Soil Survey of Karnes County, Texas - Soil Data Mart - US ...
Soil Survey of Karnes County, Texas - Soil Data Mart - US ...
Soil Survey of Karnes County, Texas - Soil Data Mart - US ...
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<strong>Karnes</strong> <strong>County</strong>, <strong>Texas</strong> 151<br />
gypsum or other soluble salts, iron oxide, and<br />
manganese oxide. Masses consisting <strong>of</strong> iron oxide<br />
or manganese oxide generally are considered a<br />
type <strong>of</strong> redoximorphic concentration.<br />
Medium textured soil. Very fine sandy loam, loam,<br />
silt loam, or silt.<br />
Mineral soil. <strong>Soil</strong> that is mainly mineral material and<br />
low in organic material. Its bulk density is more<br />
than that <strong>of</strong> organic soil.<br />
Minimum tillage. Only the tillage essential to crop<br />
production and prevention <strong>of</strong> soil damage.<br />
Miscellaneous area. An area that has little or no<br />
natural soil and supports little or no vegetation.<br />
Moderately coarse textured soil. Coarse sandy<br />
loam, sandy loam, or fine sandy loam.<br />
Moderately fine textured soil. Clay loam, sandy clay<br />
loam, or silty clay loam.<br />
Mollic epipedon. A thick, dark, humus-rich surface<br />
horizon (or horizons) that has high base saturation<br />
and pedogenic soil structure. It may include the<br />
upper part <strong>of</strong> the subsoil.<br />
Morphology, soil. The physical makeup <strong>of</strong> the soil,<br />
including the texture, structure, porosity,<br />
consistence, color, and other physical, mineral,<br />
and biological properties <strong>of</strong> the various horizons,<br />
and the thickness and arrangement <strong>of</strong> those<br />
horizons in the soil pr<strong>of</strong>ile.<br />
Mottling, soil. Irregular spots <strong>of</strong> different colors that<br />
vary in number and size. Descriptive terms are<br />
as follows: abundance—few, common, and<br />
many; size—fine, medium, and coarse; and<br />
contrast—faint, distinct, and prominent. The<br />
size measurements are <strong>of</strong> the diameter along<br />
the greatest dimension. Fine indicates less<br />
than 5 millimeters (about 0.2 inch); medium,<br />
from 5 to 15 millimeters (about 0.2 to 0.6 inch);<br />
and coarse, more than 15 millimeters (about<br />
0.6 inch).<br />
Munsell notation. A designation <strong>of</strong> color by degrees<br />
<strong>of</strong> three simple variables—hue, value, and<br />
chroma. For example, a notation <strong>of</strong> 10YR 6/4 is a<br />
color with hue <strong>of</strong> 10YR, value <strong>of</strong> 6, and chroma<br />
<strong>of</strong> 4.<br />
Neutral soil. A soil having a pH value <strong>of</strong> 6.6 to 7.3.<br />
(See Reaction, soil.)<br />
Nutrient, plant. Any element taken in by a plant<br />
essential to its growth. Plant nutrients are mainly<br />
nitrogen, phosphorus, potassium, calcium,<br />
magnesium, sulfur, iron, manganese, copper,<br />
boron, and zinc obtained from the soil and carbon,<br />
hydrogen, and oxygen obtained from the air and<br />
water.<br />
Organic matter. Plant and animal residue in the soil in<br />
various stages <strong>of</strong> decomposition. The content <strong>of</strong><br />
organic matter in the surface layer is described as<br />
follows:<br />
Very low ................................... less than 0.5 percent<br />
Low ................................................ 0.5 to 1.0 percent<br />
Moderately low .............................. 1.0 to 2.0 percent<br />
Moderate ....................................... 2.0 to 4.0 percent<br />
High ............................................... 4.0 to 8.0 percent<br />
Very high ............................... more than 8.0 percent<br />
Pan. A compact, dense layer in a soil that impedes the<br />
movement <strong>of</strong> water and the growth <strong>of</strong> roots. For<br />
example, hardpan, fragipan, claypan, plowpan,<br />
and traffic pan.<br />
Parent material. The unconsolidated organic and<br />
mineral material in which soil forms.<br />
Ped. An individual natural soil aggregate, such as a<br />
granule, a prism, or a block.<br />
Pedon. The smallest volume that can be called “a soil.”<br />
A pedon is three dimensional and large enough to<br />
permit study <strong>of</strong> all horizons. Its area ranges from<br />
about 10 to 100 square feet (1 square meter to 10<br />
square meters), depending on the variability <strong>of</strong> the<br />
soil.<br />
Percolation. The downward movement <strong>of</strong> water<br />
through the soil.<br />
Percs slowly (in tables). The slow movement <strong>of</strong> water<br />
through the soil adversely affects the specified<br />
use.<br />
Permeability. The quality <strong>of</strong> the soil that enables<br />
water or air to move downward through the<br />
pr<strong>of</strong>ile. The rate at which a saturated soil<br />
transmits water is accepted as a measure <strong>of</strong><br />
this quality. In soil physics, the rate is referred<br />
to as “saturated hydraulic conductivity,” which<br />
is defined in the “<strong>Soil</strong> <strong>Survey</strong> Manual.” In line<br />
with conventional usage in the engineering<br />
pr<strong>of</strong>ession and with traditional usage in<br />
published soil surveys, this rate <strong>of</strong> flow<br />
continues to be expressed as “permeability.”<br />
Terms describing permeability, measured in<br />
inches per hour, are as follows:<br />
Extremely slow ................................. 0.0 to 0.01 inch<br />
Very slow ........................................ 0.01 to 0.06 inch<br />
Slow .................................................. 0.06 to 0.2 inch<br />
Moderately slow ................................. 0.2 to 0.6 inch<br />
Moderate ................................ 0.6 inch to 2.0 inches<br />
Moderately rapid ............................ 2.0 to 6.0 inches<br />
Rapid ............................................... 6.0 to 20 inches<br />
Very rapid ................................. more than 20 inches<br />
Phase, soil. A subdivision <strong>of</strong> a soil series based on<br />
features that affect its use and management, such<br />
as slope, stoniness, and flooding.<br />
pH value. A numerical designation <strong>of</strong> acidity and<br />
alkalinity in soil. (See Reaction, soil.)