Official Series Description


Lab Data Summary

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

Click the image to view it full size.

Pedons used in the lab summary:

MLRALab IDPedon IDTaxonnameCINSSL / NASIS ReportsLink To SoilWeb GMap
9299P0172S1998MI131003Flintsteel7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties46.7358284,-89.5031433
9201P0416S1999MI131021Flintsteel6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties46.7452774,-89.335556
9201N0453S2000MI053018Flintsteel6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties46.6633339,-89.9824982
9201N0458S2000MI053047Flintsteel6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties46.5744514,-90.3839264
9201N0422S2000MI131036Flintsteel6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties46.9859467,-88.9670944
93B01N0428S2000MI131003Flintsteel6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties46.8055573,-89.6955566
93B01N0442S2000MI131024Flintsteel6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties46.7044411,-89.8600998

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the FLINTSTEEL 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.

Click the image to view it full size.



Click the image to view it full size.

Sibling Summary

Siblings are those soil series that occur together in map units, in this case with the FLINTSTEEL series. Sketches are arranged according to their subgroup-level taxonomic structure. Source: SSURGO snapshot , parsed OSD records and snapshot of SC database .

Click the image to view it full size.

Select annual climate data summaries for the FLINTSTEEL series and siblings. 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 FLINTSTEEL 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 .

Click the image to view it full size.

Click the image to view it full size.

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

Click the image to view it full size.

Click the image to view it full size.

Competing Series

Soil series competing with FLINTSTEEL share the same family level classification in Soil Taxonomy. Source: parsed OSD records and snapshot of the SC database .

Click the image to view it full size.

Select annual climate data summaries for the FLINTSTEEL 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 FLINTSTEEL 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.

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 FLINTSTEEL, 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-2010-09-10-15 | Ontonagon County -

    Typical pattern of soils and parent material in the Flintsteel-Big Iron-Watton association (Soil Survey of Ontonagon County, Michigan).

  2. MI-2010-09-10-19 | Ontonagon County -

    Typical pattern of soils and parent material in the Oldman-Porkies association (Soil Survey of Ontonagon County, Michigan).

  3. MI-2010-09-10-20 | Ontonagon County -

    Typical pattern of soils and parent material in the Rockland-Moquah association (Soil Survey of Ontonagon County, Michigan).

Map Units

Map units containing FLINTSTEEL 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
Flintsteel loam, 1 to 8 percent slopes280B1025514561531kw7pmi05320071:24000
Big Iron-Flintsteel complex, 0 to 4 percent slopes282B448316076791qyxmmi05320071:24000
Flintsteel silt loam, 1 to 6 percent slopes290B255614561661kw83mi05320071:24000
Zandi-Amasa-Flintsteel complex, 0 to 6 percent slopes299B227514561781kw8hmi05320071:24000
Flintsteel loam, 8 to 15 percent slopes280C162414561541kw7qmi05320071:24000
Zandi-Amasa-Flintsteel complex, 6 to 18 percent slopes299C109114561791kw8jmi05320071:24000
Flintsteel-Loggerhead complex, 18 to 35 percent slopes576D92814562751kwcmmi05320071:24000
Flintsteel silt loam, 6 to 18 percent slopes290C68214561671kw84mi05320071:24000
Flintsteel-Loggerhead complex, 1 to 6 percent slopes576B47914562731kwckmi05320071:24000
Flintsteel-Loggerhead complex, 6 to 18 percent slopes576C26414562741kwclmi05320071:24000
Flintsteel-Minocqua complex, 6 to 18 percent slopes449C8614561881kw8tmi05320071:24000
Big Iron-Flintsteel-Gull Point, frequently flooded, complex, dissected, 1 to 15 percent slopes103D6412614565201kwmjmi13120071:24000
Flintsteel loam, 1 to 8 percent slopes100B2747314565161kwmdmi13120071:24000
Flintsteel-Watton-Gull Point, frequently flooded, complex, dissected, 1 to 35 percent slopes104E1801414565211kwmkmi13120071:24000
Flintsteel loam, 8 to 15 percent slopes100D797414565171kwmfmi13120071:24000
Flintsteel-Watton-Gull Point, frequently flooded, complex, dissected, 1 to 70 percent slopes104F485214565221kwmlmi13120071:24000
Big Iron-Flintsteel complex, 0 to 4 percent slopes8282B375916748821t6vgmi13120071:24000
Flintsteel silt loam, 1 to 6 percent slopes8290B179716748941t6vvmi13120071:24000
Flintsteel silt loam, 6 to 18 percent slopes8290C110616748951t6vwmi13120071:24000

Map of Series Extent

Approximate geographic distribution of the FLINTSTEEL 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 .