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Abstract

An attempt was made to determine the correlation between the granulometric structure of bottom sediments and the content of speciation forms of phosphorus and selected metals. Using the sedimentation method, the bottom sediments of a thermally contaminated dam reservoir were divided into fast and slow-draining fractions. Measurements of granulometric composition were made, determining the volume proportions of sediment particles in the range of 0.1 m to 650 m. Particle share sizes were determined in the size range: 0.1–50 m (F1), 50–100 m (F2), 100–200 m (F3), 200–400 m. (F4). The study showed that the content of speciation forms of phosphorus and selected metals remains related to the granulometric structure of bottom sediments. The content of organic matter in sediments is determined by the proportion of the smallest particles, from 0.1 to 50 μm, at the same time these particles most strongly aff ect the reduction conditions of sediments. According to Gilford›s correlation thresholds, there was no correlation between the proportion of sediment particles with dimensions of 0.1–50 μm and the concentration of speciation forms of phosphorus. For particles with dimensions of 50–100 μm, the strongest correlation was observed for the concentration of the EP fraction and for the WDP fraction (r2 = 0.4048, r2 = 0.3636). A strong correlation between the size of sediment particles and the concentration of speciated forms of phosphorus was noted for particles with dimensions of 100–200 μm and 200–400 μm. The coeffi cient of determination was for AAP, EP, WDP and RDP, respectively: 0.8292, 0.891, 0.7934, 0.47. The relationship between particles in the 0.1–50 m range and iron (Fe) concentration, R2 – 0.3792, aluminum (Al) R– 0.3208, and zinc (Zn) R2 – 0.4608, was classifi ed as medium. For particles in the 50–100 m range, a medium correlation with calcium (Ca) and magnesium (Mg) concentrations is apparent, R2 0.4443 and 0.3818, respectively. For particles 100–200 mm and 200–400 mm, an almost full correlation is noted for iron (Fe) R2 – 0.9835, aluminum (Al) R2 – 0.9878, calcium (Ca) R2 – 0. 824, very strong for manganese (Mn) R2 – 0.6817, and zinc (Zn) R2 – 0.7343. There is a very strong correlation between the concentration of the AAP fraction with the concentration of iron (Fe) R2 – 0.8694 and a strong correlation between the concentration of EP with the concentration of iron (Fe) R2 – 0.609. There is a strong correlation between the concentration of the AAP and EP fractions with the concentration of aluminum (Al) R2 – 0. 6253 and 0.8327. The concentration of AAP and EP fractions with the concentration of calcium (Ca) R2 – 0.5941 and 0.7576 remains in a strong relationship. The correlation between the concentration of RDP fractions and the concentration of magnesium (Mg) and manganese (Mn) remains in a medium relationship. The concentration of the EP fraction (Olsen-P) is in a strong relationship with the concentration of organic matter (R2 –.0.6763). No correlation was found between the concentration of the residuum form and the concentrations of organic matter, iron (Fe) and aluminum (Al). A medium correlation was found between the concentration of the residuum form and the concentration of calcium (Ca), magnesium (Mg), manganese (Mn) – R2 = 0.4206 and zinc (Zn).
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Authors and Affiliations

Maciej Kostecki
1
ORCID: ORCID

  1. Institute of Environmental Engineering, PAS, Zabrze, Poland
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Abstract

Hydropower use of watercourses has tangible consequences for the environment, society and economy. Based on a literature review and their own research, the authors present current data on changes in the ecological status of waters within run-of-river and reservoir hydropower plants, i.e. changes in biological elements (benthic macroinvertebrates, plankton, ichthyofauna, macrophytes), as well as hydromorphological and physicochemical changes. Previous researchers have noted that the impact of hydropower use of rivers on ecological status of those rivers is extensive, consisting of, among others, changes in species structure and populations of macrophytes, benthic macroinvertebrates, plankton and ichthyofauna (positive as well as negative changes), algal blooms due to increased turbidity, constrained migration of water organisms, changes in temperature within hydroelectric power plants, the phenomenon of supersaturation, eutrophication, changes in hydrological conditions (e.g., increased amplitudes of diurnal water levels and their consequent annual reduction), and increased erosion below the damming and deposition of bottom sediments on the damming barriers. In addition to such changes in ecological status, hydropower use also has a visible impact on socio-economic conditions (e.g., living standards of the population) and the environment (e.g., quality of bottom sediments and biodiversity). The article offers an assessment of the impact of hydropower use of rivers on ecological status (biological, hydromorphological, physicochemical elements and hydrological conditions of such rivers), society, economy and environment; it also proposes a research scheme to assess the impact of hydropower structures.
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Authors and Affiliations

Paweł Tomczyk
1
Mirosław Wiatkowski
1

  1. Institute of Environmental Engineering, Wrocław University of Environmental and Life Sciences, Poland

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