Figure 9
From: The effect of tidal forcing on biogeochemical processes in intertidal salt marsh sediments
Water levels in the monitoring wells at the sediment-water interface (SWI), 15, 30, and 60 cm below the SWI recorded as a function of time in the: a) mud flat and b) creek bank sites in June 2003. Measurements were collected immediately after the wells were installed at the mud flat site, while measurements were collected two days after installation at the creek bank site. Insets show a close view of the differences in water levels at both sites.