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a USDA-ARS, Columbia Plateau Conservation Research Center, P.O. Box. 370, Pendleton, OR 97801
b USDA-ARS, Dep. of Soil, Water, and Climate, Univ. of Minnesota, St. Paul, MN 55108
* Corresponding author (hero.gollany{at}oregonstate.edu)
Long-term experiments are ideal for evaluating the influence of agricultural practices on soil organic carbon (SOC) accretion. Little is known about the influence of tillage and N fertilization on SOC distribution and silica (Si) movement in a soil. This study: (i) determined the effect of tillage and N fertilizer on SOC accretion in a Walla Walla silt loam (coarse-silty, mixed, superactive, mesic Typic Haploxeroll), and (ii) examined the subsequent influence of fine organic matter (FOM) on Si movement. A long-term wheat (Triticum aestivum L.)fallow experiment was established in 1940, in a randomized block with split-plot design. Soil cores (2-cm increments) from two tillages (moldboard plow, MP; and sweep, SW) and two N rates (45 and 180 kg N ha1) were used to measure coarse organic matter (COM), FOM, pH, bulk density (
b), water-soluble C (Cws), and water-soluble Si (Siws). The FOM fraction (6.6 kg C m2) in SW was 14% higher (5.8 kg C m2) than in MP for the 180 kg N ha1 rate. After 44 yr of N additions, the SOC storage (6.2 kg C m2) for the 180 kg N ha1 rate increased 3% above that for the 45 kg N ha1 (6.0 kg C m2). Total Siws in the B horizon were 34 and 39% greater than in the Ap horizon for the MP and SW systems, respectively. Interaction of tillage and N with Siws suggests that SOC provides a mechanism to suppress Si solubility, which impacts siliceous pan formation, reduces soil mechanical resistance, and enhances drainage and plant growth.
Abbreviations:
b, bulk density Cws, water soluble carbon COM, coarse organic matter D, soil depth FOM, fine organic matter Ksat, saturated hydraulic conductivity MP, moldboard plow tillage Siws, water soluble Si SOC, soil organic carbon SON, soil organic nitrogen SW, sweep tillage
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