Term
| oxidation state of B in soil |
|
Definition
|
|
Term
| the orincipal soil solution species of B |
|
Definition
| charge neutral boric acid (B(OH)3) |
|
|
Term
| what boric acid does in strongly alkaline solutions |
|
Definition
| hydrolyzes to make borate
B(OH)3 + H2O --> B(OH)4- + H+ |
|
|
Term
| in soil solutions, does boric acid form soluble complexes with metal cations? |
|
Definition
|
|
Term
| why does boric acid not form soluble complexes with metal cations? |
|
Definition
| because of its charge beutrality |
|
|
Term
| aqueous concentrations of B are controlled by... |
|
Definition
-adsorption to Fe and Al hydroxides -clay minerals -calcite -soil organic matter |
|
|
Term
| how B adsorption responds to pH |
|
Definition
| B adsorption increases with increasing pH |
|
|
Term
| types of minerals in the soil Al is found in |
|
Definition
| primary and secondary aluminosilicates as well as in the hydroxide and gibbsite |
|
|
Term
| oxidation state of Al in soil |
|
Definition
|
|
Term
| how Al exists in soil solution |
|
Definition
| either as free Al3+ or as a hydrolysis product (Al bound to 1 or more OH's), depending on the pH |
|
|
Term
|
Definition
| because it may exist as cationic or anionic species, depending on pH |
|
|
Term
| some things Al+ can form soluble aqueous complexes with |
|
Definition
| -OH-
-F-
-SO4-2
-H4SiO4
-organic substances containing carboxylate and phenolic functional groups |
|
|
Term
| this controls the concentration of Al in soils |
|
Definition
| the precipitation-dissolution of poor to well crystallized Al oxyhydroxides |
|
|
Term
| pH at which Al is not very detectable in soil solution |
|
Definition
|
|
Term
| the total acidity of a soil |
|
Definition
| the concentration of exchangeable Al |
|
|
Term
| in addition to participating in cation exchange, Al oxyhydroxides participate in... |
|
Definition
-ligand-exchange rxns -proton-exchange rxns |
|
|