沉积物在水结构中的行为

N. Junakova, J. Junák
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引用次数: 0

摘要

海底沉积物是水生生态系统的自然组成部分。它们日益加剧水道和水库的恶化,是一种不受欢迎的材料,造成各种严重的环境和技术问题。最重要的问题包括河床的不稳定,化学物质、营养物质和有机化合物的运输,沉积物向水库的供应。海底沉积物有能力将重金属、放射性核素、营养物质和有机物等各种主要有害物质结合在其表面。这些沉积物对水系统构成危险,可能使污染物重新进入水中。本文主要研究了斯洛伐克东部Hervartov小水库沉积物的行为及其在沉积物-水界面吸附磷的能力。结果表明,细粒和粗粒沉积物对水环境中磷的吸收效率在最低的磷输入浓度下和沉积物以上的低浓度地表水时最高。在这些浓度下,细粒沉积物吸收磷的量几乎达到99%。粗粒度沉积物吸收的磷含量高达84%。随着溶液中磷浓度的增加,沉积物的吸附效率下降,而在山梨酸浓度较高时,由于达到底部沉积物的最大吸附量,吸附过程明显稳定。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Behaviour of Sediments in Water Structures
Bottom sediments are a natural part of aquatic ecosystems. They are increasingly contributing to the deterioration of watercourses and reservoirs and are an undesirable material that causes various serious environmental and technical problems. The most significant problems include the instability of riverbeds, the transport of chemicals, nutrients and organic compounds, the supply of sediments to water reservoirs. Bottom sediments have the ability to bind to their surface various predominantly harmful substances such as heavy metals, radionuclides, nutrients and organic substances. Such sediments pose a risk to the water system in terms of possible remobilization of pollutants into the water. This paper is focused on the study of behavior of sediments in the Hervartov small water reservoir located in the east of Slovakia and their ability to adsorb phosphorus at the sediment-water interface. The results show that the efficiency of sorption of phosphorus from the aqueous environment by fine and coarse-grained sediments is the highest at the lowest input concentrations of phosphorus in solution, or at low concentrations in surface water above the sediment. At these concentrations, the amount of sorbed phosphorus by fine-grained sediments was up to almost 99%. The coarse-grained sediments sorbed phosphorus at a level of up to 84%. Increasing the concentration of phosphorus in the solution leads to a decrease in the sorption efficiency of the sediment, while at high concentrations of the sorbate, the sorption process is significantly stabilized due to reaching the maximum sorption capacity of bottom sediments.
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