Official Series Description


Lab Data Summary

Aggregate lab data for the ANTIGO soil series. This aggregation is based on all pedons with a current taxon name of ANTIGO, 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 ANTIGO 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
90A90P054689WI013001Antigo6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties45.6877785,-92.0802765
90A40A1544S1960WI119003ANTIGO5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties45.2988892,-90.7841644
90A97P0283S1995MN065019Antigo6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties45.8827705,-93.4666138
90B99P0230S1979WI067088Antigo4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties45.1633339,-89.1188889
90B81P0822S1981WI067340ANTIGO7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties45.1330566,-89.1819458
90B83P0170S1982WI017005Antigo5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties44.95623,-90.94455
90B92P0439S1991WI107006Antigo6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties45.3494453,-91.5366669
90B99P0229S1998WI067001Antigo6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties45.2008324,-89.1411819

Sibling Summary

Siblings are those soil series that occur together in map units, in this case with the ANTIGO 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 ANTIGO 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 ANTIGO 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. 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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Competing Series

Soil series competing with ANTIGO 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 ANTIGO series and competing. Series are sorted according to hierarchical clustering of median values. Source: SSURGO map unit geometry and 1981-2010, 800m PRISM data .

There are insufficient data to create the annual climate figure.

Geomorphic description summaries for the ANTIGO 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 .

There are insufficient data to create the 2D hillslope position figure.

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.

Series Association

Two views depicting soil series that occur within map units containing the ANTIGO series as a major component. Series association is a function of how frequently series-type components co-occur, weighted by component percentage. This summary should generate structures that are related to soil-landscape concepts that were used to construct map units containing the ANTIGO series. Both views are approximations of the multi-dimensional relationship between components. Note that these diagrams give only partial information on the relationships between components other than ANTIGO. Source: SSURGO snapshot .

Graph representation: each circle (vertex) is a component, lines (edges) connect components that have been mapped together, colors define groups of components that frequently co-occur, vertex proximity is proportional to co-occurrence as weighted by component percentage. Dark lines connect vertices to the queried soil series, grey lines connect other vertices.

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Dendrogram representation: branch height (relative to the left-side of the figure) is proportional to co-occurrence as weighted by component percentage, clusters of components are highlighted in this view.

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Soil series sharing subgroup-level classification with ANTIGO, 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 ANTIGO 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
Antigo-Chetek complex, 2 to 8 percent slopesC23B741914001227nzmn00920071:12000
Antigo silt loam, 0 to 2 percent slopesC49A631914000227nymn00920071:12000
Antigo silt loam, 1 to 8 percent slopes49B1446396872f9zbmn03719801:15840
Antigo-Chetek complex, 2 to 8 percent slopesC23B921316734701t5cxmn06520061:12000
Antigo silt loam, 0 to 2 percent slopesC49A755516734921t5dmmn06520061:12000
Antigo-Rock outcrop complex, 3 to 15 percent slopesC141C18916735641t5gymn06520061:12000
Antigo-Chetek complex, 2 to 8 percent slopesC23B245916763711t8dhmn09520061:12000
Antigo silt loam, 0 to 2 percent slopesC49A103016763931t8f6mn09520061:12000
Antigo silt loam, 2 to 6 percent slopes49B19616771842tnz8mn12319781:15840
Antigo silt loam, 6 to 15 percent slopes49C9116771852tnz9mn12319781:15840
Antigo silt loam, 15 to 35 percent slopes49D6316771862tnzbmn12319781:15840
Antigo silt loam, 0 to 2 percent slopes491916771832tnz7mn12319781:15840
Antigo silt loam, 2 to 6 percent slopes49B1582616770492tnz8mn16319781:15840
Antigo silt loam, 0 to 2 percent slopes49914116770482tnz7mn16319781:15840
Antigo silt loam, 6 to 15 percent slopes49C504016770502tnz9mn16319781:15840
Antigo silt loam, 15 to 35 percent slopes49D105416770512tnzbmn16319781:15840
Antigo silt loam, 2 to 6 percent slopes43B2084352762tnz8wi01320041:12000
Antigo silt loam, 6 to 15 percent slopes43C464352782tnz9wi01320041:12000
Antigo silt loam, 2 to 6 percent slopesAnB15684214822tnz8wi01719851:15840
Antigo silt loam, 6 to 15 percent slopesAnC210164214832tnz9wi01719851:15840
Antigo silt loam, 6 to 15 percent slopes43C217810572tnz9wi03120051:12000
Antigo silt loam, 2 to 6 percent slopesAoB405784210442tnz8wi06719831:20000
Antigo silt loam, 0 to 2 percent slopesAoA400654210432tnz7wi06719831:20000
Antigo silt loam, 6 to 15 percent slopesAoC400214210452tnz9wi06719831:20000
Antigo silt loam, 2 to 6 percent slopesAoB56584316062tnz8wi06919931:20000
Antigo silt loam, 6 to 15 percent slopesAoC41474316072tnz9wi06919931:20000
Pence-Antigo complex, 6 to 15 percent slopesPcC2000431642gh4ywi06919931:20000
Antigo silt loam, 2 to 6 percent slopesRsB32164314182tnz8wi07319981:20000
Antigo silt loam, 0 to 2 percent slopesRsA14624314172tnz7wi07319981:20000
Antigo silt loam, 2 to 6 percent slopesAtB24913957792tnz8wi07819981:12000
Antigo silt loam, 2 to 6 percent slopesAtB349404211432tnz8wi09519781:15840
Antigo silt loam, 0 to 2 percent slopesAtA134474211422tnz7wi09519781:15840
Antigo silt loam, 6 to 15 percent slopesAtC266994211442tnz9wi09519781:15840
Santiago-Antigo silt loams, 2 to 6 percent slopesScB5970421219g49qwi09519781:15840
Santiago-Antigo silt loams, 6 to 12 percent slopesScC3319421220g49rwi09519781:15840
Santiago-Antigo silt loams, 12 to 20 percent slopesScD613421221g49swi09519781:15840
Antigo silt loam, 6 to 15 percent slopes43C30566276042tnz9wi09920061:12000
Freeon, very stony-Antigo complex, 6 to 15 percent slopes545C2743627543p20bwi09920061:12000
Antigo silt loam, 2 to 6 percent slopes43B11756276032tnz8wi09920061:12000
Antigo silt loam, 15 to 35 percent slopes43D5076273342tnzbwi09920061:12000
Crystal Lake-Freeon, very stony-Antigo complex, 6 to 15 percent slopes3863C43914827561lrxvwi09920061:12000
Antigo silt loam, 2 to 6 percent slopes43B42236250162tnz8wi10720061:12000
Antigo silt loam, 6 to 15 percent slopes43C29756250172tnz9wi10720061:12000
Freeon, very stony-Antigo complex, 6 to 15 percent slopes545C1554625082nzfywi10720061:12000
Antigo silt loam, 15 to 35 percent slopes43D8706250182tnzbwi10720061:12000
Antigo silt loam, 2 to 6 percent slopesAoB97894221062tnz8wi10919751:15840
Santiago-Antigo complex, 6 to 12 percent slopes, erodedScC25824422194g5b5wi10919751:15840
Onamia-Antigo complex, 6 to 12 percent slopes, erodedOnC24823422166g598wi10919751:15840
Onamia-Antigo complex, 12 to 25 percent slopes, erodedOnD21666422167g599wi10919751:15840
Antigo silt loam, 0 to 2 percent slopesAoA16654221052tnz7wi10919751:15840
Santiago-Antigo complex, 12 to 25 percent slopes, erodedScD21342422195g5b6wi10919751:15840
Antigo silt loam, 6 to 15 percent slopes43C86226253492tnz9wi11320061:12000
Antigo silt loam, 2 to 6 percent slopes43B72106253482tnz8wi11320061:12000
Freeon, very stony-Antigo complex, 6 to 15 percent slopes545C3046625839p07cwi11320061:12000
Antigo silt loam, 15 to 35 percent slopes43D27706253502tnzbwi11320061:12000
Antigo silt loam, 2 to 6 percent slopesAtB12324226512tnz8wi11519811:15840
Crystal Lake-Freeon, very stony-Antigo complex, 6 to 15 percent slopes3863C2388579853mgcywi11920021:12000
Freeon, very stony-Antigo complex, 6 to 15 percent slopes545C2216435136glsnwi11920021:12000
Antigo silt loam, 6 to 15 percent slopes43C17914209852tnz9wi11920021:12000
Antigo silt loam, 2 to 6 percent slopes43B7264209842tnz8wi11920021:12000
Antigo silt loam, 15 to 35 percent slopes43D3144209862tnzbwi11920021:12000
Antigo silt loam, 2 to 6 percent slopes43B36224354622tnz8wi12920021:12000
Antigo silt loam, 6 to 15 percent slopes43C19254354632tnz9wi12920021:12000
Antigo silt loam, 15 to 35 percent slopes43D15724354642tnzbwi12920021:12000
Antigo silt loam, 1 to 3 percent slopesAnA233426424g9qmwi14119711:20000

Map of Series Extent

Approximate geographic distribution of the ANTIGO 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 .