Official Series Description


Lab Data Summary

Aggregate lab data for the REEDSLAKE soil series. This aggregation is based on all pedons with a current taxon name of REEDSLAKE, 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 REEDSLAKE 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
103UMN2780S1979MN091006 (2780)Reedslake3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties43.5103798,-94.4628677

Water Balance

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

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

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Competing Series

Soil series competing with REEDSLAKE 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 REEDSLAKE 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 REEDSLAKE 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.

Click the image to view it full size.

Click the image to view it full size.

Soil series sharing subgroup-level classification with REEDSLAKE, 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-2010-09-13-01 | Wright County -

    Typical pattern of soils and parent material in the Reedslake-Cokato-Muskego association (Soil Survey of Wright County, Minnesota).

Map Units

Map units containing REEDSLAKE 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
Reedslake-Le Sueur complex, 1 to 6 percent slopesL113B40914038152y037ia03319781:15840
Le Sueur-Reedslake-Cordova complex, 0 to 5 percent slopesL1207B97231117522y036ia03319781:15840
Reedslake-Swanlake complex, 3 to 12 percent slopesL1213B831117532y038ia03319781:15840
Reedslake-Le Sueur complex, 1 to 6 percent slopesL113B89331117542y037ia08119871:15840
Le Sueur-Reedslake-Cordova complex, 0 to 5 percent slopesL1207B28631117552y036ia08119871:15840
Reedslake-Swanlake complex, 3 to 12 percent slopesL1213B4031117562y038ia08119871:15840
Reedslake-Le Sueur complex, 1 to 6 percent slopesL113B347831117582y037ia18919841:15840
Le Sueur-Reedslake-Cordova complex, 0 to 5 percent slopesL1207B56931117572y036ia18919841:15840
Reedslake-Swanlake complex, 3 to 12 percent slopesL1213B4031117592y038ia18919841:15840
Reedslake-Le Sueur complex, 1 to 6 percent slopesL113B668531117612y037mn01319751:12000
Le Sueur-Reedslake-Cordova complex, 0 to 5 percent slopesL1207B67431117602y036mn01319751:12000
Reedslake-Swanlake complex, 3 to 12 percent slopesL1213B11731117622y038mn01319751:12000
Reedslake-Le Sueur complex, 1 to 6 percent slopesL113B408431117642y037mn01919871:12000
Le Sueur-Reedslake-Cordova complex, 0 to 5 percent slopesL1207B117131117632y036mn01919871:12000
Reedslake-Swanlake complex, 3 to 12 percent slopesL1213B1731117652y038mn01919871:12000
Reedslake-Le Sueur complex, 1 to 6 percent slopesL113B1900231117712y037mn04719771:15840
Le Sueur-Reedslake-Cordova complex, 0 to 5 percent slopesL1207B184431117702y036mn04719771:15840
Reedslake-Swanlake complex, 3 to 12 percent slopesL1213B26731117722y038mn04719771:15840
Reedslake-Le Sueur complex, 1 to 6 percent slopesL113B77131117742y037mn07919861:20000
Reedslake-Swanlake complex, 3 to 12 percent slopesL1213B4531117752y038mn07919861:20000
Le Sueur-Reedslake-Cordova complex, 0 to 5 percent slopesL1207B1131117732y036mn07919861:20000
Reedslake-Le Sueur complex, 1 to 6 percent slopesL113B2403831117772y037mn08519931:20000
Le Sueur-Reedslake-Cordova complex, 0 to 5 percent slopesL1207B741731117762y036mn08519931:20000
Reedslake-Swanlake complex, 3 to 12 percent slopesL1213B1531117782y038mn08519931:20000
Reedslake-Le Sueur complex, 1 to 6 percent slopesL113B1146231117812y037mn09319961:20000
Reedslake-Swanlake complex, 3 to 12 percent slopesL1213B12131117822y038mn09319961:20000
Le Sueur-Reedslake-Cordova complex, 0 to 5 percent slopesL1207B9131117802y036mn09319961:20000
Reedslake-Le Sueur complex, 1 to 6 percent slopesL113B1294631117842y037mn10319901:20000
Le Sueur-Reedslake-Cordova complex, 0 to 5 percent slopesL1207B499531117832y036mn10319901:20000
Reedslake-Swanlake complex, 3 to 12 percent slopesL1213B6431117852y038mn10319901:20000
Reedslake-Le Sueur complex, 1 to 6 percent slopesL113B313431117872y037mn13119961:12000
Le Sueur-Reedslake-Cordova complex, 0 to 5 percent slopesL1207B54631117862y036mn13119961:12000
Reedslake-Swanlake complex, 3 to 12 percent slopesL1213B7131117882y038mn13119961:12000
Reedslake-Le Sueur complex, 1 to 6 percent slopesL113B1341431117902y037mn14319911:20000
Le Sueur-Reedslake-Cordova complex, 0 to 5 percent slopesL1207B668131117892y036mn14319911:20000
Reedslake-Swanlake complex, 3 to 12 percent slopesL1213B20531117912y038mn14319911:20000
Reedslake-Le Sueur complex, 1 to 6 percent slopesL113B1842331117932y037mn14719671:20000
Le Sueur-Reedslake-Cordova complex, 0 to 5 percent slopesL1207B321431117922y036mn14719671:20000
Reedslake-Swanlake complex, 3 to 12 percent slopesL1213B8731117942y038mn14719671:20000
Reedslake-Le Sueur complex, 1 to 6 percent slopesL113B1845731117972y037mn16120011:12000
Reedslake-Estherville complex, 2 to 6 percent slopesL122B1600455482h8yzmn16120011:12000
Le Sueur-Reedslake-Cordova complex, 0 to 5 percent slopesL1207B120131117962y036mn16120011:12000
Reedslake-Swanlake complex, 3 to 12 percent slopesL1213B12331117982y038mn16120011:12000
Reedslake-Le Sueur complex, 1 to 6 percent slopesL113B1409531118002y037mn17119981:12000
Le Sueur-Reedslake-Cordova complex, 0 to 5 percent slopesL1207B88431117992y036mn17119981:12000
Reedslake-Swanlake complex, 3 to 12 percent slopesL1213B4231118012y038mn17119981:12000

Map of Series Extent

Approximate geographic distribution of the REEDSLAKE 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 .