Official Series Description


Lab Data Summary

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

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

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

Soil series sharing subgroup-level classification with CANNING, 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. SD-2012-03-15-38 | Haakon County - 1998

    Typical pattern of soils and parent material in the Bankard-Craft-Wendte, Ree, and Samsil-Pierre associations (Soil Survey of Haakon County, SD; 1998).

  2. SD-2012-03-15-39 | Haakon County - 1998

    Typical pattern of soils and parent material in the Nimbro, Samsil-Pierre, and Kirley-Lakoma-Vivian associations (Soil Survey of Haakon County, SD; 1998).

  3. SD-2012-03-15-40 | Haakon County - 1998

    Typical pattern of soils and parent material in the Ree association (Soil Survey of Haakon County, SD; 1998).

  4. SD-2012-03-15-56 | Jerauld County - September 1994

    Pattern of soils and parent material in the Delmont-Ree-Canning association (Soil Survey of Jerauld County, SD; 1994).

Map Units

Map units containing CANNING 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
Canning loam, 0 to 3 percent slopesCdA32263541822v66wsd04119721:24000
Ree-Canning loams, 2 to 6 percent slopesRfB4717354150cwj6sd05519921:24000
Kirley-Canning complex, 2 to 6 percent slopesKfB4595354097cwghsd05519921:24000
Canning loam, 0 to 3 percent slopesCa19633540812v66wsd05519921:24000
Ree-Canning loams, 6 to 9 percent slopesRfC1520354151cwj7sd05519921:24000
Canning loam, 0 to 3 percent slopesCaA26263532682v66wsd06519701:20000
Canning loam, 3 to 6 percent slopesCaB12613532692v66xsd06519701:20000
Ree-Canning loams, 0 to 2 percent slopesRnA3737356459cyxpsd07319871:20000
Canning-Delmont loams, 2 to 6 percent slopesCdB1648356411cyw4sd07319871:20000
Ree-Canning loams, 2 to 6 percent slopesRnB315356460cyxqsd07319871:20000
Canning loam, 0 to 3 percent slopesCaA24733534642v66wsd11719771:24000
Canning loam, 3 to 6 percent slopesCaB8153534652v66xsd11719771:24000
Canning loam, 6 to 9 percent slopesCaC3893534662v66ysd11719771:24000
Canning-Murdo loams, 6 to 15 percent slopesCbD66653543782v66zsd12319751:20000
Canning loam, 3 to 6 percent slopesCaB3833543772v66xsd12319751:20000

Map of Series Extent

Approximate geographic distribution of the CANNING 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 .