The distribution of selected soil properties in a first-order loess watershed

Wysocki, Douglas A.

doi:10.31274/rtd-180813-6876

Cited by 2 publications

(1 citation statement)

References 36 publications

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“…Laird (1987) reported beidellite as the dominant clay mineral in a soil developed from Mississippi River alluvium. Wysocki (1984) reported smectites with a beidellitic character in upland loess‐derived soils in Tama County, Iowa. Badraoui et al (1987) in a study in northwestern Minnesota identified beidellite as the dominant smectite in a soil formed in lacustrine deposits of glacial Lake Agassiz.…”

Section: Relationship Of Coefficient Of Linear Extensibility Values Tmentioning

confidence: 99%

Prediction of Coefficient of Linear Extensibility Values for Iowa Soils

Fenton

1995

Soil Horizons

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Recent changes in Soil Taxonomy have made linear extensibility an independent criterion for defining vertic subgroups. There are many soils for which extensibility values have not been determined but clay data are available. The relationship between coefficient of linear extensibility (COLE) values and clay content was studied for Iowa soils for which COLE data were available. The objective of this study was to determine if COLE values could be accurately predicted for those soils where only clay data were available. Results of this study indicate there was a good correlation between COLE values and clay content and the relationship can be used to help classify Iowa soils for which COLE data are not available.

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Section: Relationship Of Coefficient Of Linear Extensibility Values Tmentioning

confidence: 99%