SOILS 101 FINAL Flashcards
6 functions of soil
Support plant growth
Control fate of water
Nature’s recycling system
Atmosphere modifier
Habitat
Engineering medium
6 ways soils support plants
nutrients
water
air
physical support
temperature
protection from toxins
Size sand:
1-.05mm
size silt:
.05-.002mm
size clay
less than .002mm
what is weathering?
a biochemical and physical process that involves both destruction and synthesis
3 ways to physically weather soils
temperature
freeze/thaw
water, ice, and wind abrasion
biochemical processes of weathering
water and acis produced by microbes
rust
4 processes of soil formation
transformation
translocation
addition
loss
transofrmation
chemical or ohysical alteration
translocation
movement of soil by water
addition
material input from outside source such as eroded sediment
loss
material lost from soil due t water
what are the 5 master soil horizion layers?
O
A
E
B
C
O horizion
Mainly organic materials above mineral layers
A horizion
topmost mineral layer with a bit of organic matter to make it dark. coarse texture
e horizion
maximum leaching loss, eluviation of clay, often sandy and white
b horizon
zone of illuviation and clays. no longer can see parent material
c horizion
unconsolidated material under solum
what are the 5 factors that influence soil formation
parent materials
climate
biota
topography
times
when do biochemical reactions double
when they are raised 10 degrees CELS
Molic Epipedon
Thick Dark High base saturation
Melanic Epipedon
Thick Dark mineral horizoon derived from volcanic ash
histic epipedon
thick organic horizon forming inw et areas
argillic epipedon
high activity silicate clays
oxic
veyr highly weather with fe and al oxides
spodic
illuvial horizon with accumulation of organic matter and al oxide
fragipan
bx horizon of hgihly compacted dense brittle material that resisits any kind of penetration
6 soil physical properties
color
texture
structure
density
porosity
compaction
where do you find granular aggregates
a horizon
where do you find angular or blocky aggregates
b horizon
where do you find prismatic aggregates
b and c horizons
where do you find massive or structureless aggregates
any horizon
particle density
mass of solids/volume of solids
bulk density
mass of solids/volume of soil
what soil density includes pore space, and which does not?
particle density does not
bulk density does
size of macropores
greater than .08mm
size of mesopores
between .03-.08mm
size of micropores
less than .08mm
what percent of the worlds fresh water is in soil
33%
cohesion
attraction fpo water molecules to eachother
adhesion
attraction of water molecules to other surfaces
what is surface tension a result of
qwater molecules having a greater attraction to each other than air
name 3 forces that affect potential energy of water
gravity
matric
osmotic
matric force
water molecules being attracted to solid surfaces
osmotic force
attraction between water molecules and solutes
saturated soil
maximum retentive capacity 0kpa
field capacity
macropores filled with air -10 to -30 kpa
permenant wilting point
all pores filled with air
-1500 kpa
volumetric water content
volume of water per dry soil
gravimetric water content
mass of water per mass dry soil
what are the three types of water movement in soil
saturated
unsaturated
vapor
saturated flow
gravitational flow from high to low elevation
unsaturated flow
matric flow from high energy to low energy
tourtousity
soil pores are not straight like a cappillary
plant available water
volume of water present between field capacity and PWP
whta is the typical residence time of water in soil
1-2 months
evapotranspiration
wtaer lost through evaporation from soil or transpiration from leaves
when does infiltration excess occur
the rate of precipiation exceeds the rate of infiltration during hard rains
when does saturation xecess occur
amount of precipiation exceeds water holding copacity during long rains
acid mine drainage
oxidation of pyrite produces extreme acidity and soluble iron and sulfur
the best to the worst way for chemicals to travel through soil
matrix flow
marcopore flow
bypass flow
concentration fo what decreases with soil depth?
oxygen
what are the 2 methods of soil gas exchange
mass flow and diffusion
what makes diffusion happen
concentration gradients
oxidation
the loss of electrons in a substance therefore increasing valence charge
reduction
gain of electrons therefore a decrease in valence charge
what is redox potential?
a measure of how aerobic or anaerobic a system is by measuring the tendency of a substance to give up or take electrons
what can anaerobic respiration lead to?
methane ethlyne dentitrification
what is a vernalization process?
seeds requiring a cold treatment before germination
at what temperature do biological processes cease
5 degrees celsius
at what high temperature does microbial activity die?
50-60 degrees celsius
frost heaving
soil freezing and pushing objects in it upward
what does rain do to the soil in the spring?
warms cool soils
what does rain do to soils in the summer?
cools hot soils