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ID # 207
Embedded and fragmented clay coatings in a paleosolFrom the Soil Micromorphology Slide Collection
STEM Standard addressed: ESS2E - Biogeology
Appropriate Grade Level(s)
- College-level
- Classroom Lectures
- Laboratory Activities
- Soil Microbiology
Micromorphological description of slide: Microlaminated embedded clay coatings, 100-1 50 um thick with individual laminae about 10 urn thick, highly disrupted, sharp to diffuse extinction, high berefringence; 10YR 6/6 in PPL
Data for the horizon
Horizon sampled: 3ABtb
Physical and chemical data available: Sand = 4%, silt = 54%, clay = 42%
Macromorphological description of horizon: Gray (1OYR 5/1) light silty clay; strong fine and very fine subangular blocky structure; moist friable; many faint discontinuous IOYR 5/6 Fe oxide coatings on ped faces; abundant krotovinas 4-14 cm in diameter
Micromorphological description of horizon: Subangular blocky microstructure; double-spaced porphyric related distribution pattern; porostriated and random striated birefringence fabric; many clay coatings embedded and along pores; 30-35 porosity; common Fe oxide nodules; common ferriginous hypocoatings.
Data for thin section
Preparation of sample: Air dry
Impregnating medium: Polyester resin
Thickness of section: 30 µm
Orientation of section: Vertical
Physiographic position: Upland
Hill slope position: Gently sloping backslope
Parent material: Loess, possibly Sangamonian
Data for the horizon
Horizon sampled: 3ABtb
Physical and chemical data available: Sand = 4%, silt = 54%, clay = 42%
Macromorphological description of horizon: Gray (1OYR 5/1) light silty clay; strong fine and very fine subangular blocky structure; moist friable; many faint discontinuous IOYR 5/6 Fe oxide coatings on ped faces; abundant krotovinas 4-14 cm in diameter
Micromorphological description of horizon: Subangular blocky microstructure; double-spaced porphyric related distribution pattern; porostriated and random striated birefringence fabric; many clay coatings embedded and along pores; 30-35 porosity; common Fe oxide nodules; common ferriginous hypocoatings.
Data for thin section
Preparation of sample: Air dry
Impregnating medium: Polyester resin
Thickness of section: 30 µm
Orientation of section: Vertical
Physiographic position: Upland
Hill slope position: Gently sloping backslope
Parent material: Loess, possibly Sangamonian
Method
Data for 35-mm slide
Frame length: 7 mm
Light mode: Circularly polarized
Frame length: 7 mm
Light mode: Circularly polarized
References
Woida, K. 1991. The morphology and genesis of soils in a buried Pleistocene toposequence, south-central Iowa. Univ. of Iowa, Iowa City. PhD. Thesis.
Source: K. Woida
Slide CT18. Soil Science Society of America, 1993. A Reference Slide Collection for Soil Micromorphology. SSSA, Madison, WI.
Source: K. Woida
Slide CT18. Soil Science Society of America, 1993. A Reference Slide Collection for Soil Micromorphology. SSSA, Madison, WI.
Peer Review: Yes
Credit this item to: SSSAMedia Date: 1993-01-01
Provided By: (SSSA) Soil Science Society of America
Latitude: 41.2922367
Longitude: -93.98784269999999
Author(s)/Creator(s)
-
* Soil Science Society of America
SSSA
Submitted By: (SSSA) Soil Science Society of America
Keywords
- Coatings
- 3ABtb horizon
- micromorphology
- clay coatings,paleosol
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