Official Series Description


Lab Data Summary

Aggregate lab data for the SANBURN soil series. This aggregation is based on all pedons with a current taxon name of SANBURN, 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 SANBURN 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
90A97P0282S1995MN065018Sanburn6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties45.8816681,-93.4691696

Water Balance

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

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 SANBURN, 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-2010-09-10-13 | Sherburne County -

    Pattern of soils and parent material in the Stonelake-Sanburn-Pierz association (Soil Survey of Sherburne County, Minnesota).

Map Units

Map units containing SANBURN 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
Stonelake-Sanburn complex, 1 to 6 percent slopesD9B85733182sly1mn00920071:12000
Stonelake-Sanburn complex, 15 to 40 percent slopesD9E42733184sly3mn00920071:12000
Stonelake-Sanburn complex, 6 to 15 percent slopesD9C34733183sly2mn00920071:12000
Sanburn sandy loam, 3 to 8 percent slopes730B5679397759fbwymn02119931:20000
Sanburn loamy sand, 0 to 3 percent slopes731A4864397761fbx0mn02119931:20000
Sanburn sandy loam, 1 to 3 percent slopes730A4031397758fbwxmn02119931:20000
Sanburn loamy sand, 3 to 8 percent slopes731B2238397762fbx1mn02119931:20000
Sanburn sandy loam, 8 to 15 percent slopes730C1265397760fbwzmn02119931:20000
Sanburn loamy sand, 8 to 15 percent slopes731C377397763fbx2mn02119931:20000
Sanburn-Graycalm complex, 3 to 8 percent slopes844B22150436738gngbmn05719981:24000
Sanburn loamy sand, 0 to 3 percent slopes731A8156436713gnfjmn05719981:24000
Graycalm-Sanburn complex, 8 to 15 percent slopes1021C6569436493gn6fmn05719981:24000
Sanburn very stony loamy sand, 1 to 8 percent slopes, bouldery1450B882436552gn8bmn05719981:24000
Sanburn very stony loamy sand, 8 to 15 percent slopes, bouldery1450C368436553gn8cmn05719981:24000
Sanburn very stony loamy sand, 15 to 30 percent slopes, bouldery1450E229436554gn8dmn05719981:24000
Sanburn fine sandy loam, 7 to 18 percent slopes730D119024626702nnlzmn05919561:20000
Sanburn fine sandy loam, 2 to 7 percent slopes730B42124626022nnjsmn05919561:20000
Sanburn fine sandy loam, 12 to 25 percent slopes730E17724626772nnm6mn05919561:20000
Stonelake-Sanburn complex, 7 to 18 percent slopes, moderately eroded1253D215924627082nnn6mn05919561:20000
Stonelake-Sanburn complex, 2 to 7 percent slopes1253B9524626892nnmlmn05919561:20000
Stonelake-Sanburn complex, 7 to 18 percent slopes1253D6824627072nnn5mn05919561:20000
Sanburn fine sandy loam, 7 to 12 percent slopes730C4724626202nnkcmn05919561:20000
Stonelake-Sanburn complex, 12 to 25 percent slopes, severely eroded1253E32824627102nnn8mn05919561:20000
Culver-Sanburn-Cathro complex, pitted, 0 to 8 percent slopesC41B436416763871t8f0mn09520061:12000
Duluth-Sanburn-Cathro complex, pitted, 0 to 15 percent slopesC45C242216763911t8f4mn09520061:12000
Duluth-Sanburn-Cathro complex, pitted, 0 to 35 percent slopesC45E174516763921t8f5mn09520061:12000
Stonelake-Sanburn complex, 1 to 6 percent slopesD9B216764731t8hsmn09520061:12000
Stonelake-Sanburn complex, 1 to 6 percent slopes1253B3442431438ggycmn14119941:15840
Stonelake-Sanburn complex, 6 to 15 percent slopes1253C3307431439ggydmn14119941:15840
Sanburn fine sandy loam, 2 to 6 percent slopes730B2737431495gh06mn14119941:15840
Stonelake-Sanburn complex, 15 to 40 percent slopes1253E1758431440ggyfmn14119941:15840
Sanburn fine sandy loam, 0 to 2 percent slopes730A457431494gh05mn14119941:15840

Map of Series Extent

Approximate geographic distribution of the SANBURN 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 .