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Bulk Density and Fragipan Identification in Loess Soils of the Lower Mississippi River Valley
Author(s) -
Lindbo D. L.,
Rhoton F. E.,
Bigham J. M.,
Jones F. S.,
Smeck N. E.,
Hudnall W. H.,
Tyler D. D.
Publication year - 1994
Publication title -
soil science society of america journal
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 0.836
H-Index - 168
eISSN - 1435-0661
pISSN - 0361-5995
DOI - 10.2136/sssaj1994.03615995005800030036x
Subject(s) - loess , pedogenesis , soil water , geology , bulk density , lithology , horizon , soil science , hydrology (agriculture) , geomorphology , geochemistry , mathematics , geotechnical engineering , geometry
High bulk density (ρ b ) compared with overlying soil horizons has long been considered one of the principal characteristics of fragipans, yet recent investigations have noted inconsistent relationships between fragipans and ρ b . This study was conducted to evaluate the fragipan‐ρ b relationship in several major loessial soils of the lower Mississippi River Valley. Average ρ b (field‐moist, saran‐coated clods) obtained from five Memphis‐Loring‐Grenada catenas extending from northwest Tennessee to southeast Louisiana show that ρ b in the fragipans of the Loring (fine‐silty, mixed, thermic Typic Fragiudalf) and Grenada (fine‐silty, mixed, thermic Glossic Fragiudalf) pedons range from 1.45 to 1.78 Mg m −3 ( x̄ = 1.56). A wider range of 1.38 to 1.86 Mg m −3 ( x̄ = 1.55) occurred at similar depths in the Memphis (fine‐silty, mixed, thermic Typic Hapludalf) pedons. Within most Loring and Grenada pedons, the ρ b of the fragipan horizon is not statistically unique (based on Duncan's new multiple‐range test) and does not always represent the maximum for a given pedon. There is also a weak positive correlation ( r 2 = 0.44) between total sand content and ρ b , suggesting that higher ρ b in these soils are more closely related to lithologic factors than to pedogenic densification. Specifically, pedons with a significant influence of Coastal Plain sediment have higher ρ b than those developed entirely in loess, suggesting that the high ρ b are partially inherited. These results indicate that ρ b should not be used as a principal test for differentiating between fragipan and nonfragipan horizons in these soils. It appears that root and water restriction typically associated with fragipans in the lower Mississippi River Valley are related to physical or chemical characteristics of the fragipans other than ρ b .