Please use this identifier to cite or link to this item:
http://hdl.handle.net/10553/44370
DC Field | Value | Language |
---|---|---|
dc.contributor.author | Estévez, Esmeralda | en_US |
dc.contributor.author | Hernandez-Moreno, Jose Manuel | en_US |
dc.contributor.author | Fernández-Vera, Juan Ramón | en_US |
dc.contributor.author | Palacios Díaz, María Del Pino | en_US |
dc.date.accessioned | 2018-11-21T22:28:28Z | - |
dc.date.available | 2018-11-21T22:28:28Z | - |
dc.date.issued | 2014 | en_US |
dc.identifier.issn | 0048-9697 | en_US |
dc.identifier.uri | http://hdl.handle.net/10553/44370 | - |
dc.description.abstract | Ibuprofen (IB) is a high environmental risk drug and one of the most frequently prescribed in human medicine. Recently, IB has been detected in Gran Canaria in reclaimed water for irrigation and in groundwater. Adsorption was studied in four volcanic soils from three islands of the Canarian Archipelago. Once the biodegradation process has been excluded from the experimental conditions, a batch method was applied using initial concentrations of 1-5-10-20-50-100-200 mgL- 1 and two soil/water ratios (w/V): 1:5 (OECD, 2000) and 1:1. Non-linear and linearized Langmuir and Freundlich equations were well fitted. The wide IB range tested in our batch studies allowed us to measure experimental adsorption values close to the maximum adsorption capacity (Smax) as estimated by Langmuir, making it possible thereby to validate the use of the Langmuir equation when there is a burst of contamination at high concentration. The distribution coefficient (Kd), Smax and Retardation Factor (RF) varied from 0.04 to 0.5 kgL- 1, 4-200 mgkg- 1 and 1.2-1.9, respectively. The lowest Smax and Kd values were found for the 1:1 S/W ratio whereas most batch studies employ 1:5 S/W ratios, thus obtaining higher adsorption parameters than when considering field conditions (1:1). Despite the high anion retention of andic soils, similar Kd and RF to those reported for other soils were obtained in 1:5, while high Smax was found. Our results demonstrate that IB adsorption in volcanic areas responds not only to the soil properties commonly cited in adsorption studies, but also depends on andic properties, sorbent concentration and Dissolved Organic Carbon, the higher values of which are related to the lower Kd and Smax. The low RF and low detection frequency of the IB in groundwater suggests that a) reclaimed water irrigation is not the main source of IB, and b) the existence of some uncontrolled water disposal points in the zone. | en_US |
dc.language | eng | en_US |
dc.relation.ispartof | Science of the Total Environment | en_US |
dc.source | Science of the Total Environment [ISSN 0048-9697],v. 468-469, p. 406-414 | en_US |
dc.subject | 250604 Geología ambiental | en_US |
dc.subject.other | Ibuprofen | en_US |
dc.subject.other | Adsorption | en_US |
dc.subject.other | Soil properties | en_US |
dc.subject.other | Freundlich | en_US |
dc.subject.other | Langmuir | en_US |
dc.subject.other | Volcanic soil | en_US |
dc.title | Ibuprofen adsorption in four agricultural volcanic soils | en_US |
dc.type | info:eu-repo/semantics/Article | es |
dc.type | Article | es |
dc.identifier.doi | 10.1016/j.scitotenv.2013.07.068 | |
dc.identifier.scopus | 84884401039 | - |
dc.identifier.isi | 000331776000046 | |
dc.contributor.authorscopusid | 35503197300 | - |
dc.contributor.authorscopusid | 57201758079 | - |
dc.contributor.authorscopusid | 36882086000 | - |
dc.contributor.authorscopusid | 28568040900 | - |
dc.description.lastpage | 414 | - |
dc.description.firstpage | 406 | - |
dc.relation.volume | 468-469 | - |
dc.investigacion | Ciencias | en_US |
dc.type2 | Artículo | en_US |
dc.contributor.daisngid | 7230964 | |
dc.contributor.daisngid | 1942486 | |
dc.contributor.daisngid | 3913703 | |
dc.contributor.daisngid | 2739199 | |
dc.contributor.wosstandard | WOS:Estevez, E | |
dc.contributor.wosstandard | WOS:Hernandez-Moreno, JM | |
dc.contributor.wosstandard | WOS:Fernandez-Vera, JR | |
dc.contributor.wosstandard | WOS:Palacios-Diaz, MP | |
dc.date.coverdate | Enero 2014 | |
dc.identifier.ulpgc | Sí | es |
dc.description.sjr | 1,635 | |
dc.description.jcr | 4,099 | |
dc.description.sjrq | Q1 | |
dc.description.jcrq | Q1 | |
dc.description.scie | SCIE | |
item.grantfulltext | none | - |
item.fulltext | Sin texto completo | - |
crisitem.author.dept | GIR IUNAT: Geología de Terrenos Volcánicos | - |
crisitem.author.dept | IU de Estudios Ambientales y Recursos Naturales | - |
crisitem.author.dept | GIR IUNAT: Geología de Terrenos Volcánicos | - |
crisitem.author.dept | IU de Estudios Ambientales y Recursos Naturales | - |
crisitem.author.dept | Departamento de Patología Animal, Producción Animal, Bromatología y Tecnología de Los Alimentos | - |
crisitem.author.orcid | 0000-0003-4075-2592 | - |
crisitem.author.parentorg | IU de Estudios Ambientales y Recursos Naturales | - |
crisitem.author.parentorg | IU de Estudios Ambientales y Recursos Naturales | - |
crisitem.author.fullName | Fernández Vera,Juan Ramón | - |
crisitem.author.fullName | Palacios Díaz, María Del Pino | - |
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