Item talk:Q229844

From geokb

{

 "@context": "http://schema.org/",
 "@type": "WebPage",
 "additionalType": "Project",
 "url": "https://www.usgs.gov/centers/sawsc/science/groundwater-monitoring-albany-dougherty-county-area-georgia",
 "headline": "Groundwater Monitoring - Albany-Dougherty County Area, Georgia",
 "datePublished": "August 30, 2016",
 "author": [
   {
     "@type": "Person",
     "name": "Debbie Warner Gordon, PG",
     "url": "https://www.usgs.gov/staff-profiles/debbie-warner-gordon",
     "identifier": {
       "@type": "PropertyValue",
       "propertyID": "orcid",
       "value": "0000-0002-5195-6657"
     }
   }
 ],
 "description": [
   {
     "@type": "TextObject",
     "text": "October 2004"
   },
   {
     "@type": "TextObject",
     "text": "USGS Well Name , Site Name, Aquifer\n----------------------------------------------------"
   },
   {
     "@type": "TextObject",
     "text": "November 2001"
   },
   {
     "@type": "TextObject",
     "text": "These declines have raised concern over the ability of the deeper aquifers to meet the increasing demand for potable water supply. To address these concerns USGS is working with Albany Utilities to monitor water-level declines and water-quality changes."
   },
   {
     "@type": "TextObject",
     "text": "October 2007"
   },
   {
     "@type": "TextObject",
     "text": "This map shows all of the Groundwater-level recorders and monthly-monitoring sites in the Albany area. Select a well from the list to get a graph of water levels for the past year."
   },
   {
     "@type": "TextObject",
     "text": "\u2014\u2014\u2014\u2014\u2014\u2014\u2014\u2014\u2014\u2014\u2014\u2014\u2014\u2014\u2014\u2014\u2014\u2014\u2014\u2014\u2014\u2014\u2014\u2014\u2014\u2014\u2014\u2014\u2014\u2014\u2014\u2014\u2014\u2014\u2014\u2014\u2014"
   },
   {
     "@type": "TextObject",
     "text": "Long-term heavy pumping from the Claiborne, Clayton, and Upper Cretaceous aquifers, which underlie the Upper Floridan aquifer, has resulted in significant water-level declines in these deep aquifers in the Albany, Georgia area."
   },
   {
     "@type": "TextObject",
     "text": "March 1999"
   },
   {
     "@type": "TextObject",
     "text": "November 2011"
   },
   {
     "@type": "TextObject",
     "text": "November 2009"
   },
   {
     "@type": "TextObject",
     "text": "Groundwater monitoring sites"
   },
   {
     "@type": "TextObject",
     "text": "November 2010"
   },
   {
     "@type": "TextObject",
     "text": "Potentiometric Maps"
   },
   {
     "@type": "TextObject",
     "text": "October 2002"
   },
   {
     "@type": "TextObject",
     "text": "May 1998"
   },
   {
     "@type": "TextObject",
     "text": "September 2003"
   },
   {
     "@type": "TextObject",
     "text": "November 2008"
   },
   {
     "@type": "TextObject",
     "text": "Objectives"
   },
   {
     "@type": "TextObject",
     "text": "Groundwater Monitoring Program for the Albany-Dougherty County Area, Georgia \nSouth Atlantic Water Science Center"
   },
   {
     "@type": "TextObject",
     "text": "Select a well name to get a graph of water levels for the past year:"
   },
   {
     "@type": "TextObject",
     "text": "October 2005"
   },
   {
     "@type": "TextObject",
     "text": ">> Network map"
   },
   {
     "@type": "TextObject",
     "text": "Long-term heavy pumping from the Claiborne, Clayton, and Upper Cretaceous aquifers, which underlie the Upper Floridan aquifer, has resulted in significant water-level declines in these deep aquifers in the Albany area. These declines have raised concern over the ability of the deeper aquifers to meet the increasing demand for potable water supply. To provide additional water and reduce the demand on the deeper aquifers, the Albany Water Gas, and Light Commission (WGL) has developed a large well field southwest of Albany. The supply wells at this location primarily tap the Upper Floridan aquifer, a karstic unit that is the uppermost reliable source of water in the area. Because of local recharge to the aquifer, water quality may be affected by land use. The groundwater flow system and water quality of the Upper Floridan aquifer in the vicinity of the wellfield is complex. Monitoring is necessary to detect changes in the water level and water quality. The U.S. Geological Survey (USGS), in cooperation with WGL, is conducting a monitoring program for early detection of water-level declines and water-quality changes."
   },
   {
     "@type": "TextObject",
     "text": "August 2000"
   },
   {
     "@type": "TextObject",
     "text": "December 2019"
   },
   {
     "@type": "TextObject",
     "text": "Problem"
   },
   {
     "@type": "TextObject",
     "text": "Groundwater Monitoring Network"
   }
 ],
 "funder": {
   "@type": "Organization",
   "name": "South Atlantic Water Science Center (SAWSC)",
   "url": "https://www.usgs.gov/centers/sawsc"
 },
 "about": [
   {
     "@type": "Thing",
     "name": "Methods and Analysis"
   },
   {
     "@type": "Thing",
     "name": "Information Systems"
   },
   {
     "@type": "Thing",
     "name": "Science Technology"
   },
   {
     "@type": "Thing",
     "name": "Rural Water Monitoring"
   },
   {
     "@type": "Thing",
     "name": "Groundwater and Streamflow Monitoring"
   },
   {
     "@type": "Thing",
     "name": "Albany Georgia"
   },
   {
     "@type": "Thing",
     "name": "Energy"
   },
   {
     "@type": "Thing",
     "name": "Groundwater Monitoring"
   },
   {
     "@type": "Thing",
     "name": "Groundwater Contamination"
   },
   {
     "@type": "Thing",
     "name": "Environmental Health"
   },
   {
     "@type": "Thing",
     "name": "Water"
   },
   {
     "@type": "Thing",
     "name": "Water Availability and Use"
   },
   {
     "@type": "Thing",
     "name": "Geology"
   }
 ]

}