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U.S. Geological Survey Fact Sheet FS-129-02 (PDF:524k)
March 2003

Prepared in cooperation with the
NEW JERSEY DEPARTMENT OF ENVIRONMENTAL PROTECTION

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REAL-TIME GROUND-WATER-LEVEL MONITORING IN NEW JERSEY, 2002

By Walter D. Jones, Anthony S. Navoy, and Daryll A. Pope


A network of 15 observation wells that transmit ground-water-level data on a real-time basis through satellite telemetry is operating (started May 2001) in New Jersey through a cooperative effort of the U.S. Geological Survey (USGS) and the New Jersey Department of Environmental Protection (NJDEP). The water-level data from these observation wells are transmitted every 4 hours and then are immediately posted for viewing on the Internet. This fact sheet describes the rationale for real-time monitoring of ground-water levels, the design of the network, and the equipment used to measure water levels and transmit the data to the Internet. Instructions for viewing the data are included.

Background

This network was created to provide data to indicate water-level trends in shallow ground-water systems within the State of New Jersey and to make the data available in the shortest time possible. The wells in this network are located throughout New Jersey (fig. 1) and were chosen because they are completed in shallow aquifers (table 1). The monitoring of shallow aquifers is important because these aquifers are relied on for water supply and irrigation. Additionally, the natural discharge from shallow aquifers provides base flow to streams. Water levels in these aquifers respond relatively quickly to precipitation and dry periods, so the rapid reporting of water-level data is necessary to follow trends. This network, for example, provides data that allow observation of the onset of drought conditions in ground water. Also, the data from this network can be used to estimate the most recent water-level trend in surficial-aquifer wells not outfitted with satellite telemetry.

Figure 1. Location of the 15 observation wells transmitting real-time data and New Jersey Department of Environmental Protection Drought Regions.

Figure 1. Location of the 15 observation wells transmitting real-time data and New Jersey Department of Environmental Protection Drought Regions.

Table 1. Characteristics of ground-water monitoring wells with realtime data.
[USGS, U.S. Geological Survey; ID, identification; a.s., aquifer system; w.b.z., water-bearing zone]
Well nameCountyUSGS Site ID numberStart of
record
Aquifer or formationWell depth
(ft)
Lebanon SF 23-DBurlington3951500742842011955Kirkwood-Cohansey a.s.33
Winslow 5Camden3944400745931011972Kirkwood-Cohansey a.s.76
Pump Pond NCape May3901560745334011992Holly Beach w.b.z.43
Vocational School 2Cumberland3927310750924011972Kirkwood-Cohansey a.s.47
Corsalo RdHunterdon4021510745253011989Passaic Formation299
Readington School 11Hunterdon4035170744525011990Passaic Formation101
Environmental Center 1Hunterdon4034550745148011991Stockton Formation175
Cranston Farms 15Mercer4018040744326011990Stockton Formation200
Morrell 1Middlesex4021430741852011923Englishtown a.s.11
Green Pond 5Morris4102070742700011981Stratified Drift120
Black River 10Morris4049340744005011991Precambrian Erathem200
LNAS-ECOcean4002320742132011992Kirkwood Cohansey a.s.38
TaylorSussex4109140745404011988Bossardsville Limestone95
Swartswood Park 5Sussex4104490744833011991Allentown Dolomite148
Union County ParkUnion4041060741719011943Passaic Formation290


Description of the Network

Six of the wells are completed in the unconfined parts of the sand and gravel aquifers of the New Jersey Coastal Plain, namely the Kirkwood-Cohansey aquifer system, the Englishtown aquifer system, and the Holly Beach water-bearing zone. Additional information about the aquifers of the Coastal Plain can be found in Zapecza (1989). Eight of the wells are in northern New Jersey and are completed in bedrock formations, namely the Passaic Formation, the Stockton Formation, the Allentown Dolomite, and the Bossardsville Limestone, or in Precambrian Rocks (table 1). Although these wells are deeper, the fractures in the bedrock are connected to the land surface; therefore, water levels respond quickly to precipitation. One well is completed in a stratified-drift aquifer in northern New Jersey. Water levels have been collected at these 15 sites for periods that range from 11 to 80 years. Herman and others (1998) summarize the important aquifers of New Jersey.

Well locations were selected to obtain an even distribution of sites throughout New Jersey and to attempt to locate wells within each of the six Drought Regions established by NJDEP (Hoffman, 2001). The areas represented by each Drought Region (fig. 1) are based on large-scale watersheds and similarity of water-supply characteristics, and are defined "so as to match municipal boundaries in order to assist enforcement of mandated water cutbacks during drought emergencies" (Hoffman 2001, p. 1).

Figure 2. Photograph of USGS Data Collection Platform.

Figure 2. Typical equipment at a real-time ground-water-level network site, including the observation well, equipment shelter, data collection platform, solar power panel, and satellite antenna.


Description of Data Collection and Reporting System

Water levels in each well in the network are automatically measured at hourly intervals and stored by a Data Collection Platform (DCP) located on site (fig. 2). Every 4 hours, a burst of data is broadcast from the site to the GOES satellite and relayed to a ground station. The data are retransmitted by the DOMSAT satellite to a USGS ground station, decoded, and automatically posted to the New Jersey District USGS Internet web page for viewing (fig. 3). To ensure the accuracy of the data, each well is visited every 6 to 8 weeks by a USGS technician who makes a manual water-level measurement to check the automated system and to perform maintenance on the equipment.

Figure 3. Schematic drawing showing data transmission from an observation well through satellite telemetry to users on the Internet.

Figure 3. Schematic drawing showing data transmission from an observation well through satellite telemetry to users on the Internet.


Where to View Data

The ground-water level data from this network can be viewed by following these instructions:

  1. Attach to the Internet web page, http://waterdata.usgs.gov/nj/nwis/current/?type=gw. This page lists each well in the network and indicates the latest water-level measurement.
  2. Choose an observation well by clicking on its station number. This leads to a page that summarizes the characteristics of the well, lists the monthly water-level statistics, and shows a hydrograph of the hourly measurements for the latest 7 days (fig. 4).
  3. The output format can be modified to produce a table of water-level values or a hydrograph. The timeframe for the table or hydrograph can be modified from the past 7 days up to the past 31 days by changing the value for "Days" in the box located above the hydrograph and then clicking on the "get data" button. A new hydrograph will then be drawn. Note that clicking on the indicated text will produce a presentation-quality hydrograph that can be downloaded easily and printed by the viewer.
Hydrograph of USGS 392731075092401, Vocational School 2 from January 7, 2002 through January 14, 2002

Figure 4. Example of an actual ground-water hydrograph that can be viewed and printed from the real-time network web page.

The monthly statistics and historical data are provided on the web page to put the current water level in context. The number of years of data used to calculate the statistics is provided first. Statistics on the water levels are provided in terms of the depth to water below land surface. The minimum depth to water for a well actually describes the highest water level measured in that well for the month, and the maximum depth to water describes the lowest water level for the month. The 75 and 25 percent exceedance values are the water levels that were surpassed by 75 and 25 percent, respectively, of all daily mean depths to water during the month. The latest water-level value (obtained from the table or from the line above the hydrograph) can be compared to the monthly statistics.

Because the water-level data are shown automatically, the message "Provisional data subject to revision" is incorporated into the graphs and charts on the web page. If problems with the measurement, communication, or storage systems are found, revisions will be made to the USGS database at a later time to provide the corrected values. For more information about this issue, click on the "Provisional data subject to revision" heading.

For these 15 sites, daily mean depths to water below land surface also are available for the last 550 days (approximately 18 months). A location map, water-quality data, and a database of monthly water levels can be accessed from the home page for each well.

USGS, in cooperation with NJDEP and other agencies, regularly monitors water levels in about 175 other wells in New Jersey. The data from these wells, although not posted on a real-time basis, are available on the web site http://nj.usgs.gov/gw/gw_hydrographs.html. Ground-water data for all wells routinely monitored by USGS, including those of the real-time network, are summarized in an annually published report (for example, Jones, 2002).


Future Sites

The ultimate goal of this joint effor of the USGS and the NJDEP is to establish a network of about 21 wells that will provide an even geographic and hydrologic distribution of real-time monitoring wells in order to characterize shallow-ground-water conditions statewide.

--Walter D. Jones, Anthony S. Navoy, and Daryll A. Pope


References Cited

Herman, G.C., Canace, R.J., Stanford, S.D., Pristas, R.S., Sugarman, P.J., French, M.A., Hoffman, J.L., Serfes, M.S., and Mennel, W.J., 1998, Aquifers of New Jersey: New Jersey Geological Survey, Open-File Map, OFM-24, 1 sheet.

Hoffman, J. L., 2001, Development of New Jersey drought regions: New Jersey Geological Survey Technical Memorandum 01-1, 18 p.

Jones, W. D., 2002, Water Resources Data, New Jersey, Water Year 2001, Volume 2. Ground-Water Data: U. S. Geological Survey Water-Data Report NJ-01-2, 232 p.

Zapecza, O.S., 1989, Hydrogeologic framework of the New Jersey Coastal Plain: U. S. Geological Survey Professional Paper 1404-B, 49 p., 24 pl.


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