Official Series Description


Lab Data Summary

Aggregate lab data for the STURGEON soil series. This aggregation is based on all pedons with a current taxon name of STURGEON, 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 STURGEON 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
90B83P0397S1982WI073004Sturgeon5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties44.9425392,-89.7112045

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the STURGEON 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 STURGEON 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 STURGEON 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 STURGEON 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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Click the image to view it full size.

Competing Series

Soil series competing with STURGEON 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 STURGEON 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 STURGEON 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 STURGEON, 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-2012-02-06-18 | Houghton County Area - October 1991

    Diagrammatic cross section of Houghton County showing the topography, elevation, general soil texture, landforms, and dominant soils and their drainage class (Soil Survey of Houghton County Area, Michigan; October 1991).

Map Units

Map units containing STURGEON 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
Evart-Sturgeon silt loams, 0 to 2 percent slopes, frequently flooded71A174814552951kvc0mi00320071:24000
Sturgeon silt loam723599415015fxvlmi01319841:20000
Ubly-Sturgeon, frequently flooded complex, 1 to 55 percent slopes, dissected8170E7624507062n851mi01319841:20000
Sturgeon-Arnheim-Pelkie complex137A7173416076fyytmi06119891:20000
Ubly-Sturgeon, frequently flooded complex, 1 to 55 percent slopes, dissected8170E595324848102pdn5mi06119891:20000
Sturgeon silt loam36A767416127fz0gmi06119891:20000
Evart-Pelkie-Sturgeon complex, 0 to 4 percent slopes71B12919395254f894mi10319991:24000
Arnheim-Sturgeon-Pelkie complex, 0 to 3 percent slopes158A1171800773vw8dmi60520041:24000
Arnheim-Totagatic-Sturgeon complex, 0 to 6 percent slopes, frequently flooded24A32317179221vnmvmi6061:12000
Michigamme-Sturgeon, occasionally flooded, complex, 0 to 46 percent slopes54E19723782292ktr2mi6061:12000
Sturgeon-Fordum complex, river valleys, 0 to 3 percent slopes, frequently flooded1708A247630538692xk6twi01919941:20000
Sturgeon-Fordum complex, river valleys, 0 to 3 percent slopes, frequently flooded1708A199731821302xk6twi03519741:12000
Sturgeon silt loam, 0 to 2 percent slopesSt6418431423ggxwwi07319981:20000
Sturgeon-Fordum complex, river valleys, 0 to 3 percent slopes, frequently flooded1708A74430538762xk6twi09719721:20000
Sturgeon-Fordum complex, river valleys, 0 to 3 percent slopes, frequently flooded1708A416830538812xk6twi14119711:12000

Map of Series Extent

Approximate geographic distribution of the STURGEON 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 .