Test 2_Soils Flashcards
turfgrass soils definition:
a complex medium of inorganic and organic materials. the soil also ontains various gases and water.
Soil horizons (list)
O-horizon
A-horizon
B-horizon
C-horizon
O-horizon
layer of undecomposed and partially decomposed organic matter = THATCH AND MAT
A-horizon
topsoil composed of mineral particles and organic matter giving it a dark rich color
B-horizon
subsoil, low in organic matter and high in clay
C-horizon
zone of partially weathered parent material often over solid bedrock
soil texture refers to:
the proportion of sand, silt and clay particles
soil texture determines:
many chemical and physical properties of the soil
- How compaction prone is it?
- How well will it hold moisture? etc
sand characteristics
- large particles
- low CEC
- Compaction resistant
- low water holder
high infiltration
- high aeration porosity
clay characeristics
- tiny particles
- medium CEC
- compacts
- high water holder
- low infiltration
- low aeration porosity
- poor aggregation
to improve both sand and clay soils:
add organic matter
soil structure refers to:
the arrangement of mineral particles
anything that fractures or separates soil particles may promore aggregation. for example:
- root penetration
- freezing and thawing
- wetting and drying
- earthworm activity
- ripping and tilling
- core aeration
- solid tining, knifing, etc
______ may improve the potential for aggregation
calcium
clay particles have a _____ charge on their surface
negative
density =
mass per unit volume
particle density =
density of soil solids; on average it is 2.65 g/cc
bulk density:
dry weight of undisturbed soil partiles / unit volume…
desirable bulk densities vary depending upon the soil texture
bulk density details
- dry weight of a specific volume of soil
- includes both solids and pores
- expressed as grams/cc
it is important to compare soils of _____ ______ when trying to compare bulk densities
bulk densities
a well structured soil will have a sufficient amount of both _______ and ______ space
macropore and micropore
macropores:
comparatively large proes that are important for water drainage and soil aeration
micropore:
very small pores that are important in holding water for plant use
infiltration =
water moving into the soil
percolation =
water moving through the soil profile
adhesion =
attraction of water to soil particles
cohesion =
attraction of water molecules to other water molecules
imporatince of soil aeration
- root growth
- gas exchange
- microbial activity is supported by adequate aeration
as soil temperature increases….
the rates of reactions increase
thermal heatins is a result of:
- soil color
- soil moisture
- soil organic matter
specific heat is highest for ____
WATER > ORGANIC MATTER > DRY MINERAL SOIL
soil colloids are
- clay and organic material “humus”
primary soil colloids of clay
Al, Si, O
arranged as “planes” of atoms that share charges