Title: ESPM 120 Soil Characteristics
1ESPM 120Soil Characteristics
2Today
- Syllabus and expectations
- Soils and Berkeley and You
- Mini field trip (to Hilgard Hall)
3Syllabus and expectations main points
- Schedule subject to change
- Basic weekly structure
- Ask questions, be excited
- Respect each other
- Have fun
4Soils and Berkeley and You
- How are the following related to soil?
- Pizza
- Don Edwards Wildlife Refuge
- http//www.fws.gov/desfbay/habitats.htm
- Your house/apartment
5History of Pedology
- mid 19th Century no scientific study of soils
- Soil science followed closely behind development
of geology (early 19th century) and biology
(Origin of Species).
- Two key contributors to development of Pedology
- Vasili Dokuchaev (Russian geographer/mineralogist)
- Eugene Hilgard (American geologist/chemist)
6Eugene Hilgard and Soil Science at Berkeley
- Born in Germany
- Raised in American frontier (Illinois) in
intellectually oriented family
- Received PhD at University of Heidelberg
- Agricultural chemistry and geology
- Accepted position as Assistant State Geology of
Mississippi in 1855
7Hilgard in Mississippi
- Not a glamorous job
- Recognized his future with state lie not with
geology but agriculture and soils
- Produced a landmark document (next slide) with
half geology and half soils
8The Mississippi Report
- Detailed discussion of soil formation and soil
chemistry
- soil map of state.
9Hilgards Agricultural Map
- Analogous to modern generalized soil map
- Map units based on geology and vegetation
10Hilgard Moves to California
- Recruited by UC president in 1874
- Replaced first chair of agriculture (who was
fired)
11Berkeley when Hilgard arrived.
- Despite cultural isolation Hilgard seized
opportunity to expand College of Agriculture (now
CNR) and make soils a national issue
12Hilgard and John Wesley Powell (USGS)
- Prodded JW Powell to start a national soil survey
program (later adopted by USDA)
13Hilgard and his legacy.
- Mountains, lakes, streets, buildings, journals
are all named after Hilgard
- His influence was international, inspiring the
next generation of scientists, particularly Hans
Jenny
14Hans Jenny and Soil Formation
- Soils form predictably in response to
environmental factors (Dokuchaev 1880)
- Hans Jenny (1920s to 1930s) transformed
conceptual model to a more quantitative theory
following tenets of physical chemistry
15State Factor Equation
- Soil f (initial conditions, external
conditions, time)
- or, based on field observation
Soils f (climate, biota, topography, parent
material, time, . )
16Key Concepts of State Factor Theory
- Factors are independent of system
- System is small relative to surroundings
- A change in variables defines a new system
- there are essentially an infinite number of soils
17Mini Field Trip
18http//soils.usda.gov/technical/classification/osd
/index.html
19San Joaquin Series
- Extent map
- Typical pedon
- Natural vegetation
20Next Time
- Chapter 1
- Handout
- Study questions