Official Series Description


Lab Data Summary

Aggregate lab data for the AKELA soil series. This aggregation is based on all pedons with a current taxon name of AKELA, 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 AKELA 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 AKELA 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 AKELA 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 AKELA 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 AKELA 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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Competing Series

Soil series competing with AKELA 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 AKELA 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 AKELA 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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Click the image to view it full size.

Click the image to view it full size.

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 AKELA, 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-2011-05-27-28 | Pinal County, Western Part - 1991

    Generalized relationship of some soils in the survey area (Soil Survey of Pinal County, Arizona, Western Part; 1991).

Map Units

Map units containing AKELA 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
Akela-Rock outcrop-Rubble land complex, 40 to 70 percent slopes13269615078641mm1saz62720051:24000
Akela-Rock outcrop-Rubble land complex, dry, 40 to 70 percent slopes22183015078651mm1taz62720051:24000
Akela-Rock outcrop complex, 20 to 60 percent slopes62425515079251mm3raz62720051:24000
Aquarius-Akela-Rock outcrop complex, 1 to 25 percent slopes8383815078711mm20az62720051:24000
Akela-Rock outcrop complex, 15 to 65 percent slopes44135534591smhaz65319851:24000
Akela-Delthorny-Stagecoach -Rock Outcrop complex, 10 to 90 percent slopes705828531934312z8vhaz6571:24000
Akela-Rock outcrop complex, 10 to 60 percent slopes15995535331spwaz65919841:24000
Granolite-Rock outcrop-Akela complex, 5 to 45 percent slopes497229114631117gtsaz66120091:24000
Akela-Lehmans-Rock outcrop complex, 9 to 60 percent slopes115440544311tmvaz66319791:24000
Granolite-Rock outcrop-Akela complex, 5 to 45 percent slopes40439423847902l1kqaz67520091:24000
Rock outcrop-Akela family complex, 15 to 60 percent slopes1011370615992nnzqaz70120011:24000
Akela very gravelly loam, 0 to 10 percent slopesAG12721560071w8pnm02919671:24000
Akela very gravelly loam, 10 to 25 percent slopesAK6981560081w8qnm02919671:24000
Akela-Rock outcrop complex, 1 to 9 percent slopesAkC2400556201vw6nm60019731:24000
Rock outcrop-Akela complex, 10 to 50 percent slopesRBE1000556781vy2nm60019731:24000
Rock outcrop-Akela complex, 10 to 50 percent slopesRX5301558241w2snm61219701:24000
Akela-Rock outcrop complex, 1 to 9 percent slopesAR5101557521w0gnm61219701:24000
Akela very gravelly loam, moderately rolling416241564831ws1nm66019811:48000
Akela-Rock outcrop association, very steep514427565321wtmnm66019811:48000
Aftaden-Akela-Lava flows association, 1 to 15 percent slopes65612159571671xh3nm66419841:24000
Akela-Rock outcrop complexAL87824634536p98xnm6901:24000
Akela-Rochpah-Rock outcrop associationARR1491653878pydvnv61119671:24000
Akela-Rock outcrop association104019342478018j1dynv75419921:24000
Akela-Rochpah-Rock outcrop association10419786478019j1dznv75419921:24000
Canutio-Akela complex, 2 to 15 percent slopes5001891469320hrccnv78819821:24000
Akela-Rock outcrop complex, 15 to 50 percent slopes5101691469324hrchnv78819821:24000
Canutio-Akela complex, 15 to 50 percent slopes505954469323hrcgnv78819821:24000

Map of Series Extent

Approximate geographic distribution of the AKELA 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 .