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Land‐use Effects on Soil Carbon and Nitrogen on a U.S. Midwestern Floodplain
Author(s) -
Jelinski N. A.,
Kucharik C. J.
Publication year - 2009
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/sssaj2007.0424
Subject(s) - floodplain , environmental science , soil carbon , soil water , agronomy , soil horizon , nitrogen , hydrology (agriculture) , soil science , geology , chemistry , ecology , biology , geotechnical engineering , organic chemistry
Wet prairie soils in the Midwest store significant amounts of soil organic carbon (SOC) and total nitrogen (TN). Crop fields, prairie restorations of varying ages, and remnant prairies on a floodplain soil (Fine‐silty, mixed, superactive, mesic Typic Endoaquolls) in southern Wisconsin were intensively sampled to estimate changes in SOC and TN due to the conversion of native prairie to row crops and the restoration of prairie on cropped land. In the top 10 cm of soil, remnant prairies contained an additional 24 Mg SOC ha −1 and 1.7 Mg TN ha −1 , compared with currently cropped fields ( P < 0.05). In the top 25 cm, remnant prairies contained an additional 2.4 Mg TN ha −1 compared with currently cropped fields ( P < 0.05), but a difference was not detected in SOC between unplowed remnants and cropped fields. Soil inorganic carbon (SIC) was significantly greater at all depths in cropped fields than in unplowed remnants. No differences in SOC and TN mass between annually tilled (AT) and biennially tilled (BT) fields were detected, except for greater TN in the top 10 cm of BT fields. No differences between currently cropped fields and prairie restorations less than 7 yr old were detected, however a 7‐ and 45‐yr‐old restoration had greater SOC and TN mass than crop averages. These results suggest that the loss of SOC in the A horizon of the soils on this floodplain through agriculture has likely been small. Additionally, the redistribution of SIC through the soil profile has had a significant impact on the total C stored in the plow layer, but not on the net C sequestered or released to the atmosphere through land use.