9 Flashcards
describe the soil composition
Minerals
OM
Micro orgs
Gas
Liquid
how mater phases are in soil
all 3 phases: solid, liquid and gas
recognize kaolinite
layering of clay
K= silica sheets and aliumia are together, but each sheet is held via string HB
what are the physical properties of soil
particle size
texture
permeability and permebility
general pathways by which rocks get transformed into the soil (3)
physical
chemical
biological
what are the components of soil organic matter
4 main components are
finely divided material
various lvl of OG matter
water
air
what are the chemical properties of soil
OM
pH
available elements
cation exchange capacity
what are 2 characteristics of colloids
large SA and high cation exchange capacity
what are colloids
molecule that are larger than atoms but small enough to be undetected by the unaided eye. (1 nano-1 micro)
they do not settle in solution
they still have a lrg SA and are neg charged (clays and humic mat)
base saturation
The # of occupied sites by Ca Na K or Mg/ total sites. Looks to show how saturated the surface of a soil particle is by cations
what is the land composed of
rock and soil
what is soil
the producut of the weathering of rocks which is able to support plant growth
what are the soil horizons
O- humus
A- top soil (minerals and OM)
B- sub soil (minerals but low OM)
C- parent mat
D- bed rock
which minerals are most abundant in the soil
oxygen and silicon
what are the subcategories of finely divided mineral matter
primary
- minerals from their source (quartz)
secondary
-post weathering processes (silicate clays)
what is the size of clay
anything less than 2 micro meters
montmorillonite
M= aluminum layers sandwiched between silica layers. each group is held together via a mix of Ca, Mg and K iconic bonds (via neg clay surface).
this loose bonding allows for the penetration of water easily. this clay will swell and shrink with ease.
illite (differences)
aluminum layers sandwhiched between silica. Each group is healed together bia ioninc bonds by K only (and the neg clay surface). this is tight, and not water is able to pass
what type of “hedron” do silicas form?
tetrahedron
what type of “hedron” do aluminum form
octahedrons
physical weathering
by temp
erosion via water or wind
plant or animals contribute too
chemical weathering
hydration
A and B rxn- via CO2 dissolving in H2o
hydrolysis
complexation rxn
redox
hydration
a chemical weathering porecess where water moles are incorporated into minerals. common is secondary min.
minerals will swell and become deforemd
hydrolysis
water reactswith a mineral in the presence of an acid, realising ions assaioated ith OG mineral identiy