Official Series Description


Lab Data Summary

Aggregate lab data for the ANTHO soil series. This aggregation is based on all pedons with a current taxon name of ANTHO, 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 ANTHO 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
4084P047684AZ021003Antho7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties33.0278664,-111.4512634
4067C0046S1967AZ013015Antho7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties33.2052765,-111.6350021

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the ANTHO 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 ANTHO 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 ANTHO 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 ANTHO 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 ANTHO 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 ANTHO 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 ANTHO 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 hills figure.

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

Click the image to view it full size.

Click the image to view it full size.

Soil series sharing subgroup-level classification with ANTHO, 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. AZ-2011-05-27-01 | Aguila-Carefree Area, Parts of Maricopa and Pinal Counties - 1986

    Idealized soil-landscape profile (Soil Survey of Aguila-Carefree Area, Parts of Maricopa and Pinal Counties, Arizona; 1986).

Map Units

Map units containing ANTHO 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
Antho-Carrizo-Maripo complex317286530471s66az64519821:24000
Tremant-Antho complex, 1 to 5 percent slopes11510045529761s3xaz64519821:24000
Antho sandy loams17401529561s38az64519821:24000
Antho gravelly sandy loams24479530221s5daz64519821:24000
Antho-Carrizo-Maripo complex, low precipitation44390530701s6yaz64519821:24000
Antho fine sandy loamAn1541014062291j697az64619721:24000
Growler-Antho complexGr1442014062371j69haz64619721:24000
Antho soils, very gravelly variantsAo136014062301j698az64619721:24000
Antho sandy loam117114532561sdyaz64919781:24000
Antho fine sandy loam24104532671sf9az64919781:24000
Antho sandy loam, 0 to 1 percent slopesAbA32548532981sg9az65119721:20000
Antho associationAL30848532941sg5az65119721:20000
Antho-Carrizo complex, 0 to 3 percentAGB29356532921sg3az65119721:20000
Gilman-Antho associationGM19208533341shgaz65119721:20000
Antho-Valencia associationAM15217532951sg6az65119721:20000
Antho-Brios sandy loamsAe9434533021sgfaz65119721:20000
Antho gravelly sandy loam, 0 to 1 percent slopesAdA6014533011sgdaz65119721:20000
Antho-Carrizo complex, 0 to 1 percent slopesAfA3861533031sggaz65119721:20000
Antho sandy loam, saline-alkaliAc3654533001sgcaz65119721:20000
Antho gravelly sandy loam, 1 to 3 percent slopesAdB3619532971sg8az65119721:20000
Antho-Tremant complex, 1 to 5 percent slopesAHC3403532931sg4az65119721:20000
Antho-Tremant-Mohall complex, 1 to 5 percent slopesAkB3092533051sgjaz65119721:20000
Antho sandy loam, 1 to 3 percent slopesAbB1156532991sgbaz65119721:20000
Antho-Carrizo complex, 1 to 3 percent slopesAfB1106533041sghaz65119721:20000
Laveen-Antho complex, saline-alkaliLf982533661sjhaz65119721:20000
Gilman, Antho, and Glenbar soils, severely erodedGo3315533461shvaz65119721:20000
Antho sandy loam, 0 to 1 percent slopesAnA15250534961snpaz65519691:20000
Antho gravelly sandy loam, 1 to 3 percent slopesAoB9112534981snraz65519691:20000
Antho sandy loam, 1 to 3 percent slopesAnB3244534971snqaz65519691:20000
Antho loamy fine sand, 0 to 3 percent slopes3358547951v0laz65619831:20000
Antho sandy loam, 0 to 3 percent slopes3A349894054z0bgaz65619831:20000
Antho loamy fine sand22363535441sq7az65919841:24000
Antho-Superstition complex1018416455490h8z7ca68319761:24000
Antho loamy fine sand1004134455489h8z6ca68319761:24000
Antho fine sandy loam, 0 to 1 percent slopes156042925355082qpt5ca6951:24000

Map of Series Extent

Approximate geographic distribution of the ANTHO 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 .