Skip Navigation Links.
Collapse <span class="m110 colortj mt20 fontw700">Volume 12 (2024)</span>Volume 12 (2024)
Collapse <span class="m110 colortj mt20 fontw700">Volume 11 (2023)</span>Volume 11 (2023)
Collapse <span class="m110 colortj mt20 fontw700">Volume 10 (2022)</span>Volume 10 (2022)
Collapse <span class="m110 colortj mt20 fontw700">Volume 9 (2021)</span>Volume 9 (2021)
Collapse <span class="m110 colortj mt20 fontw700">Volume 8 (2020)</span>Volume 8 (2020)
Collapse <span class="m110 colortj mt20 fontw700">Volume 7 (2019)</span>Volume 7 (2019)
Collapse <span class="m110 colortj mt20 fontw700">Volume 6 (2018)</span>Volume 6 (2018)
Collapse <span class="m110 colortj mt20 fontw700">Volume 5 (2017)</span>Volume 5 (2017)
Collapse <span class="m110 colortj mt20 fontw700">Volume 4 (2016)</span>Volume 4 (2016)
Collapse <span class="m110 colortj mt20 fontw700">Volume 3 (2015)</span>Volume 3 (2015)
Collapse <span class="m110 colortj mt20 fontw700">Volume 2 (2014)</span>Volume 2 (2014)
Collapse <span class="m110 colortj mt20 fontw700">Volume 1 (2013)</span>Volume 1 (2013)
American Journal of Water Resources. 2016, 4(3), 68-76
DOI: 10.12691/AJWR-4-3-3
Original Research

Analysis of Groundwater in Puerto Rico

Méndez Tejeda Rafael1, , Richards Ronald T.2, 3 and Emiliano Anastacio2

1Atmospheric Sciences Laboratory, University of Puerto Rico at Carolina, PO Box 4800, Carolina, PR 00984

2School of Natural Science and Technology, Universidad del Turabo, Gurabo, Puerto Rico, PO Box 3030, Gurabo, PR 00725

3School of Science and Technology, Universidad del Este, Carolina, Puerto Rico Carr. #190 km 1.8 Carolina, PR 00983

Pub. Date: August 31, 2016

Cite this paper

Méndez Tejeda Rafael, Richards Ronald T. and Emiliano Anastacio. Analysis of Groundwater in Puerto Rico. American Journal of Water Resources. 2016; 4(3):68-76. doi: 10.12691/AJWR-4-3-3

Abstract

During rainfall events, the aquifers in Puerto Rico capture a small fraction of the rainfall and sometimes can store it for years. Organic pollutants are degraded over time by microbial and chemical processes. The shorter the travel time between raindrop and aquifer recharge the greater is the risk of contamination. Existing data from non-pumping observation wells have been used to identify three areas at risk from superficial contamination. High-risk areas have a high correlation between depth-to-water and temperature or respond quickly to rainfall events. The high-risk areas are in Florida and in the adjoining municipality of Quebradrillas/Camuy and Manatí/Vega Baja. It is proposed that production wells in the high-risk areas be instrumented to measure the rainfall and the temperature and specific conductance of the pumped water and the rainwater. The hypothesis of this proposed experiment is that in the high-risk areas the water pumped from the production well will show a reduction of temperature and specific conductance within 24 hours of a heavy rainfall event. In this manner the travel time from rain drop to aquifer recharge can be measured. The proposed paper will provide concrete data to improve the management of groundwater resources in Puerto Rico.

Keywords

Groundwater, Acquifers, Puerto Rico, rainfall

Copyright

Creative CommonsThis work is licensed under a Creative Commons Attribution 4.0 International License. To view a copy of this license, visit http://creativecommons.org/licenses/by/4.0/

References

[1]  Anderson MP. 2005. Heat as a Ground Water Tracer. Ground Water. 43(6): 951-968.
 
[2]  Bosque A. 2011. Economic valuation of groundwater remediation costs and benefits: Towards a more comprehensive approach. Unpublished doctoral dissertation Universidad del Turabo School of Science and Technology, Gurabo, PR.
 
[3]  Cherry GA. 2001. Simulation of flow in the upper North Coast Limestone Aquifer, Manatí-Vega Baja area, Puerto Rico. United States Geological Survey Water Resources Investigations Report 00-4266. San Juan, PR.
 
[4]  Colón-Torres JA. 2009. Climatología de Puerto Rico. La Editorial Universidad de Puerto Rico. San Juan, PR.
 
[5]  Conde-Costas C, Gómez-Gómez F. 1999, Assessment of nitrate contamination of the upper aquifer in the Manatí-Vega Baja area, Puerto Rico, U.S. Geological Survey Water-Resources Investigations Report 99-4040. San Juan, PR.
 
[6]  Dumas JA. 1999. Limestone soils: Interaction with pesticides and its impact on the north coast aquifer of Puerto Rico. Unpublished doctoral dissertation. Chemistry Department, University of Puerto Rico at Río Piedras. San Juan, PR.
 
[7]  Ecoeléctrica. 2012. Aumentado la producción de agua en el sur. [Internet] Available on http://173.83.96.97/ecolectrica/?page_id=10 (Cited on 26 November 2012).
 
[8]  Doerfliger N, Jeannin PY, Zwahlen F. 1999. Water vulnerability assessment in karst environments: a new method of defining protection areas using a multiattribute approach and GIS tools (EPIK method). Environmental Geology. 39(2):165-176.
 
[9]  Ghasemizadeh R, Hellweger F, Butscher C, Padilla I, Vesper D, Field M, Alshawabkeh A. 2012. Review of ground water flow and transport models of karst aquifers, with particular reference to the North Coast Limestone aquifer systems of Puerto Rico. Hydrogeological Journal. 20(8):1441-1461.
 
[10]  Gogu RC, Dessargues A. 2000. Current trends and future challenges in groundwater vulnerability assessment using overlay and index methods. Environmental Geology 39(6):549-559.
 
[11]  Graves RP. 1989. Water resources of the Humacao-Naguabo area, eastern Puerto Rico, U.S. Geological Survey Water-Resources Investigations Report 87-4088. San Juan, PR.
 
[12]  Hoehn E, Cirpka OA. 2006. Assessing residence times of hyporheic ground water in two alluvial flood plains of the Southern Alps using water temperature and tracers. Hydrology and Earth Systems Science. 10:553-563.
 
[13]  Hunter JM, Arbona SI. 1995. Paradise lost: an introduction to the geography of water pollution in Puerto Rico. Journal of Society, Science, and Medicine 40(10):1331-1355.
 
[14]  Janssen H. 2015. Puerto Rico residents face water rationing that lasts up to 48 hours amid historic drought. Accuweather.com [Internet] http://www.accuweather.com/en/weather-news/puerto-rico-drought-el-nino-tourism-local-water-restrictions/51647356. (Accessed on 8 Feb 2016).
 
[15]  Jones IC, Banner JL. 2003. Estimating recharge thresholds in tropical karst island aquifers: Barbados, Puerto Rico and Guam. Journal of Hydrology. 278:131-143.
 
[16]  Kuniansky EL, Gómez-Gómez F, Torres-Gonzáles S. 2003. Effects of aquifer development and changes in irrigation practices on ground-water availability in the Santa Isabel area, Puerto Rico. United States Geological Survey Water-Resources Investigative Report 03-4303. San Juan, PR.
 
[17]  Kuniansky EL, Rodríguez JM. 2010. Effects of Changes in Irrigation Practices and Agricultural Development on Ground Water Discharge to the Jobos Bay National Estuary Research Reserve near Salinas, Puerto Rico. United States Geological Survey Scientific Investigations Report 2010-5022. San Juan, PR.
 
[18]  Larsen MC. 2000. Analysis of 20th century rainfall and streamflow to characterize drought and water resources in Puerto Rico. Physical Geography. 21(6):494-521.
 
[19]  Lugo AE, Castro LM, Vale A, del Mar López T, Hernández PE, García Martinó A, Pue2nte Rolón AR, Tossas AG, McFarlane DA, Miller T, Rodríguez A, Lundberg J, Thomlinson J, Colón J, Schellekens JH, Ramos O, Helmer E. 2001. Puerto Rican karst—A vital resource. United States Forest Service General Technical Report WO-65.
 
[20]  Molina-Giraldo N, Bayer P, Blum P, Cirpka OA. 2011. Propagation of seasonal temperature signals into an aquifer upon bank infiltration. Ground Water 49(4):491-502.
 
[21]  Molina-Rivera WL. 2014. Estimated water use in Puerto Rico. US Geological Survey Open-File Report 2014-1117 35p.
 
[22]  Olcott PG. 1999. Groundwater atlas of the United States: Alaska, Hawaii, Puerto Rico and the United States Virgin Islands. HA 730 N. Puerto Rico and the United States Virgin Islands North Coast Limestone aquifer system. Available on http://pubs.usgs.gov/ha/ha730N/ch_n/N-PR_VINorth_Coast.html. (Accessed on 5 March 2016).
 
[23]  Osborne, ED. 1986. Acid rain in Puerto Rico. Final technical report to U.S. Department of the Interior. Project #G930-02. Grant Agreement #14-08-0001-G930. Engineering Research Center. University of Puerto Rico in Mayagüez.
 
[24]  Pérez-Blair F. 1996. Ground Water Resources of Alluvial Valleys in Northeastern Puerto Rico—Río Espíritu Santo to Río Demajaua Area. United States Geological Survey Water Resources Investigations Report 96-4201. San Juan, PR.
 
[25]  Puerto Rico Department of Health. 2005. Public Health Assessment—Pesticide Warehouse III, Palo Alto, Manati County, Puerto Rico EPA Facility ID: PRD987367299. U.S. Department of Health and Human Services, Agency for Toxic Substances and Disease Registry 52 p.
 
[26]  Puerto Rico Electric Power Authority (PREPA). 2013. [Internet] Available on http://www.aeepr.com/ (Cited on 20 August 2013).
 
[27]  Renken RA, Ward WC, Gill IP, Gómez-Gómez F, Rodríguez-Martínez J. 2002. Geology and Hydrogeology of the Caribbean Islands Aquifer System of the Commonwealth of Puerto Rico and the U.S. Virgin Islands: U.S. Geological Survey Professional Paper 1419. Reston, VA.
 
[28]  Richards RT. 2003. The barometric efficiency of observation wells in Puerto Rico and the U.S. Virgin Islands. Unpublished Masters Thesis, Physics Department, University of Puerto Rico at Río Piedras. San Juan, PR.
 
[29]  Rodríguez JM. 1996. Characterization of stormwater discharges at the San Isidro Industrial Park, Canóvanas, Puerto Rico. U.S. Geological Survey Open-File Report 96-348. San Juan, PR.
 
[30]  Rodríguez JM. 1999. Characterization of stormwater discharges at the Guanajibo Industrial Park, Mayagüez, Puerto Rico, 1997-98. U.S. Geological Survey Water-Resources Investigations Report. San Juan, PR.
 
[31]  Rodríguez JM. 2001. Characterization of stormwater discharges from Las Flores Industrial Park, Río Grande, Puerto Rico, 1998-99. U.S. Geological Survey Open-File Report. San Juan, PR.
 
[32]  Rodríguez JM. 2012, Evaluation of groundwater quality and selected hydrologic conditions in the South Coast Aquifer, Santa Isabel area, Puerto Rico, 2008-09: U.S. Geological Survey Scientific Investigations Report 2012-5254. San Juan, PR.
 
[33]  Rodríguez-Martínez J. 1997. Characterization of springflow in the North Coast Limestone of Puerto Rico using physical, chemical, and stable isotopic methods. U.S. Geological Survey Water-Resources Investigations Report 97-4122. San Juan, PR.
 
[34]  Ryan M, Meiman J. 1996. An Examination of Short-Term Variations in Water Quality at a Spring in Kentucky. Ground Water 34(1): 23-30.
 
[35]  Sampat P. 2000. Deep trouble: The hidden threat of ground water pollution. Worldwatch Paper 154, Worldwatch Institute, Washington DC.
 
[36]  Torres-González A. 1985. Simulation of ground-water flow in the water table aquifer near Barceloneta, Puerto Rico. United States Geological Survey Water-Resources Investigations Report 844113. San Juan, PR.
 
[37]  Torres-González S, Planert M, Rodríguez JM. 1996. Hydrogeological and simulation of the ground-water flow in the upper aquifer of the Río Camuy to Río Grande de Manatí, Puerto Rico. United States Geological Survey Water Resources Investigations Report 95-4286. San Juan, PR.
 
[38]  Troester JW. 1999. Geochemistry and hydrogeologic framework of the saline-freshwater interface and the calculation of net recharge in the Dorado area, north-central Puerto Rico, U.S. Geological Survey Water-Resources Investigations Report 98-4030. San Juan, PR.
 
[39]  Tucci P, Martínez MI. 1995. Hydrology and simulation of ground-water flow in the Aguadilla to Río Camuy area, Puerto Rico. U.S. Geological Survey Water Resources Investigations Report 95-4028. San Juan, PR.
 
[40]  United States Census Bureau (USCB). 2014. [Internet] Available on www.census.gov (cited 21 March 2016).
 
[41]  United States Geological Survey (USGS). 2015. Groundwater Levels for Puerto Rico [Internet] Available on http://nwis.waterdata.usgs.gov/pr/nwis/gwlevels (Cited on 11 October 2015).
 
[42]  Verter V, Kara BY. 2001. A GIS-based framework for hazardous materials transport risk assessment. Risk Analysis 21(6):1109-1120.