Retention of solutes by clayey Coastal Plain soils
A study was conducted to determine solute retention and movement rates under bare soil conditions on two clayey coastal plain soils, Faceville sandy loam and Greenville sandy clay loam. Both soils have high clay contents in the subsoil, but the Faceville is sandier at the surface. Nitrate (NO 3 -N)...
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Published in | Journal of soil and water conservation Vol. 49; no. 1; pp. 90 - 96 |
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Main Authors | , |
Format | Journal Article |
Language | English |
Published |
Ankeny, IA
Soil and Water Conservation Society
01.01.1994
Soil & Water Conservation Society |
Subjects | |
Online Access | Get full text |
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Summary: | A study was conducted to determine solute retention and movement rates under bare soil conditions on two clayey coastal plain
soils, Faceville sandy loam and Greenville sandy clay loam. Both soils have high clay contents in the subsoil, but the Faceville
is sandier at the surface. Nitrate (NO 3 -N) and bromide (Br) sources were applied at the rate of 125 kg/ha. Replicate samples were taken over time by depth from each
soil and analyzed for NO 3 -N and Br. Under natural rainfall, 45 to 95 percent of these highly soluble chemicals were retained in the top meter of soil
nine months after application. After one and a half years the solutes had moved to a depth of about one meter. The study showed
that agrichemicals were retained for an extended period of time in the top meter of these clayey soils. High background NO 3 -N levels found in the Faceville soil indicated that an N buildup may occur in the root zone of clayey coastal plain soils
under commonly used N application rates. |
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Bibliography: | P33 9439264 ObjectType-Article-1 SourceType-Scholarly Journals-1 ObjectType-Feature-2 content type line 23 |
ISSN: | 0022-4561 1941-3300 |