Phosphate sorption by three potential filter materials as assessed by isothermal titration calorimetry
Phosphorus eutrophication of lakes and streams, coming from drained farmlands, is a serious problem in areas with intensive agriculture. Installation of phosphate (P) sorbing filters at drain outlets may be a solution. The aim of this study was to improve the understanding of reactions involved in P...
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Published in | Journal of environmental management Vol. 143; pp. 26 - 33 |
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Main Authors | , , , |
Format | Journal Article |
Language | English |
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01.10.2014
Elsevier Academic Press Ltd |
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Abstract | Phosphorus eutrophication of lakes and streams, coming from drained farmlands, is a serious problem in areas with intensive agriculture. Installation of phosphate (P) sorbing filters at drain outlets may be a solution. The aim of this study was to improve the understanding of reactions involved in P sorption by three commercial P sorbing materials, i.e. Ca/Mg oxide-based Filtralite-P, Fe oxide-based CFH-12 and Limestone in two particle sizes (2–1 mm and 1–0.5 mm), by means of isothermal titration calorimetry (ITC), sorption isotherms, sequential extractions and SEM-EDS. The results indicate that P retention by CFH is due to surface complexation by rapid formation of strong Fe–P bonds. In contrast, retention of P by Filtralite-P and Limestone strongly depends on pH and time and is interpreted due to formation of calcium phosphate precipitate(s). Consequently, CFH can unambiguously be recommended as P retention filter material in drain outlets, whereas the use of Filtralite-P and Limestone has certain (serious) limitations. Thus, Filtralite-P has high capacity to retain P but only at alkaline pH (pH ≥ 10) and P retention by Limestone requires long-time contact and a high ratio between sorbent and sorbate.
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•The Fe oxide-based CFH is a highly efficient phosphate sorbent.•CFH rapidly forms strong Fe–P bonds on Fe oxide surfaces.•P retention by Limestone is slow and requires high sorbent:sorbate ratio.•P retention by Filtralite-P strongly depends on pH with high sorption at pH ≥ 10 but no sorption at pH ≤ 8. |
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AbstractList | Phosphorus eutrophication of lakes and streams, coming from drained farmlands, is a serious problem in areas with intensive agriculture. Installation of phosphate (P) sorbing filters at drain outlets may be a solution. The aim of this study was to improve the understanding of reactions involved in P sorption by three commercial P sorbing materials, i.e. Ca/Mg oxide-based Filtralite-P, Fe oxide-based CFH-12 and Limestone in two particle sizes (2-1 mm and 1-0.5 mm), by means of isothermal titration calorimetry (ITC), sorption isotherms, sequential extractions and SEM-EDS. The results indicate that P retention by CFH is due to surface complexation by rapid formation of strong Fe-P bonds. In contrast, retention of P by Filtralite-P and Limestone strongly depends on pH and time and is interpreted due to formation of calcium phosphate precipitate(s). Consequently, CFH can unambiguously be recommended as P retention filter material in drain outlets, whereas the use of Filtralite-P and Limestone has certain (serious) limitations. Thus, Filtralite-P has high capacity to retain P but only at alkaline pH (pH ≥ 10) and P retention by Limestone requires long-time contact and a high ratio between sorbent and sorbate. Phosphorus eutrophication of lakes and streams, coming from drained farmlands, is a serious problem in areas with intensive agriculture. Installation of phosphate (P) sorbing filters at drain outlets may be a solution. The aim of this study was to improve the understanding of reactions involved in P sorption by three commercial P sorbing materials, i.e. Ca/Mg oxide-based Filtralite-P, Fe oxide-based CFH-12 and Limestone in two particle sizes (2–1 mm and 1–0.5 mm), by means of isothermal titration calorimetry (ITC), sorption isotherms, sequential extractions and SEM-EDS. The results indicate that P retention by CFH is due to surface complexation by rapid formation of strong Fe–P bonds. In contrast, retention of P by Filtralite-P and Limestone strongly depends on pH and time and is interpreted due to formation of calcium phosphate precipitate(s). Consequently, CFH can unambiguously be recommended as P retention filter material in drain outlets, whereas the use of Filtralite-P and Limestone has certain (serious) limitations. Thus, Filtralite-P has high capacity to retain P but only at alkaline pH (pH ≥ 10) and P retention by Limestone requires long-time contact and a high ratio between sorbent and sorbate. [Display omitted] •The Fe oxide-based CFH is a highly efficient phosphate sorbent.•CFH rapidly forms strong Fe–P bonds on Fe oxide surfaces.•P retention by Limestone is slow and requires high sorbent:sorbate ratio.•P retention by Filtralite-P strongly depends on pH with high sorption at pH ≥ 10 but no sorption at pH ≤ 8. Phosphorus eutrophication of lakes and streams, coming from drained farmlands, is a serious problem in areas with intensive agriculture. Installation of phosphate (P) sorbing filters at drain outlets may be a solution. The aim of this study was to improve the understanding of reactions involved in P sorption by three commercial P sorbing materials, i.e. Ca/Mg oxide-based Filtralite-P, Fe oxide-based CFH-12 and Limestone in two particle sizes (2-1 mm and 1-0.5 mm), by means of isothermal titration calorimetry (ITC), sorption isotherms, sequential extractions and SEM-EDS. The results indicate that P retention by CFH is due to surface complexation by rapid formation of strong Fe-P bonds. In contrast, retention of P by Filtralite-P and Limestone strongly depends on pH and time and is interpreted due to formation of calcium phosphate precipitate(s). Consequently, CFH can unambiguously be recommended as P retention filter material in drain outlets, whereas the use of Filtralite-P and Limestone has certain (serious) limitations. Thus, Filtralite-P has high capacity to retain P but only at alkaline pH (pH = 10) and P retention by Limestone requires long-time contact and a high ratio between sorbent and sorbate. |
Author | Hansen, Hans C.B. Penn, Chad J. Borggaard, Ole K. Lyngsie, Gry |
Author_xml | – sequence: 1 givenname: Gry surname: Lyngsie fullname: Lyngsie, Gry email: chj177@ku.dk, grylyngsie@hotmail.com organization: University of Copenhagen, Department of Plant and Environmental Sciences, Thorvaldsensvej 40, DK-1871 Frederiksberg C, Denmark – sequence: 2 givenname: Chad J. surname: Penn fullname: Penn, Chad J. organization: Oklahoma State University, Department of Plant and Soil Sciences, 368 Agricultural Hall, Stillwater, OK 74078-6028, USA – sequence: 3 givenname: Hans C.B. surname: Hansen fullname: Hansen, Hans C.B. organization: University of Copenhagen, Department of Plant and Environmental Sciences, Thorvaldsensvej 40, DK-1871 Frederiksberg C, Denmark – sequence: 4 givenname: Ole K. surname: Borggaard fullname: Borggaard, Ole K. organization: University of Copenhagen, Department of Plant and Environmental Sciences, Thorvaldsensvej 40, DK-1871 Frederiksberg C, Denmark |
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Keywords | Limestone Filtralite-P CFH-12 P sorbing reactions Fe-oxides Calcium phosphates Sorption Calorimetry Oxides Calcium phosphate Environmental management |
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Snippet | Phosphorus eutrophication of lakes and streams, coming from drained farmlands, is a serious problem in areas with intensive agriculture. Installation of... |
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SubjectTerms | Adsorption Agriculture Animal, plant and microbial ecology Applied ecology Biological and medical sciences Calcium Carbonate Calcium phosphates Calcium Phosphates - chemistry Calorimetry - methods CFH-12 Conservation, protection and management of environment and wildlife Creeks & streams Eutrophication Fe-oxides Ferrous Compounds - chemistry Filtralite-P Filtration - instrumentation Filtration - methods Fundamental and applied biological sciences. Psychology General aspects Hydrogen-Ion Concentration Limestone Oxides P sorbing reactions Phosphates Phosphates - chemistry Phosphorus - chemistry Sorption |
Title | Phosphate sorption by three potential filter materials as assessed by isothermal titration calorimetry |
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