Published online 6 May 2005
Published in Soil Sci Soc Am J 69:893-901 (2005)
DOI: 10.2136/sssaj2004.0280
© 2005 Soil Science Society of America
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Influence of Grass and Agroforestry Buffer Strips on Soil Hydraulic Properties for an Albaqualf
Tshepiso Seobia,
S. H. Andersonb,*,
R. P. Udawattac and
C. J. Gantzerb
a North West Provincial Dep. of Agriculture, Soil Science Section, Private Bag X804, Botha Street, Potchefstroom, South Africa 2520
b Dep. of Soil, Environmental and Atmospheric Sciences, 302 Anheuser-Busch Natural Resources Building, Univ. of Missouri, Columbia, MO 65211
c Center for Agroforestry, 203 Anheuser-Busch Natural Resources Building, Univ. of Missouri, Columbia, MO 65211

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Fig. 1. Topographic map of study site with 0.5-m elevation interval contour lines (thin black lines), agroforestry buffer strips (wide gray lines), and sampling region (superimposed box). A grass waterway is located at the outflow end of the watershed (wider gray line; modified from Udawatta et al., 2002). The inset map shows location of watershed in Missouri.
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Fig. 2. Soil water retention curves for row crop (RC), grass buffer (GB), and agroforestry buffer (Ag) treatments at depths of (A) 0 to 10 cm, (B) 10 to 20 cm, (C) 20 to 30 cm, and (D) 30 to 40 cm. Bars indicate LSD (0.05) values and are presented at pressures when significant differences occurred among treatments.
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Fig. 3. Porosity values for selected pore-size classes for row crop (RC), grass buffer (GB), and agroforestry buffer (Ag) treatments as influenced by soil depth. Pore-size classes include (A) macropores (>1000-µm diam.), (B) coarse mesopores (60- to 1000-µm diam.), (C) fine mesopores (10- to 60-µm diam.), and (D) micropores (<10-µm diam.). Bars indicate LSD (0.05) values and are presented for pore-size classes with significant differences among treatments.
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Fig. 4. (A) Bulk density and (B) saturated hydraulic conductivity (Ksat) for row crop (RC), grass buffer (GB), and agroforestry buffer (Ag) treatments as influenced by soil depth. (A) The bar indicates the LSD (0.05) value for bulk density, and (B) the LDS (0.05) value for Ksat is listed on the graph due to the log scale.
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Copyright © 2005 by the Soil Science Society of America.