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North Florida’s Springs

North Florida’s Springs

Morrison Springs in Walton County is a natural spring ideal for paddling, snorkeling, and diving. Photo credit: Carrie Stevenson, UF IFAS Extensio

There is just SO much water in Florida. Besides the tremendous amount of rain and 1,350 miles of coastline and beachfront, there are endless bays, bayous, creeks, rivers, and streams. In this state, it is extraordinarily difficult to live more than a few miles from a body of water. Among the the coolest (literally) types of water bodies in Florida, though, are our springs.  Like brilliant gemstones, the state’s 700+ springs dot the Florida landscape like a strand of sapphires.

While we have springs bubbling up all over northwest Florida in areas where the underground water table meets the surface, larger springs are more common as you move east and south. Some parts of north Florida and most of the peninsula are built on a limestone platform, known by the geological term “karst.” Limestone is composed of calcium carbonate, which has a porous and easily degradable chemical structure. When this barrier is breached, it allows the cold groundwater an opening directly to the surface water—hence a spring. (Fun fact—there are surface water streams that actually disappear into a spring—these are called swallets, operating as the reverse version of a spring!)

The striking blue-green water in Three Sisters Spring is only accessible by kayak or swimming. Photo credit: Carrie Stevenson, UF IFAS Extension

A few of the largest springs in northwest Florida are Vortex, Ponce de Leon, and Morrison Springs, found in Holmes and Walton County. Vortex is a privately operated water park and scuba diving/training facility. It is where the red and white “diver down” flag was invented and has a complex underwater cavern system. Ponce de Leon and Morrison Springs are state and county-run parks with a more natural feel, surrounded by woods and basic infrastructure for access. Morrison will especially wow visitors with its tremendous turquoise coloring.

Crystal clear water in Morrison Springs. Photo credit: Carrie Stevenson, UF IFAS Extension

Before a meeting in Crystal River last week, I paddled and snorkeled through the famous Three Sisters Spring. As part of Crystal River National Wildlife Refuge, it is a popular but highly protected area. Three Sisters is well-known as a manatee gathering place, especially in winter, but during my visit was mostly unoccupied. The color was striking, though. Why do so many of these springs have such brilliant blue and turquoise coloring? The phenomenon is essentially the same as the blue-green Gulf waters in the Panhandle. The reflection of the sky on a sunny day with the backdrop of that pure white sand causes the water to reflect a color that inspired the nickname “The Emerald Coast.” In springs, the white calcium carbonate in limestone breaks down into tiny crystals, mixing with the water and reflecting the vivid shades of blue.

Alexander Springs Creek in Ocala National Forest is overrun with algae. Photo credit: Matt Cohen, UF IFAS

Besides their beauty, clarity, recreational, and wildlife value, springs pump 8 billion gallons of fresh water a day of into Florida ecosystems. Seagrass meadows in many of these springs are lush. Because they are literal windows into the underground aquifer, they are extremely vulnerable to pollution. While many springs have been protected for decades, others were seen as places to dump trash and make it “disappear.” Many have been affected by urban stormwater and agricultural pollution, losing their clarity, reducing dissolved oxygen levels, and prompting massive cleanup and buffer protection zones.

On one of these hot summer days in Florida, take the time to visit our incredible springs. While it may not be the literal “Fountain of Youth,” swimming in a spring is a unique and invigorating experience, and a beautiful way to get off the beaten path. A comprehensive guide to Florida springs, research, and statewide protection initiatives can be found at the Florida Department of Environmental Protection’s springs website.

Why do we have so many springs in Florida?

Why do we have so many springs in Florida?

Jackson Blue Springs discharging from the Floridan Aquifer. Jackson County, FL. Image: Doug Mayo, UF/IFAS Extension.

Florida has one of the largest concentrations of freshwater springs in the world. More than 1000 have been identified statewide, and here in the Florida Panhandle, more than 250 have been found.  Not only are they an important source of potable water, springs have enormous recreational and cultural value in our state. There is nothing like taking a cool swim in the crystal-clear waters of these unique, beautiful systems.

How do springs form?

We have so many springs in Florida because of the state’s geology.  Florida is underlain by thick layers of limestone (calcium carbonate) and dolomite (calcium magnesium carbonate) that are easily dissolved by rainwater that percolates into the ground. Rainwater is naturally slightly acidic (with a pH of about 5 to 5.6), and as it moves through the limestone and dolomite, it dissolves the rock and forms fissures, conduits, and caves that can store water. In areas where the limestone is close to the surface, sinkholes and springs are common. Springs form when groundwater that is under pressure flows out through natural openings in the ground. Most of our springs are found in North and North-Central Florida, where the limestone and dolomite are found closest to the surface.

Springs are windows to the Floridan Aquifer, which supplies most of Florida’s drinking water. Image: Ichetucknee Blue Hole, A. Albertin.

These thick layers of limestone and dolomite that are below us, with pores, fissures, conduits, and caves that store water, make up the Floridan Aquifer. The Floridan Aquifer includes all of Florida and parts of Georgia, South Carolina, and Alabama. The thickness of the aquifer varies widely, ranging from 250 ft. thick in parts of Georgia, to about 3,000 ft. thick in South Florida. The Floridan is one of the most productive aquifer systems in the world.  It provides drinking water to about 11 million Floridians and is recharged by rainfall.

How are springs classified?

Springs are commonly classified by their discharge or flow rate, which is measured in cubic feet or cubic meters per second. First magnitude springs have a flow rate of 100 cubic feet or more per second, 2nd magnitude springs have a rate of 10-100 ft.3/sec., 3rd magnitude flows are 1-10 ft.3/sec. and so on. We have 33 first magnitude springs in the state, and the majority of these are found in state parks. These springs pump out massive amounts of water. A flow rate of 100 ft.3/sec. translates to 65 million gallons per day. Larger springs in Florida supply the base flow for many streams and rivers.

What affects spring flow?

Multiple factors can affect the amount of water that flows from springs. These include the amount of rainfall, size of caverns and conduits that the water is flowing through, water pressure in the aquifer, and the size of the spring’s recharge basin. A recharge basin is the land area that contributes water to the spring – surface water and rainwater that falls on this area can seep into the ground and end up as part of the spring’s discharge. Drought and activities such as groundwater withdrawals through pumping can reduce flow from springs systems.

If you haven’t experienced the beauty of a Florida Spring, there is really nothing quite like it. Here in the panhandle, springs such as Wakulla, Jackson Blue, Pitt, Williford, Morrison, Ponce de Leon, Vortex, and Cypress Springs are some of the areas that offer wonderful recreational opportunities. The Florida Department of Environmental Protection has a ‘springs finder’ web page with an interactive map that can help you locate these and many other springs throughout the state.

https://nwdistrict.ifas.ufl.edu/nat/2020/04/09/the-incredible-floridan-aquifer/

Reducing the Impact of Septic Systems Through Advanced Nitrogen Treatment

Reducing the Impact of Septic Systems Through Advanced Nitrogen Treatment

Many of Florida’s historic first magnitude springs are classified as nitrogen impaired. Image credit: UF/IFAS Communications

Septic systems are an effective means of treating wastewater when they are properly designed, constructed and maintained. Conventional systems are designed from a public health perspective and have been widely used since the 1940s to remove pathogens and protect human health. About 30% of Florida’s population relies on septic systems, which treat and dispose household wastewater drained from bathrooms, kitchens and laundry machines.

However, septic systems were not designed to remove nutrients. A conventional system removes only about 30 percent of the nitrogen that flows into it. Even a well-maintained system will become a source of nitrogen (particularly nitrate-nitrogen) to the surrounding soil in the drainfield, and may leach to groundwater. Excess nitrogen in Florida’s waterbodies can be a contributing factor to ecological community degradation and increases in algae.

What alternatives are there to conventional septic systems?

Many enhanced nitrogen removal technologies exist, but only those approved by the Florida Department of Health (FDOH) can be installed. Conventional septic systems are made up of a septic tank and a drainfield (or leachfield). Advanced treatment systems add steps to conventional system processes to improve contaminant removal. Types of advanced nitrogen removal technologies available include:

  • Aerobic Treatment Units  ATUs are made of fiberglass, polyurethane or concrete. Unlike conventional systems, ATUs introduce air into the sewage in the tank using a pump. By aerating waste, the organic matter in the tank is broken down faster than in a conventional system. Effluent from an ATU is discharged into a drainfield for further treatment in the soil, just as with a conventional septic system. ATUs require higher energy input than conventional septic systems to power the aerator, and regular operation and maintenance to sustain performance   ATU example from the US EPA
  • Performance Based Treatment Systems PBTS are specialized systems designed by professional engineers to meet specific levels of contaminant removal based on site and/or situation requirements. There are many proprietary commercial options available. Designs often include an ATU. Like ATUs, PBTS require higher energy input than conventional septic systems to power pumps, and regular maintenance is needed to sustain performance.
  •  In-Ground Nitrogen Removing Biofilters INRB are also referred to as modified drainfields. These systems are passive, which means they require no electric aerators or pumps to treat wastewater, and maintenance requirements are lower than those for ATUs and PBTS. INRBs are nitrogen-reducing media layers placed underneath a conventional drainfield.

Ammonium-nitrogen in wastewater leaving the septic tank moves down through the Drainfield Area soil and an additional oxygen-rich zone (Unsaturated Nitrification Soil) to promote conversion into nitrate-nitrogen. Wastewater then passes through a low-oxygen, carbon-rich zone to promote denitrification (Woodchips/Soil Mix Denitrification Media). Denitrification is a process by which specialized bacteria convert nitrate into nitrogen gas that escapes into the atmosphere. This reduces the amount of nitrogen that can leach into groundwater.

FDOH provides comprehensive information about advanced treatment systems and requirements on their product listing and approval requirement web page.

 Where are advanced treatment systems required?

The short answer is wherever a septic system remediation plan to protect Florida Springs has been put into place. The 2016 Florida Springs and Aquifer Protection Act was passed to protect 30 ‘Outstanding Florida Springs.’ The majority are historic first magnitude springs, springs with flows of more than 100 cubic ft/second. Twenty-four of these springs are identified as nitrogen impaired by the Florida Department of Environmental Protection.

If septic systems contribute more than 20% of the nitrogen load to the impaired spring, a remediation plan takes effect in specific areas (Priority Focus Areas) that are particularly susceptible to nitrogen pollution. Septic system remediation plans require new development to connect to central sewer where available. If this isn’t an option, new construction on lots of less than 1 acre must include advanced nitrogen-removal technology. In the Panhandle, areas around Wakulla Springs and Jackson Blue Springs have remediation plans.

The best source of information about specific remediation plans and whether or not you live in a Priority Focus Area is FDOH. Contact your local County Department of Health Office to find out if you live in a PFA or if you have questions about septic tank requirements, permitting and  approved advanced nitrogen-treatment features for septic systems.

For more information and resources about conventional septic systems and advanced treatment system visit our UF/IFAS Septic Systems website.

Morrison Springs Park – Walton County, Florida

Morrison Springs Park – Walton County, Florida

Snorkeler at Morrison Springs Park

Snorkeler at Morrison Springs – Laura Tiu

Morrison Springs Bald Cypress

Morrison Springs Bald Cypress

 

 

 

 

 

 

 

 

 

 

There are over 1000 springs identified in Florida. In the Panhandle, the majority of the springs are karst or artesian springs rising deep from the Floridan Aquafer System within the states limestone base.  Springs are unique and can be identified by perennial flows, constant water temperature and chemistry, high light transparency.  This yields a freshwater ecology dependent on these features.  Springs are classified based upon the average discharge of water but can exhibit a lot of variability based on water withdrawals and rainfall. These springs are some of our most precious water resources, supplying the drinking water our communities rely on, as well as providing great recreation opportunities.

Morrison Springs is a popular spring in northwest Florida and is one of 13 springs flowing into the Choctawhatchee River Basin. It is a large, sandy-bottomed spring surrounded by old growth cypress.  The spring pool is 250 feet in diameter, discharges an average of 48 million gallons of water each day from three vents into the Choctawhatchee River as a second magnitude spring.  The spring contains an extensive underwater cave system with three cavities up to 300 feet deep and is popular for scuba diving, swimming and snorkeling, kayaking, canoeing and fishing.  Historically, it was privately owned and was a popular swimming hole for locals.  In 2004, the state of Florida purchased the land containing the spring in the Choctawhatchee River floodplain.  The land was leased to Walton County for 99 years.  The county created a 161-acre park with a picnic pavilion, restroom facilities and a wheelchair-accessible boardwalk.  A down-stream boat ramp provides access to the river away from swimmers and divers.  There is no entrance fee.

Morrison Spring is filled with abundant fish and plant life. Fish include largemouth bass, spotted bass, hybrid striped bass, bluegill, sunfish, redbreast sunfish, warmouth, black crappie, striped bass, catfish, alligator gar, bowfin, carp, mullet and flounder or hogchoakers (freshwater sole).  It is also home to some nocturnal freshwater eels that swim around the vent and delight the divers. Most are gray, about an inch in diameter and maybe a foot or two long.  The spring supports many trees, plants, and grasses including bald cypress, live oak, red maple, pawpaw, red and black titi, Cherokee bean, sweetbay, blackgum, juniper, red cedar, southern magnolia, laurel oak, tupelo, hickory, willow, wax myrtle, cabbage palm, saw palmetto blueberry, hydrangea, St. John’s wort, mountain laurel, water lily, pickerelweed, pitcher plant, broad leaved arrowhead, fern, and moss.

Morrison Springs was previously considered one of the cleanest springs in Florida until 2010 (Florida Springs Initiative). All of Florida springs are currently at risk as the state population continues to increase.  Spring flows are decreasing as the result of increasing extraction of groundwater for human uses.  Development, and the resultant over pumping, and nitrogen pollution from agriculture both have impacts on the aquifer recharge areas.  Existing groundwater pumping rates from the Floridan Aquifer in 2010 were more than 30% of average aquifer recharge (Florida Spring Initiative).  The University of Florida IFAS Extension Agents in the Panhandle occasionally conduct interpretive guided tours of the Springs to help citizens understand the importance of protecting this unique water source.