Official Series Description


Lab Data Summary

Aggregate lab data for the SANDBERG soil series. This aggregation is based on all pedons with a current taxon name of SANDBERG, 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 SANDBERG 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
102AUMN3193S1979MN1013193Sandberg3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties44.1297569,-95.6450958
102AUMN3443S1980MN153008 (3443)Sandberg4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties45.7845688,-95.0336075
102AUMN4439S1989MN1114439Sandberg2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties46.3732452,-96.0956116
56UMN1194S1970MN0691194Sandberg2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties48.5864334,-96.5461807
56UMN1264S1971MN0691264Sandberg2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties48.5885735,-96.4995193
56UMN1742S1974MN0271742Sandberg3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties46.9915237,-96.4419556
56UMN2241S1976MN0272241Sandberg2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties46.9431496,-96.4418106
56UMN3166S1979MN1673166Sandberg2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties46.5589676,-96.4686127
88UMN2497S1977MN0292497Sandberg2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties47.8499603,-95.3648529
91AUMN1717S1974MN1451717Sandberg3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties45.4113007,-94.1228409

Water Balance

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

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Click the image to view it full size.

Soil series sharing subgroup-level classification with SANDBERG, 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-2010-09-08-01 | Becker County - 1998

    Typical pattern of soils and parent material in the Arvilla-Sandberg association (Soil Survey of Becker County, Minnesota; 1998).

  2. MN-2010-09-08-09 | Marshall County - 2000

    Typical pattern of soils and underlying material in the Sandberg-Strathcona-Syrene association (Soil Survey of Marshall County, Minnesota; 2000).

  3. MN-2010-09-08-21 | Otter Tail County - 2001

    Typical pattern of soils and parent material in the Arvilla-Sverdrup-Sandberg association (Soil Survey of Otter Tail County, Minnesota; 2001).

  4. MN-2010-09-08-29 | Polk County - 2003

    Typical pattern of soils and underlying material in the Sandberg-Radium-Syrene association (Soil Survey of Polk County, Minnesota; 2003).

  5. MN-2010-09-08-31 | Polk County - 2003

    Typical pattern of soils and underlying material in the Ulen-Rosewood-Flaming association (Soil Survey of Polk County, Minnesota; 2003).

  6. MN-2010-09-10-18 | Swift County -

    Renshaw-Arvilla-Sandberg association (Soil Survey of Swift County, Minnesota).

  7. MN-2010-09-13-07 | Wright County -

    A landscape view of some soils in areas of outwash, flood plain, and glacial till in Wright County (Soil Survey of Wright County, Minnesota).

Map Units

Map units containing SANDBERG 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
Arvilla-Sandberg complex, 2 to 6 percent slopes711B5746397548fbp4mn00519941:20000
Arvilla-Sandberg complex, 6 to 12 percent slopes711C4904397549fbp5mn00519941:20000
Sandberg-Arvilla complex, 12 to 20 percent slopes1242D1901397453fbl2mn00519941:20000
Formdale-Buse-Sandberg complex, 2 to 6 percent slopes1235B1015397448fbkxmn00519941:20000
Formdale-Langhei-Sandberg complex, 6 to 12 percent slopes, eroded579C2954397544fbp0mn00519941:20000
Sandberg loamy coarse sand, 6 to 30 percent slopesD8E2777530112w8fnmn00920071:12000
Sandberg gravelly sandy loam, 6 to 30 percent slopes402E5583960902w8frmn01119901:20000
Sandberg sandy loam, 1 to 6 percent slopes402B4613960892w8fpmn01119901:20000
Sandberg-Arvilla complex, 6 to 12 percent slopesJ42C40524230532mbd0mn02319801:15840
Arvilla-Sandberg complex, 2 to 6 percent slopesJ31B29524230442mbcqmn02319801:15840
Sandberg sandy loam, 1 to 6 percent slopes258B167430263052w8fpmn02719801:20000
Sandberg loamy coarse sand, 6 to 30 percent slopesD8E122130263352w8fnmn02719801:20000
Sandberg loamy sand, 1 to 6 percent slopesD8B67830263012w8flmn02719801:20000
Sandberg loamy sand, 2 to 12 percent slopesD8C58730263182w8fmmn02719801:20000
Sandberg sandy loam, 2 to 12 percent slopes258C35430263192w8fqmn02719801:20000
Sandberg gravelly sandy loam, 6 to 30 percent slopes258E33230263342w8frmn02719801:20000
Sandberg-Radium complex, 0 to 6 percent slopesI57B7012798165prpdmn02919931:20000
Sandberg sandy loam, 1 to 6 percent slopes258B2854304712w8fpmn02919931:20000
Sandberg-Hubbard complex, Mississippi River Valley, 0 to 3 percent slopesD97A33027326842sln8mn03520091:24000
Sandberg loamy sand, 2 to 12 percent slopesD8C343930263202w8fmmn04119701:12000
Sandberg loamy sand, 1 to 6 percent slopesD8B291230263022w8flmn04119701:12000
Sandberg sandy loam, 2 to 12 percent slopes258C238930263212w8fqmn04119701:12000
Sandberg loamy coarse sand, 6 to 30 percent slopesD8E206230263372w8fnmn04119701:12000
Sandberg gravelly sandy loam, 6 to 30 percent slopes258E200830263362w8frmn04119701:12000
Sandberg sandy loam, 1 to 6 percent slopes258B61030263062w8fpmn04119701:12000
Sandberg sandy loam, 1 to 6 percent slopes402B26403980482w8fpmn05119741:20000
Sandberg sandy loam, 2 to 12 percent slopes402C22243980492w8fqmn05119741:20000
Sandberg-Radium complex, 0 to 6 percent slopesI57B8892798180prpdmn05119741:20000
Sandberg gravelly sandy loam, 6 to 30 percent slopes402D5003980502w8frmn05119741:20000
Sandberg loamy coarse sand, 6 to 30 percent slopesD8E4784516262w8fnmn05320011:12000
Sandberg loamy coarse sand, 12 to 18 percent slopesD8D212451627h4ymmn05320011:12000
Sandberg loamy sand, 2 to 12 percent slopesD8C1464516282w8fmmn05320011:12000
Sandberg loamy sand, 1 to 6 percent slopesD8B264516292w8flmn05320011:12000
Sandberg loamy coarse sand, 6 to 30 percent slopesD8E266530263392w8fnmn06719831:20000
Sandberg gravelly sandy loam, 6 to 30 percent slopes258E230730263382w8frmn06719831:20000
Radium-Sandberg-Garborg complex, 0 to 2 percent slopesI75A26492798416vx9xmn06920071:12000
Sandberg-Radium complex, 0 to 6 percent slopesI57B23342798413prpdmn06920071:12000
Sandberg gravelly sandy loam, 6 to 30 percent slopes402F4474303082w8frmn07319941:20000
Arvilla-Sandberg complex, 2 to 6 percent slopesJ31B2027114940117l1gmn08120071:12000
Sandberg-Arvilla complex, 6 to 12 percent slopesJ42C1169114951817l57mn08120071:12000
Sandberg sandy loam, 12 to 40 percent slopesJ45F609114952417l5fmn08120071:12000
Buse, moderately eroded-Sandberg complex, 12 to 18 percent slopesJ227D252114798881lnybmn08120071:12000
Sandberg-Buse-Everts complex, 12 to 40 percent slopesJ83F298991460128plmn08120071:12000
Buse-Sandberg complex, 18 to 40 percent slopesJ227F23914798891lnycmn08120071:12000
Arvilla-Sandberg sandy loams, coteau, 2 to 6 percent slopesZ176B3827653502rjd0mn08120071:12000
Renshaw-Sandberg complex, 2 to 6 percent slopesJ72B14991458128pjmn08120071:12000
Arvilla-Sandberg complex, 2 to 6 percent slopesJ31B321314862161lwjgmn08320081:12000
Sandberg-Arvilla complex, 6 to 12 percent slopesJ42C130814862171lwjhmn08320081:12000
Buse-Sandberg complex, 18 to 40 percent slopesJ227F38514862301lwjxmn08320081:12000
Buse, moderately eroded-Sandberg complex, 12 to 18 percent slopesJ227D235214862291lwjwmn08320081:12000
Sandberg sandy loam, 12 to 40 percent slopesJ45F22714862201lwjlmn08320081:12000
Sandberg sandy loam, 1 to 6 percent slopes1241B7893992082w8fpmn08719921:20000
Sandberg-Radium complex, 0 to 6 percent slopesI57B97252798932prpdmn08919941:20000
Radium-Sandberg-Garborg complex, 0 to 2 percent slopesI75A11842798947vx9xmn08919941:20000
Arvilla-Sandberg complex, 2 to 6 percent slopesJ31B1827114949617l4jmn10120081:12000
Sandberg-Arvilla complex, 6 to 12 percent slopesJ42C563114952017l59mn10120081:12000
Buse, moderately eroded-Sandberg complex, 12 to 18 percent slopesJ227D225314816591lqsgmn10120081:12000
Sandberg-Buse-Everts complex, 12 to 40 percent slopesJ83F9298890212612mn10120081:12000
Renshaw-Sandberg complex, 2 to 6 percent slopesJ72B809888991260zmn10120081:12000
Sandberg sandy loam, 12 to 40 percent slopesJ45F20114952617l5hmn10120081:12000
Sandberg-Radium complex, 0 to 6 percent slopesI57B6042799055prpdmn10719701:20000
Sandberg loamy sand, 6 to 15 percent slopesI681C1927991162sw8zmn10719701:20000
Arvilla-Sandberg complex, 6 to 12 percent slopes711C13150435906gmlhmn11119961:20000
Sandberg loamy sand, 1 to 6 percent slopesD8B737430263032w8flmn11119961:20000
Sandberg-Arvilla complex, 12 to 20 percent slopes1223D4349435570gm7nmn11119961:20000
Sandberg sandy loam, 1 to 6 percent slopes258B395930263072w8fpmn11119961:20000
Sverdrup-Sandberg complex, 2 to 6 percent slopes1221B3488435569gm7mmn11119961:20000
Sandberg-Sverdrup complex, 6 to 12 percent slopes1219C3276435568gm7lmn11119961:20000
Sandberg sandy loam, 2 to 12 percent slopes258C315030263232w8fqmn11119961:20000
Sandberg loamy sand, 2 to 12 percent slopesD8C90730263222w8fmmn11119961:20000
Arvilla-Sandberg complex, 2 to 6 percent slopes711B843435905gmlgmn11119961:20000
Sandberg loamy coarse sand, 6 to 30 percent slopesD8E72130263412w8fnmn11119961:20000
Sandberg-Radium complex, 0 to 6 percent slopesI57B2182799138prpdmn11119961:20000
Sandberg gravelly sandy loam, 6 to 30 percent slopes258E10630263402w8frmn11119961:20000
Radium-Sandberg-Garborg complex, 0 to 2 percent slopesI75A84992799220vx9xmn11320031:12000
Sandberg-Radium complex, 0 to 6 percent slopesI57B4752799203prpdmn11320031:12000
Sandberg-Buse-Everts complex, 12 to 40 percent slopesJ83F2510780524v666mn11720051:12000
Renshaw-Sandberg complex, 2 to 6 percent slopesJ72B1949780517v65zmn11720051:12000
Arvilla-Sandberg complex, 2 to 6 percent slopesJ31B340114949517l4hmn11720051:12000
Sandberg-Arvilla complex, 6 to 12 percent slopesJ42C113114951917l58mn11720051:12000
Sandberg sandy loam, 12 to 40 percent slopesJ45F24114952517l5gmn11720051:12000
Sandberg-Radium complex, 0 to 6 percent slopesI57B204872799675prpdmn11919961:20000
Sandberg loamy sand, 6 to 15 percent slopesI681C205327997392sw8zmn11919961:20000
Sandberg loamy sand, 15 to 25 percent slopesI681E166027997382sw8ymn11919961:20000
Sandberg sandy loam, 1 to 6 percent slopes258B9383522272w8fpmn11919961:20000
Sandberg sandy loam, 2 to 12 percent slopes258C2173522282w8fqmn11919961:20000
Sandberg gravelly sandy loam, 6 to 30 percent slopes258E463522302w8frmn11919961:20000
Radium-Sandberg-Garborg complex, 0 to 2 percent slopesI75A332799687vx9xmn11919961:20000
Sandberg loamy sand, 1 to 6 percent slopesD8B582130263042w8flmn12119681:20000
Sandberg gravelly sandy loam, 6 to 30 percent slopes258E425030263422w8frmn12119681:20000
Sandberg loamy coarse sand, 6 to 30 percent slopesD8E392830263432w8fnmn12119681:20000
Sandberg loamy sand, 2 to 12 percent slopesD8C328930263242w8fmmn12119681:20000
Sandberg sandy loam, 2 to 12 percent slopes258C124430263252w8fqmn12119681:20000
Sandberg sandy loam, 1 to 6 percent slopes258B108030263082w8fpmn12119681:20000
Sandberg-Radium complex, 0 to 6 percent slopesI57B16572799804prpdmn12520011:12000
Radium-Sandberg-Garborg complex, 0 to 2 percent slopesI75A02799834vx9xmn13519991:24000
Sandberg-Arvilla complex, 0 to 3 percent slopes12234925431434ggy7mn14119941:15840
Sandberg loamy sand, 1 to 6 percent slopes258B48174314702w8flmn14119941:15840
Sandberg loamy coarse sand, 6 to 30 percent slopes258E23884314722w8fnmn14119941:15840
Sandberg loamy sand, 2 to 12 percent slopes258C14794314712w8fmmn14119941:15840
Sandberg loamy sand, 2 to 12 percent slopes611C72854281712w8fmmn14519801:15840
Sandberg loamy coarse sand, 6 to 30 percent slopes611D58014281722w8fnmn14519801:15840
Sandberg sandy loam, 1 to 6 percent slopesSsB30854283752w8fpmn14919661:15840
Sandberg sandy loam, 2 to 12 percent slopesSgC11574283732w8fqmn14919661:15840
Sandberg-Radium complex, 0 to 6 percent slopesI57B72799909prpdmn14919661:15840
Arvilla-Sandberg complex, 2 to 6 percent slopesJ31B5038434811glg5mn15120001:12000
Sandberg-Arvilla complex, 6 to 12 percent slopesJ42C1236434827glgpmn15120001:12000
Sandberg gravelly sandy loam, 6 to 30 percent slopesJ45F3364348312w8frmn15120001:12000
Sandberg loamy sand, 2 to 12 percent slopes402C7174285372w8fmmn15319851:20000
Sandberg loamy coarse sand, 6 to 30 percent slopes402E4294285382w8fnmn15319851:20000
Sandberg-Radium complex, 0 to 6 percent slopesI57B102799990prpdmn16719851:20000
Sandberg-Arvilla complex, map >25, 0 to 3 percent slopes12231015435046glprmn17119981:12000
Sandberg loamy sand, 1 to 6 percent slopes258B2944337192w8flmn17119981:12000
Sandberg loamy coarse sand, 6 to 30 percent slopes258E2774337152w8fnmn17119981:12000
Sandberg loamy sand, 2 to 12 percent slopes258C974337182w8fmmn17119981:12000
Buse, moderately eroded-Sandberg complex, 12 to 18 percent slopesJ227D246214816861lqtbmn17319791:20000
Arvilla-Sandberg complex, 2 to 6 percent slopesJ31B43514816671lqsqmn17319791:20000
Buse-Sandberg complex, 18 to 40 percent slopesJ227F42014817101lqv3mn17319791:20000
Sandberg-Arvilla complex, 6 to 12 percent slopesJ42C36014816781lqt2mn17319791:20000
Sandberg sandy loam, 12 to 40 percent slopesJ45F13114817001lqtsmn17319791:20000
Arvilla-Sandberg sandy loams, coteau, 2 to 6 percent slopesZ176B17827653202rjd0sd01119951:24000
Arvilla-Sandberg sandy loams, coteau, 2 to 6 percent slopesZ176B11827129902rjd0sd03919921:20000
Arvilla-Sandberg sandy loams, coteau, 6 to 9 percent slopesZ176C7927129892rjcysd03919921:20000
Arvilla-Sandberg sandy loams, coteau, 6 to 9 percent slopesZ176C39127129342rjcysd05119771:20000
Arvilla-Sandberg sandy loams, coteau, 2 to 6 percent slopesZ176B20327129352rjd0sd05119771:20000

Map of Series Extent

Approximate geographic distribution of the SANDBERG 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 .