Official Series Description


Lab Data Summary

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

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

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Soil series sharing subgroup-level classification with SPOT, 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. MI-2010-09-07-10 | Mackinac County - 1997

    Typical pattern of soils and parent material in the Wallace-Spot association (Soil Survey of Mackinac County, Michigan; 1997).

  2. MI-2012-02-06-37 | Mackinac County - 1997

    Typical pattern of soils and parent material in the Wallace-Spot association (Soil Survey of Mackinac County, Michigan; 1997).

Map Units

Map units containing SPOT 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
Spot-Finch complex, 0 to 3 percent slopes266A113214554081kvgnmi00320071:24000
Spot peat397481912826f1dmi00719981:12000
Spot-Finch complex, 0 to 3 percent slopes89A14918631286p5x2mi09520041:24000
Spot-Dawson peats1029442631297p5xfmi09520041:24000
Tawas-Spot-Finch complex, 0 to 3 percent slopes94A8915631296p5xdmi09520041:24000
Paquin-Spot complex, 0 to 6 percent slopes176B8730399608fdtlmi09520041:24000
Wallace-Spot complex, 0 to 35 percent slopes175E6324631321p5y6mi09520041:24000
Rousseau-Spot complex, 0 to 35 percent slopes90E5353631288p5x4mi09520041:24000
Wallace-Spot complex, 0 to 15 percent slopes175D5351631320p5y5mi09520041:24000
Croswell-Spot complex, 0 to 6 percent slopes174B3558631319p5y4mi09520041:24000
Rousseau-Spot complex, 0 to 15 percent slopes90D2498631287p5x3mi09520041:24000
Rubicon-Spot complex, 0 to 15 percent slopes45D2465679964qtkbmi09520041:24000
Rubicon-Spot complex, 0 to 35 percent slopes45E2299653848pycwmi09520041:24000
Spot peat22486631413p615mi09520041:24000
Rousseau-Spot complex, 0 to 60 percent slopes90F374631289p5x5mi09520041:24000
Spot-Finch complex, 0 to 3 percent slopes89A16606416431fzb8mi09719941:20000
Markey-Spot-Finch complex, 0 to 3 percent slopes94A16002416434fzbcmi09719941:20000
Wallace-Spot complex, 0 to 15 percent slopes175D3337416352fz7qmi09719941:20000
Paquin-Spot complex, 0 to 6 percent slopes176B3126416353fz7rmi09719941:20000
Croswell-Spot complex, 0 to 6 percent slopes174B1110416351fz7pmi09719941:20000
Spot muck221033416378fz8kmi09719941:20000
Spot-Finch complex, 0 to 3 percent slopes26A2898814569541kx2jmi15320071:24000
Spot peat7268214570061kx46mi15320071:24000

Map of Series Extent

Approximate geographic distribution of the SPOT 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 .