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Carbon Management and Sequestration Center, FAES/OARDC, School of Environment and Natural Resources, Ohio State Univ., 2021 Coffey Rd., Columbus, Ohio 43210-1085
* Corresponding author (blanco.16{at}osu.edu).
Crop residues left on the soil surface conserve soil and water, but residue impacts on near-surface soil hydraulic properties have not been widely studied. Therefore, soil hydraulic properties were determined under uncropped no-tillage (NT) plots receiving three levels of wheat (Triticum aestivum L.) straw mulch (0, 8, and 16 Mg ha1 yr1) application for 10 consecutive yr on a Crosby silt loam (fine, mixed, active, mesic Aeric Epiaqualfs) in central Ohio. Water infiltration rates, earthworm population, saturated hydraulic conductivity (Ksat), soil water retention (SWR), total porosity, and pore-size distribution were determined and unsaturated hydraulic conductivity was estimated from SWR and Ksat data. Mulching significantly impacted hydraulic properties in the 0- to 3-cm soil depth (P < 0.01), but water infiltration rate was unaffected. Earthworm counts were 0 m2 in the unmulched treatment, 158 ± 52 m2 (mean ± SD) in treatments with 8 Mg ha1 yr1 of straw, and 267 ± 58 m2 in those with 16 Mg ha1 yr1 of straw. Mulched treatments had a Ksat 123 times greater and retained 40 to 60% more water between 0 and 1500 kPa than the unmulched treatment. Soil porosity increased by 28% under 8 Mg ha1yr1 of straw and by 44% under 16 Mg ha1yr1 in the 0- to 3-cm depth compared with the unmulched treatment. Pore volume of macro- and mesopores was greater in mulched treatments and that of fine mesopores was greater in the unmulched treatment in the 0- to 3-cm depth. Straw mulching appears to be a viable practice to improve near-surface hydraulic properties in long-term NT soils, although residues may not increase water infiltration rates.
Abbreviations: Ksat, saturated hydraulic conductivity K(
), unsaturated hydraulic conductivity NT, no-tillage SOC, soil organic carbon SWR, soil water retention
, volumetric water content
e, effective porosity
b, bulk density.
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