terms |
spodic |
As a noun terms
is .
As an adjective spodic is
(geology) formed by illuvial accumulation of amorphous organic matter.
spodic |
epodic |
As adjectives the difference between spodic and epodic
is that
spodic is formed by illuvial accumulation of amorphous organic matter while
epodic is pertaining to or resembling an epode.
sodic |
spodic |
As adjectives the difference between sodic and spodic
is that
sodic is of, relating to, or containing sodium while
spodic is (geology) formed by illuvial accumulation of amorphous organic matter.
matter |
spodic |
As a noun matter
is substance, material.
As a verb matter
is to be important.
As an adjective spodic is
formed by illuvial accumulation of amorphous organic matter.
organic |
spodic |
As adjectives the difference between organic and spodic
is that
organic is pertaining to or derived from living organisms while
spodic is formed by illuvial accumulation of amorphous organic matter.
As a noun organic
is an organic compound.
amorphous |
spodic |
As adjectives the difference between amorphous and spodic
is that
amorphous is lacking a definite form or clear shape while
spodic is (geology) formed by illuvial accumulation of amorphous organic matter.
accumulation |
spodic |
As a noun accumulation
is the act of amassing or gathering, as into a pile.
As an adjective spodic is
formed by illuvial accumulation of amorphous organic matter.
illuvial |
spodic |
As adjectives the difference between illuvial and spodic
is that
illuvial is of, pertaining to, or formed by illuviation while
spodic is (geology) formed by illuvial accumulation of amorphous organic matter.
spodic |
spodosol |
In geology|lang=en terms the difference between spodic and spodosol
is that
spodic is (geology) formed by illuvial accumulation of amorphous organic matter while
spodosol is (geology) a type of soil that has a spodic horizon; includes most podsols.
As an adjective spodic
is (geology) formed by illuvial accumulation of amorphous organic matter.
As a noun spodosol is
(geology) a type of soil that has a spodic horizon; includes most podsols.