Test 3 Review Flashcards
soil texture
proportion of sand, silt, and clay in the soil
soil structure
arrangement or grouping of individual soil particles into peds or aggregates
soil particles
sand, silt, clay
factors that influence bulk density (5)
- organic matter
- texture/aggregation
- structure
- compaction
- depth in soil profile
how to increase soil pH
lime
soil water at field capacity
saturated and allowed to drain freely
pedon
smallest unit of soil that contains all the horizons of a specific soil type
catena
a sequence of soils with different horizons caused by differences in their depth to the water table
soil profile
2-D representation of a vertical section of soil from the surface to deepest layers
whole thing from top to bottom
soil horizon
soil layers; roughly parallel layers in the soil with varying compositions and properties
soil color determinants (4)
- mineralogy of parent material
- organic matter
- hydrology
- soil chemistry
tool to determine soil color
Munsell Color Chart
10YR 6/3
10YR = hue
6 = value
3 = chroma
hue
proportions of red to yellow
top right corner
chroma
how bright vs dull
x-axis
value
amount of light reflected
y-axis
amount of soil nutrients
at least 16
amount of soil macronutrients
9
amount of soil micronutrients
8
fertile and infertile soil based on CEC, soil pH, silicate clay type
fertile: higher CEC, neutral pH, and montmorillonite silicate clay
infertile: low CEC, highly acid or highly alkaline pH, Fe and Al oxide silicate clays
in what pH range are N and P available for plants
5.8 - 6.8 (K tends to like more alkaline soils)
molybdenum is usually important for what crop?
soybeans (rhizobium) and legumes
in what pH range is molybdenum usually available for plants?
alkaline soils (pH 7.1+)
lime commonly comes in two forms, CaCO3 and MgCO3, what are their common names?
Ca: calcite
Mg: dolomite
decreasing pH =
sulfur
- potassium sulfate
- anything sulfate (SO4)
classifications of soil organisms
- macrofauna
- microfauna
- flora
- food - herbivores, detritivores, predators
- based on O2 demand - aerobic and anaerobic
- based on energy and C source - autotrophic and heterotrophic
producers
create their own food through photosynthesis (plants)
consumers
eat other organisms for energy (can’t make their own)
detritus
decaying organic matter
decomposers
have the ability to break down organic material releasing useful nutrients
heterotrophs
- heterotrophic from breakdown of OM (carbon)
- most numerous
immobilization
microbes absorb nutrients from the soil, making them unavailable for plant use
mineralization
- the conversion of soil organic matter to plant available nitrogen
- the release of nitrogen from the organic form to the inorganic form
nitrification
nitrifying bacteria convert ammonia (NH3) to nitrate (NO3)
denitrification
wet soil, lack of aeration, and leaching of N because of water
compaction causes the loss of what primary nutrient
nitrogen
nitrogen fixation
converting atmospheric N into usable forms
N2 -> NH4
algae: wetland
bacteria: legumes
role of bacteria
- nitrification
- nitrogen cycle
- improve soil structure
- decomposing OM
- degrading pollutants
role of algae
- producer in aquatic systems
- oxygen production
- carbon sequestration
- water purification
role of earthworms (3)
- soil fertility by producing cast
- reduce erosion and improve aggregate stability
- aeration and drainage
rhizobium
nitrogen producing bacteria found on root nodules on legumes
mycorrhiza
fungi that infect the plant roots of nearly all plants
benefits include plant nutrition (especially P), drought tolerance, disease resistance, and soil structure improvement
types of mycorrhiza and roles
- endomycorrhizae - agriculture
- ectomycorrhizae - forest