Groundwater Station: DGS Well Jd14-01
DGS Well Jd14-01
Groundwater Station: DGS Well Id55-01
DGS Well Id55-01
Groundwater Station: DGS Well Ec32-07
DGS Well Ec32-07
Groundwater Station: DGS Well Bc43-01
DGS Well Bc43-01
Hydrogeologic Resources for Delaware
Hydrogeologic data and information for Delaware. This includes the Water Conditions Report, groundwater well data, links to real-time data from DEOS and USGS, and other general information about Delaware's hydrogeology.
Summary of Water Conditions in Delaware
Delaware Water Conditions Report for current and historical periods of record.
Groundwater Station: DGS Well Qe44-01
DGS Well Qe44-01
Groundwater Station: DGS Well Mc51-01a
DGS Well Mc51-01a
Groundwater Station: DGS Well Hb14-12
DGS Well Hb14-12
Groundwater Station: DGS Well Db24-18
DGS Well Db24-18
Integration of groundwater monitoring into Delaware's water resources programs
Andres presented at the Delaware Rural Water Association and Delaware Clean Water Advisory Council
Digital Water-Table Data for New Castle County, Delaware (Digial Data Product No. 05-04)
This digital product contains gridded estimates of water-table (wt) elevation and depth to water (dtw) under dry, normal, and wet conditions for New Castle County, Delaware excluding the Piedmont. Files containing the point data used to create the grids are also included. This work is the final component of a larger effort to provide estimates of water-table elevations and depths to water for the Coastal Plain portion of Delaware. Mapping was supported by the Delaware Department of Natural Resources and Environmental Control and the Delaware Geological Survey.
These grids were produced with the same multiple linear regression (MLR) method as Andres and Martin (2005). Briefly, this method consists of: identifying dry, normal, and wet periods from long-term observation well data (Db24-01, Hb14-01); estimating a minimum water table (Sepulveda, 2002) by fitting a localized polynomial surface to elevations of surface water features (e.g., streams, swamps, and marshes); and, computing a second variable in the regression from water levels observed in wells. Separate MLR equations were determined for dry, normal, and wet periods and these equations were used in ArcMap v.9 (ESRI, 2004) to estimate grids of water-table elevations and depths to water. New Castle County was divided into a northern section and a southern section with the C&D Canal being the natural line of demarcation. A minimum water-table surface was then calculated for both the northern and southern sections of New Castle County. However, dividing the county, as well as the water-level data, into two sections did not result in sufficient regression coefficients for use in the estimation process. Therefore, the data (minimum water-table surface and water-level data) were merged together and the water-table elevation and depth to water grids for dry, normal, and wet conditions were then calculated for the county as a whole.
Digital Water-Table Data for Kent County, Delaware (Digital Data Product No. 05-03)
This digital product contains gridded estimates of water-table (wt) elevation and depth to water (dtw) under dry, normal, and wet conditions for Kent County, Delaware. Files containing the point data used to create the grids are also included. This work is the final component of a larger effort to provide estimates of water-table elevations and depths to water for the Coastal Plain portion of Delaware. Mapping was supported by the Delaware Department of Natural Resources and Environmental Control and the Delaware Geological Survey.
These grids were produced with the same multiple linear regression (MLR) method as Andres and Martin (2005). Briefly, this method consists of: identifying dry, normal, and wet periods from long-term observation well data (Hb14-01, Jd42-03, Mc51-01, Md22-01); estimating a minimum water table (Sepulveda, 2002) by fitting a localized polynomial surface to elevations of surface water features (e.g., streams, swamps, and marshes); and, computing a second variable in the regression from water levels observed in wells. A separate MLR equation was determined for dry, normal, and wet periods and these equations were used in ArcMap v.9 (ESRI, 2004) to estimate grids of water-table elevations and depths to water. Kent County was divided into three regions (south, central, north). A minimum water-table surface was calculated for each of these areas and were merged together to create a single minimum water-table surface for the entire county. This grid was filtered and smoothed to eliminate edge effects that occurred at the boundaries between each of the three regions. Water-table elevation and depth to water grids for dry, normal, and wet conditions were then calculated for the county as a whole.
Digital Water-Table Data for Sussex County, Delaware (Digital Data Product No. 05-01)
This digital product contains gridded estimates of water-table (wt) elevation and depth to water (dtw) under dry, normal, and wet conditions for Sussex County, Delaware. Files containing the point data used to create the grids are also included. This work is the final component of a larger effort to provide estimates of water-table elevations and depths to water for the Coastal Plain portion of Delaware. Mapping was supported by the Delaware Department of Natural Resources and Environmental Control and the Delaware Geological Survey.
These grids were produced with the same multiple linear regression (MLR) method as Andres and Martin (2005). Briefly, this method consists of: identifying dry, normal, and wet periods from long-term observation well data (Nc45-01, Ng11-01, Qe44-01); estimating a minimum water table (Sepulveda, 2002) by fitting a localized polynomial surface to elevations of surface water features (e.g., streams, swamps, and marshes); and computing a second variable in the regression from water levels observed in wells. A separate MLR equation was determined for dry, normal, and wet periods, and these equations were used in ArcMap v.9 (ESRI, 2004) to estimate grids of water-table elevations and depths to water. Grids produced in this project were merged with those previously completed for eastern Sussex and smoothed to minimize edge effects.
Nanticoke Watershed Water-Quality Database (Data Product No. 05-02)
The Nanticoke Watershed Water-Quality Database (NWWWQDB) is used to
store, manage, and retrieve water-quality data generated by the “Nanticoke River
Watershed” project. The database contains information on sampling stations, samples,
and field and laboratory analyses, queries to extract and analyze data, forms to input and
edit data, a main menu to navigate to forms and specific queries, and a few formatted
report templates. The database is in Microsoft Access 2003 format. Table, field, and table
relationship metadata are stored in the database as properties of those objects. The
software's metadata reporting options can be used to view the information.
Delaware Inland Bays Tributary Total Maximum Daily Load Water-Quality Database (Data Product No. 02-02)
The Delaware Inland Bays Water-Quality Database (DIBWQDB) is used to store,
manage, and retrieve water-quality data generated by the “Nutrient Inputs as a Stressor
and Net Nutrient Flux as an Indicator of Stress Response in Delawares’ Inland Bays
Ecosystem” (CISNet) and the “Inland Bays Tributary Total Maximum Daily Load”
(IBTMDL) projects. It contains information on sampling stations, samples, and field and
laboratory analyses, queries to extract and analyze data, forms to input and edit data, a
main menu to navigate to forms and specific queries, and a few formatted report
templates. The database is in Microsoft Access 2003 format. Table, field, and table
relationship metadata are stored in the database as properties of those objects. The
software's metadata reporting options can be used to view the information.
Recent and Historical Groundwater Level Data
Recent and Historical Groundwater Level Data. Data accessible on this page are a subset of DGS holdings. Click on the chart link to display a hydrograph or the data link to download all observations for the period of record.



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