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Soil Survey of Sweet Grass County Area, Montana - Soil Data Mart

Soil Survey of Sweet Grass County Area, Montana - Soil Data Mart

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<strong>Sweet</strong> <strong>Grass</strong> <strong>County</strong> <strong>Area</strong>, <strong>Montana</strong>—Part I 337<br />

by small earth ridges called border dikes, or<br />

borders.<br />

Controlled flooding.—Water is released at<br />

intervals from closely spaced field ditches and<br />

distributed uniformly over the field.<br />

Corrugation.—Water is applied to small, closely<br />

spaced furrows or ditches in fields <strong>of</strong> closegrowing<br />

crops or in orchards so that it flows in<br />

only one direction.<br />

Drip (or trickle).—Water is applied slowly and<br />

under low pressure to the surface <strong>of</strong> the soil or<br />

into the soil through such applicators as emitters,<br />

porous tubing, or perforated pipe.<br />

Furrow.—Water is applied in small ditches made<br />

by cultivation implements. Furrows are used for<br />

tree and row crops.<br />

Sprinkler.—Water is sprayed over the soil surface<br />

through pipes or nozzles from a pressure system.<br />

Subirrigation.—Water is applied in open ditches<br />

or tile lines until the water table is raised enough<br />

to wet the soil.<br />

Wild flooding.—Water, released at high points, is<br />

allowed to flow onto an area without controlled<br />

distribution.<br />

K sat<br />

. Saturated hydraulic conductivity. (See<br />

Permeability.)<br />

Kame. A moundlike hill <strong>of</strong> glacial drift, composed<br />

chiefly <strong>of</strong> stratified sand and gravel.<br />

Kame terrace. A terracelike ridge consisting <strong>of</strong><br />

stratified sand and gravel that were deposited by<br />

a meltwater stream flowing between a melting<br />

glacier and a higher valley wall or lateral moraine<br />

and that remained after the disappearance <strong>of</strong> the<br />

ice. It is commonly pitted with kettles and has an<br />

irregular ice-contact slope.<br />

Lacustrine deposit. Material deposited in lake water<br />

and exposed when the water level is lowered or<br />

the elevation <strong>of</strong> the land is raised.<br />

Lake plain. A surface marking the floor <strong>of</strong> an extinct<br />

lake, filled in by well-sorted, stratified sediments.<br />

Landslide. The rapid downhill movement <strong>of</strong> a mass<br />

<strong>of</strong> soil and loose rock, generally when wet or<br />

saturated. The speed and distance <strong>of</strong> movement,<br />

as well as the amount <strong>of</strong> soil and rock material,<br />

vary greatly.<br />

Large stones (in tables). Rock fragments 3 inches<br />

(7.6 centimeters) or more across. Large stones<br />

adversely affect the specified use <strong>of</strong> the soil.<br />

Lateral moraine. A ridgelike moraine carried on and<br />

deposited at the side margin <strong>of</strong> a valley glacier. It<br />

is composed chiefly <strong>of</strong> rock fragments derived<br />

from the valley walls by glacial abrasion and<br />

plucking or by mass wasting.<br />

Leaching. The removal <strong>of</strong> soluble material from soil<br />

or other material by percolating water.<br />

Linear extensibility. Refers to the change in length<br />

<strong>of</strong> an unconfined clod as moisture content is<br />

decreased from a moist to a dry state. Linear<br />

extensibility is used to determine the shrink-swell<br />

potential <strong>of</strong> soils. It is an expression <strong>of</strong> the volume<br />

change between the water content <strong>of</strong> the clod at<br />

1<br />

/3- or 1 /10-bar tension (33kPa or 10kPa tension)<br />

and oven dryness. Volume change is influenced<br />

by the amount and type <strong>of</strong> clay minerals in the<br />

soil. The volume change is the percent change for<br />

the whole soil. If it is expressed as a fraction, the<br />

resulting value is COLE, coefficient <strong>of</strong> linear<br />

extensibility.<br />

Liquid limit. The moisture content at which the soil<br />

passes from a plastic to a liquid state.<br />

Loam. <strong>Soil</strong> material that is 7 to 27 percent clay<br />

particles, 28 to 50 percent silt particles, and less<br />

than 52 percent sand particles.<br />

Loamy soil. Coarse sandy loam, sandy loam, fine<br />

sandy loam, very fine sandy loam, loam, silt<br />

loam, silt, clay loam, sandy clay loam, or silty clay<br />

loam.<br />

Loess. Fine grained material, dominantly <strong>of</strong> silt-sized<br />

particles, deposited by wind.<br />

Low-residue crops. Such crops as corn used for<br />

silage, peas, beans, and potatoes. Residue from<br />

these crops is not adequate to control erosion<br />

until the next crop in the rotation is established.<br />

These crops return little organic matter to the soil.<br />

Low strength. The soil is not strong enough to<br />

support loads.<br />

Marl. An earthy, unconsolidated deposit consisting<br />

chiefly <strong>of</strong> calcium carbonate mixed with clay in<br />

approximately equal amounts.<br />

Masses. Concentrations <strong>of</strong> substances in the soil<br />

matrix that do not have a clearly defined<br />

boundary with the surrounding soil material and<br />

cannot be removed as a discrete unit. Common<br />

compounds making up masses are calcium<br />

carbonate, gypsum or other soluble salts, iron<br />

oxide, and manganese oxide. Masses consisting<br />

<strong>of</strong> iron oxide or manganese oxide generally are<br />

considered a type <strong>of</strong> redox concentration.<br />

Mean annual increment (MAI). The average annual<br />

increase in volume <strong>of</strong> a tree during its entire life.<br />

Mechanical treatment. Use <strong>of</strong> mechanical<br />

equipment for seeding, brush management, and<br />

other management practices.<br />

Medium textured soil. Very fine sandy loam, loam,<br />

silt loam, or silt.

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