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Scientists recognize two major types of wetland soils: organic and mineral.
Lucky for scientists, color charts exist that key soil color with the amount of water in the soil. The U.S. Natural Resource Conservation Service also publishes a list of hydric soils. Soil content also determines the speed of draining. For example, water seeps through sandy soils faster than clay soils. Sand particles are large and irregularly shaped; they have more air pockets through which water can move. Clay particles are smaller and they can compress when wet; their smaller air pockets fill more quickly and completely.
Cypress trees, which grow in freshwater swamps, have knobs or "knees" of root material that emerge from the water; scientists speculate that these knees absorb oxygen. The roots of floating plants, such as duckweed or lilies, dangle into water and absorb oxygen. Wetlands plants also must be efficient at absorbing other nutrients such as nitrogen and phosphorus. For example, in wetlands, nitrogen is most often available as ammonia (NH4+), thus many wetlands plants have become super-efficient absorbers of ammonia. Sometimes Wetlands
Are Hard to Identify So take a look at the location: is it on high ground or a depression, slough, or other low ground? Sample the soil and study its color and composition. For example, some prairie potholes in the Dakotas may remain dry during a prolonged drought. When the rains and snow return, though, they reappear and continue to provide excellent habitat for ducks and other creatures. Soil alone won't identify these potholes, though, because even dry grasslands contain soils that resemble hydric soils. To confirm the presence of a pothole during a drought, you need to look for a layer of decomposed vegetation in the soil, lots of mottling, and the remains of aquatic insects and other invertebrates near the surface. |
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