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<br /> from well drained to poorly drained and are nearly level to steep. They . <br /> formed under deciduous hardwood forest. <br /> Soil Series Occurrence - <br /> Markey series - occupies bogs and depressional areas <br /> Rifle series - occupies depressions <br /> Selleyville series - occupies bogs <br /> Seeleyville/muck (540) - very poorly drained, moderately rapid <br /> permeability, very high available water capacity, low natural fertility, high <br /> organic matter content. <br /> Rifle muck (541) - very poorly drained, moderately rapid permeability, <br /> very high available water capacity, low natural fertility, very high organic <br /> matter content. <br /> Markey muck (543) - very poorly drained, moderately rapid permeability, <br /> very high available water capacity, low natural fertility, high organic <br /> matter content. <br /> 3. Soils formed dominantly in recent alluvium. <br /> These soils are mostly bottom-land soils that formed in recent stratified . <br /> alluvium and variable textured fill materials on flood plains. They are <br /> nearly level to very gently sloping and somewhat poorly drained. They <br /> formed under hardwood forest on bottom land. <br /> Soil Series Occurrence <br /> Algansee series - occupies flood plains <br /> Chaska series - occupies planes to slightly concave side slopes in <br /> flood plains. <br /> Chaska silt-loam (329) - poorly drained, moderate permeability, high <br /> available water capacity, medium natural fertility, moderate organic <br /> matter content. <br /> Algansee loamy sand (1821) - somewhat poorly drained, very rapid <br /> permeability, low available water capacity, low natural fertility, low <br /> organic matter content. <br /> Udorthents, wet substratum (1027) - variable drainage, variable <br /> permeability, variable water capacity, variable fertility, variable organic <br /> matter content. <br /> . <br /> VI-2 <br /> ,- --- <br />