Item talk:Q60551
From geokb
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"abstract": "Lago Lo\u00edza is a reservoir formed at the confluence of R\u00edo Gurabo and R\u00edo Grande de Lo\u00edza in the municipality of Trujillo Alto in central Puerto Rico, about 10 kilometers (km) north of the town of Caguas, about 9 km northwest of Gurabo, and about 3 km south of Trujillo Alto (fig. 1). The Carraizo Dam is owned and operated by the Puerto Rico Aqueduct and Sewer Authority (PRASA), and was constructed in 1953 as a water-supply reservoir for the San Juan Metropolitan area. The dam is a concrete gravity structure that is located in a shallow valley and has a gently sloping left abutment and steep right abutment. Non-overflow sections flank the spillway section. Waterways include an intake structure for the pumping station and power plant, sluiceways, a trash sluice, and a spillway.\n\nThe reservoir was built to provide a storage capacity of 26.8 million cubic meters (Mm3) of water at the maximum pool elevation of 41.14 meters (m) above mean sea level (msl) for the Sergio Cuevas Filtration Plant that serves the San Juan metropolitan area. The reservoir has a drainage area of 538 square kilometers (km2) and receives an annual mean rainfall that ranges from 1,600 to 5,000 millimeters per year (mm/yr). The principal streams that drain into Lago Lo\u00edza are the R\u00edo Grande de Lo\u00edza, R\u00edo Gurabo, and R\u00edo Ca\u00f1as. Two other rivers, the R\u00edo Bairoa and R\u00edo Cag\u00fcitas, discharge into the R\u00edo Grande de Lo\u00edza just before it enters the reservoir. The combined mean annual runoff of the R\u00edo Grande de Lo\u00edza and the R\u00edo Gurabo for the 1960\u20132009 period of record is 323 Mm3. Flow from these streams constitutes about 89 percent of the total mean annual inflow of 364 Mm3 to the reservoir (U.S. Geological Survey, 2009). Detailed information about Lago Lo\u00edza reservoir structures, historical sediment accumulation, and a dredge conducted in 1999 are available in Soler-L\u00f3pez and G\u00f3mez-G\u00f3mez (2005).\n\nDuring July 8\u201315, 2009, the U.S. Geological Survey (USGS) Caribbean Water Science Center (CWSC), in cooperation with PRASA, conducted a bathymetric survey of Lago Lo\u00edza to update the reservoir storage capacity and estimate the reservoir sedimentation rate by comparing the 2009 data with the previous 2004 bathymetric survey data. The purpose of this report is to document the methods used to update and present the results of the reservoir storage capacity, sedimentation rates, and areas of substantial sediment accumulation since 2004.",
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