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21 - 23 October 1997
People: Robert J. Ahrens, Lead Scientist, Soil Taxonomy, Lincoln, NE Charles Love, SDQS, Indianapolis, IN Wade Bott, MLRAPL, Winamac, IN Rex Brock, SS, Winamac, IN Shane McBurnett, SS, Winamac, IN Franklin Furr, RSS, Winamac, IN Don Ruesch, RSS, Columbia City, In Jerry Larson, SDQS, Indianapolis, IN Don Franzmeier, Agronomy Dept., Purdue University
Bill Hosteter, Soil Liaison, Indianapolis, IN
Other Potential Participants: Jerry Thomas, RSS, Greencastle, IN Scot Haley, RSS, Indianapolis, IN Larry Huber, Soil Consultant, Valparaiso, IN
Tom Ziegler, Soil consultant, Lafayette, IN
Background:
21 October 1997 Briefing on Past Studies and Sites
1975 visit by Bill McKinzie and Warren Lynn
Sites visited were in the following counties: Montgomery - muck/coprogenous earth/sand/coprogenous earth Stuben - muck/coprogenous earth/sand Stuben - muck/coprogenous earth/sand White - muck/coprogenous earth La Porte - muck/coprogenous earth
Cass - thin muck/coprogenous earth/sand (11 inches
muck) Elkhart County has Edwards and Muskego muck Starke County has Toto muck (OSD site) La Porte County has Edwards and Muskego muck
Pulaski County has Edwards and Muskego muck
Importance of special designations for limnic layers
or horizons:
Marl is difficult to consider as a "C"
horizon. Marl may have some plant parts present, but not enough
to be an "O" horizon. It may also have staining from
organic materials that make it darker than normally defined.
Coprogenous earth is also difficult to consider as
a "C" horizon. Some coprogenous earth has enough plant
parts and organic materials to be considered as "O",
but it is vastly different from our normal mucky materials. It
reacts entirely different upon drying and does not rewet. Also
it creates problems in farming when exposed on the surface.
Both marl and coprogenous earth present problems
with underground drain tiles. Both materials coat the tile and
stop or greatly reduce the amount of water entering the tile.
This often happens within a year of the time the tile is installed.
Using an "O" or a "C" designation
definitely does not provide needed information for land owners
or drainage contractors who are working with these materials.
Also this would be helpful for assessments as the organic materials
on the surface subside. The soils with marl and coprogenous earth
have little or no value for cropping as soon as the organic surface
is gone.
In Elkhart County, IN, Muskego muck presented some
difficulties in horizon designations in the coprogenous earth
materials. The organic carbon content fluctuated in the layers
and the designations fluctuated between "O" and "C"
horizons. As limnic layers the designation would remain constant
and it would present a warning that these materials would not
react like normal "C" materials that can be brought
to the surface.
The proposal to use the designations found in Soil
Taxonomy, 1975, would still do the job. These designations are:
Lca for marl (calcium)
Lco for coprogenous earth
Ldi for diatomaceous earth
Special designations are used for all kinds of inclusions
in horizons or special properties of horizons. In organic soils
we designate the types of organic materials by using "a",
"e", or "i". None of these fit the coprogenous
earth materials when the organic content is great enough to be
called an "O" horizon under the present thinking.
The investigation will involve studying Limnic materials
in La Porte, Pulaski, and Starke Counties and possibly Elkhart
County in Indiana.
Soils to be investigated will include the Edwards,
Muskego, Martisco, and possibly the Toto series. If other muck
soils underlain with Limnic materials are near, they may also
be investigated.
Arrangements will be made to excavate and sample
3 of the Limnic soils to determine the composition of the Limnic
layers.
This study should show that Limnic materials are
better defined with an "L" horizon designation rather
than the currently inconsistently used "O" or "C"
designations.
The present method of horizon designation allows
for confusion in the terminology of the horizons. Designations
can change between "O" and "C" due to a slight
change in organic carbon content of the coprogenous earth materials.
Marl has historically been considered "C" material, but is an accumulation of calcium carbonates and is not parent material to any other horizons. |