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Phosphorus fractionation in lake sediments – Lakes
Phosphorus fractionation in lake sediments – Lakes
Volvi and Koronia, N. Greece
A. Kaiserli, D. Voutsa *, C. Samara
Environmental Pollution Control Laboratory, Chemistry Department, Aristotle University, GR-54006 Thessaloniki, Greece
Received 10 July 2001; received in revised form 4 October 2001; accepted 17 October 2001
Abstract
Sediments from two lakes, the meso-to-eutrophic Volvi and the hypertrophic Koronia, located in N. Greece were
examined on the basis of P-fractionation. In both lakes, the rank order of P-fractions was HCl–P NaOH–P
BD–P NH4Cl–P. The loosely sorbed phosphorus eNH4Cl–PT represented 1% of the sedimentary inorganic
phosphorus, while the reductant phosphorus (BD–P) ranged 5–6%. The calcium bound phosphorus (HCl–P) showed
considerable contribution (59–74%) to the sedimentary inorganic P-loads. The metal oxide bound phosphorus (NaOH–
P) was higher in the hypertrophic (30–35%) than in the meso-to-eutrophic system (19–28%). Fine-sized sediments
exhibited significantly higher concentrations of HCl–P in Volvi and NH4Cl–P in Koronia. Sampling month had sig-
nificant effect in variance of most P-fractions and other sediment features in both lakes. Use was also made of mul-
tivariate statistics to identify the factors which influence the sedimentary phosphorus. NaOH–P was the most reactive
fraction in Lake Volvi. Iron compounds and organic matter seem to play a significant role in regulating this labile
P-budget. NH4Cl–P was the more reactive fraction in Lake Koronia which was influenced by sedimentation of
P-absorbed on clay/silt fine particles. 2002 Elsevier Science Ltd. All rights reserved.
Keywords: Grain size; Lakes; PCA; Phosphorus; P-fractions; Sediment; Trophic status
1. Introduction
Phosphorus has been recognized as the most critical
nutrient limiting lake productivity. The main sources of
phosphorus in lakes are external point and non-point
sources such as rainfall, runoff, soil leaching, industrial
and municipal effluents. Moreover, there
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