NRSC 200: Fundamentals of Soil Science

Professor Ray R. Weil
 
 

Profiles:
Turf response to silt cap thickness in Bridgehampton soil
Soil bodies in plowed field, central Texas
Umbrept profile on outwash plain in central Italy
Udoll in central Iowa
Ustoll in central Montana
Krotovinas in northern Illinois Udoll
Argiaquoll in Texas (Addicks loam)
Spodosol near Iron Mt., MI (U.P.)
Humic cryorthod, Quebec (Crycambod?)
Udalf near Lamy, Chech Rep.
Tatum soil in Virginia Piedmont. Clayey mixed thermic Typic Hapludults
Notice in place development from underlying rock. This is a very acid,
aluminum toxic subsoil.
Pamuncky fine sandy loam from coastal plain of Virginia near Richmond
Well drained, red colors in B horizons, lighter E and darker A horizons
Plinthite mottles in substrata 20 km. N of Marion, AL.
Note segregation of oxidized and reduced iron resulting from fluctuating
water table and long period of intense weathering.
Plinthite mottles in subsoil of Plinthic Tropudult in central Sri Lanka.
Note similarites to #14.
Wall and house in Colombo, Sri Lanka made out of bricks fashioned from hardened plinthite or laterite. Locally called "Kabuk."
Slickensides in the subsoil of a Chromustert in the Sri Lankan dry zone
Vertisol profile from Malawi "Dambo" showing deep crack with granular surface soil falling in during dry season
Large cracks in surface of Vertisol in CA. Plants are alfalfa grown for seed.
Fraternidad soil of Puerto Rico showing the granular surface structure of this Vertisol.
Andisol profile in western Tanzania
Opequon clay loam, Lithic Hapludalf on limestone in MD.  Note shallow rock with solution channel.
Installation of a water pipe alongside a road exposes the different colors of the subsoils of members of the Lilongwe catena in East Africa.
Soil variation along a catena of soils in sandy sediments of the Altantic Coastal Plain.  Note the change in the thickness of the horizon and the red to gray transition in subsoil colors.

 
Agriculture and Tillage:
Cultivating to kill weeds in an Alabama soybean field. Note that the soybeans are wilting due to root pruning by the tillage sweep.
A Sri Lankan farmer with a traditional heavy tillage hoe
A farm tractor pulling a disk harrow and rolle for secondary tillage
Close-up of the disk on a disk harrow.  The angle can be adjusted to cause a deeper "bit" and more soil turning.
Close-up of a sub-smiler or chisel plow in action (movement is to the left).
Close-up of a three bottom moldboard plow in action. Note that the plow slices thick layer of soil and inverts it, shattering it into aggregates in the process.
Man walking behind a horse drawn "walking plow" of the moldboard type.  This type of plow was typical of the tillage implements used by American farmers between 1830 and 1930.  Many farmers in developing countries still use animal draft power in this way.
Heavy sheeps foot roller used to compact soil prior to building a road bed or foundation
Outlet for a perforated pipe under-drainage system. The series of perforated pipes connected to this one under the farm field lowers the water table by hastening the lateral movement of water to the ditch.
Close-up of a partial clogged drainage pipe resulting from placement without a filter stock and with the perforations facing upward.
A grappler skidder harvesting logs near Edson, Alberta.  Such equipment causes soil compaction that may reduce subsequent tree re-growth.
Foliar symptoms of salinity toxicity of soybean.  The cultivar was very susceptible to salinity and the EC of the saturated paste was 6.0 dS/m.
A hydrangea plant treated with iron sulfate on the right side and limestone on the left.  The year after treatment, the blossoms are blue in the acidified soil side and pink on the side with roots in limed soil.
Close-up of root nodules on soybean.  Note the red interior color of the large nodule that has been sliced in half. This red color indicates active nitrogen fixation.
Shifting cultivation or Chena farming in the dry zone of Sri Lanka.  Note the uneven distribution of ashes and scattered stumps allowed to remain.  The ashes contain most of the cations that were in the vegetation, and a good part of the anions as well (much N and S goes up in smoke).
A rose showing foliar symptoms of iron deficiency. Note the intereveinal chlorosis, almost white leaves, and the fact that the symptoms are far worse on the younger leaves.

 
Soil Structure:
Lamert-Ekalaka soil landscape in ND. Leptic and Typic Natriborolls.
Profile of Lamert-Ekalaka soils in ND. Leptic and Typic Natriborolls.
Columnar structure in Lamert-Ekalaka soils in ND. Leptic and Typic Natriborolls.
Vertical view of the top of a layer of columnar structure in Leptic and Typic Natriborolls.
Making a "ribbon" of soil to determine the clay content "by feel."
Granular structure worked by earthworms under forest floor of Ultisols.
Demonstration of structural water-stability of a Beltsville silt loam after 20 years of either Bluegrass or cultivated fallow.
Appearance of surface of saturated soil after drying showing the effect of organic matter changes during a 20 period of either cultivated fallow (low O.M.) or Bluegrass sod (high O.M.).
Blocky peds with illuvial clay coatings in the Bt horizon of a Ustalf near Kasungu, Malawi
Platy structure in a Hagerstown clay loam.
Strong angular blocky structure in B horizon of a Hapludult near Christiansburg, VA.
Clayey, montmorillonitic, isothermic, Vertic Tropaqualf. Dambo near Bunda, Malawi.  Note prismatic structure and sharp boundary between A and B horizons.  Also calcium carbonate concretions in lower part.

 
Soil Color:
Redoximorphic features in hydric soils. Oxidized root zone (reddish brown) with gley matrix (gray).
The 5YR page from a Munsell Color Book.
Effect of moisture on the color (especially value) of a Udoll soil profile in Iowa.
Black color of a Terric Medisaprist (Allemands series) near Paradis, LA.

 
Soil Genesis:
An example of rock weathering by exfoliation where layers of rock are peeling off. Big Bend, TX.
Glacial till over outwash in a soil profile in ND.
Dyke clay loam showing silt cap that may have been wind blown. VA piedmont.
Horizontally bedded sandstone in Virginia


Copyright © 1995-2000 University of Maryland, College Park.
All rights reserved.
Unauthorized reproductions are prohibited without expressed permission.
For permission contact (ey9@umail.umd.edu).

  Maintained by Technology Enhanced Learning, Office of Information Technology
 Direct questions and comments to Ellen Borkowski at ey9@umail.umd.edu

Last modified Wednesday, March 1, 2000.