Official Series Description


Lab Data Summary

Aggregate lab data for the UNA soil series. This aggregation is based on all pedons with a current taxon name of UNA, 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 UNA 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
133AS99AL-131-61988AL131006Una3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties31.8591667,-87.4711111
133B03N103103AR053 Una TPUna5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties34.1971397,-92.5664749

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the UNA 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 UNA 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 UNA 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 UNA 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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Click the image to view it full size.

Competing Series

Soil series competing with UNA 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 UNA 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 UNA 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 UNA, 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. AL-2010-02-25-02 | Wilcox County - March 1999

    Generalized patterns of soils, geomorphology, and landscape relationships in the Urbo-Mooreville-Una, Annemaine-Izagora-Lenoir, Luverne-Halso, Arundel-Cantuche, and Bama-Malbis-Luverne general soil map units along the Alabama River in the central part of Wilcox County (Soil Survey of Wilcox County, Alabama; 1999).

  2. MS-2012-04-27-11 | Newton County - February 1960

    Soil associations of Newton County, Mississippi (Soil Survey of Newton County, Mississippi; February 1960).

Map Units

Map units containing UNA 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
Una silty clay, 0 to 1 percent slopes, frequently floodedUnA27332720452zkvzal00119721:20000
Urbo-Mooreville-Una complex, 0 to 3 percent slopes, frequently floodedMn269883281742svnfal00319611:20000
Una loam, pondedUnA540328245c0kkal00520011:24000
Urbo-Mooreville-Una complex, 0 to 3 percent slopes, frequently floodedUrB302503285702svnfal02319981:24000
Una clay, pondedUnA4680328613c0yfal02319981:24000
Urbo-Mooreville-Una complex, 0 to 3 percent slopes, frequently floodedUuB714303286452svnfal02520041:24000
Una clay, pondedUnA13990328638c0z7al02520041:24000
SwampSf2240329296c1ngal05119481:20000
Urbo-Mooreville-Una complex, 0 to 3 percent slopes, frequently floodedUrB362003297292svnfal06520031:24000
Una silty clay loam, pondedUnA5330329775c24xal06520031:24000
Una silty clay, pondedUnA675925146172qcvjal08520111:24000
Urbo-Una-Mooreville complex, 0 to 1 percent slopes, frequently floodedUvA18288330506c2xhal08719971:24000
Urbo-Mooreville-Una complex, 0 to 3 percent slopes, frequently floodedUuB267203306052svnfal09119971:24000
Una silty clay, pondedUnA4370330604c30nal09119971:24000
Urbo-Una complex, 0 to 1 percent slopes, frequently floodedUuA814429950492x5qpal09720181:24000
Urbo-Mooreville-Una complex, 0 to 3 percent slopes, frequently floodedUuB333329950322svnfal09720181:24000
Una silty clay loam, 0 to 1 percent slopes, pondedUnA2680330861c38yal09919841:20000
Una clayUa13940330993c3f6al10119581:20000
Una silty clay, pondedUaA643231163782svnpal10119581:20000
Urbo-Mooreville-Una complex, 0 to 3 percent slopes, frequently floodedUrB135003312722svnfal10719971:24000
Urbo-Mooreville-Una complex, 0 to 2 percent slopes, frequently floodedUuA4390331352c3ssal11319971:24000
Urbo-Mooreville-Una complex, 0 to 3 percent slopes, frequently floodedUuB3607626421442svnfal12920131:24000
Una clay, pondedUnA629826421412rrwyal12920131:24000
Urbo-Mooreville-Una complex, 0 to 3 percent slopes, frequently floodedUuB292403316802svnfal13119971:24000
Una silty clay, pondedUnA11260331679c44bal13119971:24000
Una silty clay loam, occasionally flooded8825873179426lypsar01919831:20000
Una silty clay loam, 0 to 1 percent slopes, frequently flooded17A1217617159071vljvar05320061:24000
Una silty clay loam, occasionally flooded5215530565680lzmrar05719761:20000
Una silty clay loam, 0 to 1 percent slopes, frequently floodedUnA17194721520s6svar09920001:24000
Una silty clay loam, 0 to 2 percent slopes, occasionally flooded8850015429551nskrar10920051:20000
Una silty clay loam, 0 to 1 percent slopes, frequently floodedUnA24001579208mfq4ar13919921:24000
Una silty clay loam, 0 to 1 percent slopes, pondedUpA14987579216mfqdar13919921:24000
Una silty clay loam, frequently floodedUN761914136991jg26la01919831:24000
Una silty clay, frequently floodedUn949215274881n8gtla04319821:24000
Una silty clay loam, frequently floodedUn987216001961qq47la05919861:24000
Una silty clay loamUn1555331914c4cxms01719691:20000
Bibb and Chastain fine sandy loams (bibb and una)Bc42149331969c4fpms02319631:15840
Una clay loamUn2684332112c4l9ms02519741:20000
Urbo-Mooreville-Una complex, 0 to 3 percent slopes, frequently floodedUuB1421731216932svnfms03919671:20000
Urbo-Mooreville-Una complex, 0 to 3 percent slopes, frequently floodedUuB1126626422512svnfms04120121:24000
Jena-Una-Mantachie complex, undulating, frequently floodedJuA1063626421992rryxms04120121:24000
Urbo-Mooreville-Una complex, 0 to 3 percent slopes, frequently flooded4472758731216912svnfms05919971:24000
Una-Urbo complex, frequently floodedUn4619332665c554ms06119741:20000
Una silty clayUn514333048c5khms08119681:20000
Una and Tuscumbia silty claysUt5564333221c5r2ms09519631:15840
Chastain soils (una) (0 to 2 percent slopes)Cc1997333312c5v0ms10119571:20000
Una clay, local alluvium phase (0 to 2 percent slopes)Ua1156333400c5xvms10119571:20000
Una and Urbo soils, frequently floodedUU2706334077c6mpms12919971:20000
Jena-Una-Mantachie complex, undulating, frequently floodedJnB1573924034352lnz5ms15320081:24000
Urbo-Una complex, gently undulating, frequently floodedUaB306824034922lp10ms15320081:24000
Una silty clay loam, occasionally floodedUn2788327988c098tn10919941:20000

Map of Series Extent

Approximate geographic distribution of the UNA 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 .