Midterm Flashcards
Ecosystem services from soil perform
Provide goods (water, food, medicine, lumber)
Purifies water
Decompose waste
Nutrient cycling
Biomass production
Outdoor recreation
How does soil supports plants?
Physical support
Air - remove carbon from atmosphere, release oxygen
Water - store water as groundwater
Temperature moderation - shade
Protection from toxins
Nutrient elements
Soil Profile and its layers
O - organic matter
A - organic matter and topsoil
B - minerals and salts (subsoil)
C - salts and rocks
consistuent of your soil
25% air
25% water
5% organic matter
45% mineral
Soil Texture
sand
loamy sand
sandy loam
sandy clay loam
Loam - mixture if sand, silt, and clay particles
silt loam
silt
silty clay loam
clay
clay loam
sandy clay
silty clay
Soil structure
sand
silt
clay
Weathering of rocks and minerals
Physical and Chemical
Types of rocks
Igneous - formed from molten magma (granite)
Sedimentary - formed by the break down of other rocks that are underwater and make new rocks (quartz)
Metamorphic - formed from other rocks by a process called metamorphosis (marble)
Factors influencing weather
Parent material
topography
climate
biology
time
Parent materials
those found in place
those transported by water
Basic processes of soil formation
Transformations
Translocations
Additions
Losses
Types of Soil structure
Spheroidal, platelike, blocklike, prismlike
Types of tillage
Conventional tillage - use of moldboard plow to life, twist, and invert soil
Conservation tillage - leaves at least 30% of the soil surface covered by residues
Minimum/reduced tillage - chisel plowing, stirring of the soil but leaves plant residue
Soil density
Mass measurements of soil
Bulk density
Mass of a unit volume of dry soil
includes both solids and pores
Particle density
Mass per unit volume of soil solids
Not affected by pore space
Factors that determine pore space
minerals that make up minerals
Macropores vs micropores for each soil texture
A sandy soil has more macropores
A silty soil has smaller than sand pores but bigger than clay pores
A clay soil has more micropores
Activity as humans that can affect pore space
walking, driving, tillage
Soil water properties
polarity
hydrogen bonding
hydration
cohesion (glue to another water) vs adhesion (glue to surface)
surface tension
Tillage is influenced by
aggregate formation and stability
bulk density
soil moisture content
aeration
drainage
rate of water infiltration
capillary water capacity
Alfisols
Mildly acid clay
Productive soils
Good forest growth and crop yield
Strongly weathered
high-to-medium base saturation
Andisols
High content of volcanic glass
Poor content of iron and aluminum
Humid moisture
Support intensive agriculture
Aridisols
Dry soil
low organic matter
Need irrigation for growing crops
Entisols
Gelisols
Support tundra vegetation
Rarely used in agriculture
Very cold
Histosols
> 20% organic matter
Lightweight
anaerobic
Inceptisols
Important for lowland rice-growing areas
can dominant an area
Mollisols
High fertility
Organic matter oxidized
Oxisols
Highly weathered
Spodosols
Acid
Productive when fertilized
Good for crop production
Ultisols
Strongly acidic clays
Good crop production
Productive in agriculture
Vertisols
High in swelling clays