Official Series Description


Lab Data Summary

Aggregate lab data for the FILER soil series. This aggregation is based on all pedons with a current taxon name of FILER, 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 FILER 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
9601P0377S2001MI101002Filer6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties44.228054,-86.3455582
9840A1911S1970MI057001Filer7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties43.4186134,-84.7660294

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the FILER 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 FILER 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 FILER 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 FILER 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 FILER 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 FILER 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 FILER 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 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 FILER, 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

No block diagrams are available.

Map Units

Map units containing FILER 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
Filer loam, 6 to 12 percent slopes14C72052124352tpknmi00519841:15840
Filer loam, 12 to 18 percent slopes14D30092124362w5mhmi00519841:15840
Filer loam, 18 to 35 percent slopes14E21012124372x2sxmi00519841:15840
Filer loam, 6 to 12 percent slopes24C150471860792tpknmi01519881:15840
Filer loam, 2 to 6 percent slopes24B73661860782tpkmmi01519881:15840
Filer loam, 12 to 18 percent slopes24D72241860802w5mhmi01519881:15840
Filer loam, 18 to 35 percent slopes24E50111860812x2sxmi01519881:15840
Filer loam, 6 to 12 percent slopesMaC148901863792tpknmi03719741:15840
Filer loam, 12 to 18 percent slopesMaD23251863812w5mhmi03719741:15840
Filer loam, 18 to 35 percent slopesMaE7441863832x2sxmi03719741:15840
Filer loam, 6 to 12 percent slopesMaC208441862372tpknmi04519741:15840
Filer loam, 12 to 18 percent slopesMaD36951862382w5mhmi04519741:15840
Filer loam, 18 to 35 percent slopesMaE15541862392x2sxmi04519741:15840
Filer sandy loam, 6 to 12 percent slopesMaC52551870202x2szmi05719751:12000
Filer loam, 6 to 12 percent slopesMbC11026735892tpknmi05719751:12000
Filer fine sandy loam, Saginaw Lobe, 6 to 12 percent slopesMaC94601867362w5mnmi06519771:15840
Filer loam, 2 to 6 percent slopes49B84171865592tpkmmi07319831:15840
Filer loam, 6 to 12 percent slopes49C29131865602tpknmi07319831:15840
Filer loam, 12 to 18 percent slopes49D5331865612w5mhmi07319831:15840
Filer sandy loam, 6 to 12 percent slopes101C1826735162x2szmi07319831:15840
Filer loam, 6 to 12 percent slopes36C224601871352tpknmi08119841:15840
Filer loam, 2 to 6 percent slopes36B200921871342tpkmmi08119841:15840
Filer loam, 12 to 18 percent slopes36D90691871362w5mhmi08119841:15840
Filer loam, 18 to 35 percent slopes36E38291871372x2sxmi08119841:15840
Filer fine sandy loam, 2 to 6 percent slopes13B48921924592w5mkmi10519921:15840
Filer fine sandy loam, Lake Michigan Lobe, 6 to 12 percent slopes13C13981924612w5mlmi10519921:15840
Filer sandy loam, 6 to 12 percent slopes17C53341877202x2szmi10719821:15840
Filer loam, 6 to 12 percent slopes41C52551864742tpknmi12319901:15840
Filer loam, 12 to 18 percent slopes41D9141864762w5mhmi12319901:15840
Filer fine sandy loam, 2 to 6 percent slopes13B10771889342w5mkmi12719921:15840
Filer fine sandy loam, Lake Michigan Lobe, 6 to 12 percent slopes13C1601889352w5mlmi12719921:15840
Filer loam, 12 to 18 percent slopesMlD4623944902w5mhmi15519671:12000
Filer fine sandy loam, Saginaw Lobe, 6 to 12 percent slopesMfC3824244692w5mnmi15519671:12000
Filer loam, 6 to 12 percent slopesMlC2023944992tpknmi15519671:12000
Filer loam, 18 to 35 percent slopesMlE1023944912x2sxmi15519671:12000
Filer fine sandy loam, 18 to 35 percent slopes126E229631180p5snmi61420051:12000
Filer fine sandy loam, 12 to 18 percent slopes126D1432020136s6kmi61420051:12000

Map of Series Extent

Approximate geographic distribution of the FILER 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 .