Official Series Description


Lab Data Summary

Aggregate lab data for the ALLIS soil series. This aggregation is based on all pedons with a current taxon name of ALLIS, 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 ALLIS 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
14063PA1170041963PA117004Allis4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties41.7191667,-77.3011111
14063PA1170051963PA117005Allis3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties41.9108333,-77.3222222
n/aLK-s011954-OH085-S01Allis2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Propertiesn/a
n/aAB-1121961-OH007-112Allis4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Propertiesn/a
n/aER-0231964-OH043-023Allis4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Propertiesn/a
n/aCY-0071975-OH035-007Allis4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Propertiesn/a
n/aER-0421988-OH043-042Allis4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Propertiesn/a

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the ALLIS 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 ALLIS 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 ALLIS 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 ALLIS 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 terrace figure.

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Competing Series

Soil series competing with ALLIS 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 ALLIS 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 ALLIS 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 ALLIS, 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. NY-2012-02-15-21 | Genesee County - March 1969

    Cross section showing typical soil pattern in the Fremont-Hornell-Manlius association (Soil Survey of Genesee County, New York; March 1969).

  2. OH-2012-02-16-12 | Ashtabula County - May 1973

    Soil pattern in the Conneaut-Swanton-Claverack soil association (Soil Survey of Ashtabula County, Ohio; May 1973).

Map Units

Map units containing ALLIS 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
Allis silt loamAe5942886889pdjny00119851:15840
Allis silt loamAa74025182899svnny04320181:24000
Allis silt loam, 0 to 3 percent slopesAhA14302917559slgny04519811:15840
Allis silt loam, 3 to 8 percent slopesAhB3562917569slhny04519811:15840
Allis silt loamAs21742943309w8jny09119931:24000
Tuller and Allis silt loams, 0 to 8 percent slopesTaB67852945519whnny09519651:15840
Tuller and Allis silt loams, 8 to 15 percent slopesTaC2242945529whpny09519651:15840
Allis channery silt loam, 3 to 8 percent slopesAcl4212957989xswny10719471:31680
Allis-Urban land complexAt37222872799my2oh03519781:15840
Urban land-Allis complexUc35152872719mxtoh03519781:15840
Allis silt loamAs23602872789my1oh03519781:15840
Allis clay loam, 0 to 2 percent slopesAkA40941721035s2qoh04319981:12000
Allis silt loamAs30702867889mf7oh08519761:15840
Allis silty clay loam, 0 to 2 percent slopesAlA49352877379ndvoh09319721:15840
Allis-Urban land complex, nearly levelAmA32642877389ndwoh09319721:15840
Allis loam, 0 to 2 percent slopesAkA9412877369ndtoh09319721:15840
Allis silty clay loam, 0 to 2 percent slopesAlA114125441jdvyoh10319741:15840
Allis silt loam, neutral substratum, 3 to 8 percent slopes, moderately erodedAnB2510539441l3bbpa03719651:20000

Map of Series Extent

Approximate geographic distribution of the ALLIS 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 .