Water, Air, and Soil Pollution

, Volume 204, Issue 1, pp 139–153

Phosphorus Fractionation in Sediment Cores Collected In 2005 Before and After Onset of an Aphanizomenon flos-aquae Bloom in Upper Klamath Lake, OR, USA

Authors

    • U.S. Geological Survey432 National Center study
  • Dennis Lynch
    • U.S. Geological Survey Oregon Water Science Center
  • Thomas N. Gallaher
    • Department of ChemistryJames Madison University
Article

DOI: 10.1007/s11270-009-0033-9

Cite this article as:
Simon, N.S., Lynch, D. & Gallaher, T.N. Water Air Soil Pollut (2009) 204: 139. doi:10.1007/s11270-009-0033-9

Abstract

We tested the hypothesis that there would be measurable losses of phosphorus (P) from surficial sediments of Upper Klamath Lake (UKL), Oregon, if sediments were a source of P during an algal bloom. We compared concentrations of total and forms of P at various depths in cores collected before and after the onset of a large Aphanizomenon flos-aquae bloom. Concentrations of inorganic P were determined in extraction solutions of MgCl2 (1 M, pH 8), citrate-dithionite-bicarbonate, and 1 M HCl. Sediments below 2 cm were dominated by residual P which is defined as total P minus inorganic P. During the study period, data from the top 2-cm of sediment indicated (a) significant decrease in total P concentration, primarily associated with iron oxyhydroxides at one site, and (b) significant increase in total P concentration associated with residual P at a second site. Data from two other sites indicated no net changes in concentrations of total P.

Keywords

Phosphorus fractionationResidual phosphorusCyanophyteEutrophicShallow lakeMetals

Copyright information

© US Government 2009