AUENV 233 Lecture Notes - Lecture 1: Hydrosphere, Colluvium, Lithosphere

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Soil Science Notes
Lecture 1 AUENV 233
Soil natural body made up of
definition is broad
o Solids minerals, organic matter
o Liquid
o Gas
That occurs on the land surface, occupies space, and is characterized by one or both of the
following:
o Ability to support rooted plants in a natural env
o Horizons, layers, that are distinguishable from the initial material as a result of:
Additions, losses, transfers, and transformations of energy and matter
Esker sand left behind from a glacier
o Is a soil because it can house plant roots, but has no horizons
6 Critical soil functions
1.) Home for plant growth
habitat for plant roots,
air and water,
nutrients
soil properties that determine nature of vegetation
indirectly impact the number and type of animals that can be supported PEOPLE 10% of
the land on earth is capable of food production
2.) Regulation of water supplies
every drop of water has travelled through or over soil at one point
storage and flow regulation can prevent floods [vegetation]
i. eg mud slides are a result of forest fires. No veg to soak up water.
Purification cleans the water
3.) Recycling of raw materials
Decomposition of materials
Creation of soil matter
Nutrient re-release converts from unusable forms [dead body] into more accessible forms
[nutrients C, N, P]
4.) Fosters unimaginable biodiversity
Ecosystem unto itself
Handful of soil = billions of organisms
5.) Influence the atmosphere composition
Storage and release of gases such as CO2
Key role in C cycle
i. 3rd largest pool on Earth! [next to ocean, rocks/parent material]
ii. can act as a sink or source [organisms within breathing]
management intensity has an influence. Eg - tilling can release C
dust storms large scale transfer
6.) Engineer medium
Can live in it build out of it
i. Eg - Rammed earth construction good insulation
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(-) can cause buildings to collapse. eg earthquakes. Geotechnical engineers.
History of soil science very young science not more than 150 yrs
*dot need to know names/dates
1870s V. V. Dokuchaev father of soil siee Russia
o soils = natural bodies
1920s CF Marbut
o US department of Ag
o Soil profiling & soil mapping
1940 Hans Jenny
o quantitative analysis math formula to predict soil form
o soil = fCl, O, R, P, T… none act independently.
1960 Guy Smith redid soil class sys
Influences on soil
war
crime
food
climate change
cities
Soils and Scales
Spheres [scales]
soil eists at eer sale
1.) atmosphere
2.) biosphere
3.) lithosphere
4.) hydrosphere
Geographical context
soils = otiuous ut proide otiuall arig oer oer the earth’s lad surfae
soil properties vary over spatial [vertical, horizontal] & temporal scales
o chemical, biological, physical
Looking at soil
upper boundary of soil boundary between:
o air
o shallow water
o live plants
o or plant materials that have begun to decompose
lower boundary of soil ofte diffiult to defie…
o parent material and bedrock interface
Vertical Variations
podzol
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Document Summary

Lecture 1 auenv 233: soil natural body made up of definition is broad, solids minerals, organic matter, liquid, gas. Is a soil because it can house plant roots, but has no horizons. Regulation of water supplies: every drop of water has travelled through or over soil at one point storage and flow regulation can prevent floods [vegetation, eg mud slides are a result of forest fires. No veg to soak up water: purification cleans the water. Recycling of raw materials: decomposition of materials, creation of soil matter, nutrient re-release converts from unusable forms [dead body] into more accessible forms. Fosters unimaginable biodiversity: ecosystem unto itself, handful of soil = billions of organisms. Influence the atmosphere composition: storage and release of gases such as co2, key role in c cycle, 3rd largest pool on earth! [next to ocean, rocks/parent material: can act as a sink or source [organisms within breathing, management intensity has an influence.

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