Official Series Description


Lab Data Summary

Aggregate lab data for the LITTLEFIR soil series. This aggregation is based on all pedons with a current taxon name of LITTLEFIR, 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 LITTLEFIR 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
11995MT02S1995AR097002Littlefir3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties34.5913889,-93.5855556

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the LITTLEFIR 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 LITTLEFIR 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 LITTLEFIR 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 LITTLEFIR 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 terrace figure.

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

Competing Series

Soil series competing with LITTLEFIR 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 LITTLEFIR 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 LITTLEFIR 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 LITTLEFIR, 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 LITTLEFIR 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
Littlefir-Bismarck complex, 15 to 35 percent slopes, very rocky30F591825774752y1m6ar09719971:24000
Littlefir-Bismarck complex, 8 to 15 percent slopes, very rocky30D481815774712y1m7ar09719971:24000
Sherless-Littlefir complex, 8 to 15 percent slopes, stony45D169415774972vz7var09719971:24000
Littlefir-Bismarck complex, 1 to 8 percent slopes30C139085775062y1lyar09719971:24000
Sherless-Littlefir complex, 1 to 8 percent slopes45C90685774962t5yhar09719971:24000
Sherless-Littlefir-Nashoba complex, 15 to 35 percent slopes, extremely stony46F7989577505mcy6ar09719971:24000
Sherless-Littlefir-Nashoba complex, 8 to 15 percent slopes739001515428891nshmar10920051:20000
Sherless-Littlefir complex, 1 to 8 percent slopes723378815428882t5yhar10920051:20000
Sherless-Littlefir-Nashoba complex, 15 to 35 percent slopes742189415428981nshxar10920051:20000
Nashoba-Littlefir-Sherless complex, 15 to 35 percent slopes, rubbly52407815429011nsj0ar10920051:20000
Nashoba-Bismarck-Littlefir complex, 8 to 15 percent slopes51273715428712y1mgar10920051:20000
Littlefir-Carnasaw complex, 1 to 8 percent slopes38163215429001nshzar10920051:20000
Nashoba-Bismarck-Littlefir complex, 1 to 8 percent slopes5060415428702y1m3ar10920051:20000
Sherless-Littlefir complex, 8 to 15 percent slopes, stony31D618985708742vz7var11319911:20000
Sherless-Littlefir complex, 1 to 8 percent slopes31C255715708732t5yhar11319911:20000
Sherless-Littlefir complex, 15 to 35 percent slopes, extremely stony31F12299570883m51lar11319911:20000
Bismarck-Littlefir complex, 8 to 15 percent slopes8D47715708462y1mjar11319911:20000
Bismarck-Littlefir complex, 15 to 35 percent slopes, very rocky8F45675708502y1mhar11319911:20000
Littlefir-Bismarck complex, 1 to 8 percent slopes20C38635708872y1lyar11319911:20000
Sherless-Littlefir complex, 8 to 15 percent slopes, stony31D1604117075322vz7var13319961:24000
Bismarck-Littlefir-Nashoba complex, 8 to 15 percent slopes3D1115517075002y1m0ar13319961:24000
Bismarck-Nashoba-Littlefir complex, 15 to 35 percent slopes4E531617075012y1mcar13319961:24000
Littlefir-Bismarck-Nashoba complex, 1 to 8 percent slopes17C486717074992y1m2ar13319961:24000
Sherless-Littlefir complex, 1 to 8 percent slopes31C316517075312t5yhar13319961:24000
Sherless-Littlefir-Nashoba complex, 15 to 35 percent slopes, extremely stonyNG355421625778511qfyfar14919851:20000
Littlefir-Carnasaw-Clebit complex, 3 to 15 percent slopes, extremely stonyNG298350324953801qfz3ar14919851:20000
Sherless-Littlefir-Nashoba complex, 8 to 15 percent slopes, very stonyNG354273825778501qfydar14919851:20000
Littlefir-Sherless-Nashoba complex, 1 to 8 percent slopes, very stonyNG397170224953841qfzcar14919851:20000
Littlefir-Bismarck complex, 8 to 15 percent slopesNG293125525778331qfw9ar14919851:20000
Sherless-Littlefir complex, 3 to 8 percent slopesNG350100525778491qfycar14919851:20000
Bismarck-Littlefir complex, 3 to 8 percent slopesNG2253524953971qfwnar14919851:20000
Bismarck-Littlefir complex, 8 to 15 percent slopesNG226124953961qfwlar14919851:20000

Map of Series Extent

Approximate geographic distribution of the LITTLEFIR 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 .