Citation
Pensacola area water ( FGS: Leaflet 3 )

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Title:
Pensacola area water ( FGS: Leaflet 3 )
Series Title:
( FGS: Leaflet 3 )
Creator:
Florida Geological Survey
Publisher:
Florida Geological Survey
Publication Date:

Subjects

Subjects / Keywords:
Water supply -- Pensacola (Fla.)
City of Pensacola ( local )
Santa Rosa County ( local )
City of Tallahassee ( local )
Aquifers ( jstor )
Rain ( jstor )
Geological surveys ( jstor )
Water resources ( jstor )
Streams ( jstor )

Record Information

Source Institution:
University of Florida
Holding Location:
University of Florida
Rights Management:
The author dedicated the work to the public domain by waiving all of his or her rights to the work worldwide under copyright law and all related or neighboring legal rights he or she had in the work, to the extent allowable by law.
Resource Identifier:
AAA0582 ( notis )
AJW7430 ( notis )

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Full Text
~ ~4L
\lit
law I




ACV
Printed by the Florida Geological Survey
Tallahassee, Florida
1965




LEAFLET NO. 3
WATER BUDGET
ESCAMA B SANTA ROSA
COUNTIES
THE PENSACOLA AREA'S WATER
The Pensacola area is endowed with a vital and bountiful natural resource--WATER. The water is available in large quantities. It is easily obtained, is remarkably soft, and contains very small amounts of dissolved minerals. The quality of much of this water is far better than that required for public supplies and by many industries.
To explain the occurrence of this water we must look back into the geologic history of the area. For millions of years part of the Gulf coastal area has been sinking very slowly. This lowered area has been filled to depths of 300 to 1,000 feet with sand, gravel, and clay brought in by streams. The sand and gravel beds form a vast, highly productive waterbearing formation, or aquifer, that supplies almost all the wells and part of the streamflow in the area. This surficial sand-and-gravel aquifer is replenished continually by a bountiful rainfall, which totals more than 5 feet annually. As the rain water seeps underground to recharge the aquifer, it remains almost pure because the sand and gravel is quartz, which is not very soluble in water.




of water for all
Two limestone formations of the extensive Floridan aquifer lie beneath the sand-and-gravel aquifer and contain large amounts of water. For several reasons, very little water is used from these limestones in the Pensacola area. They are deeper than the sand-and-gravel aquifer, the water contains more dissolved minerals, and the southern parts of the limestone aquifers contain salt water. However, these limestone aquifers lie waiting as a ready reserve of usable water.
The area receives fresh water from three sources--rain falling directly on the area, streams flowing in from adjacent areas, and flow through the underground system. Escambia and Santa Rosa counties receive an average yearly rainfall of 62 inches, which amounts to 5 billion gallons of water per day. Streams bring in 6Y2 billion gallons per day from adjacent areas. About 0.1 billion gallons per day of ground water flows underground into the Pensacola area through the aquifers that are fed by rain falling on the northern parts of
RAINFALL AT PENSACOLA, FLA.
1025
_W
,z
40- 0
irr
ofOfwIF eI Zo l
926 930 1935 4940 1945 150 1955 4960




GEOLOGIC SECTION ALONG THE GULF COAST
West 0J East
E
c -Fort
Mobile I, 0 Walton Choctawhatchee
BS y 4 1 E Pensacola Be ch Rivpr Sa
Level- Level 000- -1,000
oool
0 10 1 5 20 25 Miled o
30-00- -3,000




SANTA ROSA 'ESCAMBIA
COUNTY
Averog Flaw 01
MinimmlxVlFlow OUNT
0 5 BGD
IG
8.5 BGD Flows into Boys from 4 major Rivers
Escambia and Santa Rosa counties and southe Alabama. The sand-and-gravel aquifer, recharg by local rainfall, supplies most of the groui water being used.
About 3 billion gallons of water per d: that falls as rain on Escambia and Santa Ro: counties is returned to the atmosphere throu, the processes of evaporation and transpirati( (water given off by plants and trees). TA billion gallons of this rain water enters t streams as overland flow or as seepage fr( the ground and runs off into the estuaries. On a small part of the rain water leaves the ar as underground flow. Streams receive abc two-thirds of their flow from the ground, resulti in stable flows even during dry seasor
Although huge quantities of water are us every day, vast amounts remain untapped. Mc of the 87 million gallons of ground water usen each day is taken from the sand-and-gravel aquifer in the southern half of the area. Also, in this area, water from streams is used for




I0 I5 1 17 15 I9 20 21 22 23 24 25
F.b.. 1962
STAGE GRAPH CHANNEL CROSS SECTION
Di ,ohorg., I O SI. ORurrne, ItOrs "t H i tiA e IA. RHIo,s, Te NS en
STAGE-OISCHROE FLOO-FREOIJENEY Un.R1o066 LOU-FLOW FROEF
CURVE CURVE FLAW- DURATION CURVES
Z 15
Ge nS~hzed, Tend -- PERDIDO RIVER AT
1945 1950 1l5S A I1NS
TREN20 IN STREANFLAW
THE BEHAVOIR OlF A STREAM
holing and some wastes are discharged into De rivers. Even so, the southern half of the rea still has much water that may be used. [ensac ola, as do other communities, derives Is water supply from wells developed in the and-and-gravel aquifer.
i Very little water is used in the northern 'aif of the area. Over a billion gallons of ear, soft water flow from the small tributary reamns each day. Many of these streams offer ~ ellent possibilities for dams and reservoirs. reservoirs would increase the usable supply
the streams and also would make possible iesirab le: and needed recreational areas.
Reservoirs-....Water Cflfn he stored




WATER QUALITY
PARTS PER MILLION MAXIMUM ALLOWABLE o 100 200 RAYON
A CET T Er FI T
PI
17-- DISSOLVED SOLIDS AVAILABLE HARDNESS SURFACE /;\R ts0-- wGROUND WT'f
Are there any problems associated with developing and using this supply of water? There certainly are. If this water is unwisely developed or misused, problems will be multiplied many times over, both in number
GROUND WATER
ALABAMA
R
0
0
U L F O F I tI A % C O
Large quantities available
Small to moderate quantities
available
SAreas of concentrated use




THICKNESS OF SAND-AND-GRAVEL AQUIFER
I<=
GULF OF
THICKNESS
Less thon 250 feet
250 500 feet
500 1,000 feet
and severity. At best works of man frequently have detrimental effects on our water resources.
Two abuses of water supply, which can be disastrous, are excessive use and pollution. In an ideally developed water supply there is a balance between supply and demand. That is, the water is not being used at a greater rate than it is being replenished by nature. Often times excess use brings pollution or contamination such as that which results from salt-water encroachment. In several areas around Pensacola, excessive pumping has lowered the level of fresh ground water and allowed salty water to move in. In some areas, ponded industrial wastes may seep underground and contaminate water wells and streams.




Many years are required for a ground-water supply to freshen after it has been contaminated by salt water. It also takes many years of diligent effort and large sums of money to clean up a stream after it has been used as a receiver of excessive wastes. Limestone aquifers near the coast contain salty water; however, they offer possibilities of being used for disposal of industrial waste.
70
I
Wl 601
WATER LEVEL IN WELL
NORTH OF PENSACOLA
501___________3 "NORMAL -WET -DRY WETUl loo-NORMAL
TREND I

0-0
GROUND WATER AND RAINFALL NEAR PENSACOLA




HOW WAS THE WATER RESOURCE
MEASURED?
A community must know the answers to many questions in order to plan orderly industrial and urban expansion. What are the sources of water? How much is available? How does the supply fluctuate? What is the quality of the water? What are the effects of use on quantity and quality? There must be a planned program of investigation to answer these and many other questions pertaining to water resources.
Such a study was completed in 1962 by the U.S. Geological Survey with financial cooperation from the Florida Geological Survey, the City of Pensacola, Escambia County, and Santa Rosa County.
30 ALABAMA
SANTA ROSA 200
0
GU L of 1c
MINERAL CONTENT
(Ports per million)
SAND AND GRAVEL AQUIFER




USE OF GROUND WATER IN ESCAMBIA AND SANTA ROSA COUNTIES
50-
MILLION GALLONS PER DAY 40-
30
20
INDUSTRY CITY RURAL MILITARY
SUPPLIES AND
IRRIGATION
Mapping and measuring water-bearing formations: One can only imagine the confusion that would exist if there were no maps or plans of Pensacola's water works showing the source of water and the location and size of the underground pipe system. Community life might go smoothly until a break in a line occurred or an expansion of this system was necessary to take care of a population increase. At that time many questions would have to be answered hefore progres. could be made, some of which are: Where are the pipes? Are they large enough to allow for the expansion? How long has the system been here? Do the pipes leak? From where does the water come and in what amounts?
In the case of the natural water resource system that serves a complex industrial society these questions are multiplied many times. The earth structure serves both as a storage reservoir and as a distribution system. This structure is mapped by piecing together information from many sources. The services of experienced geologists, engineers, and chemists are necessary




Cooling towers conserve water by re-use
288-ft well yields 1,300 gpm from sand-and-gravel aquifer with 23-ft drawdown
to identify and measure the extent and waterbearing characteristics of the materials that make up the earth structure.
Most geologic information is obtained from wells. Existing-wells must be studied and tested, test wells drilled and logged, drill cuttings examined, water samples analyzed chemically, and water levels measured. Much information is gained by observing the reaction of ground-water levels to rainfall and to pumping. When a well is pumped the water level underground lowers
TRENDS IN WATER USE
20 200
.o4.
15 150
.ilo -00 =CL
c4.
0 '
1930 1940 1950 1960 1970




Measuring eq u ipme nt
to form a depression, similar in shape to a cone. The rate and amount of this lowering while the well is being pumped at a measured rate and the rate at which the water level recovers after pumping ceases is a measure of the ability of the formation to transmit and store water.
The behavior of a stream: All physical aspects of a stream must be measured several times during a period of years to determine how much water it carries, to ascertain its fluctuations and to determine the quality of the water. The stage of a river is changing continually. It is either rising or falling. Infrequently and for short periods it may be relatively stationary. This fluctuation of a stream has to be measured and recorded continuously for the period of study. Flow measurements are made throughout the range in stage to define the stage-discharge relation. Using the continuous record of stage and the stage-discharge relation, a continuous record of flow is computed. From an adequate record of basic flow data, several essential and useful tools can be produced, such as, flood frequency curves, low-flow frequency curves, flow duration curves, and graphs indicating long-term trends.
Variations in mineral content of water:
Samples of water taken daily or sometimes at less frequent but regular intervals are analyzed to determine the seasonal variations in surface water. Ground water is studied by sampling several wells, but often only one analysis per




well is needed. Maps showing mineral content of the water in an aquifer may be prepared from these analyses. In areas of suspected contamination, ground water must be analyzed regularly to determine changes in mineral content. Additional information on the water resources if the Pensacola area is contained in the following reports of Florida Geological Survey, prepared under the cooperative program with the U.S. Geological Survey:
Inter i m Re port on the Water Resources of Escambia
and Santa Rosa Counties, Florida: Fla. Geol.
Surv. Inf. Circ. No. 30, by R.H. Musgrove,
J.T. Barraclough, O.T. Marsh.
Aquifers and Quality of Ground Water along the
Gulf Coast of Western Florida: Fla. Geol.Surv.
Rept. of Inv. No. 29, by J. T. Barraclough and
0. T. Marsh.
Relation of Bucatunna Clay Member (Byram
Formation, Oligocene) to Geology and Ground Water of Westernmost Florida: Geol. Soc.
America Bull., v. 73, p. 243-252, byO.T.Marsh.
These reports are available in many libraries and the following offices:
Florida Geological Survey
P-O- Box 631
Tallahassee, Florida
U.S. Geological Survey
244 Federal Building
Ocala, Florida
U.S- Geological Survey
P.O. Box 2315
Tallahassee, Florida
TEXT PREPARED BY:
Musgrove, R.H.; Barraclough, J.T.; and Grantham,
R.G., U.S. Geological Survey.




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PRO13 a6db10530e2b72b1294ddd73b61fb73b 18298
00014.pro
PRO14 2556ed19f915ece70188beacc822247d 38811
00015.pro
PRO15 0e9f9e404b12d18c457f4859d6e34a5c 32596
00016.pro
PDF1 applicationpdf 8e05da5162ab270b23567a26fd358449 770265
UF00001171.pdf
METS2 unknownx-mets 45eb563fbd46f719f1b393fa2d5ae729 19518
UF00001171_00001.mets
METS:structMap STRUCT1 physical
METS:div DMDID ADMID ORDER 0 main
PDIV1 1 Cover
PAGE1 Page
METS:fptr FILEID
PAGE2 2
PDIV2 Main
PAGE3
PAGE4
PAGE5
PAGE6 4
PAGE7 5
PAGE8 6
PAGE9 7
PAGE10 8
PAGE11 9
PAGE12 10
PAGE13 11
PAGE14 12
PAGE15 13
STRUCT2 other
ODIV1
FILES1
FILES2