Aggregate lab data for the GRIGSBY soil series. This aggregation is based on all pedons with a current taxon name of GRIGSBY, and applied along 1-cm thick depth slices. Solid lines are the slice-wise median, bounded on either side by the interval defined by the slice-wise 5th and 95th percentiles. The median is the value that splits the data in half. Five percent of the data are less than the 5th percentile, and five percent of the data are greater than the 95th percentile. Values along the right hand side y-axis describe the proportion of pedon data that contribute to aggregate values at this depth. For example, a value of "90%" at 25cm means that 90% of the pedons correlated to GRIGSBY were used in the calculation. Source: KSSL snapshot Methods used to assemble the KSSL snapshot used by SoilWeb / SDE
.Pedons used in the lab summary:
MLRA | Lab ID | Pedon ID | Taxonname | CI | NSSL / NASIS Reports | Link To SoilWeb GMap |
---|---|---|---|---|---|---|
125 | 85KY-013-002 | 85KY-013-002 | Grigsby | 4 | Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties | 36.7120247,-83.783226 |
n/a | 83P0897 | 1983KY099007 | Grigsby | 5 | Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties | n/a |
n/a | 77KY-193-005 | 77KY-193-005 | Grigsby | 4 | Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties | n/a |
n/a | 83KY-099-007 | 83KY-099-007 | Grigsby | 4 | Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties | n/a |
Monthly water balance estimated using a leaky-bucket style model for the GRIGSBY soil series. Monthly precipitation (PPT) and potential evapotranspiration (PET) have been estimated from the 50th percentile of gridded values (PRISM 1981-2010) overlapping with the extent of SSURGO map units containing each series as a major component. Monthly PET values were estimated using the method of Thornthwaite (1948). These (and other) climatic parameters are calculated with each SSURGO refresh and provided by the fetchOSD function of the soilDB package. Representative water storage values (“AWC” in the figures) were derived from SSURGO by taking the 50th percentile of profile-total water storage (sum[awc_r * horizon thickness]) for each soil series. Note that this representation of “water storage” is based on the average ability of most plants to extract soil water between 15 bar (“permanent wilting point”) and 1/3 bar (“field capacity”) matric potential. Soil moisture state can be roughly interpreted as “dry” when storage is depleted, “moist” when storage is between 0mm and AWC, and “wet” when there is a surplus. Clearly there are a lot of assumptions baked into this kind of monthly water balance. This is still a work in progress.
Siblings are those soil series that occur together in map units, in this case with the GRIGSBY series. Sketches are arranged according to their subgroup-level taxonomic structure. Source: SSURGO snapshot
, parsed OSD records and snapshot of SC database .Select annual climate data summaries for the GRIGSBY series and siblings. Series are sorted according to hierarchical clustering of median values. Source: SSURGO map unit geometry and 1981-2010, 800m PRISM data
.Geomorphic description summaries for the GRIGSBY series and siblings. Series are sorted according to hierarchical clustering of proportions and relative hydrologic position within an idealized landform (e.g. top to bottom). Most soil series (SSURGO components) are associated with a hillslope position and one or more landform-specific positions: hills, mountain slopes, terraces, and/or flats. Proportions can be interpreted as an aggregate representation of geomorphic membership. The values printed to the left (number of component records) and right (Shannon entropy) of stacked bars can be used to judge the reliability of trends. Small Shannon entropy values suggest relatively consistent geomorphic association, while larger values suggest lack thereof. Source: SSURGO component records .
Soil series competing with GRIGSBY share the same family level classification in Soil Taxonomy. Source: parsed OSD records
and snapshot of the SC database .Select annual climate data summaries for the GRIGSBY series and competing. Series are sorted according to hierarchical clustering of median values. Source: SSURGO map unit geometry and 1981-2010, 800m PRISM data
.Geomorphic description summaries for the GRIGSBY series and competing. Series are sorted according to hierarchical clustering of proportions and relative hydrologic position within an idealized landform (e.g. top to bottom). Proportions can be interpreted as an aggregate representation of geomorphic membership. Most soil series (SSURGO components) are associated with a hillslope position and one or more landform-specific positions: hills, mountain slopes, terraces, and/or flats. The values printed to the left (number of component records) and right (Shannon entropy) of stacked bars can be used to judge the reliability of trends. Shannon entropy values close to 0 represent soil series with relatively consistent geomorphic association, while values close to 1 suggest lack thereof. Source: SSURGO component records .
Click a link below to display the diagram. Note that these diagrams may be from multiple survey areas.
Typical pattern of soils and their relationship to geology and topography in the Shelocta-Highsplint-Cloverlick-Kimper general soil map unit in Knott County (Soil Survey of Knott and Letcher Counties, Kentucky; 2004).
Typical pattern of soils and their relationship to geology and topography in the Handshoe-Cloverlick-Fedscreek-Marrowbone general soil map unit in Knott County (Soil Survey of Knott and Letcher Counties, Kentucky; 2004).
Typical pattern of soils and their relationship to geology and topography in the Kimper-Cloverlick-Renox-Highsplint general soil map unit in Letcher County (Soil Survey of Knott and Letcher Counties, Kentucky; 2004).
Typical pattern of soils and their relationship to geology and topography in the Alticrest-Varilla-Shelocta-Jefferson general soil map unit and the Cloverlick-Highsplint-Guyandotte-Shelocta general soil map unit in Letcher County (Soil Survey of Knott and Letcher Counties, Kentucky; 2004).
Typical pattern of soils and their relationship to geology and topography in the Shelocta-Cloverlick-Fedscreek-Dekalb general soil map unit in Letcher County (Soil Survey of Knott and Letcher Counties, Kentucky; 2004).
Typical pattern of soils and their relationship to geology and topography in the Shelocta-Cloverlick-Fedscreek-Kimper general soil map unit in Knott County (Soil Survey of Knott and Letcher Counties, Kentucky; 2004).
Typical pattern of soils, parent material, and topography in the Hazleton-Shelocta-Fiveblock and Grigsby-Shelocta-Orrville general soil map units. The Hazleton-Shelocta-Fiveblock general soil map unit is on the mountains and in the surface mined areas, and the Grigsby-Shelocta-Orrville general soil map unit is in the valleys (Soil Survey of Lawrence and Martin Counties, Kentucky; 2005).
Typical pattern of soils, parent material, and topograhy in the Upshur-Vandalia-Rarden general soil map unit. This map unit is on the mountains (Soil Survey of Lawrence and Martin Counties, Kentucky; 2005).
Typical pattern of the soils in the Huntington-Elk-Nelse-Grigsby and Holston-Monongahela-Waynesboro general soil map units and the underlying material (Soil Survey of Cumberland County, Kentucky; 1998).
Typical pattern of soils and their relationship to geology and topography in the Grigsby-Nolin-Elk-Morehead general soil map unit in Estill County (Soil Survey of Estill and Lee Counties, Kentucky; 2007).
Typical pattern of soils and their relationship to geology and topography in the Shelocta-Bledsoe-Gilpin general soil map unit in Estill County (Soil Survey of Estill and Lee Counties, Kentucky; 2007).
Typical pattern of soils and their relationship to geology and topography in the Shelocta-Gilpin general soil map unit in Lee County (Soil Survey of Estill and Lee Counties, Kentucky; 2007).
Typical pattern of soils and their relationship to geology and topography in the Shelocta-Helechawa-Gilpin-Hazleton general soil map unit in Morgan County (Soil Survey of Magoffin and Morgan Counties, Kentucky; 2002).
Typical pattern of soils and their relationship to geology and topography in the Shelocta-Pope-Helechawa-Gilpin general soil map unit in Magoffin County (Soil Survey of Magoffin and Morgan Counties, Kentucky; 2002).
Typical pattern of soils and their relationship to geology and topography in the Kimper-Shelocta-Fedscreek-Gilpin general soil map unit in Magoffin County (Soil Survey of Magoffin and Morgan Counties, Kentucky; 2002).
Typical pattern of soils and their relationship to geology and topography in the Shelocta-Gilpin-Latham-Marrowbone general soil map unit in Morgan County (Soil Survey of Magoffin and Morgan Counties, Kentucky; 2002).
Typical pattern of soils and their relationship to geology and topography in the Shelocta-Gilpin-Allegheny-Grigsby general soil map unit in Morgan County (Soil Survey of Magoffin and Morgan Counties, Kentucky; 2002).
Relationship of soils to topography and underlying material in the Newark-Nolin-Melvin association (Soil Survey of Butler and Edmonson Counties, Kentucky).
Pattern of soils, topography, and underlying material in the Rigley-Lily-Rock outcrop map unit (Soil Survey of Carter County, Kentucky; April 1983).
Pattern of soils and parent material in the Waynesboro-Nolin-Grigsby general soil map unit (Soil Survey of Clinton County, Kentucky; May 1994).
Typical pattern of soils and underlying material in the Nolichucky-Canmer general soil map unit (Soil Survey of Hart County, Kentucky; May 1993).
Typical pattern of soils and underlying material in the Riney-Sonora-Canmer general soil map unit (Soil Survey of Hart County, Kentucky; May 1993).
Typical pattern of soils and parent material in the Shelocta-Bledsoe-Gilpin map unit (Soil Survey of Jackson and Owsley Counties, Kentucky; April 1989).
Along the major tributaries in Pike County, the soils on the mountains are in the Marrowbone-Fedscreek-Kimper-Dekalb general soil map unit and those in the valleys are in the Yeager-Grigsby-Potomac-Hayter map unit (Soil Survey of Pike County, Kentucky; June 1990).
Along Elkhorn Creek and Pine Mountain, the upper faulted mountains are in the Kimper-Sharondale-Berks-Shelocta general soil map unit, the lower mountains are in the Marrowbone-Fedscreek-Kimper-Dekalb map unit, and the valley is in the Yeager-Grigsby-Potomac-Hayter map unit (Soil Survey of Pike County, Kentucky; June 1990).
Typical pattern of soils and parent material in the Jessietown-Muse-Rohan general soil map unit (Soil Survey of Powell and Wolfe Counties, Kentucky; September 1993).
Typical pattern of soils and parent material in the Grigsby-Allegheny-Knowlton general soil map unit (Soil Survey of Powell and Wolfe Counties, Kentucky; September 1993).
Diagram of a sequence of landform positions in the Appalachian Plateau area of Russell County. The soils named on the land surface are shown in their natural relationship to each other and in their relationship to landform position (Soil Survey of Russell County, Virginia; 2007).
Diagram of a sequence of landform positions along the Clinch River in areas underlain with limestone and shale in Russell County. The soils named on the land surface are shown in their natural relationship to each other and in their relationship to landform position (Soil Survey of Russell County, Virginia; 2007).
Diagram of a sequence of landform positions in the Appalachian Plateau area of Russell County. The soils named on the land surface are shown in their natural relationship to each other and in their relationship to landform position (Soil Survey of Russell County, Virginia; 2007).
Diagram of a sequence of landform positions along the Clinch River in areas underlain with limestone and shale in Russell County. The soils named on the land surface are shown in their natural relationship to each other and in their relationship to landform position (Soil Survey of Russell County, Virginia; 2007).
Typical pattern of soils and parent material in an area of the Highsplint-Matewan-Cloverlick general soil map unit (Soil Survey of Lincoln County, West Virginia; 2007).
Map units containing GRIGSBY as a major component. Limited to 250 records.
Approximate geographic distribution of the GRIGSBY soil series. 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. Source: generalization of SSURGO geometry .