Official Series Description


Lab Data Summary

Aggregate lab data for the URNESS soil series. This aggregation is based on all pedons with a current taxon name of URNESS, 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 URNESS were used in the calculation. Source: KSSL snapshot . Methods used to assemble the KSSL snapshot used by SoilWeb / SDE

There are insufficient data to create the lab data summary figure.


Water Balance

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

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Competing Series

Soil series competing with URNESS 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 URNESS 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 URNESS 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.

Soil series sharing subgroup-level classification with URNESS, 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-2010-09-08-20 | Otter Tail County - 2001

    Typical pattern of soils and parent material in the Chapett-Sisseton-Friberg association (Soil Survey of Otter Tail County, Minnesota; 2001).

  2. MN-2010-09-08-22 | Otter Tail County - 2001

    Typical pattern of soils and parent material in the Forman-Buse-Peever association (Soil Survey of Otter Tail County, Minnesota; 2001).

Map Units

Map units containing URNESS 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
Quam, Cathro, and Urness soils, frequently ponded, 0 to 1 percent slopes122727823974452w8fgmn00519941:20000
Urness mucky silty clay loam, occasionally ponded, 0 to 1 percent slopes3357653975132w0m0mn00519941:20000
Quam, Cathro, and Urness soils, frequently ponded, 0 to 1 percent slopesJ43A118930264492w8fgmn02319801:15840
Urness mucky silty clay loam, occasionally ponded, 0 to 1 percent slopesJ41A10024230522w0m0mn02319801:15840
Quam, Cathro, and Urness soils, frequently ponded, 0 to 1 percent slopes105591133569362w8fgmn02719801:20000
Urness mucky silt loam, 0 to 1 percent slopesI837A78727981442sw9kmn02719801:20000
Urness mucky silty clay loam, occasionally ponded, 0 to 1 percent slopes3355983569562w0m0mn02719801:20000
Quam, Cathro, and Urness soils, frequently ponded, 0 to 1 percent slopesMh73543972962w8fgmn04119701:12000
Urness mucky silty clay loam, occasionally ponded, 0 to 1 percent slopesUp56783973312w0m0mn04119701:12000
Urness mucky silt loam, peaty subsoil variantUs942397332fbg5mn04119701:12000
Quam, Cathro, and Urness soils, frequently ponded, 0 to 1 percent slopes105329363980212w8fgmn05119741:20000
Urness mucky silty clay loam, occasionally ponded, 0 to 1 percent slopes3352403980342w0m0mn05119741:20000
Quam, Cathro, and Urness soils, frequently ponded, 0 to 1 percent slopesJ43A739430264502w8fgmn06719831:20000
Urness silt loam335204185903220dgsmn08320081:12000
Quam, Cathro, and Urness soils, frequently ponded, 0 to 1 percent slopes180470713992122w8fgmn08719921:20000
Urness mucky silty clay loam, occasionally ponded, 0 to 1 percent slopes3354293992252w0m0mn08719921:20000
Quam, Cathro, and Urness soils, frequently ponded, 0 to 1 percent slopesMh10743572522w8fgmn10719701:20000
Quam, Cathro, and Urness soils, frequently ponded, 0 to 1 percent slopes1227125704355712w8fgmn11119961:20000
Urness mucky silty clay loam, occasionally ponded, 0 to 1 percent slopes33532134357262w0m0mn11119961:20000
Urness mucky silt loam, 0 to 1 percent slopesI837A7627991602sw9kmn11119961:20000
Quam, Cathro, and Urness soils, frequently ponded, 0 to 1 percent slopes1055199629474172w8fgmn11919961:20000
Quam, Cathro, and Urness soils, frequently ponded, 0 to 1 percent slopesMk58404013712w8fgmn12119681:20000
Urness mucky silty clay loam, occasionally ponded, 0 to 1 percent slopesBh14724013242w0m0mn12119681:20000
Quam, Cathro, and Urness soils, frequently ponded, 0 to 1 percent slopes105533004280702w8fgmn14519801:15840
Urness mucky silty clay loam, occasionally ponded, 0 to 1 percent slopes3521674281272w0m0mn14519801:15840
Quam, Cathro, and Urness soils, frequently ponded, 0 to 1 percent slopesMh10934283562w8fgmn14919661:15840
Urness mucky silty clay loam, occasionally ponded, 0 to 1 percent slopesBh3954283182w0m0mn14919661:15840
Quam, Cathro, and Urness soils, frequently ponded, 0 to 1 percent slopesJ43A45804348282w8fgmn15120001:12000
Urness mucky silty clay loam, sandy substratum, ponded, 0 to 1 percent slopesJ59A4104434852glhhmn15120001:12000
Urness mucky silty clay loam, occasionally ponded, 0 to 1 percent slopesJ41A36344347922w0m0mn15120001:12000
Urness mucky silt loam, 0 to 1 percent slopesI837A420828004642sw9kmn16719851:20000
Quam, Cathro, and Urness soils, frequently ponded, 0 to 1 percent slopes10555483573902w8fgmn16719851:20000
Urness mucky silty clay loam, occasionally ponded, 0 to 1 percent slopes335613574152w0m0mn16719851:20000

Map of Series Extent

Approximate geographic distribution of the URNESS 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 .