Unit 4: Chapters 14, 15, 16 Flashcards
What are the differences between physical and chemical weathering?
mechanical weathering is the physical disintegration of rock material without any change in its chemical composition.
chemical weathering is the decomposition of rock by the chemical alteration of its minerals.
<p>
| With what geographic regions are physical and chemical weathering most associated?</p>
<p>
| warm regions close to the equator</p>
What is the process or cause of frost action?
water gets into rock, expands, starts splitting rock
What is the process or cause of oxidation?
if rock has iron, rusts
What is the process or cause of hydrolysis?
water exposed like in oxidation
What is the process or cause of granular disintegration?
acid rain, causes splits sedimentary rocks
Describe the process of landslides as concerned to mass wasting
quickest and most dangerous process of mass wasting
move large amts of material in small amt of time
destroy whole towns
Describe the process of mudflows as concerned to mass wasting
similar to landslides
primarily caused my huge rains
soil can only retain so much water, so it starts slipping
Describe the process of slumping as concerned to mass wasting
Describe the process of solifluction as concerned to mass wasting
Describe the process of soil creep as concerned to mass wasting
slowest form
tomb stone shifts, for example
very slow – shifts land beneath things
Know the relationship between average soil depth and the weathering and erosional properties of environments as one traverses from the equator to the polar regions.
mirror each other
erosion in tropics, soil depth is really deep
Soil profiles - O horizin
organic – o1 - dead leaves and sticks, o2 - decomposition (animals)
Soil profiles - A horizin
transition between leeching and organic
Soil profiles - B horizin
zone of leeching, nutrients and minerals are being pulled from A to B
Soil profiles - C horizin
mix of rocks, not a lot of mineral
Soil profiles - D or R horizin
bedrock
Know what is meant by soil texture
sand – can’t hold water, but water can pass
silt – retains water, doesn’t let it move through
clay – water repellent, makes it slippery
How does soil texture relate to the general quality of the soil regarding tilage
33% of each for ideal soil texture, easy to move it
How does soil texture relate to the general quality of the soil regarding water holding capacity
sand – can’t hold water, but water can pass
silt – retains water, doesn’t let it move through
clay – water repellent, makes it slippery
macro soil nutrients
nitrogen
phosphorus
potassium
micro soil nutrients
argon, specific nutrients for certain plants
soil pH
roses – acid soil
different pH’s can change composition / color of plants
soil forming processes: podzolization
soil that develops in high latitude regions tends to be acidic