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01
Presentation on Soil Profile
Presented By
Md. Rasel Ali
Reg:AGRW2017000494
Faculty of
Agriculture
EBAUB
Soil Profile
02
Different Horizon in Soil Profile
03
⬥ Organic matter Horizon
⬥ Dark in color, soft in texture
⬥ Several O-layers can occur
in some soils, consisting O-
Horizon.
⬥ Humus
⬥ Leaf litter
04
O
Horizon
⬥ Top soil or Biomantle horizon,
mineral soil
⬥ Dark in color and 2-10 feet depts.
⬥ Smallest and finest soil particle.
05
A
Horizon
⬥ Leaching Layer
⬥ Small layer between A & B horizons
⬥ Light in color
⬥ Poor mineral and clay content due to
leaching
⬥ Soil particles larger than in A horizon but
smaller than in B horizon 06
E
Horizon
⬥ Some organic material may reach
here through leaching.
⬥ Plant roots can extend into this
layer.
⬥ At depths of 10-30 feet
⬥ Red/brown in color due to oxides
of Fe & clay
⬥ Rich in clay and minerals
07
B
Horizon
⬥ The “Regolith” Horizon
⬥ The soil layer lying beneath the B
horizon.
⬥ At depths of 30-48 feet
⬥ Rich in minerals that leached
(moved down) from the A or E
horizons and accumulated here.
08
C
Horizon
⬥ The “Bedrock” Horizon
⬥ Deepest soil horizon in the soil
profile.
⬥ At depths of 48+ feet
⬥ The layer of partially weathered or
unweathered bedrock at the base of
the soil profile.
9
R
Horizon
importance of soil profile
⬥ The soil profile is an important tool in nutrient management.
⬥ It helps to determine the best soil suitable for agriculture.
⬥ It identifies the part where plant nutrients can be found, that is
the top soil, is the richest part of the soil.
⬥ It also helps to determine the level in which water can be
available in the soil.
⬥ The nature of the parent material will also determine the type of
mineral salts available to plants.
10
Thank you for your
patience
ANY QUESTIONS?
11

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Presentation on soil profile

  • 1. 01 Presentation on Soil Profile Presented By Md. Rasel Ali Reg:AGRW2017000494 Faculty of Agriculture EBAUB
  • 3. Different Horizon in Soil Profile 03
  • 4. ⬥ Organic matter Horizon ⬥ Dark in color, soft in texture ⬥ Several O-layers can occur in some soils, consisting O- Horizon. ⬥ Humus ⬥ Leaf litter 04 O Horizon
  • 5. ⬥ Top soil or Biomantle horizon, mineral soil ⬥ Dark in color and 2-10 feet depts. ⬥ Smallest and finest soil particle. 05 A Horizon
  • 6. ⬥ Leaching Layer ⬥ Small layer between A & B horizons ⬥ Light in color ⬥ Poor mineral and clay content due to leaching ⬥ Soil particles larger than in A horizon but smaller than in B horizon 06 E Horizon
  • 7. ⬥ Some organic material may reach here through leaching. ⬥ Plant roots can extend into this layer. ⬥ At depths of 10-30 feet ⬥ Red/brown in color due to oxides of Fe & clay ⬥ Rich in clay and minerals 07 B Horizon
  • 8. ⬥ The “Regolith” Horizon ⬥ The soil layer lying beneath the B horizon. ⬥ At depths of 30-48 feet ⬥ Rich in minerals that leached (moved down) from the A or E horizons and accumulated here. 08 C Horizon
  • 9. ⬥ The “Bedrock” Horizon ⬥ Deepest soil horizon in the soil profile. ⬥ At depths of 48+ feet ⬥ The layer of partially weathered or unweathered bedrock at the base of the soil profile. 9 R Horizon
  • 10. importance of soil profile ⬥ The soil profile is an important tool in nutrient management. ⬥ It helps to determine the best soil suitable for agriculture. ⬥ It identifies the part where plant nutrients can be found, that is the top soil, is the richest part of the soil. ⬥ It also helps to determine the level in which water can be available in the soil. ⬥ The nature of the parent material will also determine the type of mineral salts available to plants. 10
  • 11. Thank you for your patience ANY QUESTIONS? 11