Dos métodos matemáticos para estudiar la eutrofización por fósforo de un humedal en Puerto Rico
Introducción: Laguna Cartagena (LC), es un humedal en Lajas, Puerto Rico, que ha sido afectado negativamente por nutrientes, principalmente escorrentía de fósforo de las actividades agrícolas hasta el final del cultivo de la caña de azúcar a fines del siglo XX. Estas condiciones han propiciado que,...
- Autores:
-
Paredes Gutiérrez, Marlio
Torres Velasquez, Brenda Carolina
Sanchez Colon, Yashira Marie
Schaffner Gibbs, Fred Charles
- Tipo de recurso:
- Article of journal
- Fecha de publicación:
- 2019
- Institución:
- Corporación Universidad de la Costa
- Repositorio:
- REDICUC - Repositorio CUC
- Idioma:
- eng
- OAI Identifier:
- oai:repositorio.cuc.edu.co:11323/12206
- Palabra clave:
- total phosphorus
soluble reactive phosphorus
total nitrogen
equilibrium point
eutrophication
hypereutrophication
grey cluster method
phosphorus dynamics
fósforo total
fósforo soluble reactivo
nitrógeno total
punto de equilibrio
eutrofización
hipereutrofización
método de agrupamiento de grises
dinámica del fósforo
- Rights
- openAccess
- License
- INGE CUC - 2019
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|
dc.title.spa.fl_str_mv |
Dos métodos matemáticos para estudiar la eutrofización por fósforo de un humedal en Puerto Rico |
dc.title.translated.eng.fl_str_mv |
Two mathematical approaches to study the phosphorus eutrophication of a wetland in Puerto Rico |
title |
Dos métodos matemáticos para estudiar la eutrofización por fósforo de un humedal en Puerto Rico |
spellingShingle |
Dos métodos matemáticos para estudiar la eutrofización por fósforo de un humedal en Puerto Rico total phosphorus soluble reactive phosphorus total nitrogen equilibrium point eutrophication hypereutrophication grey cluster method phosphorus dynamics fósforo total fósforo soluble reactivo nitrógeno total punto de equilibrio eutrofización hipereutrofización método de agrupamiento de grises dinámica del fósforo |
title_short |
Dos métodos matemáticos para estudiar la eutrofización por fósforo de un humedal en Puerto Rico |
title_full |
Dos métodos matemáticos para estudiar la eutrofización por fósforo de un humedal en Puerto Rico |
title_fullStr |
Dos métodos matemáticos para estudiar la eutrofización por fósforo de un humedal en Puerto Rico |
title_full_unstemmed |
Dos métodos matemáticos para estudiar la eutrofización por fósforo de un humedal en Puerto Rico |
title_sort |
Dos métodos matemáticos para estudiar la eutrofización por fósforo de un humedal en Puerto Rico |
dc.creator.fl_str_mv |
Paredes Gutiérrez, Marlio Torres Velasquez, Brenda Carolina Sanchez Colon, Yashira Marie Schaffner Gibbs, Fred Charles |
dc.contributor.author.spa.fl_str_mv |
Paredes Gutiérrez, Marlio Torres Velasquez, Brenda Carolina Sanchez Colon, Yashira Marie Schaffner Gibbs, Fred Charles |
dc.subject.eng.fl_str_mv |
total phosphorus soluble reactive phosphorus total nitrogen equilibrium point eutrophication hypereutrophication grey cluster method phosphorus dynamics |
topic |
total phosphorus soluble reactive phosphorus total nitrogen equilibrium point eutrophication hypereutrophication grey cluster method phosphorus dynamics fósforo total fósforo soluble reactivo nitrógeno total punto de equilibrio eutrofización hipereutrofización método de agrupamiento de grises dinámica del fósforo |
dc.subject.spa.fl_str_mv |
fósforo total fósforo soluble reactivo nitrógeno total punto de equilibrio eutrofización hipereutrofización método de agrupamiento de grises dinámica del fósforo |
description |
Introducción: Laguna Cartagena (LC), es un humedal en Lajas, Puerto Rico, que ha sido afectado negativamente por nutrientes, principalmente escorrentía de fósforo de las actividades agrícolas hasta el final del cultivo de la caña de azúcar a fines del siglo XX. Estas condiciones han propiciado que, la concentración de P permaneciera alta en un estado hipereutrófico, el cual era irremediable incluso después de una reducción de 5 veces en la concentración de nutrientes del agua fuente. Objetivo: El objetivo principal de este artículo de investigación es aplicar dos métodos matemáticos diferentes para evaluar el nivel de eutrofización de un humedal en Puerto Rico. Metodología: El Método de Agrupamiento de Grises (GCM) se usó para clasificar el estado eutrófico de LC aplicando los estándares tróficos internacional y chino y dos parámetros, Fósforo Total (TP) y Nitrógeno Total (TN). La media de TP y TN en el sustrato del fondo consolidado de LC y las muestras de floculencia se utilizaron para clasificar LC. Para analizar si LC puede recuperarse, se utilizó fósforo reactivo soluble (SRP) y TP a partir de muestras de agua a la entrada, salida y centro de LC para modelar (ecuación diferencial) la entrada y pérdida de fósforo en LC y determinar si existe un punto de equilibrio. El análisis GCM clasificó a la LC como un humedal eutrófico utilizando el estándar internacional e hipereutrófico utilizando el estándar chino. Resultados: La clasificación del estado trófico no presentó variaciones con el uso del sustrato de fondo consolidado versus las muestras de floculencia. El modelo de ecuaciones diferenciales mostró que los niveles de SRP y TP dentro de LC fueron más altos que los niveles de SRP y TP que entran en LC, lo que podría ser causado por un proceso de reciclaje de nutrientes dentro de LC que puede predecir el fracaso de los esfuerzos de remediación. Se encontró un punto de equilibrio a nivel eutrófico, lo que significa que incluso si hay una reducción en la entrada de fósforo, no habrá un cambio en el estado eutrófico de LC. Conclusiones: El estándar trófico chino indicó que la LC estaba en un estado hipertrófico. Se encontraron resultados similares usando el estándar internacional. El modelo de ecuaciones diferenciales mostró que LC es irreversible. |
publishDate |
2019 |
dc.date.accessioned.none.fl_str_mv |
2019-03-07 00:00:00 2024-04-09T20:15:09Z |
dc.date.available.none.fl_str_mv |
2019-03-07 00:00:00 2024-04-09T20:15:09Z |
dc.date.issued.none.fl_str_mv |
2019-03-07 |
dc.type.spa.fl_str_mv |
Artículo de revista |
dc.type.coar.eng.fl_str_mv |
http://purl.org/coar/resource_type/c_6501 http://purl.org/coar/resource_type/c_2df8fbb1 |
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Text |
dc.type.driver.eng.fl_str_mv |
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Journal article |
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http://purl.org/redcol/resource_type/ART |
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0122-6517 |
dc.identifier.uri.none.fl_str_mv |
https://hdl.handle.net/11323/12206 |
dc.identifier.url.none.fl_str_mv |
https://doi.org/10.17981/ingecuc.15.1.2019.06 |
dc.identifier.doi.none.fl_str_mv |
10.17981/ingecuc.15.1.2019.06 |
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2382-4700 |
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0122-6517 10.17981/ingecuc.15.1.2019.06 2382-4700 |
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https://hdl.handle.net/11323/12206 https://doi.org/10.17981/ingecuc.15.1.2019.06 |
dc.language.iso.eng.fl_str_mv |
eng |
language |
eng |
dc.relation.ispartofjournal.spa.fl_str_mv |
Inge Cuc |
dc.relation.references.eng.fl_str_mv |
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Thomas, “Potential effects of sediment dredging on internal phosphorus loading in a shallow, subtropical lake”, Lake and Reservoir Management, vol. 23, no. 1, pp. 27—38, Jan. 2009. https://doi.org/10.1080/07438140709353907 R. G. Wetzel, Limnology: Lake and River Ecosystems. New York, USA: Elsevier Academic Press, 2001. M. M. Fisher and K. R. Reddy, “Phosphorus flux from wetland soils affected by long-term nutrient loading”, Journal of Environmental Quality, vol. 30, no. 1, pp. 261—271, Jan. 2001. https://doi.org/10.2134/jeq2001.301261x L. Bartoszek and J. A. Tomaszek, “Phosphorus distribution in the bottom sediments of the Solina-Myczkowce Reservoirs”, Environment Protection Engineering, vol. 33, no. 2, pp. 25—33, 2007. Available http://epe.pwr.wroc.pl/2007/Bartoszek_2-2007.pdf L. E. 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Gale, “Phosphorus retention in streams and wetlands: a review”, Critical Reviews in Environmental Science and Technology, vol. 29, no. 1, pp. 83—146, Jun. 2010. https://doi.org/10.1080/10643389991259182 S. P. Seitzinger, “Denitrification in freshwater and coastal marine ecosystems: Ecological and geochemical significance”, Limnology and Oceanography, vol. 33, no. 4, pp. 702—724, Jul. 1988. https://doi.org/10.4319/lo.1988.33.4part2.0702 D. L. Saunders and J. Kalff, “Nitrogen retention in wetlands, lakes and rivers”, Hydrobiologia, vol. 433, no. 1, pp. 205—212, Jan. 2001. https://doi.org/10.1023/A:1017506914063 S. L. Whitmire and S. K. Hamilton, “Rapid removal of nitrate and sulfate in freshwater wetland sediments”, Journal of Environmental Quality, vol. 34, no. 6, pp. 2062—2071, Nov. 2005. https://doi.org/10.2134/jeq2004.0483 A. J. Burgin and S. K. Hamilton, “Have we overemphasized the role of denitrification on aquatic ecosystem? 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Likens, “Controlling eutrophication: nitrogen and phosphorus”, Science, vol. 323, no. 5917, pp. 1014—1015, Feb. 2009. https://doi.org/10.1126/science.1167755 D. P. Hamilton, N. Salmaso and H. W. Paerl, “Mitigating harmful cyanobacterial blooms: strategies for control of nitrogen and phosphorus load”, Aquatic Ecology, vol 50, no. 3, pp 351—366, Sept. 2016. https://doi.org/10.1007/s10452-016-9594-z |
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Paredes Gutiérrez, MarlioTorres Velasquez, Brenda CarolinaSanchez Colon, Yashira MarieSchaffner Gibbs, Fred Charles2019-03-07 00:00:002024-04-09T20:15:09Z2019-03-07 00:00:002024-04-09T20:15:09Z2019-03-070122-6517https://hdl.handle.net/11323/12206https://doi.org/10.17981/ingecuc.15.1.2019.0610.17981/ingecuc.15.1.2019.062382-4700Introducción: Laguna Cartagena (LC), es un humedal en Lajas, Puerto Rico, que ha sido afectado negativamente por nutrientes, principalmente escorrentía de fósforo de las actividades agrícolas hasta el final del cultivo de la caña de azúcar a fines del siglo XX. Estas condiciones han propiciado que, la concentración de P permaneciera alta en un estado hipereutrófico, el cual era irremediable incluso después de una reducción de 5 veces en la concentración de nutrientes del agua fuente. Objetivo: El objetivo principal de este artículo de investigación es aplicar dos métodos matemáticos diferentes para evaluar el nivel de eutrofización de un humedal en Puerto Rico. Metodología: El Método de Agrupamiento de Grises (GCM) se usó para clasificar el estado eutrófico de LC aplicando los estándares tróficos internacional y chino y dos parámetros, Fósforo Total (TP) y Nitrógeno Total (TN). La media de TP y TN en el sustrato del fondo consolidado de LC y las muestras de floculencia se utilizaron para clasificar LC. Para analizar si LC puede recuperarse, se utilizó fósforo reactivo soluble (SRP) y TP a partir de muestras de agua a la entrada, salida y centro de LC para modelar (ecuación diferencial) la entrada y pérdida de fósforo en LC y determinar si existe un punto de equilibrio. El análisis GCM clasificó a la LC como un humedal eutrófico utilizando el estándar internacional e hipereutrófico utilizando el estándar chino. Resultados: La clasificación del estado trófico no presentó variaciones con el uso del sustrato de fondo consolidado versus las muestras de floculencia. El modelo de ecuaciones diferenciales mostró que los niveles de SRP y TP dentro de LC fueron más altos que los niveles de SRP y TP que entran en LC, lo que podría ser causado por un proceso de reciclaje de nutrientes dentro de LC que puede predecir el fracaso de los esfuerzos de remediación. Se encontró un punto de equilibrio a nivel eutrófico, lo que significa que incluso si hay una reducción en la entrada de fósforo, no habrá un cambio en el estado eutrófico de LC. Conclusiones: El estándar trófico chino indicó que la LC estaba en un estado hipertrófico. Se encontraron resultados similares usando el estándar internacional. El modelo de ecuaciones diferenciales mostró que LC es irreversible.Introduction: Laguna Cartagena (LC), a wetland in Lajas, Puerto Rico, has been negatively impacted by nutrients, mainly phosphorus run-off from agricultural activities until the end of sugar cane cultivation in the late 1900s.  This led to P concentration remain high at hypereutrophic state that was irremediable even after a 5-fold reduction in source water nutrient concentration. Objective: The main goal of this research paper is to apply two different mathematical approaches to assess the eutrophication level of a wetland in Puerto Rico. Method:   Grey Cluster Method (GCM) was used to classify LC’s eutrophic state by applying the International and Chinese trophic standards and two parameters, total phosphorous (TP) and total nitrogen (TN).  Mean TP and TN from LC consolidated bottom substrate and flocculence samples were used to classify LC.  To address whether LC can recover, soluble reactive phosphorus (SRP) and TP from LC inlet, outlet and center water samples were used to model (differential equation) the input and loss of phosphorus in LC and determine whether an equilibrium point exists.  GCM analysis classified LC as a eutrophic wetland using the International standard and hypereutrophic using the Chinese standard. Results:  Trophic state classification did not vary with use of consolidated bottom substrate versus flocculence samples. The differential equation model showed that SRP and TP levels within LC were higher than levels of SRP and TP entering LC, which could be caused by a nutrient recycling process within LC that may predict failure of remediation efforts.  An equilibrium point was found at the eutrophic level, which means that even if there is a reduction in phosphorus input, there will not be a change in LC’s eutrophic state. Conclusions: Chinese trophic standard indicated LC was in a hypertrophic state. Similar results were found using the international standard. The differential equation model showed that LC is irreversible.application/pdftext/htmlapplication/xmlengUniversidad de la CostaINGE CUC - 2019http://creativecommons.org/licenses/by-nc-nd/4.0info:eu-repo/semantics/openAccessEsta obra está bajo una licencia internacional Creative Commons Atribución-NoComercial-SinDerivadas 4.0.http://purl.org/coar/access_right/c_abf2https://revistascientificas.cuc.edu.co/ingecuc/article/view/1873total phosphorussoluble reactive phosphorustotal nitrogenequilibrium pointeutrophicationhypereutrophicationgrey cluster methodphosphorus dynamicsfósforo totalfósforo soluble reactivonitrógeno totalpunto de equilibrioeutrofizaciónhipereutrofizaciónmétodo de agrupamiento de grisesdinámica del fósforoDos métodos matemáticos para estudiar la eutrofización por fósforo de un humedal en Puerto RicoTwo mathematical approaches to study the phosphorus eutrophication of a wetland in Puerto RicoArtículo de revistahttp://purl.org/coar/resource_type/c_6501http://purl.org/coar/resource_type/c_2df8fbb1Textinfo:eu-repo/semantics/articleJournal articlehttp://purl.org/redcol/resource_type/ARTinfo:eu-repo/semantics/publishedVersionhttp://purl.org/coar/version/c_970fb48d4fbd8a85Inge CucS. 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