HOLDREGE SOIL SERIES DESCRIPTION

Uly-Penden complex, 6 to 20 percent slopes. Component association is a function of how frequently components co-occur, weighted by component percentage. Harney-Uly complex, 1 to 3 percent slopes. NE Custer County – July Typical pattern of soils and relationship of soils to topography and parent material in three associations: This summary should generate structures that are related to soil-landscape concepts that were used to construct map units containing the ULY series. Uly and Coly silt loams, 11 to 30 percent slopes. Uly silt loam, 6 to 11 percent slopes, eroded. Soil type subdivides the series on the basis of surface texture, while phases are determined by slope, erosion, or salt content.

Coly-Uly-Hobbs silt loams, 3 to 60 percent slopes. Soil series sharing subgroup-level classification with ULY, arranged according to family differentiae. Not all prohibited bases apply to all programs. Note that these diagrams may be from multiple survey areas. Coly-Uly silt loams, 3 to 11 percent slopes, eroded. Uly-Harney complex, 1 to 3 percent slopes, eroded. Uly and Coly silt loams, 11 to 30 percent slopes.

Soil Data Explorer – ULY

Typical pattern of soils and relationship to topography and parent material in the Hord-Hobbs association 3 and the Holder-Geary association 8 Soil Survey of Hamilton County, Nebraska; March Uly-Hobbs silt loams, 0 to 30 percent slopes.

Dark lines connect vertices to the queried soil series, grey lines connect other vertices. Coly-Uly silt loams, 6 to 11 percent slopes, eroded. Persons with disabilities who require alternative means for communication of program information Braille, large print, audiotape, etc.

Holdrege Soil Profile Surface layer: Coly and Uly silt loams, 11 to 30 percent slopes. Uly-Holdrege silt loams, 6 to 12 percent slopes.

Holdrege (soil) – Wikipedia

Uly-Holdrege silt loams, 7 to 11 percent slopes, eroded. A soil series, type and phase name might be, for example: Soil type subdivides the series on the basis of surface texture, while phases are determined by slope, erosion, or salt content.

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Component association is a function of how frequently components co-occur, weighted by component percentage. Examples of soil series are Holdrege, Nora, Sharpsburg and Valentine. The Holdrege series was established in Phelps County, Nebraska, in Holdrege soils are extensive, making up about 1. Uly silt loam, 3 to 11 percent slopes. Nuckolls, Uly, and Canlon soils, 11 to 30 percent slopes.

Department of Agriculture USDA prohibits discrimination in descripption its programs and activities on the basis of race, color, national descrjption, age, holfrege, and where applicable, sex, marital status, familial status, parental status, religion, sexual orientation, genetic information, political beliefs, reprisal, or because all or a part of an individual’s income is derived from any public assistance program.

Uly-Hobbs silt loams, 0 to 30 percent slopes, eroded. Coly-Uly-Hobbs silt loams, 3 to 60 percent slopes.

Holdrege (soil)

Both views are approximations of the multi-dimensional relationship between components. Penden-Uly complex, 7 to 20 percent slopes. Holdrege-Uly silt loams, 3 to 7 percent slopes, eroded. Typical pattern of soils and relationship of soils to topography and parent material in three associations: Click a link below to display the diagram. Holdrege and Uly soils, 3 to 7 percent slopes, seriss. Uly, eroded-Hersh complex, 11 to 60 percent slopes.

Harney-Uly silt loams, 0 to 1 percent slopes. Aggregate lab data for the ULY soil series.

Five percent of the data are less than the 5th percentile, and five percent of the data are greater than the 95th percentile. Uly-Corinth complex, 1 to 3 percent slopes. The average annual precipitation is about 22 inches, and the annual average snowfall is about 22 inches. KSSL snapshot as of September Many areas are irrigated. Coly-Uly silt loams, 11 to 30 percent slopes. Uly-Coly silt loams, 11 to 17 percent slopes, eroded.

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Uly-Coly silt loams, 11 to 30 percent slopes. Sharpsburg silty clay loam, 5 to 9 percent slope, eroded.

Uly-Roxbury silt loams, 0 to 30 percent slopes. Typical pattern of soils in the Uly-Coly association and relationship of soils to topography and parent material Soil Survey of Custer County, Nebraska; July Any opinions, findings, conclusions or recommendations expressed in this publication are those of the author s and do not necessarily reflect the views of the USDA or NSF. The median is the value that splits the data in half. Uly-Harney complex, 1 to 3 percent slopes, eroded.

Typical pattern of soils in the Holdrege-Hall-Hord association and relationship of soils to topography and parent material Soil Survey of Custer County, Nebraska; July Values along the right hand side y-axis describe the proportion of pedon data that contribute to aggregate values at this depth.

Uly-Coly silt loams, 6 to 11 percent slopes, eroded. Copyright Plant and Soil Sciences eLibrary To learn more about how this distribution was mapped, or to compare this soil series extent to others, use the Series Extent Explorer SEE application. Coly-Uly silt loams, 3 to descriprion percent slopes, eroded.

Uly, eroded-Hobbs silt loams, 2 to 40 percent slopes.

Uly and Holdrege silt loams, 6 to 11 percent slopes.

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