Official Series Description


Lab Data Summary

Aggregate lab data for the FLAK soil series. This aggregation is based on all pedons with a current taxon name of FLAK, 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 FLAK 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
5782P006681MN153006Flak7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties45.9404984,-94.7624969
5782P071982MN097005Flak7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties45.9705315,-94.5586472
57UMN3266S1980MN0973266Flak4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties45.9539299,-94.5248795
90A40A2038S1954MN035034Flak4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties46.7527695,-93.9141388
90AUMN3363S1980MN097041 (3363)Flak2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties46.1406898,-94.0407028
90AUMN3630S1982MN001006 (3630)Flak2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties46.8486099,-93.7510605
91AUMN1265S1971MN1451265Flak3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties45.5198746,-94.2545242

Water Balance

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

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

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Competing Series

Soil series competing with FLAK 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 FLAK 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 FLAK 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.

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

Soil series sharing subgroup-level classification with FLAK, 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. MN-2010-09-08-05 | Cass County - 1997

    Typical pattern of soils and parent material in the Wabedo-Flak-Nokay general soil map unit (Soil Survey of Cass County, Minnesota; 1997).

Map Units

Map units containing FLAK 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
Flak sandy loam, 3 to 8 percent slopes144B641432852gjdzmn00119961:20000
Flak sandy loam, 8 to 15 percent slopes144C151432853gjf0mn00119961:20000
Flak sandy loam, 3 to 8 percent slopes144B8339397702fbv3mn02119931:20000
Flak sandy loam, 8 to 15 percent slopes144C3121397703fbv4mn02119931:20000
Flak sandy loam, 3 to 8 percent slopes, very stony742B1850397766fbx5mn02119931:20000
Flak sandy loam, 8 to 15 percent slopes, very stony742C576397767fbx6mn02119931:20000
Brainerd-Flak complex, 4 to 8 percent slopesC164B1619927326692slmqmn03520091:24000
Flak-Brainerd complex, 6 to 15 percent slopesC169C352727327192slpmmn03520091:24000
Flak sandy loam, 4 to 8 percent slopes144B7584400342ffl8mn09719871:20000
Flak sandy loam, 8 to 15 percent slopes144C4568400343ffl9mn09719871:20000
Flak sandy loam, 15 to 25 percent slopes144E1304400344fflbmn09719871:20000
Flak sandy loam, 4 to 8 percent slopes144B10173428079gcg0mn14519801:15840
Flak sandy loam, 8 to 15 percent slopes144C1868428080gcg1mn14519801:15840
Cushing and Flak sandy loams, steep1842F1384428095gcgjmn14519801:15840
Flak sandy loam, 15 to 25 percent slopes144E631428081gcg2mn14519801:15840
Flak sandy loam, 2 to 6 percent slopes144B2706428501gcwmmn15319851:20000
Flak sandy loam, 6 to 12 percent slopes144C1128428502gcwnmn15319851:20000

Map of Series Extent

Approximate geographic distribution of the FLAK 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 .