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Slides for Weathering and Soils | EAS 101, Study notes of Environmental Science

Material Type: Notes; Professor: Kirschner; Class: Earth's Dynamic Environment I; Subject: Earth & Atmospheric Sciences; University: Saint Louis University; Term: Unknown 1989;

Typology: Study notes

2009/2010

Uploaded on 02/24/2010

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Quote of Day
Never let the fear of striking out
get in your way.
(George "Babe" Ruth )
http://www.baberuth.com/
Babe Ruth led the American League in home runs 12 seasons ,
but he also struck out 16% of the time!
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Quote of Day

Never let the fear of striking out

get in your way.

George "Babe" Ruth

http://www.baberuth.com/

Babe Ruth led the American League in home runs 12 seasons ,

but he also struck out 16% of the time!

Chapter 6

Weathering and Soils

(from Brady and Weil “The Nature and Properties of Soils”

http://www.dailyweeder.com/wp-content/uploads/fertilizer.jpg

Factors controlling soil formation

  1. Parent material composition

Some soils create better soils than others; for example, granitic materialcreates good soils while quartz-dominated beach sands create thin, poor soils

controls rate of weathering / soil formation

influences chemistry of soil and soil moisture, and thus the type andabundance of plants (e.g., grapes) that can grow in the soil.

“terra rosa” soil developed from limestoneproduces excellent red wines on LimestoneCoast of South Australia

http://highbank.com.au/photogallery.html

Book on the importance of differentsoils in determining quality / kind ofwine produced in France.

http://images.amazon.com/images/P/1891267221.01.LZZZZZZZ.jpg

  1. Time

Amount of time for soil formation varies for differentsoils depending on geologic and climatic conditions

With really long times, soils generally become redderdue to relative increase in iron, contain more clays,have lower pH, and fewer nutrients (less fertile)

Average global rate of growth is ~1 cm/180 years

Info and photos from http://www.soils.agri.umn.edu/academics/classes/soil2125/doc/s2chap4.htm

Example

: Different age soils that developed

on sandy material adjacent to Lake Michigan

Layer leached of humus, iron,and enriched in CaCO

Layer enriched inhumus & iron

  1. Plants and animals

Influence the soil’s physical and chemical properties (e.g., amount ofhumus in soil)

  1. Topography

Steep slopes often have poorly developed soils

Optimum terrain is a flat-to-undulating upland surface

Poor environment for soil development

Good environment for soil development

Soil profile ¾

Soil forming processes operate fromthe surface downward

¾

Vertical differences are calledhorizons, zones, or layers of soil

O horizon – organic matte

r

A horizon – organic and mineralmatter

High biological activity

E horizon – little organic matter

Zone of eluviation (removalof fine particles) and leaching

B horizon – zone of accumulation

C horizon – partially alteredparent material

Unweathered parent material

Figure 6.

Soil erosion Natural rates of soil erosion depend on

Soil characteristics

Climate - high rainfall promotes erosion

Slope - steeper slopes have higher ratesof erosion

Type of vegetation

In many regions, soil erosion >> soil formation http://www.accessexcellence.org/BF/bf04/sarukhan/slides/saruk_img20.jpg

http://www.iqi.ru/indexes/Soil%20Erosion.jpg

Significant erosion of farmland

Deforestation

Subsequent erosion

http://www.geography.ndo.co.uk/images/forestloss1.gif

http://www.isd77.k12.mn.us/schools/dakota/dust.jpg http://www.mtnbrook.k12.al.us/tech/k6/dustbowl.gifhttp://www.sdcoe.k12.ca.us/score/dust/title.JPG

The “

dustbowl

” of the 1930’s caused great

hardship in the country and was due to 1) poor farming practices that encouragederosion of soil 2) drought conditions It’s effects were compound by the 1929 crashof the stock market and subsequent depression.

Good farming practice 1) contour plowing -

contours inhibit the flow of surface water downhill and thus

reduce the loss of soil downhill.

http://www.uwsp.edu/geo/faculty/ozsvath/images/contour%20plowing.jpg

http://extension.missouri.edu/explore/images/g01653art01.jpg

Good farming practice 3) Vegetative barriers –

densely planted, noncrop

vegetation in fields, along

fields, adjacent to roads and streams slow down water flow and thusinhibit soil loss off of the field.

In the field between corn rows

Along the edge of field

http://plantandsoil.unl.edu/croptechnology2005/UserFiles/Image/siteImages/P36LG.jpg

http://www.oh.nrcs.usda.gov/programs/Lake_Erie_Buffer/images/windbreak_hancock_co.jpg

Good farming practice 4) Windbreaks –

impede the flow of wind across the farm fields

and thus protect the soil from wind erosion.