Temperature, specific conductance, and salinity data collected with a YSI 30 handheld system in Greenwich Bay, Rhode Island, May 15, 2009 on U.S. Geological Survey Field Activity 2009-021-FA

As part of a larger investigation to understand groundwater-surface water interactions in Greenwich Bay, Rhode Island, a geophysical survey was conducted from a small research boat on 14-15 May 2009. The specific research objective was to gain an improved understanding of the role of direct groundwater discharge in delivery of excess nitrogen to the bay, which may have contributed to the development of low-oxygen conditions in waters of the bay and associated fish kills. Data collected in this survey included digital navigation information, continuous resistivity profiling (CRP) data, and point salinity measurements. The CRP method is a survey and data processing approach that is sensitive to differences in electrical properties of surface water and underlying porewater in sediments that have contrasting salinities. During the survey, Greenwich Bay salinity was approximately 27 ppm, so surface water would be expected to have low electrical resistivity (high conductivity), and any areas of active groundwater discharge from less salty aquifer sources would yield relatively higher resistivity values. This survey is identified as field activity 09021 (also referenced as 2009-021-FA) by the U.S. Geological Survey, Woods Hole, Massachusetts, and additional information is available from: https://cmgds.marine.usgs.gov/fan_info.php?fan=2009-021-FA.

Data and Resources

Field Value
accessLevel public
bureauCode {010:12}
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identifier http://datainventory.doi.gov/id/dataset/usgs-a47b4b26-db29-4927-a513-10b03e4ed849
metadata_type geospatial
modified 2024-03-18T00:00:00Z
old-spatial -71.446261, 41.654557, -71.371875, 41.681668
publisher U.S. Geological Survey
resource-type Dataset
source_datajson_identifier true
source_hash ab2224226746827147bd0094d786e4fdb1057a335cf66e056718d82305f6ce71
source_schema_version 1.1
spatial {"type": "Polygon", "coordinates": [[[-71.446261, 41.654557], [-71.446261, 41.681668], [ -71.371875, 41.681668], [ -71.371875, 41.654557], [-71.446261, 41.654557]]]}
theme {geospatial}
Groups
  • AmeriGEOSS
  • National Provider
  • North America
Tags
  • AmeriGEO
  • AmeriGEOSS
  • CKAN
  • GEO
  • GEOSS
  • National
  • North America
  • United States
  • cmgp
  • coastal-and-marine-geology-program
  • conductivity
  • field-activity-number-2009-021-fa
  • geoscientificinformation
  • geospatial-datasets
  • greenwich-bay
  • info-bank-id-b-21-09-ri
  • marine-chemistry
  • narragansett-bay
  • north-america
  • ocean-salinity
  • oceans
  • rhode-island
  • salinity
  • temperature
  • u-s-geological-survey
  • united-states
  • usgs
  • usgs-a47b4b26-db29-4927-a513-10b03e4ed849
  • warwick-ri
  • whcmsc
  • woods-hole-coastal-and-marine-science-center
  • ysi-30
isopen False
license_id notspecified
license_title License not specified
maintainer VeeAnn A. Cross
maintainer_email vatnipp@usgs.gov
metadata_created 2025-09-23T16:31:17.636717
metadata_modified 2025-09-23T16:31:17.636723
notes As part of a larger investigation to understand groundwater-surface water interactions in Greenwich Bay, Rhode Island, a geophysical survey was conducted from a small research boat on 14-15 May 2009. The specific research objective was to gain an improved understanding of the role of direct groundwater discharge in delivery of excess nitrogen to the bay, which may have contributed to the development of low-oxygen conditions in waters of the bay and associated fish kills. Data collected in this survey included digital navigation information, continuous resistivity profiling (CRP) data, and point salinity measurements. The CRP method is a survey and data processing approach that is sensitive to differences in electrical properties of surface water and underlying porewater in sediments that have contrasting salinities. During the survey, Greenwich Bay salinity was approximately 27 ppm, so surface water would be expected to have low electrical resistivity (high conductivity), and any areas of active groundwater discharge from less salty aquifer sources would yield relatively higher resistivity values. This survey is identified as field activity 09021 (also referenced as 2009-021-FA) by the U.S. Geological Survey, Woods Hole, Massachusetts, and additional information is available from: https://cmgds.marine.usgs.gov/fan_info.php?fan=2009-021-FA.
num_resources 1
num_tags 32
title Temperature, specific conductance, and salinity data collected with a YSI 30 handheld system in Greenwich Bay, Rhode Island, May 15, 2009 on U.S. Geological Survey Field Activity 2009-021-FA