land breaking
& cultivated agriculture
dominated the landscape
Wheat-Summerfallow Rotation
Land was seeded to
spring wheat and
fallowed every other
year.
The land was left bare
and cultivated to kill
weeds and store
moisture!
Cropping System
Wheat - Fallow
• Advantages
–Land was left in fallow every second year
–Store moisture for the next crop year
–Used for weed control
• Disadvantages
–No protective soil cover
–Land prone to soil erosion
–Decreased organic matter
–Increased salinity
Soil cultivation + summerfallow
led to severe wind erosion by
the dry 1930’s
Wind Erosion - Impacts
• Wind erosion physically removed the most fertile part of
the soil - the lighter, less dense soil:
– organic matter
– clays
– silts which lowered the soil productivity
• Wind erosion:
– Reduced soil productivity
– Reduced crop yields
– Reduced economic returns.
Wind erosion:
–Major topsoil losses in the 1930’s, 60’s and to
a lesser extent in 80’s
Effects of Cropping and
Cultivation on Soil Quality
• Summerfallowed land was tilled 3 to 4 times -
–Combination of cultivation, oxygen and
moisture stimulated soil microbial activity
• Result: Soil Organic Matter decomposition by
microbes occurred-
–Organic Matter levels declined by about
40% in first 40 years of cultivation.
Effect of Wheat Fallow on Crop Production
Comment #5:
Wheat-Fallow cropping system and cultivation
resulted in: Serious Soil Degradation on the
Blood Reserve and millions of acres across the
Northern Great Plains Region!
Dryland Agriculture
• Wheat-Fallow system was not sustainable
–Million acres of land were seriously eroded
• For farming to be sustainable - New ways of
farming had to be developed
–Researchers and innovative farmers took on the
challenge!
Soil Management
A. E. Palmer (1888-1984) “Trash Cover Palmer”
• 1921–1953 at Lethbridge Experimental Station
• Made great efforts to address the soil drifting crisis in
the 1930’s
• Collaborate with innovative farmers, such as Charles
Noble, to develop new practices such as strip farming
and sub-tillage
• Undertook technology transfer to farmers – that was
against Ottawa’s directives
• Strong advocate for conservation tillage
Soil Conservation
Charles Noble (1873-1957) - Farmer
• Concerned with dryland farming problems.
• Developed the Noble Blade, a cultivator that cut off
roots below ground, leaving the soil-holding "trash"
intact on the surface.
• He tested and began producing the cultivators in 1936
– by 1940 a manufacturing shop was set up in
Nobleford.
Comment #6
Forward thinking scientists and
farmers led the way to strip
farming and “trash cover” farming
to conserve the soil in the 1940’s
and 1950’s !
Effects of cropping practices in
the past 100 yrs on the prairies.
Rotation A-B-C AAFC Lethbridge
• nnn
Long-term dry land crop rotation established in 1911
WF -CW-WWF rotation – 103 years old!
(Rotation A-B-C, Lethbridge - Janzen et al. 1986)
Lessons:
• Soil quality declined as a result of cultivation,
summerfallow and no fertilizer additions
• Lessons:
–Continuous cropping is best - minimize
summerfallow
–Soil nutrients must be replaced for farming
to be sustainable in the long-term
•Maintain good soil fertility with adequate
fertilization
Comment #7 - Long-term
studies are invaluable!
• Long term studies have shown that annual
cropping is best for the soil – summerfallow should
not be part of a crop rotation!
• Nutrients removed by crops must be replaced –
–When fertilizers are used – soil quality improves!
Advanced Soil Conservation Efforts
• Since the 1930’s agricultural scientists and
leading farmers have strived to develop and
adopt conservation tillage !
• Dr. Wayne Lindwall – led no-till cropping
research in the 1970’s into 1990’s at
Lethbridge
Direct Seeding Seedbed
Thatch Layer Stubble
Direct seeding is now common
- Land is only tilled at seeding
Result:
- Soil quality is improving
- Crop yields are higher
Zero till – Direct Seeding
• Widespread adoption began in the 1990’s as
equipment manufacturers developed and
improved seeding equipment.
–Seeding equipment
–Harvest – straw management
–Weed control
• Today – most of the dryland fields are direct
seeded on the Blood Reserve
Benefits of Conservation Tillage
• Soil organic matter levels have improved
• Soil structure has improved
• Increased soil fertility
• Residue cover has greatly reduced soil erosion
• More soil water is conserved for crop growth
• Summerfallow has been mostly eliminated
• Greater crop diversification
–Reduced production risk
–Increased farm income
–Improved soil health
Comment #8
Farmers have excelled at adoption of direct-
seeding technology which has led to improved
soil quality and crop productivity!
Blood Reserve
and lands
across Alberta
have significant
oil and gas
reserves!
Well sites – on north end of Reserve
Note – land fragmentation
Abandoned Wells
0
20,000
40,000
60,000
80,000
100,000
120,000
140,000
160,000
#
1905 1915 1925 1935 1945 1955 1965 1975 1985 1995 2005
1905
1915
1925
1935
1945
1955
1965
1975
1985
1995
2005
Area scale of actual to shown
dot features; 113:1
Area scale of actual to shown
linear features; 26:1
Source: Dr. B. Stelfox, 2005
Pipelines can affect soils and crop
production well into the future
Soil cannot be fully reclaimed to be as
productive as it was prior to disturbance.
Comment #9:
Should well sites and pipelines have greater
restrictions on the Blood Reserve on amount
of land that is disturbed?
Should drilling sites and pipelines have higher
land reclamation standards!
– presently companies reclaim back to 80%
of production potential!
Electrical transmission lines, windmills
and other developments permanently
occupy land and cause challenges!
Comment #10:
In the Future - consider have limitations on
transmission lines, windmill sites and other
industrial developments to preserve land
and protect very sensitive lands from
fragmentation and degradation?
Soil Salinity
-Soils that are affected by soluble salts
-Some saline areas occur naturally
-Expanding areas are caused by agricultural
practices
Saline Soils
A
Carmangay
Site
Comment #11
Soil salinity is an issue on the Blood
Reserve – cropping systems to control Soil
Salinity should be considered
Final Comments -
SOIL and LAND are essential to sustain human life and
provide economic sustainability to the people of the Blood
Reserve.
Final Comments:
• Work with agricultural land users to use sustainable crop
rotations and cropping practices to conserve your soil for
future generations.
• Carefully consider the long term effects of developments
including rural residences, roads, oil and gas wells,
pipelines, transmission lines, wind mills etc to protect
your land for future generations.
Questions ?
Ross H. McKenzie
Lethbridge, Alberta
Phone: 403-328-1001
rossmckenzie@shaw.ca

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SOIL – Your Very Important Natural Resource

  • 1. SOIL – Your Very Important Natural Resource Ross H. McKenzie McKenzie Ag Consulting KEPA Conference Taking Care of the Land Standoff, AB Nov 20, 2014
  • 2. Outline: • Introduction to Soil • Soils – How soils have formed and developed • Discuss important soil and land conservation issues • Provide my thoughts and comments
  • 3. How many soil micro-organisms are in a handful of fertile soil? Soil is alive and teeming with life! More than 1,000,000,000
  • 4. Soils have developed as a result of various soil forming factors : 1. Parent Geologic Material: 2. Climate: 3. Vegetation: 4. Topography: 5. Drainage:
  • 5. Northern Great Plains – 10,000 years ago! After that last glacial period – the Prairie landscape was transformed leaving behind varying types of parent material and topography.
  • 7. Types of Soil Parent Material 1. Glacial Till Deposits 2. Outwash (Gravel and sand deposits) 3. Fluvial (stream deposited; moving water). 4. Lacustrine (Glacial lakes; fine sediments) 5. Fluvial-Lacustrine (slow moving water) 6. Aeolian (Loess) (Wind deposited)
  • 8. Dark Gray & Gray Luvisolic Soils in North Central & Northern AB Brown Soils in SE Alberta Black Soils in Central Alberta Dark Brown Soils in Southern Central Alberta Major Zonal Soil or Agro-Ecological Areas of Alberta
  • 9. Black Soils Dark Brown Soils Major Soil Zones of Alberta
  • 10. Major Agro-ecological Areas on the Blood Reserve • F1 - Dark Brown soil, slopes <5%, medium to fine texture with 2A climate class • J1- Black soil, slopes <5%, medium to fine soil texture with 2AH climatic class • J3- Black soil, slopes 5 to 15%,medium to fine soil texture with 4H to 5H climatic class
  • 11. My Comment #1. • Soils on the Blood Reserve have formed and developed over the past 10,000 years –Dark Brown soils – in the Northern portion of the reserve –Thin Black soils – in the Central & Southern portion of the reserve
  • 12. Soil Survey in Alberta • Initiated in the early 1920’s with the Report #1 published in 1925 of the Ft MacLeod Sheet by Wyatt and Newton • The last report, #56 was published in 1996 of the Gleichen Sheet by Walker and Pettapiece
  • 13. AGRASID Agricultural Region of Alberta Soil Inventory DatabaseAGRICULTURE,FOODAND RURALDEVELOPMENT ConservationandDevelopmentBranch Alberta Land Resource Unit
  • 15. Example of Soil Survey Info
  • 16.
  • 17. Comment #2 • Forward thinking soil scientists ensured that soil survey’s were conducted across Alberta including the Blood Reserve. • Soil classification information is readily available via the internet using AGRASID!
  • 18. Agricultural Land Suitability Rating -Spring seeded small grains Classification Limitations to Cropping 1 None to slight 2 Slight 3 Moderate 4 Severe 5 Very severe 6 Extremely severe 7 Not suitable
  • 19. Question: How much Class 1 Agricultural land is: -On the Blood Reserve? -In Alberta? Class 1 – No to slight soil or climatic limitations for agriculture
  • 20. Comment #3: • NONE - on the Blood Reserve!! • NONE - in Alberta!! • Alberta does not have any “Class 1 Land” for annual crop production!
  • 21.
  • 23. Comment #4 • Much of the land on the Blood Reserve is Class 2 and 3 which is suitable for annual crop production! • Limitations: –Limited precipitation – more frequently in the northern part of the reserve. –Shorter growing season – more frequently a concern in the southwestern part of the reserve.
  • 24. First Nations People • Lived in harmony with the land for +10,000 years. • Fur traders began venturing into the western prairies in the late 1700’s • By the 1870’s the native way of life was changing dramatically – the land and the landscape was undergoing major changes!
  • 25. Land Development 1880 to 1900 Cattle ranching & grazing dominated the landscape 1900 to 1920 Dramatic Shift – to land breaking & cultivated agriculture dominated the landscape
  • 26. Wheat-Summerfallow Rotation Land was seeded to spring wheat and fallowed every other year. The land was left bare and cultivated to kill weeds and store moisture!
  • 27. Cropping System Wheat - Fallow • Advantages –Land was left in fallow every second year –Store moisture for the next crop year –Used for weed control • Disadvantages –No protective soil cover –Land prone to soil erosion –Decreased organic matter –Increased salinity
  • 28. Soil cultivation + summerfallow led to severe wind erosion by the dry 1930’s
  • 29. Wind Erosion - Impacts • Wind erosion physically removed the most fertile part of the soil - the lighter, less dense soil: – organic matter – clays – silts which lowered the soil productivity • Wind erosion: – Reduced soil productivity – Reduced crop yields – Reduced economic returns.
  • 30. Wind erosion: –Major topsoil losses in the 1930’s, 60’s and to a lesser extent in 80’s
  • 31. Effects of Cropping and Cultivation on Soil Quality • Summerfallowed land was tilled 3 to 4 times - –Combination of cultivation, oxygen and moisture stimulated soil microbial activity • Result: Soil Organic Matter decomposition by microbes occurred- –Organic Matter levels declined by about 40% in first 40 years of cultivation.
  • 32. Effect of Wheat Fallow on Crop Production
  • 33.
  • 34.
  • 35. Comment #5: Wheat-Fallow cropping system and cultivation resulted in: Serious Soil Degradation on the Blood Reserve and millions of acres across the Northern Great Plains Region!
  • 36. Dryland Agriculture • Wheat-Fallow system was not sustainable –Million acres of land were seriously eroded • For farming to be sustainable - New ways of farming had to be developed –Researchers and innovative farmers took on the challenge!
  • 37. Soil Management A. E. Palmer (1888-1984) “Trash Cover Palmer” • 1921–1953 at Lethbridge Experimental Station • Made great efforts to address the soil drifting crisis in the 1930’s • Collaborate with innovative farmers, such as Charles Noble, to develop new practices such as strip farming and sub-tillage • Undertook technology transfer to farmers – that was against Ottawa’s directives • Strong advocate for conservation tillage
  • 38. Soil Conservation Charles Noble (1873-1957) - Farmer • Concerned with dryland farming problems. • Developed the Noble Blade, a cultivator that cut off roots below ground, leaving the soil-holding "trash" intact on the surface. • He tested and began producing the cultivators in 1936 – by 1940 a manufacturing shop was set up in Nobleford.
  • 39. Comment #6 Forward thinking scientists and farmers led the way to strip farming and “trash cover” farming to conserve the soil in the 1940’s and 1950’s !
  • 40. Effects of cropping practices in the past 100 yrs on the prairies.
  • 41. Rotation A-B-C AAFC Lethbridge • nnn Long-term dry land crop rotation established in 1911 WF -CW-WWF rotation – 103 years old!
  • 42.
  • 43. (Rotation A-B-C, Lethbridge - Janzen et al. 1986)
  • 44. Lessons: • Soil quality declined as a result of cultivation, summerfallow and no fertilizer additions • Lessons: –Continuous cropping is best - minimize summerfallow –Soil nutrients must be replaced for farming to be sustainable in the long-term •Maintain good soil fertility with adequate fertilization
  • 45. Comment #7 - Long-term studies are invaluable! • Long term studies have shown that annual cropping is best for the soil – summerfallow should not be part of a crop rotation! • Nutrients removed by crops must be replaced – –When fertilizers are used – soil quality improves!
  • 46. Advanced Soil Conservation Efforts • Since the 1930’s agricultural scientists and leading farmers have strived to develop and adopt conservation tillage ! • Dr. Wayne Lindwall – led no-till cropping research in the 1970’s into 1990’s at Lethbridge
  • 47.
  • 49. Direct seeding is now common - Land is only tilled at seeding Result: - Soil quality is improving - Crop yields are higher
  • 50. Zero till – Direct Seeding • Widespread adoption began in the 1990’s as equipment manufacturers developed and improved seeding equipment. –Seeding equipment –Harvest – straw management –Weed control • Today – most of the dryland fields are direct seeded on the Blood Reserve
  • 51. Benefits of Conservation Tillage • Soil organic matter levels have improved • Soil structure has improved • Increased soil fertility • Residue cover has greatly reduced soil erosion • More soil water is conserved for crop growth • Summerfallow has been mostly eliminated • Greater crop diversification –Reduced production risk –Increased farm income –Improved soil health
  • 52. Comment #8 Farmers have excelled at adoption of direct- seeding technology which has led to improved soil quality and crop productivity!
  • 53. Blood Reserve and lands across Alberta have significant oil and gas reserves!
  • 54. Well sites – on north end of Reserve Note – land fragmentation
  • 55. Abandoned Wells 0 20,000 40,000 60,000 80,000 100,000 120,000 140,000 160,000 # 1905 1915 1925 1935 1945 1955 1965 1975 1985 1995 2005 1905 1915 1925 1935 1945 1955 1965 1975 1985 1995 2005 Area scale of actual to shown dot features; 113:1 Area scale of actual to shown linear features; 26:1 Source: Dr. B. Stelfox, 2005
  • 56. Pipelines can affect soils and crop production well into the future
  • 57. Soil cannot be fully reclaimed to be as productive as it was prior to disturbance.
  • 58. Comment #9: Should well sites and pipelines have greater restrictions on the Blood Reserve on amount of land that is disturbed? Should drilling sites and pipelines have higher land reclamation standards! – presently companies reclaim back to 80% of production potential!
  • 59. Electrical transmission lines, windmills and other developments permanently occupy land and cause challenges!
  • 60. Comment #10: In the Future - consider have limitations on transmission lines, windmill sites and other industrial developments to preserve land and protect very sensitive lands from fragmentation and degradation?
  • 61. Soil Salinity -Soils that are affected by soluble salts -Some saline areas occur naturally -Expanding areas are caused by agricultural practices
  • 63. A Carmangay Site Comment #11 Soil salinity is an issue on the Blood Reserve – cropping systems to control Soil Salinity should be considered
  • 64. Final Comments - SOIL and LAND are essential to sustain human life and provide economic sustainability to the people of the Blood Reserve. Final Comments: • Work with agricultural land users to use sustainable crop rotations and cropping practices to conserve your soil for future generations. • Carefully consider the long term effects of developments including rural residences, roads, oil and gas wells, pipelines, transmission lines, wind mills etc to protect your land for future generations.
  • 66. Ross H. McKenzie Lethbridge, Alberta Phone: 403-328-1001 rossmckenzie@shaw.ca