Nebraskaland

NEBRASKAland Aug/Sept 2018

NEBRASKAland Magazine is dedicated to outstanding photography and informative writing with an engaging mix of articles and photos highlighting Nebraska’s outdoor activities, parklands, wildlife, history and people.

Issue link: http://mag.outdoornebraska.gov/i/1008599

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Nebraska's Saline Wetlands • NEBRASKAland Magazine LIMESTONE STREAM-DEPOSITED CLAY, SILT, SAND, AND GRAVEL SALINE MEADOW SALT FLAT SALINE MARSH PRAIRIE Salt Crust on Bare Soil Water Table Seep Foxtail Barley Spearscale Marsh Elder Saltwort Sea Blite Sago Pondweed Saltwater Bulrush Upward Saline Groundwater Flow ILLUSTRATION BY TIM REIGERT salt concentrations. The portion of the salt flat nearest the center of the wetland is the wettest, keeping salts in solution, and salinity levels moderately high. Here, saltwort, a state listed endangered plant found nowhere else in Nebraska, thrives. Beyond the wetter, inner ring of the salt flat, evaporation frequently dries the soil surface, concentrating salt near the surface. Sea blite occupies this slightly drier, central portion of the salt flat zone. Inland saltgrass, dwarfed in stature and sparsely spaced, is often the only plant which can survive on the dry, salt- encrusted outer portion of the salt flat. The greatest diversity of plants on a saline wetland is found in the saline meadow, a transition zone between the salt flat and prairie at the outer edge of the wetland. Closest to the salt flat, foxtail barley and marsh elder dominate, but many other species also grow here, including spearscale and saltmarsh aster. In the saline marsh, sago pondweed and saltwater bulrush thrive. The plants of a saline wetland are seldom arranged in so orderly a manner. The boundaries between zones where one species or another is favored are constantly changing as soil saturation and salinity fluctuate, and a mixing and merging of plant species occurs. Frequently, the most consistently wet portion of a saline wetland is not at the center, but below seeps emerging from the base of hills at the edge of the floodplain, as illustrated here. Salt flats on large basins may have small depressions or "pans" which periodically hold water, where plants most tolerant of high salinity and saturated soils grow. ■

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