Official Series Description


Lab Data Summary

Aggregate lab data for the ALBION soil series. This aggregation is based on all pedons with a current taxon name of ALBION, 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 ALBION were used in the calculation. Source: KSSL snapshot . Methods used to assemble the KSSL snapshot used by SoilWeb / SDE

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Pedons used in the lab summary:

MLRALab IDPedon IDTaxonnameCINSSL / NASIS ReportsLink To SoilWeb GMap
7940A182558KS155002Albion6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties37.8194427,-98.0808334
7906N0255S05KS155002Albion7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties37.8681946,-98.2237854
80A88P046088OK003001Albion6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties36.663887,-98.2494431

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the ALBION 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.

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Sibling Summary

Siblings are those soil series that occur together in map units, in this case with the ALBION series. Sketches are arranged according to their subgroup-level taxonomic structure. Source: SSURGO snapshot , parsed OSD records and snapshot of SC database .

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Select annual climate data summaries for the ALBION series and siblings. Series are sorted according to hierarchical clustering of median values. Source: SSURGO map unit geometry and 1981-2010, 800m PRISM data .

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Geomorphic description summaries for the ALBION 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 .

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There are insufficient data to create the 3D mountains figure.

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There are insufficient data to create the 3D flats position figure.

Competing Series

Soil series competing with ALBION share the same family level classification in Soil Taxonomy. Source: parsed OSD records and snapshot of the SC database .

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Select annual climate data summaries for the ALBION series and competing. Series are sorted according to hierarchical clustering of median values. Source: SSURGO map unit geometry and 1981-2010, 800m PRISM data .

There are insufficient data to create the annual climate figure.

Geomorphic description summaries for the ALBION 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 .

There are insufficient data to create the 2D hillslope position figure.

There are insufficient data to create the 3D hills figure.

There are insufficient data to create the 3D mountains figure.

There are insufficient data to create the 3D terrace figure.

There are insufficient data to create the 3D flats position figure.

Soil series sharing subgroup-level classification with ALBION, arranged according to family differentiae. Hovering over a series name will print full classification and a small sketch from the OSD. Source: snapshot of SC database .

Block Diagrams

Click a link below to display the diagram. Note that these diagrams may be from multiple survey areas.

  1. KS-2010-09-03-03 | Reno County - 2002

    Typical pattern of soils and parent material in the Shellabarger-Albion-Nalim association (Soil Survey of Reno County, Kansas; 2002).

  2. KS-2012-01-20-25 | Clark County - December 1982

    Typical pattern of soils in the Albion-Shellabarger association (Soil Survey of Clark County, Kansas; 1982).

  3. KS-2012-01-20-36 | Comanche County - June 1989

    Typical pattern of soils and parent material in the Albion-Shellabarger association (Soil Survey of Comanche County, Kansas; 1989).

  4. KS-2012-01-25-15 | Pratt County - September 1968

    Major soils of associations 8 and 9 and the positions they normally occupy on the landscape (Soil Survey of Pratt County, Kansas; 1968).

Map Units

Map units containing ALBION as a major component. Limited to 250 records.

Map Unit Name Symbol Map Unit Area (ac) Map Unit Key National Map Unit Symbol Soil Survey Area Publication Date Map Scale
Albion and Shellabarger sandy loams, 6 to 15 percent slopes585010278513824482xlhqks00719731:24000
Albion-Shellabarger sandy loams, 3 to 15 percent slopes58592275313824541hdk9ks00719731:24000
Albion-Shellabarger sandy loams, 1 to 3 percent slopes5858142313824532tt5mks00719731:24000
Albion-Kaski complex, 0 to 15 percent slopes585710313824522tt79ks00719731:24000
Albion sandy loam, 1 to 3 percent slopes58539413824492wtx2ks00719731:24000
Albion sandy loam, 3 to 6 percent slopes, eroded58551813824512wtx4ks00719731:24000
Albion sandy loam, 3 to 6 percent slopes58541513824502wtx3ks00719731:24000
Albion-Shellabarger sandy loams, 3 to 15 percent slopes58591526813816961hcrvks02519801:24000
Albion-Shellabarger sandy loams, 3 to 15 percent slopes58594953513812371hc91ks03319871:24000
Albion sandy loam, 1 to 3 percent slopes58531558113812361hc90ks03319871:24000
Shellabarger and Albion soils, 7 to 15 percent slopes5946628613827342tt5nks07719651:24000
Albion and Shellabarger sandy loams, 6 to 15 percent slopes5850316513826652xlhqks07719651:24000
Albion sandy loam, 6 to 15 percent slopes585648913826662wtx5ks07719651:24000
Albion sandy loam, 6 to 15 percent slopes58565821214447722wtx5ks09519771:24000
Albion sandy loam, 1 to 3 percent slopes58531482714447692wtx2ks09519771:24000
Albion sandy loam, 3 to 6 percent slopes58541128014447702wtx3ks09519771:24000
Albion sandy loam, 0 to 1 percent slopes5852110914447682wtx1ks09519771:24000
Albion and Shellabarger sandy loams, 6 to 15 percent slopes5850107514447672xlhqks09519771:24000
Albion sandy loam, 3 to 6 percent slopes, eroded585567114447712wtx4ks09519771:24000
Albion-Shellabarger sandy loams, 1 to 3 percent slopes585826314447732tt5mks09519771:24000
Shellabarger, eroded, and Albion soils, 6 to 15 percent slopes595919914448152tt5tks09519771:24000
Albion-Shellabarger sandy loams, 3 to 15 percent slopes58591089013804851hbhsks09719831:24000
Albion sandy loam, 1 to 3 percent slopes5853152213804842wtx2ks09719831:24000
Albion and Shellabarger sandy loams, 6 to 15 percent slopes585091914549222xlhqks09719831:24000
Albion and Shellabarger sandy loams, 6 to 15 percent slopes58502989214451232xlhqks15119651:24000
Albion sandy loam, 1 to 3 percent slopes58531048314451242wtx2ks15119651:24000
Albion-Kaski complex, 0 to 15 percent slopes5857925414451262tt79ks15119651:24000
Albion sandy loam, 3 to 6 percent slopes, eroded5855187814451252wtx4ks15119651:24000
Albion-Shellabarger sandy loams, 1 to 3 percent slopes58582378914438202tt5mks15519991:24000
Shellabarger, eroded, and Albion soils, 6 to 15 percent slopes5959509814438522tt5tks15519991:24000
Albion sandy loam, 0 to 1 percent slopes5852151714438192wtx1ks15519991:24000
Albion-Shellabarger sandy loams, 1 to 3 percent slopes5858219514439692tt5mks17319761:24000
Albion and Shellabarger sandy loams, 6 to 15 percent slopes585076014439672xlhqks17319761:24000
Albion sandy loam, 6 to 15 percent slopes58561614439682wtx5ks17319761:24000
Albion sandy loam, 1 to 3 percent slopes5853123914436442wtx2ks18519751:24000
Albion-Shellabarger sandy loams, 1 to 3 percent slopes58585114436452tt5mks18519751:24000
Shellabarger and Albion soils, 7 to 15 percent slopes5946514446202tt5nks19119741:24000

Map of Series Extent

Approximate geographic distribution of the ALBION 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 .