Official Series Description


Lab Data Summary

Aggregate lab data for the LINDSTROM soil series. This aggregation is based on all pedons with a current taxon name of LINDSTROM, 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 LINDSTROM 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
105UMN1219S1970MN0491219Lindstrom3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties44.5050888,-92.6136093
105UMN2348S1975MN055074Lindstrom3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties43.8325042,-91.6140322
105UMN2739S1978MN1692739Lindstrom3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties43.9518204,-92.0192337

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the LINDSTROM 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 LINDSTROM 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 LINDSTROM 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 LINDSTROM 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 LINDSTROM 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 LINDSTROM 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 LINDSTROM 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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Click the image to view it full size.

There are insufficient data to create the 3D mountains figure.

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Click the image to view it full size.

Soil series sharing subgroup-level classification with LINDSTROM, 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-2012-02-06-04 | Olmsted County - March 1980

    Pattern of soils and underlying material in the Mt. Carroll-Marlean-Arenzville association (Soil Survey of Olmsted County, Minnesota; March 1980).

  2. WI-2012-03-22-06 | Grant County - June 1961

    Landscape of Grant County showing the relationship of the major soil series (Soil Survey of Grant County, WI; 1961).

  3. WI-2012-03-23-01 | Iowa County - July 1962

    Two landscapes of upland soils showing the relationship of the major soils. The upper illustration shows soils formed under prairie, and the lower one, soils formed under forest. By Soil Survey Division, University of Wisconsin (Soil Survey of Iowa County, WI; 1962).

Map Units

Map units containing LINDSTROM 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
Lindstrom silt loam, till plain, 2 to 6 percent slopes301B38903968322zwnxmn03719801:15840
Lindstrom fine sandy loam, 18 to 45 percent slopesLd108822167542zwnvmn04520081:12000
Lindstrom silt loam, 12 to 20 percent slopes, moderately erodedN518D294822167532zwntmn04520081:12000
Lindstrom silt loam, 6 to 12 percent slopes, moderately erodedN518C267822167562zwnmmn04520081:12000
Lindstrom silt loam, 2 to 6 percent slopesN518B32722167552zwnjmn04520081:12000
Lindstrom silt loam, 6 to 12 percent slopes, moderately erodedN518C2117217116292zwnmmn04920071:12000
Lindstrom silt loam, 12 to 20 percent slopes, moderately erodedN518D2116417116312zwntmn04920071:12000
Lindstrom silt loam, 2 to 6 percent slopesN518B100617116282zwnjmn04920071:12000
Lindstrom silt loam, 6 to 12 percent slopesN518C14983982652zwnlmn05519811:15840
Lindstrom silt loam, 2 to 6 percent slopesN518B14823982642zwnjmn05519811:15840
Lindstrom loam, 12 to 20 percent slopes1906D6663982482zwnqmn05519811:15840
Lindstrom silt loam, 2 to 6 percent slopesN518B88514007532zwnjmn10919771:15840
Lindstrom silt loam, 6 to 12 percent slopesN518C25824007542zwnlmn10919771:15840
Lindstrom silt loam, glaciated, 2 to 4 percent slopes301B5616772272zwnhmn12319781:15840
Lindstrom silt loam, till plain, 2 to 6 percent slopes301B27084296402zwnxmn13119961:12000
Lindstrom silt loam, till plain, 6 to 12 percent slopes301C5854296412zwnymn13119961:12000
Lindstrom silt loam, 6 to 12 percent slopes, moderately erodedN518C246622161442zwnmmn15720081:12000
Lindstrom silt loam, 12 to 20 percent slopes, moderately erodedN518D235022161452zwntmn15720081:12000
Lindstrom silt loam, 2 to 6 percent slopesN518B2587213852zwnjmn15720081:12000
Lindstrom silt loam, glaciated, 2 to 4 percent slopes301B387816770922zwnhmn16319781:15840
Lindstrom silt loam, 2 to 6 percent slopesN518B65834290332zwnjmn16919871:20000
Lindstrom silt loam, 6 to 12 percent slopesN518C11404290342zwnlmn16919871:20000
Lindstrom silt loam, 12 to 20 percent slopesN518D9344290352zwnzmn16919871:20000
Lindstrom silt loam, 6 to 12 percent slopes, moderately eroded104C2205125617712zwnmwi01119601:20000
Lindstrom silt loam, 12 to 20 percent slopes, moderately eroded104D2188125617722zwntwi01119601:20000
Lindstrom silt loam, 20 to 30 percent slopes, moderately eroded104E279725617732zwnwwi01119601:20000
Lindstrom silt loam, 20 to 30 percent slopes, moderately eroded104E230825017062zwnwwi02319601:12000
Lindstrom silt loam, 12 to 20 percent slopes, moderately eroded104D216425017042zwntwi02319601:12000
Lindstrom silt loam, 6 to 12 percent slopes, moderately eroded104C23525017022zwnmwi02319601:12000
Lindstrom silt loam, 20 to 30 percent slopes, moderately eroded104E22164242922zwnwwi04319591:20000
Lindstrom silt loam, 6 to 12 percent slopes, moderately eroded104C2944242912zwnmwi04319591:20000
Lindstrom silt loam, 6 to 12 percent slopes, moderately eroded104C297415911962zwnmwi04519691:12000
Lindstrom silt loam, 12 to 20 percent slopes, moderately eroded104D26414252952zwntwi04519691:12000
Lindstrom sandy loam, 12 to 20 percent slopes, moderately erodedLnD22734252932zwnswi04519691:12000
Lindstrom sandy loam, 6 to 12 percent slopes, moderately erodedLnC21704252922zwnpwi04519691:12000
Lindstrom silt loam, 12 to 20 percent slopes, moderately eroded104D238627747852zwntwi04919601:20000
Lindstrom silt loam, 6 to 12 percent slopes, moderately eroded104C220927747842zwnmwi04919601:20000
Lindstrom silt loam, 2 to 6 percent slopes104B794246502zwnjwi04919601:20000
Lindstrom silt loam, 6 to 12 percent slopes, moderately eroded104C22064248422zwnmwi06519641:15840
Lindstrom silt loam, 12 to 20 percent slopes, moderately eroded104D21264248432zwntwi06519641:15840
Lindstrom silt loam, 2 to 6 percent slopes104B624248412zwnjwi06519641:15840
Lindstrom silt loam, 6 to 12 percent slopes, moderately eroded104C2725017032zwnmwi12319651:12000
Lindstrom silt loam, 12 to 20 percent slopes, moderately eroded104D2125017052zwntwi12319651:12000

Map of Series Extent

Approximate geographic distribution of the LINDSTROM 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 .