A short steep slope formed gradually at the downslope margin of a field by deposition against a hedge, a stone wall or other similar barrier.
A sloping heap of loose rock fragments Iying at the foot of a cliff or steep slope.
A class at any categorical level of a taxonomic system of classification.
A device for measuring the negative pressure or tension, of water in soil in situ; a porous permeable ceramic cup connected through a tube to a manometer or vacuum gauge.
A nearly level usually narrow plain bordering a river, lake or sea. Rivers sometimes are bordered by a number of terraces at different levels. There are also manmade terraces.
An unconsolidated mineral substratum underlying organic soil material.
See texture (soil).
The relative proportions of the various soil separates in a soil as described by the classes of soil texture shown in Figure1. The names of textural soil classes may be modified by adding suitable adjectives when coarse fragments are present in substantial amounts; for example, "Gibraltar stony sandy loam," or "Saint-Jovite silt loam, stony phase." For other modifications see coarse fragments. The sand, loamy sand, and sandy loam are further subdivided on the basis of the proportions of the various sand separates present. The limits of the various classes and subclasses are:
Figure 1 Soil textural classes. Percentages of clay and sand in the main textural classes of soils; the remainder of each class is silt.
A method ot analyzing a soil sample for constituents, based on the differential rate of heating of the unknown and standard samples when a uniform source of heat is applied.
The rate of transfer of heat to or from a point in the soil.
Soils with properties that have been influenced primarily by high soil temperature as the dominant soil-formation tactor developed in subtropical and equatorial regions.
An organism that grows best at temperatures of 50°C or higher.
A sequence of related soils that differ, one from the other, primariiy as a result of temperature as a soil-formation factor.
The minimum moisture condition measured in terms of either moisture content or moisture stress, at which biological activity just becomes measurable.
Areas of nearly flat, barren mud periodically covered by tidal waters. Normally these materials have an excess of soluble salt. A miscellaneous land type.
A depth subdivision used in the classification of Organic soils. (1) surface tier: The upper 40 cm (16 inches) of peat. (2) middle tier: The tier just below the surface tier. It is 80 cm (32 inches) thick or extends to a lithic or hydric contact. The great group classification of Organic soils is usually based on this tier. (3) bottom tier: The tier below the middle tier. It is 40 cm (16 inches) thick or extends to a lithic or hydric contact. The subgroup classification of Organic soils is based partly on this tier.
A compact, relatively impervious and tenacious soil or subsoil which may or may not be plastic.
Pipe piaced at suitable depths and spacings in the soil or subsoil to provide water outlets from the soil. The pipe may be concrete, ceramic, fiber, plastic or any other suitable material.
Unstratified glacial drift deposited directly by the ice and consisting of clay, sand, gravel, and boulders intermingled in any proportion.
To plow and prepare for seeding; to seed or cultivate the soil.
The operation, practice, or art of tilling land to improve it for agricultural purposes.
The physical condition of soil as related to its ease of tillage, fitness as a seedbed, and impedance to seedling emergence and root penetration.
The physical features of a district or region, such as those represented on a map, taken collectively; especially the relief and contours of the land.
A photomap on which topographic or terrain-form lines are shown as on topographic quadrangles. See also photomap and planisaic.
toposequence toposequence A sequence of related soils that differ one from the other primarily because of topography as a soil-formation factor. See also clinosequence.
(1) The layer of soil moved in cultivation. See also surface soil. (2) The A horizon. (3) The Ah horizon. (4) Presumably fertile soil material used to topdress road-banks, gardens, and lawns.
See water / soil.
See water, soil.
See micronutrient.
See pressure or induced pan.
A soil with properties intermediate between those of two different soils and genetically related to them. See also intergrade / soil.
Having lost all or part of the upper soil horizon or horizons.
Volcanic ash usually more or less stratified and in various states of consolidation.
A level or undulating treeless plain characteristic of arctic regions.
Any soil in the tundra region.
(1) A unit in the natural system of soil classification; a subdivision of a soil series consisting of or describing soils that are alike in all characteristics including the texture of the A horizon. (2) In Europe the term is roughly equivalent to a great soil group.