HOME HELP FEEDBACK SUBSCRIPTIONS ARCHIVE SEARCH TABLE OF CONTENTS		QUICK SEARCH:   [advanced] Author: Keyword(s): Year:  Vol:  Page:

This Article Full Text (PDF) Alert me when this article is cited Alert me if a correction is posted Services Similar articles in this journal Alert me to new issues of the journal Download to citation manager Citing Articles Citing Articles via Google Scholar Google Scholar Articles by Shaw, J. F. H. Articles by Prepas, E. E. Search for Related Content PubMed Articles by Shaw, J. F. H. Articles by Prepas, E. E. Agricola Articles by Shaw, J. F. H. Articles by Prepas, E. E.

Exchange of Phosphorus from Shallow Sediments at Nine Alberta Lakes

Dep. of Zoology and Meanook Biological Res. Station, CW-312 Biological Sciences Ctr., The Univ. of Alberta, Edmonton, AB T6G 2E9.

^* Corresponding author.

ABSTRACT

Potential exchange of P between sediments and lakewater and particulate sediments and porewater was evaluated in nine eutrophic lakes in Alberta. Lakewater above the sediments, porewater, and sediments were collected from shallow depths during May to August 1986. Lakewater soluble-reactive P concentrations ([SRP]) were positively correlated with porewater [SRP] (P < 0.01) and negatively with the Fe/P molar ratio in porewater (P < 0.001). Potential release of SRP from sediments to lakewater (by molecular diffusion) was positively correlated with particulate P fractions that are known to exchange P with water (P < 0.01). In porewater, [SRP] was positively correlated with Fe²⁺ concentration and weakly correlated with pH (P < 0.001 and 0.05, respectively). These results indicate (i) potential transport of P from sediments to lakewater when Fe is not abundant, (ii) common sources and similar mobilities of Fe and P, and (iii) importance of pH in regulation of P exchange between particulate sediments and porewater. No significant relationships (P > 0.05) were found between porewater [SRP] and particulate P fractions. In this study, correlation coefficients were generally low, which suggests (i) the chemical fractionation of particulate sediments failed to isolate the exchangeable P fraction and (ii) partitioning of P within sediments and the release of P from sediments to lakewater are complex processes, only partially regulated by pH and Fe²⁺ in porewater. To gain better understanding of P release from shallow sediments, future studies should include possible interactions between P and redox potential, Al, Mn, Ca, and S.