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Factors influencing the accumulation of Pb in sediments of deep and shallow dam reservoirs Cover

Factors influencing the accumulation of Pb in sediments of deep and shallow dam reservoirs

Open Access
|May 2017

Figures & Tables

Figure 1

Location of the sampling sites. Identification of groups (clusters) with similar sediment granulations
Location of the sampling sites. Identification of groups (clusters) with similar sediment granulations

Figure 2

Distribution of selected parameters in Czorsztyn and Goczałkowice Reservoirs (A,B,C,D,E,F – lengthwise transects)
Distribution of selected parameters in Czorsztyn and Goczałkowice Reservoirs (A,B,C,D,E,F – lengthwise transects)

Figure 3

Hierarchical cluster analysis based on sediment granulation in Czorsztyn (CR) and Goczałkowice (GR) Reservoirs. The content of clay and silty clay fractions (range) as well as Pb (mean) in different clusters is given.
Hierarchical cluster analysis based on sediment granulation in Czorsztyn (CR) and Goczałkowice (GR) Reservoirs. The content of clay and silty clay fractions (range) as well as Pb (mean) in different clusters is given.

Relationship (Pearson’s correlation coefficients) between the particle size, the content of organic matter and Pb in sediment, and depth of Czorsztyn Reservoir (N=26) and Goczałkowice Reservoir (N=26)

ReservoirParameterSilty clay fractionSand fractionOrganic matterDepthPb
CzorsztynClay fractionns-0.75p = 0.0000.74p = 0.0000.93p = 0.0000.69p = 0.000
Silty clay fraction-0.93p = 0.0000.69p = 0.000ns0.73p = 0.000
Sand fraction

– concentration of Pb in the 0.2-0.063 mm sand fraction; ns – statistically insignificant (level of significance p>0.05)

-0.83p = 0.000-0.61p = 0.001-0.83p = 0.000
Organic Matter0.62p = 0.0010.86p = 0.000
Depth0.60p = 0.001
GoczałkowiceClay fraction0.53p = 0.005-0.70p = 0.0000.58p = 0.0020.75p = 0.0000.84p = 0.000
Silty clay fraction-0.98p = 0.0000.73p = 0.000ns0.73p = 0.000
Sand fraction

– concentration of Pb in the 0.2-0.063 mm sand fraction; ns – statistically insignificant (level of significance p>0.05)

-0.76p = 0.000-0.58p = 0.002-0.83p = 0.000
Organic matterns0.77p = 0.000
Depth0.74p = 0.000

Mean Pb concentrations and values of the environmental parameters in the sediments of Czorsztyn Reservoir and Goczałkowice Reservoir in the studied clusters

ReservoirClusterPb(μg g-1)Organic matter(%)Depth(m)Fraction (%)
SandSilty clayClay
CzorsztynI8.12.06.773.222.14.7
II18.55.02.744.150.75.2
III20.45.312.625.261.113.6
IV27.48.17.37.480.312.3
V31.69.025.43.170.326.6
GoczałkowiceI15.31.52.491.56.22.2
II23.33.93.461.930.77.5
III41.89.94.429.455.615.0
IV48.29.96.48.777.813.5

Significant differences in the values of the environmental parameters and Pb concentrations in the sediments of Czorsztyn Reservoir and Goczałkowice Reservoir between the clusters (Mann-Whitney test)

ClustersPbOrganic matterDepthSandSilty clayClay
significance level (p)
Czorsztyn Reservoir (CR)
I, II0.02010.0196-0.02010.0201-
I, III---0.02530.02530.0253
I, IV0.03390.0339-0.03390.03390.0339
I, V0.01410.01640.01340.01400.01400.0143
II, III--0.00720.00620.01760.0062
II, IV0.01090.01030.01210.01050.01050.0105
II, V0.00300.00420.00150.00190.00300.0019
III, IV-0.0275-0.01430.0143-
III, V0.00830.01830.00770.00340.02810.0281
IV, V0.0500-0.0061-0.00660.0066
Goczałkowice Reservoir (GR)
I, II-0.0085-0.00520.00540.0344
I, III0.00870.0054-0.00530.00530.0054
I, IV0.02090.02090.02190.01940.02020.0384
II, III0.00410.0023-0.00030.00030.0132
II, IV0.00550.00540.03700.00540.0054-
III, IV---0.00540.0054-

Mean Pb concentrations, standard deviations and the significance levels of Pb concentrations between the old Dunajec river bed and the Czorsztyn Reservoir and the old Vistula river bed and the Goczałkowice Reservoir (Mann-Whitney test)

ReservoirAreaNPb (μg∙g-1)Significance level
CzorsztynOld river bed729.1 ± 4.90.046
Remaining area1920.9 ± 9.4
GoczałkowiceOld river bed941.7 ± 14.20.025
Remaining area1727.3 ± 12.7

Characteristics of Czorsztyn and Goczałkowice dam reservoirs (Mazurkiewicz-Boroń 2002; Czaplicka-Kotas 2004)

ParameterCzorsztyn Reservoir (CR)Goczałkowice Reservoir (GR)
In operation since19971956
Normal Water Level (NWL)529.0257.0
Capacity (million m3)231.9166.7
Surface area (km2)10.532
Mean depth (m)19.05.3
Max depth (m)4614
Length (km)1112
Width (km)ca. 12-6
Water exchange (times per year)3.31.5
Water exchange (days)111238

Differences in the values of environmental parameters and Pb concentrations in the sediments of Czorsztyn Reservoir and Goczałkowice Reservoir between the studied transects (Mann-Whitney test); only significant differences are noted

ReservoirParameterTransectsZp
CzorsztynPbA-B-2.150.031
A-C-2.170.030
Sand fractionA-B2.050.041
Silty clay fractionA-C-2.260.024
Organic matterA-B-2.050.042
A-C-2.170.030
GoczałkowicePbE-F2.570.010
Sand fractionE-F-2.050.041
Clay fractionE-F3.260.001
Organic matterE-F2.050.041
DepthE-F2.210.027
DOI: https://doi.org/10.1515/ohs-2017-0018 | Journal eISSN: 1897-3191 | Journal ISSN: 1730-413X
Language: English
Page range: 174 - 185
Submitted on: Jul 15, 2016
Accepted on: Sep 16, 2016
Published on: May 31, 2017
Published by: University of Gdańsk
In partnership with: Paradigm Publishing Services
Publication frequency: 4 issues per year

© 2017 Anna Czaplicka, Ewa Szarek-Gwiazda, Zbigniew Ślusarczyk, published by University of Gdańsk
This work is licensed under the Creative Commons Attribution-NonCommercial-NoDerivatives 4.0 License.