Approximately 95% of the total P in runoff from clean tilled row-crop fields is transported with the eroded sediment (about 2 lb total P per ton of sediment or 0.1%). In close-seeded crops, such as alfalfa and small grain, erosion is minimal and about 95% of the total P is dissolved with the water. In general, total P losses are not large. For some 30-plus surface irrigated fields, the median P loss was 4.9 lbs/A for an irrigation season while the soluble P loss was 3.5 lbs P/A (Table 3).
Total P concentration in surface irrigation runoff
correlates with sediment concentration, but not soil test P concentrations
(Table
4). Runoff dissolved P (DRP) and biologically available P (FeO-P)
concentrations, on the other hand, correlate with soil test P concentrations,
but not with runoff sediment concentration.
Table 3. Surface Irrigation Seasonal Losses
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| Soil Erosion, tons/A |
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| Soluble P, lbs/A |
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| Total P, lbs/A |
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Table 4. Linear Correlation Coefficients Between Average Runoff P Concentrations and Furrow Soil P Tests
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| Average Runoff P |
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| DRP |
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| FeO-P |
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| Total-P |
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