. Building salt marshes along the coasts of the continental United States. Marsh ecology; Marshes. Figure 8. Erosion scarp along edge of smooth cordgrass-needle rush marsh growing on peat. percent in shoot growth alone, a figure that compares favorably with upland field crops. The potential for substantial recycling and ex- porting of nutrients to the estuary exists. The absorption, conversion, and recycling abilities of marsh plants offer real opportunities for improving water quality^ (Woodhill, 1977). d. Sediment Accumulation. Marshes perform a valuable role in trapping sediments, thereby r
. Building salt marshes along the coasts of the continental United States. Marsh ecology; Marshes. Figure 8. Erosion scarp along edge of smooth cordgrass-needle rush marsh growing on peat. percent in shoot growth alone, a figure that compares favorably with upland field crops. The potential for substantial recycling and ex- porting of nutrients to the estuary exists. The absorption, conversion, and recycling abilities of marsh plants offer real opportunities for improving water quality^ (Woodhill, 1977). d. Sediment Accumulation. Marshes perform a valuable role in trapping sediments, thereby reducing turbidity in bays, sounds, and estuaries. Turbidity reduction is highly beneficial in protecting shellfish beds from excessive siltation and increasing light penetra- tion which promotes phytoplankton production. Chapman (1938) esti- mates accretion rates in New England salt marshes to be to centimeter per year and Ranwell (1964) reported an average value of to centimeter per year for temperate European marshes. Higher rates probably occur in certain marshes growing in sediment-rich 23. Please note that these images are extracted from scanned page images that may have been digitally enhanced for readability - coloration and appearance of these illustrations may not perfectly resemble the original Woodhouse, W. W. (William Walton), 1910-. Ft. Belvoir, Va. : U. S. Army, Corps of Engineers, Coastal Engineering Research Center
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