Plant & Soil Sciences eLibraryPRO
Loading
control panel control panel
 

Soil Genesis and Development, Lesson 4 - Soil Profile Development

Rate Me

4.4 - Soil Horizon Development Over Time

Because of the diversity of landscapes and controlling variables of soil formationsuch as glaciations, flooding, erosion, and tectonicssoil horizons are often found in multiple combinations of vertical arrangement. To simplify the concept, consider a landscape where a river has deposited several meters of silty, gray, limestone-rich sediments (alluvium).  At this stage, the profile would be C; since no soil forming processes have occurred yet, it is not yet a soil.  The annual precipitation at this location is 75 to 100 cm (30 to 40 inches).  The climate is temperate with warm summers and cool winters.  Over geologic time these sediments develop a soil profile:
 

  • 050 years: Plants (grasses and forbs) begin to establish on the surface.  Plant growth is good, roots proliferate below ground and senesced plant material falls to the surface in the fall.  Worms, ants, beetles, and other organisms break these leaves into smaller pieces and mix them in the upper layers of the soil.  A thin, dark A horizon begins to form (addition) over the existing C horizon.  Profile horizons are A-C.
  • 50500 years: The plants continue to grow, and the A horizon becomes thicker (addition).  The silty sediments contain calcium carbonate, CaCO3, which is easily dissolved in the temperate, humid environment.  The CaCO3 begins to leach out of the upper part of the soil and move deeper as rain and snowmelt move down through the soil (translocation). Some of the CaCO3 moves all the way through the soil profile and into the groundwater (loss).  Some of the iron in the sediments begins to oxidize (rust) and the soil starts to turn from gray to yellow.  This is the formation of a weak B horizon.  Profile horizons are A-B-C.
  • 5005,000 years: The A horizon has stabilized and is fairly thick and dark for this soil. High productivity and lots of biotic activity continually recycle the organic matter. The original minerals in the soil begin to weather and form new clay minerals.  This clay is moved by water flowing downward through the soil from the A horizon and accumulates in the B horizon (translocation).  New clay minerals precipitate from minerals dissolved in the soil water thickening the B horizon and increasing its clay content (transformation).  The depth to the C horizon increases as the combined thickness of the A and B horizons increases.  Profile horizons are A-B-C.
  • 5,00050,000: The above sequence of events continues. Most of the CaCO3 is leached out of the soil or is very deep in the C horizon (loss). The continued accumulation of clay thickens and makes the B horizon more dense (transformation, translocation). Viewing the C horizon requires a lot of digging.
  • 50,000500,000: The A horizon has been continually mixed by the plants and animals, possibly even a plow. But it is still thick and dark and weathering. Below where the organic matter makes the soil dark, iron, clay and other soil pigments have been stripped away; a lighter, coarser textured E horizon may become evident. The clay and iron from the A and E horizons have moved downward and accumulated in a very thick, very dense B horizon. To reach the C horizon, a backhoe is needed. Profile horizons are A-E-B-C.
  • Then, one day, a very large sheet of ice, a glacier, comes out of the cold north, and scrapes the weathered glacial till away, creating a blank slate for a new soil to form when things warm up again.

The following questions build on the ideas of soil profile development in this lesson and also the soil forming factors of Lesson 3.

 

 
Question 11:  A soil is developing in the Southeastern United States, on a geologically old, forested landscape, the temperatures are warm, and precipitation plentiful but the soil is well drained. Which of the following soil profile arrangements will best fit this scenario?

      A.   O, A, C
      B.   O, A, B, C
      C.   A, R
      D.   O, R


 
Question 12:  This soil is developing in an active floodplain in central China. The silty alluvial soils are somewhat poorly drained and the climate is on the cool side. The vegetative cover is grasses and other small forbs. Which of the following is the most likely horizon scenario?

        A.   O, R
        B.   A, B, C
        C.   A, E, B, C, R
        D.   A, C
       


 

Comments

Be the first to write a comment...

Control Panel cancel

Create activities for your moodle courses. Moodle Go to moodle
Select and group e-Library Lessons to create your own package... My Communities
Community Blogs Community Media

My Joined Communities

 
My Blogs - a journal of my thoughts... My Blogs
 
My Comments - my thoughts expressed as a feedback... My Comments
 
Classes that I am taking Registered Classes
Class Blogs Class Media
 
Check the scores of assesments that you have taken Taken Assessments
 
clear
Please confirm your selection.