Hydric soil means a soil that formed under conditions of saturation, flooding, or ponding long enough during the growing season to develop anaerobic conditions in the upper part.
Hydric soil means a soil that is saturated, flooded or ponded long enough during the growing season to develop anaerobic conditions in the upper part. The presence of hydric soil shall be determined following the methods described in the “Federal Manual for Identifying and Delineating Jurisdictional Wetlands.”
Hydric soil means a soil that is saturated, flooded, or ponded long enough during the growing season to develop anaerobic conditions in the upper part. The presence of hydric soil shall be determined following the methods described in the Washington State Wetland Identification and Delineation Manual (RCW 36.70A.175).
Examples of Hydric soil in a sentence
Landform: Escarpments Landform position (three-dimensional): Riser Typical profile H1 - 0 to 60 inches: variable Interpretive groups Land capability classification (irrigated): None specified Land capability classification (nonirrigated): 8 Hydric soil rating: No Data Source Information Soil Survey Area: San Diego County Area, California Survey Area Data: Version 15, May 27, 2020 Paragraph Description Submittal Requirement 5 A.
More Definitions of Hydric soil
Hydric soil means is a soil that formed under conditions of saturation, flooding, or ponding long enough during the growing season to develop anaerobic conditions in the upper part (Field Indicators of Hydric Soils in the United States, NTCHS, 1994).
Hydric soil means soil that, in its undrained condition, is saturated, flooded, or ponded long enough during a growing season to develop an anaerobic condition that supports the growth and regeneration of hydrophytic vegetation.
Hydric soil means a soil that in its undrained condition is saturated, flooded, or ponded long enough during the growing season to develop anaerobic conditions that favor the growth and regeneration of hydrophytic vegetation. These soils may be described in several places, including New Jersey's Official List of Hydric Soils, developed by the Natural Resources Conservation Service; the National Wetlands Inventory, entitled "The Wetlands of New Jersey", published in 1985 by the United States Fish and Wildlife Service; or in the 1989 Federal manual. Alluvial land, as mapped on soil surveys, or other soils exhibiting hydric characteristics identified through field investigation as described in Part III of the 1989 Federal manual may also be considered a hydric soil for the purposes of wetland classification. Also, wet phases of somewhat poorly drained soils not on New Jersey's Official List of Hydric Soils may be associated with a wetland and therefore for the purposes of this chapter shall be considered a hydric soil.
Hydric soil means a soil that is saturated, flooded or ponded long enough during the growing season to develop anaerobic conditions in the upper part of the soil column. The presence of hydric soil shall be determined following the methods described in the Corps of Engineers Wetlands Delineation Manual (1987, as amended), with “Washington Regional Guidance on the 1987
Hydric soil means a soil that is saturated, flooded or ponded long enough during the growing season to develop anaerobic conditions in the upper part. The presence of hydric soil shall be determined following the methods described in the U.S. Army Corps Wetlands Delineation Manual and Western Mountains, Valleys, and Coast regional supplement (2010).
Hydric soil means a soil that is saturated, flooded or ponded long enough during the growing season to develop anaerobic conditions in the upper part. The presence of hydric soil shall be determined following the methods described in the approved federal wetland delineation manual and applicable regional supplements.
Hydric soil means a soil that is saturated, flooded, or ponded long enough during the growing season to develop anaerobic conditions.