Soil Survey of McHenry County, Illinois Part I - Soil Data Mart
Soil Survey of McHenry County, Illinois Part I - Soil Data Mart
Soil Survey of McHenry County, Illinois Part I - Soil Data Mart
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58 <strong>Soil</strong> <strong>Survey</strong> <strong>of</strong><br />
A typical soil series description with range in<br />
characteristics is included, in alphabetical order, in this<br />
section. Additional information specific to this map<br />
unit, such as horizon depth and textures, is available<br />
in the “<strong>Soil</strong> Properties” section in <strong>Part</strong> II <strong>of</strong> this<br />
publication.<br />
Composition<br />
Grundelein and similar soils: 85 percent<br />
Dissimilar soils: 15 percent<br />
Similar soils:<br />
• soils that have no subsurface layer<br />
• soils that contain more sand in the upper one-half <strong>of</strong><br />
the pr<strong>of</strong>ile<br />
• soils that contain sandy and gravelly deposits at a<br />
depth <strong>of</strong> less than 32 inches or more than 50 inches<br />
• soils that contain carbonates at a depth <strong>of</strong> more<br />
than 50 inches<br />
• soils that contain less gravel in the lower part <strong>of</strong> the<br />
pr<strong>of</strong>ile<br />
Dissimilar soils:<br />
• the poorly drained Dunham soils and the very<br />
poorly drained Houghton and Palms soils in<br />
depressions and drainageways<br />
• the well drained Bowes and Waupecan soils in the<br />
higher positions on the landform<br />
Management<br />
For general and detailed information about<br />
managing this map unit, see the following sections in<br />
<strong>Part</strong> II <strong>of</strong> this publication:<br />
• “Agronomy” section<br />
• “Wildlife Habitat” section<br />
• “Engineering” section<br />
• “<strong>Soil</strong> Properties” section<br />
Harpster Series<br />
Drainage class: Poorly drained<br />
Permeability: Moderate<br />
Landform: Outwash plains and moraines<br />
Parent material: Calcareous drift<br />
Slope range: 0 to 2 percent<br />
Taxonomic classification: Fine-silty, mesic Typic<br />
Calciaquolls<br />
Typical Pedon for MLRA 95B<br />
Typical pedon <strong>of</strong> Harpster silt loam, 0 to 2 percent<br />
slopes, undrained, 1,100 feet south and 400 feet west<br />
<strong>of</strong> the northeast corner <strong>of</strong> sec. 5, T. 45 N., R. 8 E.<br />
Ak1—0 to 3 inches; black (10YR 2/1) silt loam, dark<br />
gray (10YR 4/1) dry; moderate fine granular<br />
structure; very friable; many very fine and fine<br />
roots; 10 percent fine snail-shell fragments;<br />
violently effervescent; moderately alkaline; clear<br />
smooth boundary.<br />
Ak2—3 to 11 inches; black (N 2.5/0) silty clay loam,<br />
dark gray (10YR 4/1) dry; moderate fine and<br />
medium granular structure; friable; common very<br />
fine and fine roots; 20 percent fine snail-shell<br />
fragments; violently effervescent; moderately<br />
alkaline; clear smooth boundary.<br />
ABk—11 to 18 inches; 80 percent very dark gray (N<br />
3/0) and 20 percent dark gray (5Y 4/1) silty clay<br />
loam; moderate fine and medium subangular<br />
blocky structure; friable; common very fine and<br />
fine roots; 10 percent fine snail-shell fragments;<br />
common fine prominent grayish brown (2.5Y 5/2)<br />
iron depletions in the matrix; 1 percent gravel;<br />
strongly effervescent; moderately alkaline; clear<br />
smooth boundary.<br />
Bg—18 to 28 inches; light olive gray (5Y 6/2) silty clay<br />
loam; few thin strata <strong>of</strong> clay loam; moderate<br />
medium prismatic structure parting to moderate<br />
fine and medium subangular blocky; firm; common<br />
very fine roots; common fine strong brown (7.5YR<br />
4/6) very weakly cemented iron oxide concretions<br />
throughout; many fine prominent yellowish brown<br />
(10YR 5/4) masses <strong>of</strong> iron accumulation in the<br />
matrix; 2 percent gravel; strongly effervescent;<br />
moderately alkaline; clear wavy boundary.<br />
BCg—28 to 34 inches; light olive gray (5Y 6/2) silty<br />
clay loam; few thin strata <strong>of</strong> clay loam; weak<br />
medium and coarse prismatic structure parting to<br />
weak medium subangular blocky; firm; common<br />
very fine and few medium roots; few distinct very<br />
dark gray (2.5Y 3/1) organic coatings in root<br />
channels and in pores; common fine and medium<br />
strong brown (7.5YR 5/6) very weakly cemented<br />
iron oxide concretions throughout; many fine and<br />
medium prominent yellowish brown (10YR 5/4)<br />
masses <strong>of</strong> iron accumulation in the matrix; 1<br />
percent gravel; strongly effervescent; slightly<br />
alkaline; clear wavy boundary.<br />
Cg1—34 to 43 inches; gray (5Y 6/1) silty clay loam;<br />
few thin strata <strong>of</strong> loam; massive; firm; common<br />
very fine and few medium roots; common fine and<br />
medium strong brown (7.5YR 5/6) very weakly<br />
cemented iron oxide concretions throughout;<br />
many fine and medium prominent yellowish brown<br />
(10YR 5/6) masses <strong>of</strong> iron accumulation in the<br />
matrix; 4 percent gravel; violently effervescent;<br />
moderately alkaline; clear smooth boundary.<br />
Cg2—43 to 60 inches; 50 percent gray (5Y 6/1), 40<br />
percent olive brown (2.5Y 4/4), and 10 percent<br />
gray (2.5Y 5/1), stratified silty clay loam, sand,