Official Series Description


Lab Data Summary

Aggregate lab data for the SARTELL soil series. This aggregation is based on all pedons with a current taxon name of SARTELL, 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 SARTELL 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
88UMN2911S1979MN0612911Sartell2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties47.8794098,-93.2433777
88UMN3397S1980MN137029 (3397)Sartell2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties47.4292488,-92.3584595
91AUMN3365S1980MN097028 (3365)Sartell1Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties45.8961983,-94.2809143
91B40A1699S1960MN141004Sartell6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties45.5161018,-93.8594055
91BUMN1223S1965MN0031223Sartell3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties45.3780479,-93.1633606

Water Balance

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

Competing Series

Soil series competing with SARTELL 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 SARTELL 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 SARTELL 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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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 SARTELL, 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 SARTELL 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
Sartell fine sand, 2 to 6 percent slopesSbB9834395966f913mn00319721:15840
Sartell fine sand, 6 to 12 percent slopesSbC1709395967f914mn00319721:15840
Sartell fine sand, 12 to 24 percent slopes, erodedSbD2503395969f916mn00319721:15840
Sartell fine sand, 6 to 12 percent slopes, erodedSbC2346395968f915mn00319721:15840
Sartell loamy fine sand, 1 to 6 percent slopes328B979397626fbrnmn00719911:24000
Sartell, till substratum-Bushville complex, 1 to 6 percent slopesC42B648753009t8kmmn00920071:12000
Sartell fine sand, till substratum, 6 to 12 percent slopesC62C77753008t8klmn00920071:12000
Sartell fine sand, 1 to 6 percent slopes328B8622396569f9nkmn02519901:15840
Sartell fine sand, 12 to 25 percent slopes328D1208396571f9nmmn02519901:15840
Sartell fine sand, 6 to 12 percent slopes328C1163396570f9nlmn02519901:15840
Sartell loamy fine sand, 1 to 6 percent slopes328B3237400385ffmnmn09719871:20000
Sartell loamy fine sand, 6 to 12 percent slopes328C336400386ffmpmn09719871:20000
Sartell fine sand, 2 to 6 percent slopesZaB763428062gcfgmn13919881:20000
Sartell fine sand, 6 to 12 percent slopes, moderately erodedZaC2431428064gcfjmn13919881:20000
Sartell fine sand, 0 to 2 percent slopesZaA306428060gcfdmn13919881:20000
Sartell fine sand, 2 to 6 percent slopes, moderately erodedZaB2176428063gcfhmn13919881:20000
Sartell fine sand, 0 to 2 percent slopes, moderately erodedZaA250428061gcffmn13919881:20000

Map of Series Extent

Approximate geographic distribution of the SARTELL 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 .