Official Series Description


Lab Data Summary

Aggregate lab data for the ABELA soil series. This aggregation is based on all pedons with a current taxon name of ABELA, 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 ABELA were used in the calculation. Source: KSSL snapshot . Methods used to assemble the KSSL snapshot used by SoilWeb / SDE

There are insufficient data to create the lab data summary figure.


Water Balance

Monthly water balance estimated using a leaky-bucket style model for the ABELA 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 ABELA 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 ABELA 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 ABELA 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 flats position figure.

Competing Series

Soil series competing with ABELA 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 ABELA series and competing. Series are sorted according to hierarchical clustering of median values. Source: SSURGO map unit geometry and 1981-2010, 800m PRISM data .

Click the image to view it full size.

Geomorphic description summaries for the ABELA 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 .

Click the image to view it full size.

Click the image to view it full size.

Click the image to view it full size.

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There are insufficient data to create the 3D flats position figure.

Soil series sharing subgroup-level classification with ABELA, 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. UT-2010-11-05-04 | Tooele County Area - 2000

    Typical pattern of soils and parent material in the Borvant-Abela-Kapod general soil map unit (adjacent to the Lodar-Reywat-Lundy general soil map unit) (Soil Survey of Tooele County Area, Utah; 2000).

  2. UT-2012-03-22-15 | Tooele Area - 2000

    Typical pattern of soils and parent material in the Borvant-Abela-Kapod general soil map units (adjacent to the Lodar-Reywat-Lundy general soil map unit). (Soil Survey of Tooele Area, Utah; Tooele County and Parts of Box Elder, Davis, and Juab Counties, Utah, and Parts of White Pine and Elko Counties, Nevada; 2000).

  3. UT-2012-03-22-17 | Tooele Area - 2000

    Typical pattern of soils and parent material in the Lodar-Reywat-Lundy and Dateman-Podmor-Rock outcrop general soil map units (adjacent to the Borvant-Abela-Kapod general soil map unit). (Soil Survey of Tooele Area, Utah; Tooele County and Parts of Box Elder, Davis, and Juab Counties, Utah, and Parts of White Pine and Elko Counties, Nevada; 2000).

Map Units

Map units containing ABELA 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
Abela gravelly loam, 10 to 20 percent slopesABE17951481314j4v8ut60219691:20000
Abela stony loam, 6 to 20 percent slopesAEE3688481315j4v9ut60219691:20000
Abela very gravelly loam, 5 to 15 percent slopes237001482123j5pcut61119921:24000
Abela gravelly loam, 2 to 8 percent slopes123999482111j5nzut61119921:24000
Abela very gravelly sandy loam, 8 to 25 percent slopes3013201483821j7g4ut63419971:24000
Pavant-Abela complex, 2 to 25 percent slopes4463086483984j7mdut63419971:24000
Abela cobbly loam, 2 to 8 percent slopes300954483820j7g3ut63419971:24000
Abela, stony-Hiko Peak families, association, 5 to 30 percent slopes101580984mhkfut6491:24000
Pavant-Abela families, complex, 5 to 25 percent slopes180581650mj7xut6491:24000

Map of Series Extent

Approximate geographic distribution of the ABELA 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 .