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Modeling the Impact of Tidal Inundation on Submerging Coastal Landscapes of the Chesapeake Bay

Dep. of Natural Resource Sciences and Landscape Architecture, Univ. of Maryland, College Park, MD 20742

View larger version (23K): [in a new window]   Fig. 1. Topographic cross section of Cedar Creek research site showing elevation of sampled pedons relative to mean high water (MHW)

View larger version (23K): [in a new window]   Fig. 2. Topographic cross section of Hell Hook research site showing elevation of sampled pedons relative to mean high water (MHW)

View larger version (16K): [in a new window]   Fig. 3. Hypothetical depiction of changes in soil properties (such as salinization or alkalinization) in a submerging coastal landscape with time

View larger version (20K): [in a new window]   Fig. 4. Chronofunctions for electrical conductivity (EC) and exchangeable sodium percentage (ESP) for the Hell Hook (HH) and Cedar Creek (CC) research sites, constructed using the weighted mean values for the entire soil profile

View larger version (20K): [in a new window]   Fig. 5. Chronofunctions for electrical conductivity (EC) and exchangeable sodium percentage (ESP) for the Hell Hook (HH) and Cedar Creek (CC) research sites, constructed using the weighted mean values for the upper 50 cm of the soil

View larger version (22K): [in a new window]   Fig. 6. Sigmoidal chronofunctions for electrical conductivity (EC) and exchangeable sodium percentage (ESP) for the Hell Hook (HH) and Cedar Creek (CC) research sites, constructed using the weighted mean values for the entire soil profile. Early and intermediate stages were based on site data, and two possible scenarios for the late stage were projected using theoretical maxima for EC and ESP

View larger version (20K): [in a new window]   Fig. 7. Estimates of weighted mean electrical conductivity (EC) and exchangeable sodium percentage (ESP) for a pedon located 0.5 m above mean high water at the Hell Hook (HH) and Cedar Creek (CC) sites, developed using the sigmoidal chronofunction and three possible sea level rise scenarios