Official Series Description


Lab Data Summary

Aggregate lab data for the TRYON soil series. This aggregation is based on all pedons with a current taxon name of TRYON, 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 TRYON 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
6592P034791NE031022Tryon6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties42.4305573,-100.8136139
6540A2185S1977NE089005Tryon6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties42.3980446,-98.8526154
6540A2186S1977NE149003Tryon6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties42.3430443,-99.472641

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the TRYON 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 TRYON 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 TRYON 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 TRYON 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 TRYON 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 TRYON series and competing. 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 TRYON 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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There are insufficient data to create the 3D mountains figure.

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Click the image to view it full size.

Soil series sharing subgroup-level classification with TRYON, 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-2012-02-08-06 | Blaine County - September 1993

    Typical pattern of soils and parent material in the Valentine-Els-Ipage association (Soil Survey of Blaine County, Nebraska; September 1993).

  2. NE-2012-02-13-08 | Garfield County - February 1988

    Typical pattern of soils and parent material in the Els-Valentine-Tryon association (Soil Survey of Garfield County, Nebraska; February 1988).

  3. NE-2012-02-13-27 | Holt County - March 1983

    Typical pattern of soils in the Els-Valentine-Ipage association and their relationship to topography and parent material (Soil Survey of Holt County, Nebraska; March 1983).

  4. NE-2012-02-13-28 | Holt County - March 1983

    Typical pattern of soils in the Valentine-Els association and their relationship to topography and parent material (Soil Survey of Holt County, Nebraska; March 1983).

  5. NE-2012-02-13-37 | Kearney County - September 1984

    Typical pattern of soils in the Valentine association (Soil Survey of Kearney County, Nebraska; September 1984).

  6. NE-2012-02-13-52 | Loup County - October 1990

    Typical pattern of soils and parent material in the Valentine-Tryon-Ipage association (Soil Survey of Loup County, Nebraska; October 1990).

  7. NE-2012-02-13-77 | Rock County - May 1985

    Typical pattern of soils and parent material in the Els-Valentine-Tryon association (Soil Survey of Rock County, Nebraska; May 1985).

  8. NE-2012-02-14-17 | Wheeler County - September 1988

    Pattern of soils and parent material in the Els-Valentine-Ipage association (Soil Survey of Wheeler County, Nebraska; September 1988).

  9. NE-2012-02-14-18 | Wheeler County - September 1988

    Pattern of soils and parent material in the Valentine-Els association (Soil Survey of Wheeler County, Nebraska; September 1988).

Map Units

Map units containing TRYON 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
Valentine-Tryon, complex, 0 to 24 percent slopes477268124357482s814ne00519731:24000
Ipage-Tryon complex, 0 to 3 percent slopes4655553816994922v9vsne00919881:20000
Els-Tryon complex, 0 to 3 percent slopes4563449622191532wgdqne00919881:20000
Tryon loamy fine sand, 0 to 3 percent slopes4746130216995002s816ne00919881:20000
Tryon loamy fine sand, frequently ponded, 0 to 3 percent slopes475169716995012s817ne00919881:20000
Els-Tryon complex, 0 to 3 percent slopes4563851622191732wgdqne01719871:20000
Valentine-Tryon, complex, 0 to 24 percent slopes, moist4887719227388442s815ne01719871:20000
Tryon loamy fine sand, 0 to 3 percent slopes474655911000282s816ne01719871:20000
Tryon loamy fine sand, frequently ponded, 0 to 3 percent slopes475117311000292s817ne01719871:20000
Valentine-Tryon, complex, 0 to 24 percent slopes4772128427388432s814ne01719871:20000
Valentine-Tryon fine sands, 0 to 24 percent slopes488918322191782s813ne01719871:20000
Tryon fine sandy loam, 0 to 3 percent slopes47409122191752s81cne01719871:20000
Tryon fine sandy loam, frequently ponded47431522191762s81dne01719871:20000
Ipage-Tryon complex, 0 to 3 percent slopes4655832661004002v9vsne03119951:24000
Valentine-Tryon fine sands, 0 to 24 percent slopes4889820191004572s813ne03119951:24000
Els-Tryon complex, 0 to 3 percent slopes4563475031003712wgdqne03119951:24000
Tryon fine sandy loam, 0 to 3 percent slopes4740135701004332s81cne03119951:24000
Tryon fine sandy loam, frequently ponded474392911004342s81dne03119951:24000
Tryon-Ipage complex, 0 to 3 percent slopes47581105916998062wgfpne07119841:20000
Tryon loamy fine sand, frequently ponded, 0 to 3 percent slopes4751839416998052s817ne07119841:20000
Tryon loamy fine sand, 0 to 3 percent slopes4746676216998042s816ne07119841:20000
Tryon loamy fine sand, frequently ponded, 0 to 3 percent slopes475189316988492s817ne07519731:24000
Tryon loamy fine sand, drained, 0 to 3 percent slopes475043616988501v0smne07519731:24000
Valentine-Tryon, complex, 0 to 24 percent slopes477215924796862s814ne07519731:24000
Ipage-Tryon, wet, complex, silty substratum, 0 to 3 percent slopes4657336017001541v24pne07920031:12000
Valentine-Tryon, silty substratum, complex, 0 to 9 percent slopes4890112517001921v25xne07920031:12000
Els-Tryon complex, 0 to 3 percent slopes4563109917001181v23jne07920031:12000
Tryon loamy fine sand, 0 to 3 percent slopes4746236801001582s816ne08919811:20000
Tryon loamy fine sand, frequently ponded, 0 to 3 percent slopes4751112241001592s817ne08919811:20000
Ipage-Tryon complex, 0 to 3 percent slopes465577181001082v9vsne08919811:20000
Valentine-Tryon fine sands, 0 to 24 percent slopes, moist488850611001702s812ne08919811:20000
Els-Ipage-Tryon loamy sands, 0 to 6 percent slopes454861122196242dhpsne08919811:20000
Els-Tryon complex, 0 to 3 percent slopes4563722196272wgdqne08919811:20000
Valentine-Tryon, complex, 0 to 24 percent slopes4772180826687042s814ne09119611:24000
Els-Tryon complex, 0 to 3 percent slopes456329122289012dtc1ne09319681:12000
Ipage-Tryon, wet, complex, silty substratum, 0 to 3 percent slopes46573122289022dtc2ne09319681:12000
Tryon loamy fine sand, rarely flooded425776316918721tsjjne09919821:20000
Tryon loamy fine sand, 0 to 3 percent slopes4746152616993782s816ne11319691:24000
Tryon-Ipage complex, 0 to 3 percent slopes4758546516995542wgfpne11519861:20000
Els-Tryon complex, 0 to 3 percent slopes4563213716995532wgdqne11519861:20000
Tryon loamy fine sand, frequently ponded, 0 to 3 percent slopes4751198916995522s817ne11519861:20000
Tryon loamy fine sand, 0 to 3 percent slopes4746108716995512s816ne11519861:20000
Valentine-Tryon, complex, 0 to 24 percent slopes4772971617002372s814ne11719661:31680
Els-Tryon complex, 0 to 3 percent slopes4563416741002602wgdqne14919821:20000
Tryon loamy fine sand, 0 to 3 percent slopes4746114911002582s816ne14919821:20000
Els-Ipage-Tryon loamy sands, 0 to 6 percent slopes454870721002373c9gne14919821:20000
Tryon loamy fine sand, frequently ponded, 0 to 3 percent slopes475149441002592s817ne14919821:20000
Tryon-Ipage complex, 0 to 3 percent slopes4758922198452wgfpne14919821:20000
Tryon fine sandy loam, 0 to 3 percent slopes474037701006422s81cne16119921:20000
Tryon fine sandy loam, frequently ponded474320521006432s81dne16119921:20000
Els, calcareous-Tryon complex, 0 to 3 percent slopes45417681005853cnpne16119921:20000
Tryon loamy fine sand, 0 to 3 percent slopes4746646422198892s816ne18319841:20000
Tryon loamy fine sand, frequently ponded, 0 to 3 percent slopes4751129116998582s817ne18319841:20000
Valentine-Tryon fine sands, 0 to 24 percent slopesT163E462213901302s813sd00720041:20000
Els-Tryon complex, 0 to 3 percent slopesT055A142013900602wgdqsd00720041:20000
Ipage-Tryon complex, 0 to 3 percent slopesT085A109713900922v9vssd00720041:20000
Tryon fine sandy loam, frequently pondedT141A27313901152s81dsd00720041:20000
Tryon fine sandy loam, 0 to 3 percent slopesT140A25213901142s81csd00720041:20000
Valentine-Tryon fine sands, 0 to 24 percent slopesT163E94713919982s813sd12119671:31680
Els-Tryon complex, 0 to 3 percent slopesT055A72313915482wgdqsd12119671:31680
Ipage-Tryon complex, 0 to 3 percent slopesT085A57213915612v9vssd12119671:31680
Tryon fine sandy loam, 0 to 3 percent slopesT140A13513919862s81csd12119671:31680
Tryon fine sandy loam, frequently pondedT141A2713919872s81dsd12119671:31680
Valentine-Tryon fine sands, 0 to 24 percent slopesT163E37025827952s813sd61320111:24000
Els-Tryon complex, 0 to 3 percent slopesT055A30325827642wgdqsd61320111:24000
Ipage-Tryon complex, 0 to 3 percent slopesT085A25225827772v9vssd61320111:24000
Tryon fine sandy loam, frequently pondedT141A1425827872s81dsd61320111:24000
Tryon fine sandy loam, 0 to 3 percent slopesT140A1025827862s81csd61320111:24000

Map of Series Extent

Approximate geographic distribution of the TRYON 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 .