Official Series Description


Lab Data Summary

Aggregate lab data for the ARIS soil series. This aggregation is based on all pedons with a current taxon name of ARIS, 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 ARIS 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
150A12N7957S2012TX2911013Aris7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties29.9757222,-94.5168889
150B12N7633S11TX2452366Aris7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties29.8530111,-94.1340611

Water Balance

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

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.

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Competing Series

Soil series competing with ARIS 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 ARIS 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 ARIS 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 ARIS, 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. TX-2010-11-03-27 | Hardin County - 2006

    Pattern of soils and underlying material in the Aris-League-Labelle general soil map unit (Soil Survey of Hardin County, Texas; 2006).

Map Units

Map units containing ARIS 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
Edna-Aris complex, 0 to 1 percent slopes15259823630462vv5qtx03919791:20000
Aris fine sandy loam, 0 to 1 percent slopes152813630402zqwytx03919791:20000
Leton, occasionally flooded-Aris, rarely flooded complex, 0 to 1 percent slopes28393036306030s7gtx03919791:20000
Anahuac-Aris complex, 0 to 1 percent slopesAnhA485827606872thmstx07119691:24000
Anahuac-Aris complex, 0 to 1 percent slopes, rarely floodedAniA315427606882thmttx07119691:24000
Aris-Levac complex, 0 to 1 percent slopesArsA87727606902thn1tx07119691:24000
Orcadia-Aris complex, 0 to 1 percent slopesOsaA82027607092thpdtx07119691:24000
Aris-Urban land complex, 0 to 1 percent slopesAsuA15927607462thn4tx07119691:24000
Aris loam, 0 to 1 percent slopesArlA14727606892thmytx07119691:24000
Aris-Spindletop complex, 0 to 1 percent slopes, rarely floodedAstA14527607322thn3tx07119691:24000
Aris-Spindletop complex, 0 to 1 percent slopesAspA13227606912thn2tx07119691:24000
Leton, occasionally flooded-Aris, rarely flooded complex, 0 to 1 percent slopesLs690936608530s7gtx16719851:24000
Edna-Aris complex, 0 to 1 percent slopesEs9253660662vv5qtx16719851:24000
Aris fine sandy loam, 0 to 1 percent slopesAr4363660572zqwytx16719851:24000
Orcadia-Aris complex, 0 to 1 percent slopesOsaA5427606822thpdtx16719851:24000
Aris-Spindletop complex, 0 to 1 percent slopesAspA1560627607602thn2tx19919981:24000
Aris-Levac complex, 0 to 1 percent slopesArsA633427607592thn1tx19919981:24000
Anahuac-Aris complex, 0 to 1 percent slopesAnhA167827607582thmstx19919981:24000
Aris-Urban land complex, 0 to 1 percent slopesAs1827428882442thn4tx20119731:20000
Anahuac-Aris complex, 0 to 1 percent slopesAnhA238827607842thmstx20119731:20000
Aris loam, 0 to 1 percent slopesArlA91827607852thmytx20119731:20000
Anahuac-Aris complex, 0 to 1 percent slopesAnhA1661428882472thmstx29119861:24000
Orcadia-Aris complex, 0 to 1 percent slopesOsaA1247328882612thpdtx29119861:24000
Aris-Levac complex, 0 to 1 percent slopesArsA713428882492thn1tx29119861:24000
Aris loam, 0 to 1 percent slopesArlA520328882482thmytx29119861:24000
Aris-Spindletop complex, 0 to 1 percent slopesAspA328428883302thn2tx29119861:24000
Aris-Urban land complex, 0 to 1 percent slopesAsuA54728883222thn4tx29119861:24000
Anahuac-Aris complex, 0 to 1 percent slopesAnhA1154628884802thmstx62319961:24000
Aris-Spindletop complex, 0 to 1 percent slopesAspA1080028884832thn2tx62319961:24000
Orcadia-Aris complex, 0 to 1 percent slopesOsaA769028885012thpdtx62319961:24000
Aris-Spindletop complex, 0 to 1 percent slopes, rarely floodedAstA518528885262thn3tx62319961:24000
Orcadia-Aris complex, 0 to 1 percent slopes, rarely floodedOsdA486928885382thpftx62319961:24000
Anahuac-Aris complex, 0 to 1 percent slopes, rarely floodedAniA359628884812thmttx62319961:24000
Aris-Levac complex, 0 to 1 percent slopesArsA162628884822thn1tx62319961:24000

Map of Series Extent

Approximate geographic distribution of the ARIS 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 .