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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

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