Soil Colloids characteristics
Implications of adsorbed cations in colloids
-adsorbed cations exchange with cations in soil solution
Cation Exchange Capacity (CEC)
what is a mole
-weight of element that contains 6.02 x 10^23 atoms (molecular weight
What is a centimole?
= to .01 mole
Equivalent weight
- the amount needed to generate a charge
How to convert mass to charge
- convert to cmol(c) by multiplying .01
Organic colloids
- primarily C, H, O
What are the 2 major types of colloids
- organic
What is the source of the net negative charge in organic colloids
Dissociation is ________
pH dependent
-high pH, low acidity
Mineral colloids (3 types)
What is the source of the net negative charge in for mineral (inorganic) colloids
- replacement of 1 atom by another of similar size
acid saturation
(H+Al)/CEC x 100
-percentage of CEC accounted for by H and Al ions
Cation saturation
Genesis of silicate clays
Strength of attraction of cations____
-depends on valance, hydrated radius
CEC determination
- Unbuffered methods (extraction solution at pH of soil with neutral salt)
ECEC
- the total amount of exchangeable cations, which are mostly sodium, potassium, calcium and magnesium
Soil acidity (pH) is correlated with _
- organism activity
-one pH unit means ____ difference in H+
10^-4
Source of H+ dissociation
-wear inorganic acids (high pKa, ex. carbonic acid), stronger organic acids (low pKa)
Al and Al hydroxides generate acidity by ____
hydrolyzing water
hydrolysis of water
Three conceptual pools of acidity
1) Active acidity (pool)
2) Salt replaceable acidity (pool)
3) Residual acidity (pool)