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Tidal Inundation of Transgressive Coastal Areas

Pedogenesis of Salinization and Alkalinization

A.H. Hussein and M.C. Rabenhorst

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



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Fig. 1. Topographic cross section of Cedar Creek research site

 


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Fig. 2. Topographic cross section of Hell Hook research site

 


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Fig. 3. High-tide comparison: Solomons Island vs. Hell Hook (HH) and Cedar Creek (CC) marshes

 


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Fig. 4. Frequency distribution of high tides expected at Hell Hook (HH-M) and Cedar Creek (CC-M) marshes, based upon 50-yr tidal records at Solomons Island

 


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Fig. 5. The depth distribution of electrical conductivity (EC), exchangeable sodium percentage (ESP), and exchangeable acidity (EA%) for all pedons along Hell Hook (HH) and Cedar Creek (CC) transects

 


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Fig. 6. The relationship of the weighted mean electrical conductivity (EC) and exchangeable sodium percentage (ESP) vs. cumulative number of high tides for upland pedons at the Hell Hook transect

 





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