New York City water supply system

A 1798 watercolor of Collect Pond. Bayard's Mount, a 110-foot (34 m) hillock, is in the left foreground. Prior to being levelled around 1811 it was located near the current intersection of Mott and Grand Streets. New York City, which then extended to a stockade which ran approximately north–southeast from today's Chambers Street and Broadway, is visible beyond the southern shore.

Until the eighteenth century, New York City solely depended on primitive means, such as wells and rainwater reservoirs to collect water for daily use. The first public well was dug in Bowling Green in 1677, and the first reservoir was built on the East Side of Manhattan in 1776 after the population grew up to 22,000.[3]

Collect Pond, or "Fresh Water Pond",[4] was a body of fresh water in what is now Chinatown in Lower Manhattan. For the first two centuries of European settlement in Manhattan, it was the main water supply system for the growing city. Later, the city was aware of its deteriorated water quality, owing to its rapid population growth (60,000 to 200,000 from 1800 to 1830), which had a considerable danger of causing epidemics.

In April 1831, a new water supply and distribution system opened, for fighting fires. It included a well and cistern on 13th Street between Bowery (today 4th Avenue) and Third Avenue, which was then at the northern fringes of the city.[lower-alpha 1] The well was immense—16 feet across and 112 feet deep—blasted largely through rock, resulting in a quarry of over 175,000 gallons of water. A steam engine had the capacity to lift nearly half a million gallons a day. An octagonal iron tank, 43 feet in diameter and 20 feet high was installed atop a 27-foot-high stone tower. Mains under Broadway and the Bowery delivered the water to hydrants on Pearl, William, Hudson, and a dozen other major streets, in six-, ten-, and twelve-inch pipes, delivering water to a height of 60 feet above the highest streets.[5]

The Old Croton Aqueduct was opened for public use in 1842, and apart from a few inspections during the Civil War era the system has been running unceasingly ever since. In the late 1800s, additional aqueducts were systematically installed in to meet the increasing demand.[6]

The city's first aqueduct, the Croton Aqueduct, was built during 1837 to 1842, from the Croton River in Westchester County, down to Manhattan, a distance of 41 miles (66 km).[6] The Old Croton Aqueduct's capacity was around 90 million gallons per day. To meet the city's growing needs, the city started construction of the New Croton Aqueduct in 1885.[6] The new aqueduct opened for operation in 1890 with a capacity of 300 million gallons per day.[7]

In 1905, the city's newly established Board of Water Supply launched the Catskill Aqueduct project, which would play an additional role in supplying the city's ever-growing population of residents and visitors. Construction of the system began in 1907. Portions of the Catskill system began operation in 1916, and the overall system of dams, reservoirs and tunnels was complete by 1924.[8] The Schoharie Reservoir was added to the system and began operation in 1926.[9] The Catskill system has an operational capacity of approximately 850 million gallons per day. Within the city's overall water system, the Catskill Aqueduct is the furthest away from the city, approximately 125 miles (201 km).[2]

The Board of Water Supply submitted a request to the Board of Estimate and Apportionment in 1927 to use the Delaware River as an additional water source for New York City. Even though the request was approved, the Delaware Aqueduct project was delayed due to a Supreme Court case filed by the State of New Jersey to prevent the State of New York from using the Delaware River as a water source. New York won the case in May 1931 and construction of the Delaware Aqueduct began in March 1937. The aqueduct was completed in 1944. From 1950 to 1964, Rondout, Neversink, Pepacton and Cannonsville reservoirs were established successively to complete the Delaware System.[6] The Delaware Aqueduct supports half of the whole city's water usage by supplying more than 500 million gallons of water daily.

The DEP has a workforce of over 7,000 employees. It includes three bureaus in charge of, respectively, the upstate water supply system, New York City's water and sewer operations, and wastewater treatment:

• The Bureau of Water Supply manages, operates, and protects New York City's upstate water supply system to ensure the delivery of a sufficient quantity of high quality drinking water. The Bureau is also responsible for the overall management and implementation of the city's $1.5 billion Watershed Protection Program.
• The Bureau of Water and Sewer Operations operates and maintains the water supply and sewerage system. It is also responsible for the operation of the Staten Island Bluebelt, a natural alternative to storm sewers, which occupies approximately 15 square miles (39 km²) of land in the South Richmond area of Staten Island. This project preserves streams, ponds and other wetland ("bluebelt") areas, allowing them to perform their natural function of conveying, storing and filtering storm water.
• The Bureau of Wastewater Treatment operates 14 water pollution control plants treating an average of 1.5 billion US gal (5.7 million m³) of wastewater a day; 95 wastewater pump stations; eight dewatering facilities; 490 sewer regulators; and 7,000 miles (11,000 km) of intercepting sewers.[10]

The NYW finances the capital needs of the water and sewer system of the city through the issuance of bonds, commercial paper, and other debt instruments. It is a public-benefit corporation created in 1985 pursuant to the New York City Municipal Water Finance Authority Act. The authority is administered by a seven-member Board of Directors. Four of the members are ex officio members: the Commissioner of Environmental Protection of the City, the Director of Management and Budget of the City, the Commissioner of Finance of the City, and the Commissioner of Environmental Conservation of the State. The remaining three members are public appointments: two by the Mayor, and one by the Governor.[11]

The New York City Water Board was established in 1905. It sets water and sewer rates for New York City sufficient to pay the costs of operating and financing the system, and collects user payments from customers for services provided by the water and wastewater utility systems of the City of New York. The five Board members are appointed to two-year terms by the mayor.[12]

The water system has a storage capacity of 550 billion US gal (2.1 billion m³) and provides over 1.2 billion US gal (4.5 million m³) per day of drinking water to more than eight million city residents, and another one million users in four upstate counties bordering on the system. Three separate sub-systems, each consisting of aqueducts and reservoirs, bring water from Upstate New York to New York City:

• The New Croton Aqueduct, completed in 1890, brings water from the New Croton Reservoir in Westchester and Putnam counties.
• The Catskill Aqueduct, completed in 1916, is significantly larger than New Croton and brings water from two reservoirs in the eastern Catskill Mountains.[14]
• The Delaware Aqueduct, completed in 1945, taps tributaries of the Delaware River in the western Catskill Mountains and provides approximately half of New York City's water supply.[15]

The latter two aqueducts provide 90% of New York City's drinking water, and the watershed for these aqueducts extends a combined 1 million acres (400,000 ha). Two-fifths of the watershed is owned by the New York City, state, or local governments, or by private conservancies. The rest of the watershed is private property that is closely monitored for pollutants; development upon this land is restricted.[14] The DEP has purchased or protected over 130,000 acres (53,000 ha) of private land since 1997 through its Land Acquisition Program.[1] Water from both aqueducts is stored first in the large Kensico Reservoir and subsequently in the much smaller Hillview Reservoir closer to the city.[14]

The water is monitored by robotic buoys that measure temperature as well as pH, nutrient, and microbial levels in the reservoirs. A computer system then analyzes the measurements and makes predictions for the water quality. In 2015, the buoys took 1.9 million measurements of the water in the reservoirs.[14]

The water in the Kensico Reservoir flows to the Catskill-Delaware Water Ultraviolet Disinfection Facility, located in Westchester County.[16][14] Although the city water system uses chlorination as a basic disinfection technology, the ultraviolet disinfection (UV) facility was built to control microorganisms such as giardia and cryptosporidium which are resistant to chlorine treatment. Ultraviolet treatment was seen as the least risky way to control such microorganisms and avoid higher levels of chlorination, which can lead to unintended health effects.[14] The UV facility opened on October 8, 2013, and was built at a cost of $1.6 billion.[17] The compound is the largest ultraviolet germicidal irradiation plant in the world; it contains 56 UV reactors that could treat 2.2 billion US gal (8.3 billion L) per day.[16][18]

While all the water goes through the disinfection process, only 10% of the water is filtered. The Croton Water Filtration Plant, completed in 2015 at a cost of over $3 billion,[19][20] was built 160 feet (49 m) under Van Cortlandt Park in the Bronx and filters water delivered by the New Croton Aqueduct.[21] The 830-by-550-foot (250 by 170 m) plant, which is bigger than Yankee Stadium,[19] is New York City's first water filtration plant.[20] The plant was built after the U.S. Environmental Protection Agency (EPA), the U.S. Department of Justice and the State of New York filed suit against the city in 1997 for violating the Safe Drinking Water Act and the New York State Sanitary Code.[22] The city government agreed to rehabilitate the New Croton Aqueduct and build a filtration plant. The plant includes a UV disinfection system.[23] The city had been studying possible sites for such a plant for more than 20 years in both the Bronx and Westchester.[24]

From the Hillview reservoir water flows by gravity to three tunnels under New York City. Water rises again to the surface under natural pressure, through a number of shafts.[14] The three tunnels are:

1. New York City Water Tunnel No. 1, completed in 1917.[14] It runs from the Hillview Reservoir under the central Bronx, Harlem River, West Side, Midtown,[14] and Lower East Side of Manhattan, and under the East River to Brooklyn where it connects to Tunnel 2. It is expected to undergo extensive repairs upon completion of Tunnel No. 3.
2. New York City Water Tunnel No. 2, completed in 1935. It runs from the Hillview Reservoir under the central Bronx, East River, and western Queens to Brooklyn, where it connects to Tunnel 1 and the Richmond Tunnel to Staten Island. When completed, it was the longest large diameter water tunnel in the world.[25]
3. The partially-completed New York City Water Tunnel No. 3, the largest capital construction project in New York City's history (see Ongoing repairs and upgrades).[26] It starts at Hillview Reservoir in Yonkers, New York then crosses under Central Park in Manhattan, to reach Fifth Avenue at 78th Street. From there it runs under the East River and Roosevelt Island into Astoria, Queens. From there it will continue on to Brooklyn.

The distribution system is made up of an extensive grid of water mains stretching approximately 6,800 miles (10,900 km). As of 2015, it costs the city $140 million to maintain these mains.[14]

There are 965 water sampling stations in New York City. The water-sampling system has been in use since 1997. They consist of small cast-iron boxes with spigots inside them, raised 4.5 feet (1.4 m) above the ground.[27] Scientists from the city measure water from 50 stations every day. The samples are then tested for microorganisms, toxic chemicals, and other contaminants that could potentially harm users of the water supply system. In 2015, the DEP performed 383,000 tests on 31,700 water samples.[14]