Environment & Nature

Pixabay photo

By Joan Nickeson

Inspired by the beautification of Dutch parks filled with daffodil blooms, Old Town Blooms and the Port Jefferson Station/Terryville Chamber of Commerce are hosting the second annual Daffodil Dash. This hybrid event includes a virtual 5k and 10k, taking place now through the end of April.

The 1k Daffodil Dash fun run/walk/wheel has an in-person option with three trips around the Chamber Train Car Park on Saturday, April 23. Arrive at 9 a.m. for a 9:30 a.m. start. Virtual participants can upload their race times and photos as of April 16. The first 100 registrants receive a t-shirt and a Bloomer Buff. All race participants receive a Daffodil Dash medal. Profits go to community beautification by Old Town Blooms, and the Chamber Flag Fund.

April 23rd was chosen for the 1k Fun Run to commemorate both Earth Day and Arbor Day. Sunburst Tree Experts will be giving away tree saplings to the first 100 attendees this day. There will be also be free bicycle inspections and a shred event from 9 a.m. to 1 p.m.

Sponsors also include Bass Electric, Buttercup’s Dairy, Christmas Decor, Coach Realty, Emerald Magic Lawn Care, Flushing Bank, Got Poison Ivy, Old Town Blooms, Suffolk Legislator Kara Hahn, Port Jefferson Physical Therapy, Sunburst Tree Experts, Team Perrone Realty, and TREK. The Chamber Train Car Park is located at the intersection of NYS Rte 112/Rte 347/Canal Road. Entrance is on Rose Avenue in Port Jefferson Station. For more information or to register, visit events.elitefeats.com/22daffodil or www.pjstchamber.com. Joan

Joan Nickeson is an active member of the PJS/Terryville community and community liaison to the PJS/T Chamber of Commerce.

Heather Lynch

As part of its Ecology and Climate Change lecture series, the Suffolk County Vanderbilt Museum, 180 Little Neck Road, Centerport will welcome Stony Brook University’s Heather Lynch for a presentation titled Mapping Penguins with Satellites, Drones and Other Technologies in the Charles and Helen Reichert Planetarium on April 14 at 7 p.m.

In Mapping Penguins, with Satellites, Drones, and Other Technologies, Professor Lynch will share insights from her innovative research into the population dynamics of penguins on the Antarctic Peninsula. To better understand rises and falls in this population due to climate change, tourism, and fishing, Lynch marries traditional field work with a range of technologically sophisticated methods including satellite remote sensing, drone imaging, and advanced computational models.

“Penguin populations have been changing rapidly over the last 40 years,” says Lynch. “But understanding why those changes have occurred and what we might expect for the future is a surprisingly difficult challenge. [In this lecture,] I’ll discuss the threats facing Antarctic penguins and how scientists are bringing together new technology, artificial intelligence, and advanced predictive modeling to help guide policymakers in their work to protect one of the world’s last remaining wildernesses.”

Dr. Heather J. Lynch is the Institute for Advanced Computational Sciences Endowed Chair for Ecology & Evolution at Stony Brook University. She earned a B.A. in Physics from Princeton University, an M.A. in Physics from Harvard University, and a Ph.D. in Organismal and Evolutionary Biology from Harvard. She is also a National Geographic Explorer and past winner of the Blavatnik Award for Young Scientists.

Join Lynch as she shares her insight and research. $6 per person, members free. To register, visit www.vanderbiltmuseum.org.

LOVE CONNECTION

Dennis Whittam of Port Jefferson Station snapped this incredible photo of a pair of ospreys at West Meadow Beach in Stony Brook earlier this week. He writes, ‘The ospreys have returned to Long Island and are working on their nests as they prepare for future chicks.’

Send your photo of the week to [email protected]

 

Photo by John Turner

By John L. Turner

This is the second in a two-part series on Long Island’s water supply.

‘We Have Met the Enemy and He is Us’ — Pogo

Imagine, for a moment, you’re driving on a road that skirts one of New York City’s water supply reservoirs such as the Croton or Ashokan reservoir. You come around a bend and in a large gap in the forest, offering a clear and sweeping view of the reservoir, you see thousands of houseboats dotting the reservoir’s surface. An unease falls over you — after all this is a drinking water reservoir that supplies drinking water to millions of people — and letting people live on their water supply doesn’t seem like a very good idea to ensure the purity or even the drinkability of the water.

Pixabay photo

Shift your focus to Long Island and you can see these “houseboats.” They’re in the form of hundreds of thousands of homes and businesses sitting on the surface. The drinking water reservoir however is invisible beneath our feet, leading to a “out-of-sight, out-of-mind” mentality, which, in turn, has led to decades of mistreatment by the approximately 2.7 million Long Islanders who live, work, and play above a water supply they cannot see. Perhaps it is this visual disconnection which explains the checkered stewardship.

At the risk of understatement, Long Island’s drinking water system, and the coastal waters hydrologically connected to it, are facing significant, big-time challenges. By just about any measure (a few exceptions include detergents and several types of pesticides) there are more contaminants in greater concentrations in Long Island’s groundwater than any time in its history. 

In a way this is not surprising as Long Island has built out with a land surface containing ever increasing numbers of actual and potential sources of contamination, and hundreds of poorly vetted chemicals coming on the market every year. Layer on this the quantity dimension: that in certain areas there’s simply not enough water to meet current or projected human demand and the needs of ecosystems (like wetlands) and it’s not surprising that Long Island’s drinking water system is under stress like never before.

To be clear, government agencies have not sat passively by in an effort to protect and manage the aquifer system. There are many examples over the past several decades where various government agencies, statutorily responsible for safeguarding our water resources, have delineated a problem and moved to address it. Let’s run through a few.

You’ve heard the expression: “oil and water don’t mix.” The same is true for gasoline, as evidenced by the many leak and spill incidents in the past caused by hundreds of gasoline stations scattered throughout Nassau and Suffolk Counties. As more and more contamination was discovered from gasoline plumes in the Upper Glacial aquifer half a century ago, gasoline storage tanks buried at every filling station were becoming known as “ticking time bombs”. This is because tanks installed many decades ago were single-wall, and made of corrodible cast iron — two undesirable traits for tanks containing thousands of gallons of gasoline buried in the ground. 

The solution? Both counties mandated tank replacement; Suffolk County through the enactment of Article 12 of the Suffolk County Sanitary Code. New requirements included double-walled fiberglass or specialized steel tanks with a leak detection system in between the two walls to detect a leak in the inner wall. Older readers may remember, years ago, the presence of excavators and backhoes in gas stations throughout the island as the industry moved to comply with this important new water quality safety measure. Because of these two county laws gasoline leaks — and subsequent plumes — from station tanks are almost entirely a thing of the past.

Another pollutant that is largely a thing of the past is salt. Before the adoption of legislation mandating the enclosed covering of salt piles managed by transportation and public works departments, stockpiled for winter road deicing applications, salt piles would sit outside exposed to the elements. Not surprisingly, plumes of salty water, well above drinking water standards, often formed under these piles. In some cases plumes beneath salt piles located near public water supply wells ended up contaminating these wells. Today, by law, all highway department salt stockpiles have to be covered or indoors to prevent saltwater plumes.

Nitrogen pollution has been a more intractable problem. Emanating from centralized sewage treatment plants, agricultural and lawn fertilizers, and many thousands of septic tanks and cesspools (there’s an estimated 360,000 of them in Suffolk County alone), nitrogen is ubiquitous. This excess nitrogen has fueled adverse ecological changes in our estuaries including loss of salt marshes and various types of toxic algae blooms, which in turn, have killed off scallops, clams, diamondback terrapins, and blue-claw crabs. Too much nitrogen in drinking water can have adverse health consequences for humans, especially babies, a concern since an increasing number of public wells have nitrogen levels exceeding the state health limit of 10 parts per million.

So how to get ahead of the nitrogen curve? Generally there are three ways, each relating to each of the major sources of contamination — 1) nitrogen laden water from home septic tanks/cesspools, 2) nitrogen laden water from sewage treatment plants, and 3) nitrogen pollution stemming from fertilizer use, most notably in farming but also by homeowners for lawn care.

Through the Septic Improvement Program, under its “Reclaim Our Water” Initiative, Suffolk County has thrown its eggs in the “septic tank/cesspool” basket by attacking the nitrogen generated by homeowners. How? By working with companies that have made vast improvements in the technology used to treat household sewage; basically these companies have developed mini-sewage treatment plants in place of septic tanks/cesspools, resulting in much lower nitrogen levels in the water recharged into the ground (from 70 to 80 parts per million ppm nitrogen to 10-20 ppm. 

The County now provides financial subsidies to homeowners to replace aging systems with new Innovative/Advanced systems (known as I/A systems). The downside with this approach is that because of the huge number of homes that need to convert their cesspools/septic tanks to I/A systems (remember the 360,000 figure from above?) it will take many decades to bend the nitrogen-loading curve meaningfully downward, to the point we’ll begin to see a difference.

An additional complimentary approach to reduce nitrogen loadings, but likely able to do so more quickly, is through the tried and true strategy of “water reuse.” Here, highly treated wastewater from sewage treatment plants (STP’s) which contains low concentrations of nitrogen, is used in ways which “pulls out” the nitrogen. Water reuse is common practice in many places in the United States including Florida and California where the trademark purple-colored distribution piping is commonplace. Approximately 2.6 billion gallons of water is reused daily in the country, mostly for golf course irrigation but also for irrigating certain foods such as citrus trees.

The largest water reuse example on Long Island involves the Riverhead STP-Indian Island County Golf Course. With this project, from April to October, highly treated wastewater is directed to the adjacent Indian Island County Golf Course rather than being discharged into the Peconic River. According to engineering projections, the effort annually results in about 1.4 less tons of nitrogen entering the estuary, being taken up by the grass, and keeps about 63 million gallons of water in the ground since golf course wells no longer need to pump irrigation water from the aquifers.

With funding support the Seatuck Environmental Association has hired Cameron Engineering & Associates to develop an islandwide “Water Reuse Road Map” to guide future reuse projects. A potential local project, similar to the Riverhead example, tentatively identified in the roadmap involves redirecting wastewater from the SUNY Stony Brook STP which currently discharges into Port Jefferson Harbor and use it to irrigate the St. Georges Golf Course and Country Club, situated several hundreds away from the STP on the east side of Nicolls Road in East Setauket.

The third source of nitrogen contamination — fertilizers — has also received focus although progress here has been slower. A Suffolk County law, among other things, prohibits fertilizer applications from November 1st through April 1st when the ground is mostly frozen and little plant growth occurs. It also prohibits, with certain exemptions such as golf courses, fertilizer applications on county-owned properties. Several bills, both at the county and state level, have been introduced to limit the fraction of nitrogen in fertilizer formulations and to require “slow release” nitrogen so it can be taken up by plants and not leach into groundwater.

A basic concept that has emerged from a better understanding of how Long Island’s groundwater system works and the threats to it, is the value of the aforementioned “deep-flow recharge areas” serving as groundwater watersheds, these watersheds recharging voluminous amounts of water to the deepest portions of the underlying aquifers. And we’ve also learned “clean land means clean water.” 

Where the land surface is dominated by pine and oak trees, chipmunks, native grasses, blueberries, etc., the groundwater beneath is pure, as there no sources of potential contamination on the surface. It has become clear that Long Island’s forested watersheds play an important role in protecting Long Island’s groundwater system.

In recognition of the direct relationship between the extent to which a land surface is developed and the quality of drinking water below it, a state law was passed establishing on Long Island SGPA’s — “Special Groundwater Protection Areas” — lightly developed to undeveloped landscapes within the deep-flow recharge zones that recharge clean water downward, replenishing the three aquifers; the 100,000 acre Pine Barrens forest being the largest and most significant SGPA. 

There are seven other SGPA’s including the Oak Brush Plains SGPA just east of Commack Road and south of the Pilgrim State Hospital property; the South Setauket SGPA in northwestern Brookhaven Town, bisected by Belle Meade Road; one on the North Fork; two on the South Fork; and two in northern Nassau County. These areas collectively recharge tens of millions of gallons of high to pristine quality water to the groundwater system on a daily basis. The state law mandated the development of a comprehensive plan designed to safeguard the land surface and the water beneath it in all the SGPA’s. Landscape protection took a step further in the Pine Barrens, where state law has safeguarded nearly 100 square miles of land from development.

Protecting a community’s water supply has been a challenge throughout recorded history. Many past dynasties and civilizations (e.g. China, Bolivia, Cambodia, Egypt, Syria, southwest United States) have collapsed or been compromised by failing to ensure adequate supplies of clean water. In modern times maintaining the integrity of a water supply has become one of the fundamental responsibilities of government. It is clear that various levels of government, from Washington, DC, to Albany, to local governments, have advanced a host of laws, regulations, strategies, and programs all designed to safeguard our water supply. 

The jury is still out, though, as to whether this collective governmental response will be adequate enough. While Pogo has been correct so far — we, the 2.7 million Long Islanders in the two counties have been the enemy — perhaps with the implementation of additional proactive responses we might prove the little opossum wrong.

A resident of Setauket, John Turner is conservation chair of the Four Harbors Audubon Society, author of “Exploring the Other Island: A Seasonal Nature Guide to Long Island” and president of Alula Birding & Natural History Tours.

From left, Supervisor Ed Romaine; DIME CEO Kevin M. O’Connor; Town Commissioner of Recycling and Sustainable Materials Management, Christine Fetten; Councilwoman Jane Bonner; Councilman Dan Panico and DIME Executive VP and Chief Banking Officer James J. Manseau. Photo from TOB

On March 22, Supervisor Ed Romaine accepted a $4,000 check from DIME Chief Executive Officer Kevin M. O’Connor to co-sponsor the Town of Brookhaven’s 2022 community recycling events. Each year the Town holds two recycling events in each Council District that include paper shredding, e-waste disposal and a supervised prescription drug drop-off program.

The scheduled recycling events will help residents properly dispose of sensitive documents which, when improperly discarded, can fall into the hands of identity thieves. Residents can also dispose of e-waste including TV’s, VCR and DVD players, fax machines, printers, calculators, modems, cables, routers, copiers, radios/stereos, laptops, keyboards and cell phones as well as expired prescription drugs in an environmentally safe manner. 

Documents brought in for shredding will be fed into an industrial shredder, enabling each participant to witness the secure destruction of sensitive papers. Paper can be brought in boxes or bags. Documents can remain stapled together, but paper clips and other metal must be removed along with any other contaminants such as rubber bands. 

The 2022 schedule of events are as follows:

CD-3 Councilman Kevin LaValle

Saturday, April 2 – 9:30 a.m. to 1:30 p.m. 

Middle Country Public Library, 101 Eastwood Blvd., Centereach

CD-1 Councilmember Jonathan Kornreich

Saturday, April 23 – 9 a.m. to 1 p.m.

Comsewogue Public Library, 170 Terryville Road, Port Jefferson Station

CD-2 Councilwoman Jane Bonner

Saturday, April 30 – 9 a.m. to 1 p.m.

Rose Caracappa Senior Center, 739 Route 25A, Mt. Sinai

CD-4 Councilman Michael Loguercio

Saturday, May 21 – 9:30 a.m. to 1 p.m.

Brookhaven Town Hall, South Parking Lot, 1 Independence Hill, Farmingville

CD-3 Councilman Kevin LaValle

Saturday, Sept. 10 – 9:30 a.m. to 1:30 p.m.

Sachem Public Library, 150 Holbrook Road, Holbrook

CD-2 Councilwoman Jane Bonner

Saturday, October 1 – 9 a.m. to 1 p.m.

Rose Caracappa Senior Center, 739 Route 25A, Mt. Sinai

CD-1 Councilmember Jonathan Kornreich

Saturday, October 22 – 9 a.m. to 1 p.m.

Setauket Fire Department, 394 Nicolls Road, Setauket

The 2022 recycling events are open to all Brookhaven Town residents for their personal, household material. For more information, call 451-TOWN (8696) or visit www.brookhavenny.gov/recyclingevents.

Legislator Stephanie Bontempi (wearing sunflower towards rear of group) with colleagues from multiple levels of government, trade union members and leaders. Photo courtesy of Bontempi's office

On Friday, March 25th, Legislator Stephanie Bontempi (Centerport) joined with a wide variety of elected officials from the town, county and state levels to call on the governor to prevent a ban on fuel connections in new construction.  Standing side-by-side with the electeds were trade union members and leaders, who spelled out very clearly what such a ban would mean – the loss of jobs and technologies that do not yet have full replacements.

“Although we can all confidently say that we are committed to the environment, we have to be realistic and fair in the policies we put in place,” said Bontempi.  “Seeing the increasing use of cleaner energy technologies is a positive thing, but we cannot pretend that everything older can be replaced overnight.  Newer technologies replacing older ones need to be adopted in stages so that we can properly adapt to the changes and ensure we are getting a better product or service in the end.”

Essentially, some of the proposals being considered by New York State lawmakers include banning the installation of natural gas and/or mixed use fuel connections in new construction by the year 2024.  Proposals of this nature are raising the ire of many in communities across the state who rely on fuels such as natural gas in a time when oil prices are rising quickly.

“We have to look at the needs of the people and balance them with the capabilities of the technologies that are available both new and old.  Doing anything less is shortsighted and dangerous,” added Bontempi.

Photo from Town of Brookhaven

Supervisor Ed Romaine (pictured with “Curby,” the Town’s recycling mascot) has announced that registration for the 14th Annual Great Brookhaven Clean Up is now open. The event, which is co-sponsored by the Town of Brookhaven’s Department of Recycling and Sustainable Materials Management and TEACHERS Federal Credit Union, will be held on Saturday, May 14th at various locations throughout Brookhaven Town. It is part of a national effort by Keep America Beautiful, Inc. that draws over 500,000 volunteers in more than 15,000 communities across America who come together to pick up litter and clean miles of roadway, rivers, lakes, and more. In 2020 the Great Brookhaven Clean Up drew approximately 2,000 residents.

Supervisor Romaine said, “Keeping Brookhaven clean is a top priority of my administration and this is a great opportunity for people to do their part and make a difference in their community. I thank TEACHERS Federal Credit Union for their co-sponsorship, and I look forward to working with our residents on May 14th to help make Brookhaven a cleaner, greener place to live.”

Free gloves, trash bags and t-shirts will be provided by the Town for the Great Brookhaven Clean Up volunteers. The supplies will be available for pick up at the Department of Recycling and Sustainable Materials Management’s third floor office at Town Hall by appointment only. Brookhaven Town Hall is located at 1 Independence Hill in Farmingville. Individuals or groups can register online for the Great Brookhaven Clean Up and get more information at the Town website or by calling 451-TOWN (8696).

Photo from TOB

On March 22, Supervisor Ed Romaine accepted a $4,000 check from DIME Chief Executive Officer Kevin M. O’Connor to co-sponsor the Town of Brookhaven’s 2022 community recycling events. Each year the Town holds two recycling events in each Council District that include paper shredding, e-waste disposal and a supervised prescription drug drop-off program.

The 12 scheduled recycling events will help residents properly dispose of sensitive documents which, when improperly discarded, can fall into the hands of identity thieves. Residents can also dispose of e-waste and expired prescription drugs in an environmentally safe manner. Pictured (left to right) are Supervisor Ed Romaine; DIME CEO Kevin M. O’Connor; Town Commissioner of Recycling and Sustainable Materials Management, Christine Fetten; Councilwoman Jane Bonner; Councilman Dan Panico and DIME Executive VP and Chief Banking Officer James J. Manseau.

The 2022 recycling events are open to all Brookhaven Town residents for their personal, household material. No business records or medical practices will be accepted. For more information, call 451-TOWN (8696) or visit www.brookhavenny.gov/recyclingevents.

Residents are urged to bring the following electronic items to be recycled:

TV’s VCR & DVD Players Computer Mice Printers
 Calculators Hard Drives Electronic Typewriters Circuit Boards
Projectors Camcorders Laptops Power Supplies
Radios/Stereos Servers Backup Batteries PDAs
Mainframes Pagers Monitors Routers
Telephones Scanners Cell Phones Answering Machines
Hubs Modems Fax Machines Keyboards
Copiers Cables Gameboys & other Handheld Electronic Toys

Documents brought in for shredding will be fed into an industrial shredder, enabling each participant to witness the secure destruction of sensitive papers. Paper can be brought in boxes or bags. Documents can remain stapled together, but paper clips and other metal must be removed along with any other contaminants such as rubber bands. The 2022 schedule of events are as follows:

CD-3 Councilman Kevin LaValle
Saturday, April 2 9:30 AM – 1:30 PM
Middle Country Public Library, 101 Eastwood Blvd., Centereach

CD-5 Councilman Neil Foley
Saturday, April 9 9:00 AM – 1:00 PM
Patchogue-Medford High School, 181 Buffalo Avenue, Medford

CD-1 Councilmember Jonathan Kornreich
Saturday, April 23 9:00 AM – 1:00 PM
Comsewogue Public Library, 170 Terryville Road, Port Jefferson Station

CD-2 Councilwoman Jane Bonner
Saturday, April 30 9:00 AM – 1:00 PM
Rose Caracappa Center, 739 Route 25A, Mt. Sinai

CD-4 Councilman Michael Loguercio
Saturday, May 21 9:30 AM – 1:30 PM
Brookhaven Town Hall, South Parking Lot, 1 Independence Hill, Farmingville

CD-6 Councilman Dan Panico
Saturday, June 4 9:00 AM – 1:00 PM
William Floyd Middle School, 630 Moriches-Middle Island Road, Moriches

CD-3 Councilman Kevin LaValle
Saturday, September 10 9:30 AM – 1:30 PM
Sachem Public Library, 150 Holbrook Road, Holbrook

CD-5 Councilman Neil Foley
Saturday, September 17 9:00 AM – 1:00 PM
Blue Point Fire Department, 205 Blue Point Avenue, Blue Point

CD-2 Councilwoman Jane Bonner
Saturday, October 1 9:00 AM – 1:00 PM
Rose Caracappa Center, 739 Route 25A, Mt. Sinai

CD-6 Councilman Dan Panico
Saturday, October 15 9:00 AM – 1:00 PM
Center Moriches Library, 235 Montauk Highway, Center Moriches

CD-1 Councilmember Jonathan Kornreich
Saturday, October 22 9:00 AM – 1:00 PM
Setauket Fire Department, 394 Nicolls Road, Setauket

CD-4 Councilman Michael Loguercio
Saturday, November 5 9:30 AM – 1:30 PM
South Country Public Library, 22 Station Road, Bellport

 

Pixabay photo

By John L. Turner

This is the first in a two-part series on Long Island’s water supply.

When thinking about Long Island’s groundwater supply — its drinking water aquifers — it is helpful to visualize a food you might eat while drinking water — say, a three-tiered, open-faced turkey sandwich — a slice of cheese on top, a juicy, thick tomato disk in the middle, a slice of turkey on the bottom, all resting on a piece of hard, crusty bread. 

Well, substitute the Upper Glacial Aquifer for the cheese, the thicker Magothy Aquifer for the tomato, the Lloyd Aquifer for the turkey, and a “basement of bedrock” for the bread and you’ve got Long Island’s tiered groundwater system. It is this collection of groundwater aquifers — these sections of the sandwich — that are the sole source of water for all the uses Long Islanders use water for. Hydrologists estimate there’s about 90 trillion gallons of water contained in Long Island’s groundwater supply.

Our sandwich model described above is not fully accurate in that there is another layer called the Raritan Clay formation separating the Magothy and Lloyd Aquifers. This clay layer, about 200 feet thick, retards water movement (for a number of reasons water moves painfully slow through clay) and is referred to as an aquitard. So, in our sandwich model let’s make the thin but impactive clay formation a layer of mustard or mayonnaise. With the exception of this clay-confining layer, Long Island is essentially a million-acre sandpile whose geology is generally distinguished by subtle changes in the composition, texture, and porosity of its geological materials — varying mixtures of silt, clay, sand, gravel and cobbles which affects rates of water transmissivity or movement.

The basement of bedrock (the bread in our sandwich) that underlies all of Long Island is metamorphic rock estimated to be about 400 million years old. It slants from the northwest to the southeast dipping at about 50 feet to the mile. So, while the thickness of the freshwater aquifers in northwest Queens is only a few hundred feet, it is approximately 2,000 feet thick in western Southampton.

On the North and South Forks and the south shore barrier islands, freshwater doesn’t extend all the way to bedrock as it does in Nassau County and much of western and central Suffolk County. It is shallowest on the barrier islands, the freshwater lens extending down only several dozen feet. 

On the North Fork it goes a little deeper before the water becomes salty and it is deepest on the wide South Fork where the freshwater lens extends downward about 550-600 feet. The depth of the aquifer is influenced by how many feet above sea level the water table is. There’s a hydrological formula, called the Ghyben-Herzberg principle, that states for every foot of water above sea level there’s 40 feet of freshwater beneath.

The water in the groundwater aquifers isn’t stored in large subterranean pools or caverns, as it is in some other places in the country with markedly different geology, Rather, the water is situated between the tiny, interstitial spaces existing between the countless sand particles that collectively make up Long Island. Given this, it is not surprising that groundwater flows (under the influence of gravity) slowly downward and sideways (depending where in the aquifer the water is located) moving on the order of just a few feet a day at most but typically in the ballpark of about one foot per day. 

It takes dozens to hundreds to thousands of years for water to move through the system, all depending where it first landed on the island’s surface. Water pumped from the seaward edge of the lowest aquifer — the Lloyd Aquifer — may have fallen as rain many years before the beginning of the ancient Greek Empire.

In the late 1970’s several governmental studies helped us to better understand some of the basics as to how the groundwater system works. One of the important takeaways from this research was that it is the middle half to two-thirds of the island that is most important for recharge — this segment is known as the “deep-flow recharge area” because a raindrop that lands here will move vertically downward recharging the vast groundwater supply. 

The middle of this area is knows as the “groundwater divide”; a water drop that lands to the south of the divide will move downward and then laterally in a southern direction discharging into one of the south shore bays or the salty groundwater underneath the Atlantic Ocean while a drop to the north will move eventually into Long Island Sound or the sandy sediments beneath it.

Hydrologists have determined that for every square mile of land (640 acres) an average of about two million gallons of rain water lands on the surface with about one million gallons recharging the groundwater supply on a daily basis. What happens to the other one million gallons? It evaporates, runs off into streams and other wetlands, or is taken up by trees and other plants that need it to sustain life processes such as transpiration (a large oak tree needs about 110 gallons of water daily to survive). 

In contrast, raindrops that land in locations nearer to the coasts such as in Setauket, northern Smithtown, southern Brookhaven, Babylon, or other places along the north and south shores don’t become part of the vast groundwater reservoir; instead, after percolating into the ground the water moves horizontally, discharging either into a stream that flows to salty water or into the salty groundwater that surrounds Long Island. These landscape segments are referred to as “shallow-flow recharge areas.”

The higher elevations along the Ronkonkoma Moraine (the central spine of Long Island created by glacial action about 40,000 years ago) are also the highest points in the water table although the water table elevation contours are a dampened expression of the land surface. So, in the West Hills region of Huntington where Jayne’s Hill is located, the highest point on Long Island topping out at a little more than 400 feet, the elevation of the water table is about 80 feet above sea level. 

Below the water table is the saturated zone and above it the unsaturated zone where air, instead of water, exists in the tiny spaces between the sand particles (in the Jayne’s Hill case the unsaturated zone runs about 320 feet). It is the water (more precisely its weight) in the higher regions of the saturated zones that pushes on the water beneath it, driving water in the lower portions to move at first sideways or laterally and then to upwell into the salty groundwater under the ocean. Due to the weight of the water the freshwater-saltwater interface is actually offshore on both coasts, meaning you could drill from a platform a mile off Jones Beach and tap into freshwater if you were to drill several hundred feet down.

A wetland forms where the land surface and water table intersect. It may be Lake Ronkonkoma, the Nissequogue or Peconic River, or any of the more than one hundred streams that drain the aquifer discharging into bays and harbors around Long Island. So when you’re gazing at the surface of Lake Ronkonkoma you’re looking at the water table — the top of the Long Island groundwater system. Since the water table elevations can change due to varying amounts of rain and snow and pumping by water suppliers these wetlands can be affected; in wet years they may enlarge and discharge more water while in droughts wetlands can largely dry up which happened on Long Island in the 1960’s.

It is clear, given the isolated nature of our water supply — our freshwater bubble surrounded by hostile salt water — that we are captains of our own fate. Our groundwater supply is the only source of water to meet all of our collective needs and wants. There are no magical underground freshwater connections to Connecticut, mainland New York, or New Jersey. We are not tied into, nor is it likely we will ever be able to tap into, New York City’s water supply, provided by the Delaware River and several upstate reservoirs. As the federal Environmental Protection Agency has declared — Long Island is a “sole source aquifer.” To paraphrase the late Senator Daniel Patrick Moyhihan: “Long Islanders all drink from the same well.” Indeed we do.

The next article will detail the quality and quantity problems facing our groundwater supply.

A resident of Setauket, John Turner is conservation chair of the Four Harbors Audubon Society, author of “Exploring the Other Island: A Seasonal Nature Guide to Long Island” and president of Alula Birding & Natural History Tours.