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tOfficial Series Description - LERDAL Series Page 1 of 3 <br /> ' LOCATION LERDAL MN <br /> Established Series <br /> ' Rev. JUS-ELB-JFB-KDS <br /> 2/98 <br /> LERDAL SERIES <br /> ' The Lerdal series consists of very deep, somewhat poorly drained soils that formed in clayey glacial till <br /> or flow till on glacial moraines. Permeability is slow. Slopes range from 1 to 18 percent. Mean annual <br /> precipitation is about 29 inches. Mean annual air temperature is about 48 degrees F. <br /> TAXONOMIC CLASS: Fine, smectitic, mesic Aeric Vertic Epiaqualfs <br /> ' TYPICAL PEDON: Lerdal silty clay loam with a plane slope of about 4 percent on a glacial moraine at <br /> an elevation of 1,290 feet in a pasture field. (Colors are for moist soil unless otherwise stated.) <br /> Ap--O to 7 inches; black(1 OYR 2/1) silty clay loam, dark gray (1 OYR 4/1) dry; weak very fine <br /> subangular blocky structure; friable; about 2 percent gravel, mostly shale; slightly acid; abrupt smooth <br /> ' boundary (6 to 10 inches thick) <br /> E--7 to 9 inches; very dark gray (I OYR 3/1) silty clay loam, gray(I OYR 6/1) dry; many fine faint dark <br /> ' gray (1 OYR 4/1) Fe depletions; moderate fine subangular blocky structure; friable; about 2 percent <br /> gravel,mostly shale; moderately acid; clear wavy boundary. (0 to 6 inches thick) <br /> Btl--9 to 14 inches; dark grayish brown(I OYR 4/2) silty clay loam, few medium prominent light olive <br /> brown(2.5Y 5/6)Fe concentrations; moderate fine and medium subangular blocky structure; firm; <br /> common faint very dark grayish brown(1 OYR 3/2)coatings and clay films on faces of peds; about 2 <br /> percent gravel, mostly shale; moderately acid; clear wavy boundary. (0 to 10 inches thick) <br /> Bt2--14 to 20 inches; olive brown(2.5Y 4/4) silty clay loam; common fine distinct light olive brown <br /> (2.5Y 5/6) Fe concentrations;moderate fine and medium subangular blocky structure; very firm; . <br /> common distinct very dark grayish brown(2.5Y 3/2) coatings and clay films on faces of peds; about 2 <br /> percent gravel, mostly shale; very strongly acid; clear wavy boundary. <br /> ' Btgl--20 to 30 inches; grayish brown(2.5Y 5/2) silty clay; common fine distinct light olive brown <br /> (2.5Y 5/6)Fe concentrations;moderate medium and coarse prismatic structure; very firm; common <br /> distinct very dark grayish brown(10YR 3/2)clay films on faces of peds; about 2 percent gravel, mostly <br /> shale; strongly acid; clear wavy boundary. <br /> ' Btg2--30 to 42 inches; grayish brown(2.5Y 5/2) clay loam; many fine and medium distinct light olive <br /> brown(2.5Y 5/4) Fe concentrations; weak coarse prismatic structure; firm; common faint very dark <br /> grayish brown(2.5Y 3/2) clay films on faces of peds and in root channels; about 5 percent gravel, <br /> ' mostly shale; slightly acid; abrupt wavy boundary. (Combined thickness of Bt and Btg horizons is 15 to <br /> 36 inches.) <br /> ' Bw--42 to 47 inches; olive brown(2.5Y 4/4) clay loam; many fine and medium faint light olive brown <br /> (2.5Y 5/4) Fe concentrations; weak coarse prismatic structure; firm; common prominent clay films in <br /> htt ://ortho.ftw.nres.usda. ov/c i-bin/osd/osdname.c i?-P 11/2/2004 <br /> P g g g <br />