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U.S. Geological Survey Open-File Report 2012-1099

Summary of Oceanographic and Water-Quality Measurements near the Blackwater National Wildlife Refuge, Maryland, 2011


Introduction

Click on figures for larger images
thumbnail image of figure 1 and link to larger figure.  Map showing experimental region in the context of the region
Figure 1. Map of the region (left) with an inset showing the experimental area with sites on the Blackwater and Transquaking Rivers marked. © 2012 Mapquest, © 2012 Google.
thumbnail image of figure 2A and link to larger figure. Map showing all sites in the study area.
Figure 2A. Image showing the entire experimental area with mooring ID's shown. The upstream sites are indistinguishable at this scale, but enlargements of the upstream regions (2B and 2C) show the detail. Green markers indicate the sites used in the spring deployment, and yellow ones the fall. This figure was created with ESRI ArcGIS using the i-cubed Nationwide Prime database (June 2012).
thumbnail image of figure 2B and link to larger figure. Enlargement showing Blackwater River upstream sites.
Figure 2B. Enlargement of the Blackwater River upstream sites with mooring ID's shown. Green markers indicate the sites used in the spring deployment, and yellow one the fall. This figure was created with ESRI ArcGIS using the i-cubed Nationwide Prime database (June 2012).
thumbnail image of figure 2C and link to larger figure. Enlargement showing Transquaking River upstream site.
Figure 2C. Enlargement of the Transquaking River upstream sites with mooring ID's shown. Green markers indicate the sites used in the spring deployment, and yellow one the fall. This figure was created with ESRI ArcGIS using the i-cubed Nationwide Prime database (June 2012).
Skip past contents information This report presents oceanographic and water-quality observations measured at several locations near the Blackwater National Wildlife Refuge (BNWR) in Maryland during spring and fall of 2011 (fig. 1). Wetlands within BNWR have been experiencing rapid disintegration due to multiple factors, including sea-level rise, atmospheric forcing, and invasive species (Stevenson and others, 1985). The suspended-sediment concentrations and net fluxes to and from wetlands may provide insight into the relative stability. Therefore we occupied sites in two contrasting wetland complexes: one adjacent to the Blackwater River, and a more stable complex adjacent to Fishing Bay and the Transquaking River.

Study sites on both rivers were occupied in both spring and fall (fig. 2A). Because the scale of figure 2A is too large to show detail of the upstream sites, enlargements of these areas are provided (Blackwater River fig. 2B; Transquaking River fig. 2C).

Between March and May 2011, continuous measurements were collected at three sites in the Blackwater complex (moorings 903, 904, 905) and three sites in the Fishing Bay complex (moorings 906, 907, 908). Between September and October 2011, continuous measurements were collected at two sites in the Blackwater complex (moorings 916, 917) and two sites in the Fishing Bay complex (moorings 915, 918). Parameters measured include water level, velocity, salinity, temperature, pH,  disolved oxygen and turbidity.

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