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<shortName>CCU groundwater and resistivity study - Winter 2013</shortName>
<title>CCU groundwater and resistivity study - Winter 2013</title>
<creator>
<individualName>
<salutation>Dr.</salutation>
<givenName>Richard</givenName>
<givenName>N.</givenName>
<surName>Peterson</surName>
</individualName>
<organizationName>Coastal Carolina University</organizationName>
<address>
<deliveryPoint>Center for Marine and Wetland Studies</deliveryPoint>
<deliveryPoint>1270 Atlantic Avenue, Room 111</deliveryPoint>
<deliveryPoint>Coastal Carolina University</deliveryPoint>
<city>Conway</city>
<administrativeArea>South Carolina</administrativeArea>
<postalCode>29526</postalCode>
<country>USA</country>
</address>
<electronicMailAddress>rpeters2@coastal.edu</electronicMailAddress>
</creator>
<metadataProvider><organizationName>Georgia Coastal Ecosystems LTER Project</organizationName>
<address>
<deliveryPoint>Dept. of Marine Sciences</deliveryPoint>
<deliveryPoint>University of Georgia</deliveryPoint>
<city>Athens</city>
<administrativeArea>Georgia</administrativeArea>
<postalCode>30602-3636</postalCode>
<country>USA</country>
</address>
<electronicMailAddress>gcelter@uga.edu</electronicMailAddress>
<onlineUrl>https://gce-lter.marsci.uga.edu/</onlineUrl>
</metadataProvider>
<associatedParty>
<individualName>
<salutation>Dr.</salutation>
<givenName>Richard</givenName>
<givenName>N.</givenName>
<surName>Peterson</surName>
</individualName>
<organizationName>Coastal Carolina University</organizationName>
<address>
<deliveryPoint>Center for Marine and Wetland Studies</deliveryPoint>
<deliveryPoint>1270 Atlantic Avenue, Room 111</deliveryPoint>
<deliveryPoint>Coastal Carolina University</deliveryPoint>
<city>Conway</city>
<administrativeArea>South Carolina</administrativeArea>
<postalCode>29526</postalCode>
<country>USA</country>
</address>
<electronicMailAddress>rpeters2@coastal.edu</electronicMailAddress>
<role>Principal investigator</role>
</associatedParty>
<associatedParty>
<individualName>
<givenName>Matthew</givenName>
<surName>Carter</surName>
</individualName>
<organizationName>Coastal Carolina University</organizationName>
<address>
<deliveryPoint>Center for Marine and Wetland Studies</deliveryPoint>
<deliveryPoint>1270 Atlantic Avenue</deliveryPoint>
<deliveryPoint>Coastal Carolina University</deliveryPoint>
<city>Conway</city>
<administrativeArea>South Carolina</administrativeArea>
<postalCode>29526</postalCode>
<country>USA</country>
</address>
<electronicMailAddress>mlcarte2@g.coastal.edu</electronicMailAddress>
<role>Co-investigator</role>
</associatedParty>
<associatedParty>
<individualName>
<salutation>Dr.</salutation>
<givenName>Richard</givenName>
<givenName>F.</givenName>
<surName>Viso</surName>
</individualName>
<organizationName>Coastal Carolina University</organizationName>
<address>
<deliveryPoint>Center for Marine and Wetland Studies</deliveryPoint>
<deliveryPoint>1270 Atlantic Avenue</deliveryPoint>
<deliveryPoint>Coastal Carolina University</deliveryPoint>
<city>Conway</city>
<administrativeArea>South Carolina</administrativeArea>
<postalCode>29526</postalCode>
<country>USA</country>
</address>
<electronicMailAddress>rviso@coastal.edu</electronicMailAddress>
<onlineUrl>http://ww2.coastal.edu/rviso/</onlineUrl>
<role>Co-investigator</role>
</associatedParty>
<pubDate>2026</pubDate>
<abstract>
<section>
<title>Project Goals</title>
<para>Our goal during this research effort will include: 1.) Collect shallow marsh sediment cores with the use of a vibracore sampling system 2.) Electrical resistivity measurements. </para>
<para>Vibracore sampling: A shore normal transect of cores will be taken at 3 sites to characterize the shallow marsh sediment. The sediment cores will be taken back to Coastal Carolina for further analyses that include grain-size analysis, radon sediment equilibration, and bench-top sediment salinity resistivity calibration.   </para>
<para>Geophysical measurements: subsurface resistivity time-series measurements will be conducted by laying a resistivity cable (100m) along a transect form the upland through the marsh and into the river. The cable will remain on the ground surface for about 24hrs measuring the subsurface resistivity.</para>
<para>In addition to the resistivity measurements, we will collect 6-L groundwater grab samples from existing piezometers located at Moses Hammock. This effort will use a self-contained peristaltic pump and tubing to collet water into our gas tight radon analysis bottles.</para>
<para>
</para>
</section>
<section>
<title>Associated GCE LTER research questions</title>
<para>Area 2: Patterns within the Domain (<ulink url="http://gce-lter.marsci.uga.edu/public/research/gce3_area2.asp">more information</ulink>)</para>
</section>
</abstract>
<keywordSet name="habitat">
<keyword>marsh</keyword>
</keywordSet>
<keywordSet name="measurement">
<keyword>salinity</keyword>
<keyword>sedimentology</keyword>
</keywordSet>
<keywordSet name="organization">
<keyword>LTER</keyword>
<keyword>NSF</keyword>
</keywordSet>
<keywordSet name="site">
<keyword>GCE</keyword>
</keywordSet>
<keywordSet name="theme">
<keyword>geology</keyword>
<keyword>geophysics</keyword>
</keywordSet>
<coverage>
<geographicCoverage>
<geographicDescription>Overall geographic extent of the research project</geographicDescription>
<boundingCoordinates>
<westBoundingCoordinate>-81.295500</westBoundingCoordinate>
<eastBoundingCoordinate>-81.277455</eastBoundingCoordinate>
<northBoundingCoordinate>31.459769</northBoundingCoordinate>
<southBoundingCoordinate>31.416170</southBoundingCoordinate>
</boundingCoordinates>
</geographicCoverage>
<temporalCoverage>
<rangeOfDates>
<beginDate>
<calendarDate>2013-12-03</calendarDate>
</beginDate>
<endDate>
<calendarDate>2013-12-06</calendarDate>
</endDate>
</rangeOfDates>
</temporalCoverage>
</coverage>
<funding>
<section>
<para>GCE-LTER sub-award for groundwater quantification, NSF, $75K</para>
</section>
</funding>
<studyAreaDescription>
<descriptor name="hydrology" citableClassificationSystem="false">
<descriptorValue>estuary marsh complex</descriptorValue>
</descriptor>
<coverage>
<geographicCoverage>
<geographicDescription>LumberLanding - Lumber Landing dock on the Duplin River at Sapelo Island, Georgia</geographicDescription>
<boundingCoordinates>
<westBoundingCoordinate>-81.277455</westBoundingCoordinate>
<eastBoundingCoordinate>-81.277455</eastBoundingCoordinate>
<northBoundingCoordinate>31.459769</northBoundingCoordinate>
<southBoundingCoordinate>31.459769</southBoundingCoordinate>
</boundingCoordinates>
</geographicCoverage>
<geographicCoverage>
<geographicDescription>Marsh_Landing_ML - Marsh_Landing_ML sampling site used by Amy Kunza in 2005 to study plant species richness</geographicDescription>
<boundingCoordinates>
<westBoundingCoordinate>-81.295500</westBoundingCoordinate>
<eastBoundingCoordinate>-81.295500</eastBoundingCoordinate>
<northBoundingCoordinate>31.416170</northBoundingCoordinate>
<southBoundingCoordinate>31.416170</southBoundingCoordinate>
</boundingCoordinates>
</geographicCoverage>
</coverage>
<associatedMaterial category="data">
<distribution>
<online>
<onlineDescription>Map (Google Earth KML/KMZ or map image)</onlineDescription>
<url>https://gce-lter.marsci.uga.edu/private/registration/files/Maps/GCE-53-2013_Maps_Duplin_River_Field_Survey_December_2013.kmz</url>
</online>
</distribution>
</associatedMaterial>
</studyAreaDescription>
<designDescription>
<description>
<section>
<title>Project Location</title>
<para>Ferry landing sediment cores:</para>
<para>31°25'5.18"N 81°17'43.15"W</para>
<para>31°25'3.78"N 81°17'39.10"W</para>
<para>31°25'1.51"N 81°17'36.44"W</para>
<para>Lumber landing sediment cores:</para>
<para>31°27'29.12"N 81°16'41.75"W</para>
<para>31°27'29.04"N 81°16'41.08"W</para>
<para>Moses Hammock sediment cores:</para>
<para>31°28'39.53"N 81°16'21.13"W</para>
<para>31°28'39.70"N 81°16'20.83"W</para>
<para>Electrical Resistivity Transect in line with the Moses Hammock sediment core GPS.</para>
<para>
</para>
</section>
<section>
<title>Equipment</title>
<para>A 100 meter electrode array and control box will be deployed in a short 24 hour period. After the survey is conducted the electrode array will be removed.  The vibracore system consists of an 8ft. aluminum tripod, a small portable generator, a vibracore head, and 7 (2.5 meter) aluminum core pipes. This deployment will be broken down daily.</para>
</section>
</description>
</designDescription>
<associatedMaterial category="publication" id="gce.1118" date="2019">
<distribution>
<offline>
<mediumName>Peterson, R.N., Meile, C., Peterson, L., Carter, M. and Miklesh, D.M. 2019. Groundwater discharge dynamics into a salt marsh tidal river. Estuarine, Coastal and Shelf Science. 218:324-333. (DOI: 10.1016/j.ecss.2019.01.007)</mediumName>
</offline>
</distribution>
</associatedMaterial>
<associatedMaterial category="publication" id="gce.1056" date="2017">
<distribution>
<offline>
<mediumName>Peterson, R.N., Meile, C., Carter, M., Peterson, L., Waldorf, A. and Miklesh, D.M. 2017. Poster: Groundwater inputs to a back-barrier salt marsh tidal river. 2017 Chemical Oceanography Gordon Research Conference, July 2017, Holderness, NH.</mediumName>
</offline>
</distribution>
</associatedMaterial>
</lter:researchProject>
