Soil physical and hydrological properties under three biofuel crops in Ohio |
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Authors: | Catherine Bonin Rattan Lal Matthias Schmitz S. Wullschleger |
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Affiliation: | 1. The Ohio State University , School of Environment and Natural Resources, Carbon Management and Sequestration Center , 210 Kottman Hall, 2021 Coffey Rd, Columbus , OH , USA bonin.8@osu.edu;3. The Ohio State University , School of Environment and Natural Resources, Carbon Management and Sequestration Center , 210 Kottman Hall, 2021 Coffey Rd, Columbus , OH , USA;4. Rheinische Friedrich/Wilhelms-Universitaet Bonn, Steinmann Institut für Geologie , Mineralogie und Palaeontologie Nussallee 8 , 53115 , Bonn , Germany;5. The Oakridge National Laboratory , Oakridge , TN , USA |
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Abstract: | Abstract While biofuel crops are widely studied and compared for their energy and carbon footprints, less is known about their effects on other soil properties, particularly hydrologic characteristics. Soils under three biofuel crops, corn (Zea mays), switchgrass (Panicum virgatum), and willow (Salix spp.), were analyzed seven years after establishment to assess the effects on soil bulk density (ρb), penetration resistance (PR), water-holding capacity, and infiltration characteristics. The PR was the highest under corn, along with the lowest associated water content, while PR was 50–60% lower under switchgrass. In accordance with PR data, surface (0–10 cm) bulk density also tended to be lower under switchgrass. Both water infiltration rates and cumulative infiltration amounts varied widely among and within the three crops. Because the Philip model did not fit the data, results were analyzed using the Kostiakov model instead. Switchgrass plots had an average cumulative infiltration of 69 cm over 3 hours with a constant infiltration rate of 0.28 cm min?1, compared with 37 cm and 0.11 cm min?1 for corn, and 26 cm and 0.06 cm min?1 for willow, respectively. Results suggest that significant changes in soil physical and hydrologic properties may require more time to develop. Soils under switchgrass may have lower surface bulk density, higher field water capacity, and a more rapid water infiltration rate than those under corn or willow. |
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