Official Series Description


Lab Data Summary

Aggregate lab data for the BLENDON soil series. This aggregation is based on all pedons with a current taxon name of BLENDON, 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 BLENDON 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
55C40A2393S1950SD059005Blendon7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties44.7083321,-98.75
7180P04161980NE121165Blendon7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties41.2177778,-98.0019444
7185P02291984NE077012Blendon5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties41.4119444,-98.6644444

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the BLENDON 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 BLENDON 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 BLENDON 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 BLENDON 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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Competing Series

Soil series competing with BLENDON 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 BLENDON series and competing. Series are sorted according to hierarchical clustering of median values. Source: SSURGO map unit geometry and 1981-2010, 800m PRISM data .

Click the image to view it full size.

Geomorphic description summaries for the BLENDON 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 .

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Click the image to view it full size.

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.

Soil series sharing subgroup-level classification with BLENDON, 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. NE-2012-02-10-17 | Colfax County - January 1982

    Typical pattern of soils and parent material in associations 7, 9, and 10 (Soil Survey of Colfax County, Nebraska; January 1982).

  2. NE-2012-02-13-18 | Greeley County - April 1993

    Typical pattern of soils and parent material in the Hord-Cozad and the Boel-Loup-Leshara associations (Soil Survey of Greeley County, Nebraska; April 1993).

  3. NE-2012-02-14-11 | Valley County - October 1985

    Typical pattern of soils and parent material in the Cozad-Hord and Boel-Loup-Leshara associations (Soil Survey of Valley County, Nebraska; October 1985).

Map Units

Map units containing BLENDON 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
Blendon sandy loam, 0 to 3 percent slopes1011680953573671co62519751:24000
Blendon fine sandy loam, 0 to 2 percent slopes650819544269302y20yne00319751:20000
Blendon fine sandy loam, 2 to 6 percent slopes651011994269312y210ne00319751:20000
Blendon fine sandy loam, 2 to 6 percent slopes65101100357613d03xne01519761:20000
Blendon fine sandy loam, 0 to 2 percent slopes6508499357612d03wne01519761:20000
Blendon loam, 0 to 2 percent slopes65131774170003130rssne01919671:20000
Blendon fine sandy loam, 0 to 2 percent slopes6508911170002930rsnne01919671:20000
Blendon-Muir complex, 0 to 2 percent slopes6518360716912632znsgne02319791:20000
Blendon fine sandy loam, 0 to 2 percent slopes6508109816912612y20yne02319791:20000
Blendon fine sandy loam, 2 to 6 percent slopes651029816912622y210ne02319791:20000
Blendon fine sandy loam, 2 to 6 percent slopes651030214270852y210ne02719821:20000
Blendon loam, 0 to 2 percent slopes65131238427086gbdzne02719821:20000
Blendon fine sandy loam, 0 to 2 percent slopes650876414278752y20yne03719801:20000
Blendon loam, 2 to 6 percent slopes6515351427876gc7gne03719801:20000
Blendon fine sandy loam, 0 to 2 percent slopes65086564266602y20yne05119751:20000
Blendon loam, 0 to 2 percent slopes65131134169992830rssne07719871:20000
Blendon fine sandy loam, 0 to 2 percent slopes6508623169992730rsnne07719871:20000
Blendon loam, 0 to 2 percent slopes65132864170010130rssne07920031:12000
Blendon fine sandy loam, 0 to 2 percent slopes6508419211442132y20yne10719891:20000
Blendon fine sandy loam, 0 to 2 percent slopes650833354273862y20yne11919811:20000
Blendon fine sandy loam, 0 to 2 percent slopes65082908170962330rsnne12119781:20000
Blendon fine sandy loam, 2 to 6 percent slopes651050617096241vd05ne12119781:20000
Blendon loam, 0 to 2 percent slopes651357222825830rssne12119781:20000
Blendon fine sandy loam, 0 to 2 percent slopes6508633222897030rsnne12519581:20000
Blendon fine sandy loam, 0 to 2 percent slopes650832122171422y20yne13919701:20000
Blendon fine sandy loam, 0 to 2 percent slopes650832204276192y20yne14119841:20000
Blendon fine sandy loam, 1 to 3 percent slopes6509176416922782znsdne14319671:20000
Blendon fine sandy loam, 0 to 2 percent slopes650853416922771tsylne14319671:20000
Blendon fine sandy loam, 0 to 2 percent slopes650818084268142y20yne16719801:20000
Blendon fine sandy loam, 0 to 2 percent slopes65082572169987130rsnne17519831:20000
Blendon fine sandy loam, clayey substratum, 1 to 6 percent slopes65111149426776gb2zne17919701:20000
Blendon fine sandy loam, 2 to 6 percent slopes65101322173252y210ne17919701:20000
Blendon fine sandy loam, 3 to 6 percent slopesBnB1872354831cx75sd00319791:20000
Blendon fine sandy loam, 0 to 3 percent slopesBnA1164354830cx74sd00319791:20000
Carthage-Blendon fine sandy loams, 0 to 2 percent slopesCbA13744354558cwycsd00519761:20000
Carthage-Blendon fine sandy loams, 2 to 6 percent slopesCbB2864354559cwydsd00519761:20000
Blendon fine sandy loam, 0 to 2 percent slopesBnA1875354552cwy5sd00519761:20000
Henkin-Blendon fine sandy loams, 2 to 6 percent slopesHkB119417737g0pdsd02519921:20000
Blendon fine sandy loam, 0 to 2 percent slopesBmA25417694g0n0sd02519921:20000
Blendon sandy loam, 0 to 3 percent slopesBmA5680352903cv6zsd03519661:20000
Blendon-Firesteel complex, 0 to 3 percent slopesBnA992352904cv70sd03519661:20000
Henkin-Blendon fine sandy loams, 2 to 6 percent slopesHbB1818354899cx9csd04319791:20000
Henkin-Blendon fine sandy loams, 0 to 2 percent slopesHbA1547354898cx9bsd04319791:20000
Henkin-Blendon fine sandy loams, 0 to 4 percent slopesHaA529353804cw51sd06919921:20000
Henkin-Blendon fine sandy loams, 2 to 6 percent slopesHbB114417484g0f7sd07719921:20000
Blendon loam, 0 to 5 percent slopesBdB513418007g0z3sd08719761:20000
Blendon-Henkin fine sandy loams, 2 to 6 percent slopesBhB1121446004gz37sd09919951:24000
Blendon fine sandy loam, cool, 0 to 3 percent slopesBfA10644460032y20zsd09919951:24000
Blendon fine sandy loam, cool, 0 to 3 percent slopesBeA19014183052y20zsd10119851:20000
Blendon fine sandy loam, 0 to 2 percent slopesBcA1963354757cx4ssd11119781:20000
Blendon fine sandy loam, 2 to 6 percent slopesBcB814354758cx4tsd11119781:20000
Henkin-Blendon fine sandy loams, 0 to 2 percent slopesHsA2276356653cz3ysd11519971:24000
Henkin-Blendon fine sandy loams, 2 to 6 percent slopesHsB857356654cz3zsd11519971:24000
Blendon fine sandy loam, cool, 0 to 3 percent slopesBkA9674182072y20zsd12519801:20000
Blendon-Henkin fine sandy loams, 2 to 6 percent slopesBmB773418208g15lsd12519801:20000
Blendon-Thurman complex, 0 to 6 percent slopesBhB1224418056g10psd13519771:20000

Map of Series Extent

Approximate geographic distribution of the BLENDON 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 .