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• W2010099012 abstract "Agroforestry buffers have been introduced in temperate areas to improve water quality and diversify farm income. The objective of this study was to evaluate saturated hydraulic conductivity and water retention for soils managed under rotationally grazed (RG) pasture, continuously grazed (CG) pasture, grass buffers (GB), and agroforestry buffers (AgB). Pasture and GB areas included red clover (<i>Trifolium pretense</i> L.) and lespedeza (<i>Kummerowia stipulacea</i> Maxim.) planted into fescue (<i>Festuca arundinacea</i> Schreb.) while AgB included Eastern cottonwood trees (<i>Populus deltoids</i> Bortr. ex Marsh.) planted into fescue. Water retention data were measured at -0.4, -1.0, -2.5, -5.0, -10, -20, and -30 kPa (-0.058, -0.145, -0.363, -0.725, -1.45, -2.90, -4.35 pounds per square inch [psi]) soil water pressures using 76 mm (3.00 in) diameter by 76 mm long cores from the 0 to 10 cm, 10 to 20 cm, 20 to 30 cm, and 30 to 40 cm (0 to 3.94 in, 3.94 to 7.87 in, 7.87 to 11.81 in, and 11.81 to 15.75 in) depths. Soil bulk density was 12.6% higher for the RG and CG treatments (1.41 and 1.45 g cm^-3 [88.02 and 90.52 lb ft^-3]) than the GB and AgB treatments (1.25 and 1.29 g cm^-3 [78.03 and 80.53 lb ft^-3). Soil water content at high soil water potentials (0 and -0.4 kPa) was greater in the buffer treatments relative to the other treatments for the 0 to 10 cm soil depth. Soil macroporosity (>1,000 µm [>0.0394 in] diameter) was 5.7, 4.5, and 3.9 times higher, respectively, for the AgB, GB, and RG treatments compared to the CG treatment for the 0 to 10 cm soil depth. Buffer treatments had greater macroporosity (>1,000 µm diameter), coarse (60 to 1,000 µm [0.00236 to 0.0394 in] diameter) and fine mesoporosity (10 to 60 µm [0.000394 to 0.00236 in] diameter), but lower microporosity (<10 µm diameter) compared to RG and CG treatments. Saturated hydraulic conductivity values for GB and AgB treatments were 16.7 times higher (56.95 vs. 61.33 mm h^-1 [2.24 vs. 2.41 in hr^-1]) compared with RG and CG (3.98 vs. 3.11 mm h^-1 [0.157 vs. 0.122 in hr^-1]). This study illustrates that agroforestry and grass buffers maintained higher values for soil hydraulic properties compared to grazed pasture systems." @default.
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• W2010099012 date "2008-07-01" @default.
• W2010099012 modified "2023-10-03" @default.
• W2010099012 title "Soil hydraulic properties influenced by agroforestry and grass buffers for grazed pasture systems" @default.
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• W2010099012 doi "https://doi.org/10.2489/jswc.63.4.224" @default.
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