Phosphorus and Iron Retention in Sediments Measured by Mass Budget Calculations and Directly

Abstract
Retention of P and Fe was estimated from mass budget calculations of Bob Lake, Ontario [Canada]. Ratios of Fe to P in sediment cores were used to test the reliability of the concurrent retention estimated. A 300% range in Fe to P ratios measured in vertical profiles in sediments was many times larger than the uncertainty associated with mass budget measurements. Sediment cores showed a near-surface maximum of Fe but not P. For P retention, mass budget computation agreed reasonably well with sediment accumulation methods, though the latter were slightly higher.

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