Lecture 23 (Friday, March 15, 2002): Soils II
Brief outline of this lecture:
Soil development through time
Soils around the world
Soil fertillity and fertilization
Soils in Georgia
Paleosols
Main points of this lecture:
Soils take a log time to develop.
Soil horizons vary with climatic and vegetative setting
Soil mineralogy varies with climatic and vegetative setting.
Soil fertility varies with climate and parent material.
Georgia's soils differ with different parent material and have lost much of their A horizon.
Ancient soils (paleosols) can be preserved where buried under later layers of sedimentary or volcanic rock.
Figures used in this lecture:
Differences in soils across climate zones
Soil fertility in different settings
Soil development through time
Soils in Georgia
Elements used in fertilizers
Paleosols - ancient soils
The soil map shown comes from the US Department of Agriculture.
Reading assignment: pp. 253-268.
Next Lecture
Email to Railsback (rlsbk@gly.uga.edu)
Railsback's main 1121 web page
Railsback's main web page
UGA Geology Department web page