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Updated: Jun 26, 2026

Laboratory-determined Phosphorus Flux from Lake Sediments as a Measure of Internal Phosphorus Loading
Published on: March 6, 2014
Phosphorus retention patterns along the Tisza River, Hungary
A Kovács1, Zs Kozma, V Istvánovics
1Department of Sanitary and Environmental Engineering, Budapest University of Technology and Economics, Miiegyetem rakpart 3, H-1111, Budapest, Hungary. kovax@vkkt.bme.hu
This study assessed suspended solids (SS) and total phosphorus (TP) retention in the Tisza River. The river retained 42% of TP, with reservoirs significantly impacting this pattern.
Area of Science:
- Environmental Science
- Hydrology
- Water Quality Management
Background:
- Large rivers play a crucial role in nutrient cycling and sediment transport.
- Understanding in-stream nutrient retention is vital for effective water resource management.
- The Tisza River, a significant European watercourse, faces challenges related to water quality and flow dynamics.
Purpose of the Study:
- To quantify in-stream retention of suspended solids (SS) and total phosphorus (TP) in the Tisza River under low flow conditions.
- To analyze the influence of river morphology and flow dynamics on SS and TP transport and retention.
- To investigate the impact of storage reservoirs on longitudinal nutrient retention patterns.
Main Methods:
- Conducted a longitudinal water quality survey along the Hungarian section of the Tisza River (approx. 600 km).
- Collected manual water samples for SS and TP analysis and utilized on-line turbidity data for SS concentration estimation.
- Employed a 1D hydrodynamic model to calculate the velocity field and applied a first-order equation to model SS transport and TP retention.
Main Results:
- Total phosphorus (TP) retention reached 42% along the studied section of the Tisza River at a flow rate of 110 m(3) s(-1).
- Storage reservoirs significantly altered the longitudinal retention pattern, with net TP retention of 73% upstream of Dam II.
- The downstream section of the river acted as a source of TP, indicating complex nutrient dynamics.
Conclusions:
- The Tisza River exhibits substantial in-stream TP retention, particularly influenced by reservoir structures.
- Flow velocity and riverbed characteristics are key factors governing SS and TP transport and deposition.
- Effective management strategies for the Tisza River should consider the role of reservoirs in nutrient retention and potential downstream TP release.
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