Soil mottling definition

Soil mottling means a soil color pattern consisting of patches of different color or shades of color interspersed with the dominant soil color which results from prolonged saturation of the soil.
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Soil mottling means low chroma equal to or less than 2 and a value of 4 or more (Munsell-Color Chart.)
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Soil mottling means a soil color pattern consisting of patches of different color or shades of color interspersed with the dominant soil color which results from prolonged saturation of the soil. "Subdivision" means the division or redivision of a lot, tract or other parcel of land into two or more lots,tracts, parcels or other divisions of land including changes in existing lot lines. The enumerating of lots shall include as a lot that portion of the original tract or tracts remaining after other lots have been subdivided therefrom.(2 amended Dec. 14, 1994, P.L.1250, No.149) Compiler's Note: Section 502(c) of Act 18 of 1995, which created the Department of Conservation and Natural Resources and renamed the Department of Environmental Resources as the Department of Environmental Protection, provided that the Environmental Quality Board shall have the powers and duties currently vested in it, except as vested in the Department of Conservation and Natural Resources by Act 18 of 1995, which powers and duties include those set forth in section 2.Compiler's Note: Section 11 of Act 149 of 1994, which amended the definition of "individual residential spray irrigation system," provided that, on the effective date of the amendment, permits shall be issued under Act 537. Before the effective date of the amendment, permits shall be issued under the act of June 22, 1937 (P.L.1987, No.394), known as The Clean Streams Law. Section 12 of Act 149 provided that the amendment shall take effect in 550 days.
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Examples of Soil mottling in a sentence

  • Soil mottling (redoximorphic features)—a soil color pattern consisting of patches of different colors or shades of color interspersed with the dominant soil color which results from prolonged saturation of the soil.

  • Soil mottling (redoximorphic features), seasonal high water table elevation, apparent water table elevation, and apparent source of water (localized lenses, regional water table, or irrigation- induced water table).

  • Soil mottling, winter water studies, and other available resources are used to determine the highest seasonal water table.

  • Soil mottling (sometimes a banded mixture of gray iron depleted soil and brownish-red iron-rich soils) is one indicator of a periodically high-water table level.

  • Soil mottling observed during the site evaluation by a qualified professional may be used to determine the seasonal high groundwater level.

  • Soil mottling (redoximorphic features)—An obsolete term referring to a soil color pattern consisting of patches of different colors or shades of color interspersed with the dominant soil color which results from prolonged saturation of the soil.

  • Soil mottling (redoximorphic features) is not necessarily an indicator of the regional high water table, but is an indication of soil saturation.

  • Soil mottling is described in terms of abundance, size, contrast, boundary (with soil matrix), and colour (FAO 2006).

  • Soil mottling may indicate the presence of a sea- sonal high water table.

  • Soil mottling indicative of ESHGW was observed in test pits SH-TP-102, SH-TP-302, SH-TP-303, SH-TP-307, SH-TP-410 and SH-TP-503 through SH-TP-506 in the lowland sand and gravel terrace between approximately 4 feet to 7 feet bgs (between approximately El. 211 to 215.3 feet).


More Definitions of Soil mottling

Soil mottling means a soil color pattern consisting of
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Soil mottling means the presence of irregular areas of different colors in the soil observed during a soil evaluation. Such mottling indicates poor aeration and impeded drainage characteristics, usually from seasonal saturation of the soil. Anaerobic activity in the saturated zone triggers a reduction process, changing the color of minerals in the soil, and enabling a determination of the high ground water elevation when present.
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