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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<strong>McHenry</strong> <strong>County</strong>, <strong>Illinois</strong>—<strong>Part</strong> I 123<br />
35 percent very dark grayish brown (2.5Y 3/2)<br />
loam, dark grayish brown (10YR 4/2) dry; weak<br />
fine and medium subangular blocky structure;<br />
friable; common very fine roots; neutral; clear<br />
smooth boundary.<br />
Btg1—15 to 20 inches; dark grayish brown (2.5Y 4/2)<br />
loam; weak medium prismatic structure parting to<br />
moderate medium subangular blocky; friable;<br />
common very fine roots; few distinct dark gray<br />
(2.5Y 4/1) clay films and black (10YR 2/1) organic<br />
coatings on faces <strong>of</strong> peds and in pores; common<br />
fine distinct olive brown (2.5Y 4/4) masses <strong>of</strong> iron<br />
accumulation in the matrix; common fine and<br />
medium faint grayish brown (2.5Y 5/2) iron<br />
depletions in the matrix; 1 percent gravel; neutral;<br />
gradual smooth boundary.<br />
Btg2—20 to 30 inches; grayish brown (2.5Y 5/2) clay<br />
loam; moderate medium subangular blocky<br />
structure; friable; common very fine roots; few<br />
distinct dark gray (2.5Y 4/1) and grayish brown<br />
(2.5Y 4/2) clay films on faces <strong>of</strong> peds and in<br />
pores; common fine strong brown (7.5YR 4/6)<br />
very weakly cemented iron oxide concretions<br />
throughout; common fine and medium distinct light<br />
olive brown (2.5Y 5/4) masses <strong>of</strong> iron<br />
accumulation in the matrix; 2 percent gravel;<br />
neutral; gradual smooth boundary.<br />
Btg3—30 to 42 inches; light olive gray (5Y 6/2) clay<br />
loam; weak medium and coarse subangular<br />
blocky structure; friable; few very fine roots; few<br />
distinct olive gray (5Y 5/2) clay films on faces <strong>of</strong><br />
peds and in pores; very dark gray (10YR 3/1)<br />
krotovina; common fine strong brown (7.5YR 4/6)<br />
very weakly cemented iron oxide concretions<br />
throughout; common fine and medium prominent<br />
light olive brown (2.5Y 5/4) masses <strong>of</strong> iron<br />
accumulation in the matrix; 2 percent gravel;<br />
neutral; clear smooth boundary.<br />
2BCg—42 to 47 inches; grayish brown (2.5Y 5/2)<br />
sandy loam; weak medium subangular blocky<br />
structure; very friable; few very fine roots;<br />
common medium and coarse distinct light olive<br />
brown (2.5Y 5/4) masses <strong>of</strong> iron accumulation in<br />
the matrix; 4 percent gravel; neutral; clear wavy<br />
boundary.<br />
2Cg—47 to 60 inches; grayish brown (2.5Y 5/2) loamy<br />
sand; massive; very friable; common medium and<br />
coarse prominent yellowish brown (10YR 5/6)<br />
masses <strong>of</strong> iron accumulation in the matrix; 4<br />
percent gravel; neutral.<br />
MLRA Series Range in Characteristics<br />
Thickness <strong>of</strong> the mollic epipedon: 10 to 20 inches<br />
Depth to sandy outwash: 35 to 55 inches<br />
Depth to carbonates: Greater than 35 inches<br />
Thickness <strong>of</strong> the solum: 35 to 55 inches<br />
Ap or A horizon:<br />
Hue—10YR, 2.5Y, or N<br />
Value—2 or 3<br />
Chroma—0 to 2<br />
Texture—clay loam, loam, or silt loam<br />
Btg horizon:<br />
Hue—10YR, 2.5Y, 5Y, or N<br />
Value—4 to 6<br />
Chroma—0 to 2<br />
Texture—loam, clay loam, sandy clay loam, sandy<br />
loam, silty clay loam, or silt loam<br />
2Cg or 2C horizon:<br />
Hue—10YR, 2.5Y, or 5Y<br />
Value—5 or 6<br />
Chroma—1 to 4<br />
Texture—sand or loamy sand<br />
529A—Selmass loam, 0 to 2 percent<br />
slopes<br />
Setting<br />
Landform: Outwash plains and stream terraces<br />
Position on the landform: Footslopes and toeslopes<br />
Slope range: 0 to 2 percent<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 unit,<br />
such as horizon depth and textures, is available in the<br />
“<strong>Soil</strong> Properties” section in <strong>Part</strong> II <strong>of</strong> this publication.<br />
Composition<br />
Selmass and similar soils: 85 percent<br />
Dissimilar soils: 15 percent<br />
Similar soils:<br />
• soils that contain less sand and more silt in the<br />
upper and middle parts <strong>of</strong> the pr<strong>of</strong>ile<br />
• soils that contain sandy outwash at a depth <strong>of</strong> less<br />
than 35 inches<br />
• soils that have a thinner subsurface layer<br />
• soils that contain less clay in the subsoil<br />
Dissimilar soils:<br />
• the well drained Dakota and somewhat poorly<br />
drained Lahoguess soils in the higher positions on the<br />
landform<br />
• the calcareous Hooppole soils in positions on the<br />
landform similar to those <strong>of</strong> the Selmass soil<br />
• the very poorly drained Houghton and Palms soils<br />
in depressions