Official Series Description


Lab Data Summary

Aggregate lab data for the FORDUM soil series. This aggregation is based on all pedons with a current taxon name of FORDUM, 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 FORDUM 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 FORDUM 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 FORDUM 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 FORDUM 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 FORDUM 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 FORDUM 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 FORDUM 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 FORDUM 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 FORDUM, 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-2010-09-13-07 | Wright County -

    A landscape view of some soils in areas of outwash, flood plain, and glacial till in Wright County (Soil Survey of Wright County, Minnesota).

  2. WI-2012-03-23-33 | Shawano County - October 1982

    Relationship of sols and substratum in the Menahga-Croswell-Mahtomedi general map unit (Soil Survey of Shawano County, WI; 1982).

Map Units

Map units containing FORDUM 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
Fordum-Winterfield complex, 0 to 2 percent slopes, frequently floodedFo183885885yqtymn00319721:15840
Fordum-Winterfield complex, 0 to 2 percent slopes, frequently flooded1011A2519189959421rp7mn00920071:12000
Fordum loam, 0 to 2 percent slopes, occasionally floodedD39A17753013t8krmn00920071:12000
Fordum sandy loam, frequently flooded7924016396598f9phmn02519901:15840
Fordum, Fairdale, and Lamoure soils, frequently flooded11471834430390gfvkmn02919931:20000
Fordum-Winterfield complex, 0 to 4 percent slopes, flooded1011A37727326872slncmn03520091:24000
Fordum-Winterfield complex, 0 to 2 percent slopes, frequently floodedD19A466451585h4x8mn05320011:12000
Elkriver-Fordum complex, 0 to 2 percent slopes, occasionally floodedD35A190435222glwfmn05320011:12000
Fordum fine sandy loam7923237398914fd36mn07719891:24000
Fordum, Fairdale, and Lamoure soils, frequently flooded11476311399198fddcmn08719921:20000
Fordum-Winterfield complex, 0 to 2 percent slopes, frequently flooded1011A62216763351t8cbmn09520061:12000
Fordum-Winterfield complex19469973400358fflsmn09719871:20000
Fordum-Winterfield complex, 0 to 2 percent slopes, frequently flooded19465324431467ggz9mn14119941:15840
Fordum silt loam, occasionally flooded19851529428783gd5qmn15919871:20000
Fordum-Winterfield complex, 0 to 2 percent slopes, frequently flooded1946390435090glr5mn17119981:12000
Fordum loam, 0 to 2 percent slopes, occasionally flooded1378369435076glqqmn17119981:12000
Fordum fine sandy loam, 0 to 2 percent slopes, frequently flooded79299433798gkdhmn17119981:12000
Winterfield-Fordum complex, river valleys, 0 to 3 percent slopes, frequently flooded1758A476830538662xk6rwi00119781:20000
Fordum, Totagatic, and Bowstring soils, 0 to 1 percent slopes, frequently flooded9050A840614445571kh5mwi00320061:12000
Moppet, occasionally flooded-Fordum, frequently flooded complex, 0 to 3 percent slopes755A177615427131ns9ywi00320061:12000
Fordum silt loam, 0 to 2 percent slopes, frequently flooded555A66014444421kh1xwi00320061:12000
Fordum silt loam, 0 to 2 percent slopesFm5800431297ggstwi00519931:20000
Fordum silt loam, river valleys, 0 to 2 percent slopes, frequently flooded709A275031820592yt2rwi00519931:20000
Fordum, Totagatic, and Bowstring soils, 0 to 1 percent slopes, frequently flooded9050A330913839491hg3jwi00720051:12000
Fordum silt loam, 0 to 2 percent slopes, frequently flooded555A227782479v878wi00720051:12000
Fordum silt loam, 0 to 2 percent slopes, frequently flooded555A818816939wf2wwi01320041:12000
Moppet, occasionally flooded-Fordum, frequently flooded complex, 0 to 3 percent slopes755A107816941wf2ywi01320041:12000
Fordum loam, 0 to 2 percent slopesFm6127421525g4mlwi01719851:15840
Fordum silt loam, river valleys, 0 to 2 percent slopes, frequently flooded709A433831820602yt2rwi01719851:15840
Dechamps-Fordum complex, river valleys, 0 to 3 percent slopes, frequently flooded1638A43131820612yt2wwi01719851:15840
Moppet-Fordum complex, 0 to 3 percent slopesMxA10422431905ghffwi01919941:20000
Fordum silt loam, 0 to 2 percent slopesFm7793431868ghd7wi01919941:20000
Sturgeon-Fordum complex, river valleys, 0 to 3 percent slopes, frequently flooded1708A247630538692xk6twi01919941:20000
Winterfield-Fordum complex, river valleys, 0 to 3 percent slopes, frequently flooded1758A38630538682xk6rwi01919941:20000
Winterfield-Fordum complex, river valleys, 0 to 3 percent slopes, frequently flooded1758A4731820412xk6rwi02119721:15840
Fordum silt loam, 0 to 2 percent slopes, frequently flooded555A305781346v71qwi03120051:12000
Dechamps-Fordum complex, river valleys, 0 to 3 percent slopes, frequently flooded1638A561831820752yt2wwi03320031:12000
Fordum silt loam, river valleys, 0 to 2 percent slopes, frequently flooded709A20525186992yt2rwi03320031:12000
Sturgeon-Fordum complex, river valleys, 0 to 3 percent slopes, frequently flooded1708A199731821302xk6twi03519741:12000
Winterfield-Fordum complex, river valleys, 0 to 3 percent slopes, frequently flooded1758A108631821322xk6rwi03519741:12000
Fordum silt loam, river valleys, 0 to 2 percent slopes, frequently flooded709A5324217392yt2rwi03519741:12000
Dechamps-Fordum complex, river valleys, 0 to 3 percent slopes, frequently flooded1638A8231820772yt2wwi03519741:12000
Fordum loam, 0 to 2 percent slopesFm3297430005gfg4wi03719951:12000
Fordum loam, 0 to 2 percent slopesFm4442429838gf8rwi04119951:12000
Fordum silt loam, 0 to 2 percent slopes, frequently flooded555A159782214v7yqwi05120061:12000
Fordum, Totagatic, and Bowstring soils, 0 to 1 percent slopes, frequently flooded9050A10117012611v39dwi05120061:12000
Moppet, occasionally flooded-Fordum, frequently flooded complex, 0 to 3 percent slopes755A2417012541v395wi05120061:12000
Winterfield-Fordum complex, river valleys, 0 to 3 percent slopes, frequently flooded1758A70430538722xk6rwi05319941:12000
Winterfield-Fordum complex, river valleys, 0 to 3 percent slopes, frequently flooded1758A1326625615242xk6rwi05719871:12000
Fordum mucky silt loamFm3316421050g448wi06719831:20000
Fordum loam, 0 to 2 percent slopesFh5425431616gh43wi06919931:20000
Fordum silt loam, 0 to 1 percent slopesFh20998431367ggw2wi07319981:20000
Fordum mucky very fine sandy loam, 0 to 2 percent slopesFh4256421085g45dwi08519881:20000
Dechamps-Fordum complex, river valleys, 0 to 3 percent slopes, frequently flooded1638A16131820862yt2wwi09320061:12000
Dechamps-Fordum-Caryville complex, 0 to 6 percent slopes, commonly flooded26B36124276872mh6hwi09519781:15840
Fordum-Ausable complex, 0 to 2 percent slopes, frequently flooded5555A17124276972mh6twi09519781:15840
Fordum silt loam, 0 to 2 percent slopes, frequently flooded555A7124871432ph2fwi09519781:15840
Winterfield-Fordum complex, river valleys, 0 to 3 percent slopes, frequently flooded1758A511530538782xk6rwi09719721:20000
Sturgeon-Fordum complex, river valleys, 0 to 3 percent slopes, frequently flooded1708A74430538762xk6twi09719721:20000
Moppet, occasionally flooded-Fordum, frequently flooded complex, 0 to 3 percent slopes755A7748627567p213wi09920061:12000
Fordum, Totagatic, and Bowstring soils, 0 to 1 percent slopes, frequently flooded9050A604713957401hvcwwi09920061:12000
Fordum silt loam, 0 to 2 percent slopes, frequently flooded555A4793627534p201wi09920061:12000
Fordum silt loam, 0 to 2 percent slopes, frequently flooded555A10686625084nzg0wi10720061:12000
Moppet, occasionally flooded-Fordum, frequently flooded complex, 0 to 3 percent slopes755A5865625118nzh3wi10720061:12000
Winterfield-Fordum complex, river valleys, 0 to 3 percent slopes, frequently flooded1758A23931820972xk6rwi11119771:15840
Fordum, Totagatic, and Bowstring soils, 0 to 1 percent slopes, frequently flooded9050A761913861081hjc5wi11320061:12000
Moppet, occasionally flooded-Fordum, frequently flooded complex, 0 to 3 percent slopes755A2626626778p16nwi11320061:12000
Fordum silt loam, 0 to 2 percent slopes, frequently flooded555A2562625849p07pwi11320061:12000
Fordum loamFu9868422670g5tjwi11519811:15840
Fordum silt loam, 0 to 2 percent slopes555A10491420999g42mwi11920021:12000
Moppet-Fordum complex, 0 to 3 percent slopes755A6332421026g43hwi11920021:12000
Fordum silt loam, 0 to 2 percent slopes, frequently flooded555A700449021h27kwi12920021:12000
Fordum loamFa8682422710g5vtwi13519821:15840
Winterfield-Fordum complex, river valleys, 0 to 3 percent slopes, frequently flooded1758A728730538792xk6rwi14119711:12000
Sturgeon-Fordum complex, river valleys, 0 to 3 percent slopes, frequently flooded1708A416830538812xk6twi14119711:12000

Map of Series Extent

Approximate geographic distribution of the FORDUM 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 .