The Term Laterite in Comparison to
Geophysics and Other Disciplines
The term laterite is becoming an issue in the world of
geophysics. People who argue against the term claim that
laterite is interchangeable with other words that mean a soil
substrate or substance. Other proponents state that the term
laterite is a borrowed definition that is taken from another
scientific source that does not have to do with the
discipline.

There seems to be no clear definition though some state that
it refers to the identification of the soil additives that make
it more defined. Defenders of the term claim gives justice to
its use in geophysics language though laterite is a very large
class and cannot be grouped in any one homogenous
class.
The idea that laterite is a single term that cannot define a
single entity or substance has not been substantiated. Even
when considered in a clay or hard soil sample, there are two
many mineral and chemical compounds that makes that sample
unique. The term is used more when the soil referred to has
large amounts of aluminum compounds or iron.
In the garden industry the term laterite refers to a soil
that would have poor growth success because of the makeup of
the soil and the number of metallic compounds found in it. This
would mean that the metallic compounds were at such a level
that the soil and dirt itself could not provide the organic
material in sufficient amounts to grow new life.
This is true of most all soils that are considered laterite.
The soils are never pure and contain materials that could be
considered impurities such as sand, gravel, rocks, and organic
materials. The materials are inert and non-reactive. This
composition may be good to use in an aquatic environment that
would not saturate itself with water or harm the organic
resources for plant and animal growth.
This would backfire if the laterite contained large amounts
of iron. Iron would stimulate growth or the organic materials
but in an aquatic or semi-damp environment invite the growth of
algae, mosses, and other water borne parasitic and symbiotic
growth.
Laterite is used in determining long term changes in
atmosphere and weather by several different disciplines. The
iron and clay mixture can take on qualities on the climate that
they experience and can be used in finding out what that
ancient climate was like in terms of moisture, dryness, cold,
or hot.
Once water has left the saturated laterite, fossil records
can be studied to find out what life forms the era produced by
matching the laterite with the flora or fauna fossilized
within. This can be translated in the world of geology,
geophysics, and other earth based sciences.
There are many different types of laterite. Though this
article discussed iron, there are also nickel, aluminum, and
other metallic components that can be infused in the clay or
soil to be labeled as a laterite in geophysical terms. As the
disciplines converge on this one term that means a different
thing to each discipline, an understanding of the true meaning
of laterite will arise and sub-categories of laterite may be
used to explain the majority of the substance that makes the
compound.
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