Phosphate removal by peat from peat mining drainage water during overland flow wetland treatment

• Published in: Journal of Environmental Quality
• Main Authors: Heikkinen, Kaisa, Ihme, Raimo, Osma, Anna-Mari, Hartikainen, Helinä
• Format: Article in Journal/Newspaper
• Language: English
• Published: 1995
• Subjects: Langmuir; Northern Finland
• Online Access: https://cris.vtt.fi/en/publications/ca8e0e74-489a-442f-af2a-6abcd1e59c00; https://doi.org/10.2134/jeq1995.00472425002400040007x

Overland flow technique, which involves conducting wastewater across a natural mire, has during the recent years been widely used in Finland to decrease the loading of P and other elements from peat mining areas to the watercourses. In this study the applicability of laboratory tests in estimating the P retention by overland flow areas was assessed at a site in northern Finland. The ability of peat to retain PO4-P was determined by adsorption isotherms, and the data were compared with the actual decreases in P loads obtained in the field. The PO4-P retention curves obeyed rather well the conventional adsorption models, which suggests that sorption can be an important mechanism removing PO4-P from the peat mining drainage water during overflow treatment. The Freundlich equation gave a better fit to the P sorption than did the one-surface Langmuir model. The constants describing the sorption characteristics of the peat showed spatial and temporal variation. They indicated, however, that the theoretical effective P sorption time for the overland flow area can be 20 to 25 yr. The ability of peat to retain P increased with increasing concentrations of oxalate extractable Fe and Al. Sorption reactions were found to be important in the annual decreases in PO4-P from drainage waters in an overland flow area, but their efficiency in removing P from the peat mining drainage water appears to depend on hydrological conditions. In the first experimental year, the sorption calculated from the isotherm data amounted to 60% of the retention obtained in the field. Owing to the high flow conditions in the second year, the decrease in the loading of P in the field was decisively lower than estimated