Official Series Description


Lab Data Summary

Aggregate lab data for the FOSSUM soil series. This aggregation is based on all pedons with a current taxon name of FOSSUM, 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 FOSSUM 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
56UMN2257S1976MN0272257Fossum2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties46.7636795,-96.4850998

Water Balance

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

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Soil series sharing subgroup-level classification with FOSSUM, 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. ND-2012-02-08-21 | McHenry County - October 1990

    Typical pattern of soils and parent material in the Hecla-Aylmer-Ulen association (Soil Survey of McHenry County, North Dakota; October 1990).

  2. ND-2012-02-08-23 | McHenry County - October 1990

    Typical pattern of soils and parent material in the Towner-Swenoda-Hecla association (Soil Survey of McHenry County, North Dakota; October 1990).

  3. SD-2012-03-14-07 | Brown County - April 1993

    Typical pattern of soils and parent material in the Serden-Hamar-Venlo and Hecla-Hamar-Ulen associations (Soil Survey of Brown County, SD; 1993).

Map Units

Map units containing FOSSUM 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
Fossum sandy loam, 0 to 2 percent slopesJ5A3419434762gldlmn15120001:12000
Fossum fine sandy loam, 0 to 1 percent slopesF33A56725877812q3vynd0051:12000
Fossum fine sandy loam, 0 to 1 percent slopesG33A44425737312q4htnd0051:12000
Fossum fine sandy loam, 0 to 1 percent slopes, frequently pondedF32A4125876772q3vxnd0051:12000
Fossum fine sandy loam, 0 to 1 percent slopes, frequently pondedF32A147525859682q3vxnd00919811:20000
Fossum fine sandy loam, 0 to 1 percent slopesG33A180225752822q4htnd02119891:20000
Fossum fine sandy loam, 0 to 1 percent slopes, frequently pondedG32A75725753192q50gnd02119891:20000
Stirum-Fossum fine sandy loams, 0 to 1 percent slopesG361A7525753222q50pnd02119891:20000
Fossum fine sandy loam, 0 to 1 percent slopesG33A107325754292q4htnd0271:12000
Fossum fine sandy loam, 0 to 1 percent slopesF33A1491425858142q3vynd04919871:20000
Fossum fine sandy loam, 0 to 1 percent slopes, frequently pondedF32A668025856682q3vxnd04919871:20000
Fossum fine sandy loam, 0 to 1 percent slopes, frequently pondedG32A215425713602q50gnd04919871:20000
Fossum fine sandy loam, 0 to 1 percent slopesG33A136825713442q4htnd04919871:20000
Aylmer-Fossum complex, 0 to 6 percent slopesF386B136725857222q54rnd04919871:20000
Fossum fine sandy loam, 0 to 1 percent slopesC13A22425666442q2h2nd05519741:20000
Fossum fine sandy loam, 0 to 1 percent slopesG33A13725772702q4htnd0631:12000
Fossum fine sandy loam, 0 to 1 percent slopesF33A510425873042q3vynd06919751:20000
Fossum fine sandy loam, 0 to 1 percent slopesG33A393225822712q4htnd06919751:20000
Fossum fine sandy loam, 0 to 1 percent slopes, frequently pondedF32A241725872342q3vxnd06919751:20000
Aylmer-Fossum complex, 0 to 6 percent slopesF386B136225872552q54rnd06919751:20000
Fossum fine sandy loam, 0 to 1 percent slopes, frequently pondedG32A118225823012q50gnd06919751:20000
Fossum fine sandy loam, saline, 0 to 1 percent slopesF351A57025871922q545nd06919751:20000
Fossum fine sandy loam, 0 to 1 percent slopesG33A7525811402q4htnd07319921:20000
Fossum fine sandy loam, 0 to 1 percent slopes, frequently pondedF32A68625880982q3vxnd07919901:24000
Fossum fine sandy loam, 0 to 1 percent slopesF33A1325882362q3vynd07919901:24000
Fossum fine sandy loam, 0 to 1 percent slopesG33A333825794742q4htnd08119591:12000
Stirum-Fossum fine sandy loams, 0 to 1 percent slopesG361A238025794752q50pnd08119591:12000
Fossum fine sandy loam, 0 to 1 percent slopes, frequently pondedG32A150425794542q50gnd08119591:12000
Venlo-Fossum fine sandy loams, 0 to 1 percent slopesG72A122625794392q4npnd08119591:12000
Fossum loamy sand, 0 to 1 percent slopesG74A77925819642q4nynd08319901:20000
Fossum fine sandy loam, 0 to 1 percent slopesC13A47425667842q2h2nd08319901:20000
Fossum fine sandy loam, 0 to 1 percent slopesG33A8625819542q4htnd08319901:20000
Venlo-Fossum fine sandy loams, 0 to 1 percent slopesG72A7625819612q4npnd08319901:20000
Fossum fine sandy loam, 0 to 1 percent slopes, frequently pondedG32A4725819842q50gnd08319901:20000
Fossum fine sandy loam, 0 to 1 percent slopesG33A59625813482q4htnd09319901:24000
Fossum fine sandy loam, 0 to 1 percent slopesC13A9625668322q2h2nd09319901:24000
Fossum fine sandy loam, 0 to 1 percent slopesG033A120027976512q4htsd01319871:20000
Fossum fine sandy loam, 0 to 1 percent slopes, frequently pondedG032A79427976682q50gsd01319871:20000
Stirum-Fossum fine sandy loams, 0 to 1 percent slopesG361A49927976692q50psd01319871:20000
Venlo-Fossum fine sandy loams, 0 to 1 percent slopesG072A9327976532q4npsd01319871:20000
Fossum sandy loamFx173416862fzs5sd03919921:20000
Fossum fine sandy loam, 0 to 1 percent slopes, frequently pondedG032A29727992872q50gsd09119701:20000
Venlo-Fossum fine sandy loams, 0 to 1 percent slopesG072A4727992792q4npsd09119701:20000
Stirum-Fossum fine sandy loams, 0 to 1 percent slopesG361A2127992882q50psd09119701:20000
Fossum fine sandy loam, 0 to 1 percent slopesG033A1727992782q4htsd09119701:20000

Map of Series Extent

Approximate geographic distribution of the FOSSUM 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 .