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Edward P. Simonds

Publications and source records attributed to Edward P. Simonds.

4 recordsLinked to original sources

Water resources data, Florida, water year 2004, Volume 1B: northeast Florida ground water

Water resources data for the 2004 water year in Florida consist of continuous or daily discharge for 405 streams, periodic discharge for 12 streams, continuous or daily stage for 159 streams, periodic stage for 19 streams, peak stage and discharge for 30 streams; continuous or daily elevations for 14 lakes, periodic elevations for 23 lakes; continuous ground-water levels for 408 wells, periodic ground-water levels for 1,157 wells; quality-of-water data for 140 surface-water sites and 239 wells. The data for northeast Florida include continuous or daily discharge for 140 streams, periodic discharge for 4 streams, continuous or daily stage for 58 streams, periodic stage for 3 streams; peak stage and discharge for 0 streams; continuous or daily elevations for 10 lakes, periodic elevations for 20 lakes; continuous ground water levels for 50 wells, periodic ground-water levels for 522 wells; quality-of-water data for 40 surface-water sites and 66 wells. These data represent the National Water Data System records collected by the U.S. Geological Survey and cooperating local, State and Federal agencies in Florida.

Water Data Report↗

Shallow ground-water conditions and vegetation classification, central Volusia County, Florida

In the early 1970's, the Volusia County Council recognized the need to develop new sources of freshwater for future growth and development. County Council, using data from the U.S. Geological Survey and private consultants, concluded that the central wetlands were an optimal area for well-field development. With this in mind, Volusia County requested that the State of Florida buy land in the central wetlands of Volusia County under the Land Conservation Act of 1972, hoping to protect both the environmentally endangered lands and a potential water resource. In 1974, the State acquired 7.28mi 2 within this area, and present (1979) plans to acquire and additional 3.33mi 2 . The State later became concerned that wetland protection may not be compatible with development of water resources due to the vegetation changes that might occur if shallow ground-water levels are lowered by producing well field. Consequently, because of mutual interest, the U.S. Geological Survey with the State entered into a program of documenting for future reference the vegetation in the State-owned land. The purposes of this report and associated map (fig. 1) are (1) to document existing vegetation in approximately 140 mi 2 in central Volusia County, and (2) to investigate natural water-level fluctuations in selected vegetative communities to the extent possible with relatively short-term data. The study area (fig. 2) is that part of the Talbot Terrace bounded on the east by Rima Ridge, to the west by De Land Ridge, to the north by State Road 40, and to the south by 28 ° 57'.

Florida↗

Hydrology of the Lake Deaton and Lake Okahumpka area, Northeast Sumter County, Florida

The Floridan aquifer in the Lake Deaton and Lake Okahumpka area is 50 to 130 feet below land surface. During the 16-year period 1963-78 lake evaporation exceeded rainfall by 0.4 inches. Drainage from Lake Deaton and its surrounding area goes into Chitty Chatty Creek and on the Hogeye Sink when the altitude of the potentiometric surface of the Floridan aquifer is low. During a higher altitude of the Floridan potentiometric surface, Hogeye Sink may discharge water; this water, along with the normal runoff, goes into Lake Okahumpka. Average lake fluctuation is 1.5 to 2.0 feet per year. Lake Deaton supports a large population of blue-green algae and Lake Okahumpka is choked with aquatic plants. The water quality of the two lakes differ, with Lake Deaton having a sodium chloride water and Lake Okahumpka having a calcium bicarbonate water. Analysis of water and bottom material samples showed that only cadmium and mercury exceeded the Florida Department of Environmental Regulation 's criteria for Class III waters; however, the amounts detected were at or slightly above the limits of the analytical method. (USGS)

Open-File Report↗