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Figure 1 | Geochemical Transactions

Figure 1

From: The effect of tidal forcing on biogeochemical processes in intertidal salt marsh sediments

Figure 1

Geographic location of Skidaway Island, the Salt marsh Ecosystem Research Field station (SERF), and sampling sites along the boardwalk across the salt marsh. The mud flat site (MF) is located 122 m from the island in the unvegetated part of the salt marsh. The creek bank site (CB) is located 168 m from the island in a perennial channel off the main creek. Four monitoring wells (mw), positioned approximately 30 cm apart, were inserted at each site to monitor fluid advection. Arrows indicate direction of the surface water flow at ebb tide.

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