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 61<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 />
Harvard and similar soils: 85 percent<br />
Dissimilar soils: 15 percent<br />
Similar soils:<br />
• soils that have a lighter colored surface layer<br />
• soils that have a thicker surface layer<br />
• soils that contain loamy outwash at a depth <strong>of</strong> more<br />
than 40 inches<br />
• soils that contain sandy and gravelly deposits in the<br />
lower part <strong>of</strong> the pr<strong>of</strong>ile<br />
Dissimilar soils:<br />
• the somewhat poorly drained Brenton and Millbrook<br />
soils in the lower positions on the landform<br />
• the poorly drained Pella soils in drainageways<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 />
344B—Harvard silt loam, 2 to 5 percent<br />
slopes<br />
Setting<br />
Landform: Outwash plains and stream terraces<br />
Position on the landform: Summits, shoulders, and<br />
backslopes<br />
Slope range: 2 to 5 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<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 />
Harvard and similar soils: 85 percent<br />
Dissimilar soils: 15 percent<br />
Similar soils:<br />
• soils that have a lighter colored surface layer<br />
• soils that have a thicker surface layer<br />
• soils that contain loamy outwash at a depth <strong>of</strong> more<br />
than 40 inches<br />
• soils that contain sandy and gravelly deposits in the<br />
lower part <strong>of</strong> the pr<strong>of</strong>ile<br />
Dissimilar soils:<br />
• the somewhat poorly drained Brenton and Millbrook<br />
soils in the lower positions on the landform<br />
• the poorly drained Pella soils in drainageways<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 />
Herbert Series<br />
Drainage class: Somewhat poorly drained<br />
Permeability: Moderate in the upper part and<br />
moderately slow in the lower part<br />
Landform: Moraines and till plains<br />
Parent material: Silty material and the underlying<br />
loamy till<br />
Slope range: 0 to 2 percent<br />
Taxonomic classification: Fine-silty, mixed, mesic<br />
Udollic Epiaqualfs<br />
Typical Pedon for MLRA 95B<br />
Typical pedon <strong>of</strong> Herbert silt loam, 335 feet south and<br />
306 feet east <strong>of</strong> the northwest corner <strong>of</strong> sec. 14, T. 42<br />
N., R. 4 E.<br />
Ap—0 to 8 inches; very dark brown (10YR 2/2) silt<br />
loam, dark grayish brown (10YR 4/2) dry;<br />
moderate very fine granular structure; friable;<br />
many very fine and fine roots; slightly acid; abrupt<br />
smooth boundary.<br />
E—8 to 12 inches; dark grayish brown (10YR 4/2) silt<br />
loam; weak medium and thick platy structure<br />
parting to moderate fine granular; friable; many<br />
very fine roots; few fine faint brown (10YR 5/3)<br />
masses <strong>of</strong> iron accumulation in the matrix; slightly<br />
acid; clear smooth boundary.<br />
Bt1—12 to 16 inches; brown (10YR 4/3) silty clay<br />
loam; moderate very fine subangular blocky<br />
structure; firm; many very fine roots; common<br />
distinct discontinuous dark grayish brown (10YR<br />
4/2) clay films on faces <strong>of</strong> peds; few fine faint<br />
brown (10YR 5/3) masses <strong>of</strong> iron accumulation in<br />
the matrix; few fine distinct grayish brown (2.5Y