Official Series Description


Lab Data Summary

Aggregate lab data for the LITTLESWAN soil series. This aggregation is based on all pedons with a current taxon name of LITTLESWAN, 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 LITTLESWAN were used in the calculation. Source: KSSL snapshot . Methods used to assemble the KSSL snapshot used by SoilWeb / SDE

Click the image to view it full size.

Pedons used in the lab summary:

MLRALab IDPedon IDTaxonnameCINSSL / NASIS ReportsLink To SoilWeb GMap
88UMN3389S1980MN137008 (3389)Littleswan2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties47.0976601,-92.7368622
88UMN3388S1980MN137011 (3388)Littleswan2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties47.0774002,-92.7721329

Water Balance

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

Click the image to view it full size.



Click the image to view it full size.

Sibling Summary

Siblings are those soil series that occur together in map units, in this case with the LITTLESWAN series. Sketches are arranged according to their subgroup-level taxonomic structure. Source: SSURGO snapshot , parsed OSD records and snapshot of SC database .

Click the image to view it full size.

Select annual climate data summaries for the LITTLESWAN series and siblings. 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 LITTLESWAN 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 .

Click the image to view it full size.

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.

Click the image to view it full size.

Competing Series

Soil series competing with LITTLESWAN share the same family level classification in Soil Taxonomy. Source: parsed OSD records and snapshot of the SC database .

Click the image to view it full size.

Select annual climate data summaries for the LITTLESWAN 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 LITTLESWAN 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 LITTLESWAN, 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 LITTLESWAN 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
Spooner-Littleswan complex, 0 to 2 percent slopesB54A763131151542z32hmn00119961:20000
Littleswan silt loam, 0 to 3 percent slopesB57A361631151532z32gmn00119961:20000
Baudette-Littleswan complex, 0 to 6 percent slopesB57B129431151522z32fmn00119961:20000
Littleswan silt loam, 0 to 3 percent slopesB57A177431151572z32gmn00719911:24000
Baudette-Littleswan complex, 0 to 6 percent slopesB57B116831151562z32fmn00719911:24000
Spooner-Littleswan complex, 0 to 2 percent slopesB54A15531151582z32hmn00719911:24000
Spooner-Littleswan complex, 0 to 2 percent slopesB54A75531151622z32hmn02119931:20000
Littleswan silt loam, 0 to 3 percent slopesB57A69931151612z32gmn02119931:20000
Baudette-Littleswan complex, 0 to 6 percent slopesB57B16731151602z32fmn02119931:20000
Littleswan silt loam, 0 to 3 percent slopesB57A929531151652z32gmn06119821:24000
Baudette-Littleswan complex, 0 to 6 percent slopesB57B784431151642z32fmn06119821:24000
Spooner-Littleswan complex, 0 to 2 percent slopesB54A639231151662z32hmn06119821:24000
Spooner-Littleswan complex, 0 to 2 percent slopesB54A710331151702z32hmn07719891:24000
Littleswan silt loam, 0 to 3 percent slopesB57A381031151692z32gmn07719891:24000
Baudette-Littleswan complex, 0 to 6 percent slopesB57B306031151682z32fmn07719891:24000
Spooner-Littleswan complex, 0 to 2 percent slopesB54A244831151742z32hmn13519991:24000
Littleswan silt loam, 0 to 3 percent slopesB57A238531151732z32gmn13519991:24000
Baudette-Littleswan complex, 0 to 6 percent slopesB57B45131151722z32fmn13519991:24000
Baudette-Littleswan complex, 1 to 8 percent slopesF192B844524079492ltnsmn61320161:24000
Littleswan-Spooner complex, 0 to 3 percent slopesF191A498924079502ltntmn61320161:24000
Baudette-Littleswan complex, 0 to 8 percent slopes2srqy77129437282srqymn61320161:24000
Littleswan-Spooner complex, 0 to 3 percent slopes2srr428729439122srr4mn61320161:24000
Voyageurs, oxyaquic-Littleswan-Conic, very stony complex, 0 to 12 percent slopes, rocky2srqv10129437262wgm0mn61320161:24000
Spooner-Littleswan complex, 0 to 2 percent slopesB54A30231151782z32hmn61720071:24000
Littleswan silt loam, 0 to 3 percent slopesB57A20531151772z32gmn61720071:24000
Spooner-Buhl-Littleswan complex, 0 to 3 percent slopesB73A84186149820h1bmn61720071:24000
Baudette-Littleswan complex, 0 to 6 percent slopesB57B3531151762z32fmn61720071:24000
Spooner-Littleswan complex, 0 to 2 percent slopesB54A738131151822z32hmn61920091:24000
Littleswan silt loam, 0 to 3 percent slopesB57A695631151812z32gmn61920091:24000
Baudette-Littleswan complex, 0 to 6 percent slopesB57B545931151802z32fmn61920091:24000
Lahti-Gowan-Littleswan complex, 1 to 3 percent slopesB267B105624256692mf3dmn61920091:24000
Alborn-Littleswan complex, 0 to 3 percent slopesB270A980194679223bsrmn61920091:24000
Spooner-Buhl-Littleswan complex, 0 to 3 percent slopesB73A589194686923bw7mn61920091:24000
Spooner-Littleswan complex, 0 to 2 percent slopesB54A91531151862z32hmn62120061:24000
Littleswan silt loam, 0 to 3 percent slopesB57A64131151852z32gmn62120061:24000
Spooner-Buhl-Littleswan complex, 0 to 3 percent slopesB73A314843501x9qqmn62120061:24000
Baudette-Littleswan complex, 0 to 6 percent slopesB57B7731151842z32fmn62120061:24000
Spooner-Littleswan complex, 0 to 2 percent slopesB54A1097031151902z32hmn62520151:24000
Baudette-Littleswan complex, 0 to 6 percent slopesB57B880031151882z32fmn62520151:24000
Littleswan silt loam, 0 to 3 percent slopesB57A653531151892z32gmn62520151:24000
Baudette-Littleswan complex, 1 to 8 percent slopesF192B544029438242pftymn62520151:24000
Littleswan-Spooner complex, 0 to 3 percent slopesF191A460529438232pftvmn62520151:24000
Littleswan-Spooner complex, 0 to 3 percent slopes2srr493029438692srr4mn62520151:24000
Voyageurs, oxyaquic-Littleswan-Conic, very stony complex, 0 to 12 percent slopes, rocky2srqv20329438782wgm0mn62520151:24000
Voyageurs, oxyaquic-Littleswan-Conic, very stony complex, 0 to 12 percent slopes, rocky2srqv442427422372wgm0mn62720151:12000
Littleswan-Spooner complex, 0 to 3 percent slopes2srr4424827422452srr4mn62720151:12000
Baudette-Littleswan complex, 0 to 8 percent slopes2srqy29027422402srqymn62720151:12000

Map of Series Extent

Approximate geographic distribution of the LITTLESWAN 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 .