Clues and Impediments to the Understanding of SE US ...€¦ · Clues and Impediments to the...
Transcript of Clues and Impediments to the Understanding of SE US ...€¦ · Clues and Impediments to the...
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Clues and Impediments to the Understanding of SE US
Coastal Plain Soils Acknowledgments:
Personnel who contributed to the Florida Soil Survey Program. Data generated through their effort prompted research reported in this talk.
Collaboration of UF Soil and Water Science colleagues.
Florida soil scientists who shared soil photographs.
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In memory of two people who enriched my life …
Dr. Earl StoneDr. Vic Carlisle
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Topics Addressed
• Clues– At E-Bt boundaries– At E-Bh boundaries
• Impediments– Terms that confound communication– Terms that mislead– Horizon designation mismatch with genetic
context
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Clues
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Florida Soil Survey Data Tell a Story
E-Bt mineral distributions
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?
In effect …
No matter how deep the boundary, clay mineralogy changes there
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Ap
E
Bt
Btg
Example, one ofmany
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Bw
E
Coated vs. Clean Sand Grains
High HIVin clay
Conclusion: HIV is large proportion of small amount of clay in grain coatings
No HIVIn clay
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Coated vs. Clean Sand Grains (cont.)
Coated
CleanClean
Coated
Coated
Lakeland Myakka St. Lucie
… in Panhandle &N. Central Florida… no matter howdeep or thick
Coated = high HIVin clay
Clean = high quartz,
maybe smectitein clay
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Coatings
• Patchy, not uniform • About 2-8 % of sandy soil mass• Contain similar proportions of silt & clay• Silt – mostly quartz• Clay – quartz, phyllosilicates, gibbsite, & oxides of Al & Fe• NOT “iron oxide coatings”, although …• Al- & Fe oxides largely control P sorption• Al- & Fe oxides serve as “cement”
Characteristics of Sand Grain Coatings
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HIV-rich silts have platy grains containing K
Potassium as a Clue …
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HIV
But despite K, mica evades detection by x-ray diffraction
X-ray diffraction pattern of HIV concentrated inMedium silt
gibbsitequartz
(mica peakwould be
here)
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A Glimpse of Ghostly Mica … Finally!
Evidence of occluded mica zones in HIV grains
1.0-nm
lattice fringe image of mica in HIV grain
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Mica – Metal Oxide – Grain Coating Connections:
Mica as a Ghostly Clue …
Theory to explain HIV-kaolinite distribution
Non-quartz mineral abundance grossly exaggerated for illustration purposes.
(Mica is considered a weatherable mineral, too.)
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To Bt
Mica as a Ghostly Clue …
Theory to explain HIV-kaolinite distribution (cont.)
• Clay dispersed & mobilized
• New clay generated by weathering
• Mica weathers in-situ
• Al- & Fe oxides form and bind other components
• Mica products (HIV) & some kaolinite become incorporated into coatings
• HIV less subject to eluviation than kaolinite, explaining depth trend
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E-Bt pedological vs lithological issue
• Dominant-sand to total-sand ratio• Heavy mineral abundance• Heavy mineral species
Most data I’ve read or collected support pedological
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Sand grain coatings are again clues …
Initial observations:
• Looks like a coating redistribution
• Bh fades upward as seasonal high water table drops
E-Bh and fluctuating water table
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Morphological & mineralogicalevidence of coating redistribution Clean
Coated
Coated
• Aquod to Psamment sequence moving up from the shore of a sandhill lake
• About a 10-m transect
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… but why is a fluctuating water table required?
Florida Soil Survey Program data suggesting Bh is clay-enriched, too
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Why is a fluctuating water table required? Some ideas -
• Metal sources for Bh - metal oxides – stable on well-drained landscapes
• Redox partially depletes Fe on poorly drained uplands (“flatwoods”)
• Al => less crystalline & more vulnerable to organic complextion
• Thresholds in frequency & duration of saturation dissolve Al oxide via• Organic acids reach activities & kinetic thresholds• Reduced movement and microbial degradation rate
• Al oxide dissolution releases all coating components
• C moves Al, but Al eventually stops C within a finer matrix of colloid origin
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Impediments
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• Candler and Apopka– Candler-Apopka, Levy Co.
• Ortega and Blanton– Blanton-Ortega, Lafayette Co.
• Ridgewood and Albany– Albany-Ridgewood, Lafayette Co.
• Tavares and Millhopper– Tavares-Millhopper, Hillsborough Co.
• Penney and Otela– Otela-Penney, Gilchrist Co.
Horizon designations of Psamments on older landscapes
Examples of Landscape Associations,Psamment and Udult or Udalf:
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Sand
Sandy Clay Loam
Layers1
2
3
OrtegaBlanton
A
EC
A
Bt
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Sand
Sand
Layers1
2
3
DuetteSt. Lucie
AA
CE
Bh
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Concept of “inert sand”
Sand
Sandy Clay Loam
Layers1
2
3
Ortega BlantonA A
C E
Bt
Inert sandprecluded pedogenesis
Intense pedogenesis produced inert sand
Inert sand
It can’t be both
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Lake, etc. Candler, etc. St. Lucie, etc.
“Coated” “Uncoated” “Uncoated”
Has Fe & Al Has Fe & Al No Fe & AlSome P retention Some P retention No P retention
Grains un-strippedGrains un-stripped Grains stripped
Family “Coated” – “Uncoated” distinction
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Data that do NOT support presumptions of Bh being a “hardpan”
Means of selected data for Bh, Bh1, Bh2, and Bh3 horizons sampled during the Florida Soil Survey Program
SaturatedHydraulic
Conductivitycm/h
BulkDensityg/cm-3
OrganicCarbon
%Clay
%
Non-Ortstein(vfr or fr)
14.10n=440
1.50n=440
1.38n=466
3.50n=466
Ortstein(vfi or fi)
8.05n=43
1.51n=42
2.59n=43
5.71n=43
Bh and Bt horizons as “hardpans”
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Myakka Very friableMany fine & medium roots
Leon Firm to friableMany fine & medium roots
Immokalee Friable to looseCommon fine & medium roots
Wabasso friable
Common fine & medium roots
Bh horizon consistence & roots as described on OSDs of Alaquods of large extent
Data that do NOT support presumptions of Bh being a “hardpan”
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Conclusions• Soil survey data are a powerful resource in
understanding soil genesis• Sand grain coatings and their distribution are major
clues to genesis of SE USA Coastal Plain soils• Horizon designation precedes and remains
independent of soil classification • Words ill chosen can lead to misunderstanding
(e.g., “hardpan”) and hamper communication (e.g., “uncoated”)