Official Series Description


Lab Data Summary

Aggregate lab data for the ANGUS soil series. This aggregation is based on all pedons with a current taxon name of ANGUS, 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 ANGUS 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
10340A1681S1960MN171001Angus6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties45.2569351,-93.9069061
10340A1682S1960MN171002Angus6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties45.1736031,-93.9210739

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the ANGUS 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 ANGUS 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 ANGUS 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 ANGUS 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 ANGUS 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 ANGUS 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 ANGUS 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 ANGUS, 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-2010-09-13-04 | Wright County -

    Typical pattern of soils and parent material in the Angus-Le Sueur-Cordova association (Soil Survey of Wright County, Minnesota).

  2. MN-2010-09-13-06 | Wright County -

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

  3. 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 ANGUS 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
Angus loam, 2 to 6 percent slopes1236B342014285092syrqia18720061:12000
Angus-Urban land complex, 2 to 5 percent slopes4235B61816123211r3rcia18720061:12000
Angus loam, 6 to 10 percent slopes1236C58014534922syrria18720061:12000
Angus loam, 2 to 6 percent slopes1236B772824624802syrqia19520121:12000
Angus loam, 5 to 9 percent slopes, moderately eroded1236C2396324625542nnh7ia19520121:12000
Angus loam, 2 to 5 percent slopes, moderately eroded1236B2142324624832nndyia19520121:12000
Angus loam, 6 to 10 percent slopes1236C79024625072syrria19520121:12000
Angus loam, 2 to 6 percent slopesL37B254594527702syrqmn05320011:12000
Angus-Kilkenny complex, 2 to 6 percent slopesL40B6800452773h64lmn05320011:12000
Angus-Moon complex, 2 to 5 percent slopesL60B1440434672gl9pmn05320011:12000
Angus-Malardi complex, 2 to 6 percent slopesL17B906434671gl9nmn05320011:12000
Angus loam, 2 to 6 percent slopes1362B144674295592syrqmn13119961:12000
Angus-Kilkenny complex, 2 to 6 percent slopes1408B1743429568gf01mn13119961:12000
Angus-Kilkenny complex, 2 to 6 percent slopesL40B6354455481h8yymn16120011:12000
Angus-Le Sueur complex, 1 to 6 percent slopes1901B596254350942vvgsmn17119981:12000
Angus loam, 2 to 6 percent slopes1362B276964350822syrqmn17119981:12000
Angus-Cordova complex, 0 to 5 percent slopes1094B12279435028glp5mn17119981:12000
Angus-Malardi complex, 2 to 6 percent slopes1087B2587435030glp7mn17119981:12000
Angus fine sandy loam, 2 to 5 percent slopes1036B426434997gln5mn17119981:12000
Angus-Kilkenny complex, 2 to 6 percent slopes1408B171435061glq7mn17119981:12000

Map of Series Extent

Approximate geographic distribution of the ANGUS 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 .