lecture 8 Flashcards
5 reasons soils are important
- Foundation of terrestrial ecosystems, influence ecosystem function
- Provides nutrients, water, anchoring medium for plants
- Influences plant sp. Composition and productivity
- Habitat for diverse below ground community, esp. decomposers
Ecosystem services: C storage, water filtration and storage, decomp, etc
soil comp (rough %)
25% air, 25% water, 45% mineral, rest om
5 soil horizons?
O (LFH)
A
B
C
what is soil development a balance btwn
balance between formation and loss
what 5 state factors influence soil development
○ CLIMATE
○ Topography
○ Biological activity
○ Time
Parent material
is soil always there
- Soil we see isnt always there -result of dynamic processes that span geological time and short daily cycles
BALANCE between forces that produce soils and forces that erode it
parent material origins? what factors impact it?
- Parent material - origins
○ Granular soils - air from geological processes + production with climate- Topography is important - where it is, how it is made
biological activity = source of organic matter in the soil = important for life
- Topography is important - where it is, how it is made
briefly describe A- C horizons
- At the topLFH - organic matter, a result of things growing and falling into the soil - dark coloration due to decomp - *
Lfh - organic horizon, active process of decomp- Organic matter and middle components interact more at A horizon, shallow roots
- At B horizon - anything going down has to leech down from the top - lighter coloration, deeper roots,
C - less organic material (30-40% organic material at most)
are soil horizons the same at every biome
- Layers may differ in proportion in different biomes
Rainforest - more rain = clearing of substantial amount of lower horizon
what are soil properties strongly influenced by
The physical and chemical properties of rocks strongly influence soil properties
chemical properties of soil?
properties
* Chemical properties:
Ph, elements, nutrient status, toxins, cations, anions
physical properties of soil
- Physical properties:
Particle size/surface area: movement and retention of water and nutrients
how does parent material turn into soil
Parent material comes from earth - magma comes to the surface, forms igneous rocks then cools, weathered and broken down into sediments, weight + temp = sedimentary rocks, heat and pressure = metamorphic rocks which melt back into magma
what two ways can parent material form soil
Sedentary - formed in place (consolidated)
Transported - moved from elsewhere (unconsolidated)
describe sedentary PM
- Sedentary - formed in place (consolidated)
- Cumulous - organic (preserved plant residues)
Residual (bedrock)
- Cumulous - organic (preserved plant residues)