Official Series Description


Lab Data Summary

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

Click the image to view it full size.

Pedons used in the lab summary:

MLRALab IDPedon IDTaxonnameCINSSL / NASIS ReportsLink To SoilWeb GMap
5602N0764S2001ND077008Antler8Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties46.2010841,-96.6802521

Water Balance

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

Click the image to view it full size.



Click the image to view it full size.

Sibling Summary

Siblings are those soil series that occur together in map units, in this case with the ANTLER series. Sketches are arranged according to their subgroup-level taxonomic structure. Source: SSURGO snapshot , parsed OSD records and snapshot of SC database .

Click the image to view it full size.

Select annual climate data summaries for the ANTLER series and siblings. Series are sorted according to hierarchical clustering of median values. Source: SSURGO map unit geometry and 1981-2010, 800m PRISM data .

Click the image to view it full size.

Geomorphic description summaries for the ANTLER 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 .

Click the image to view it full size.

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.

Click the image to view it full size.

Competing Series

Soil series competing with ANTLER share the same family level classification in Soil Taxonomy. Source: parsed OSD records and snapshot of the SC database .

Click the image to view it full size.

Select annual climate data summaries for the ANTLER series and competing. Series are sorted according to hierarchical clustering of median values. Source: SSURGO map unit geometry and 1981-2010, 800m PRISM data .

Click the image to view it full size.

Geomorphic description summaries for the ANTLER 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 .

Click the image to view it full size.

There are insufficient data to create the 3D hills figure.

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 ANTLER, 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. ND-2012-02-08-02 | Grand Forks County - May 1981

    Typical pattern of soils and parent material in the Antler-Gilby-Svea association (Soil Survey of Grand Forks County, North Dakota; May 1981).

Map Units

Map units containing ANTLER 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
Antler-Mustinka complex, 0 to 2 percent slopesI397A1231827981992wfh0mn05119741:20000
Antler clay loam, 0 to 2 percent slopesI405A30227982002mbq5mn05119741:20000
Antler silt loam, 0 to 2 percent slopesI156A327827990822mb9gmn10719701:20000
Antler-Mustinka complex, 0 to 2 percent slopesI397A232627991492wfh0mn11119961:20000
Antler clay loam, 0 to 2 percent slopesI405A140727991502mbq5mn11119961:20000
Antler clay loam, 0 to 2 percent slopesI405A67327999192mbq5mn14919661:15840
Antler-Mustinka complex, 0 to 2 percent slopesI397A927999172wfh0mn14919661:15840
Antler-Mustinka complex, 0 to 2 percent slopesI397A3496127999452wfh0mn15519861:20000
Antler clay loam, 0 to 2 percent slopesI405A1198827999582mbq5mn15519861:20000
Antler clay loam, 0 to 2 percent slopesI405A6942928004302mbq5mn16719851:20000
Antler-Mustinka complex, 0 to 2 percent slopesI397A3742328000102wfh0mn16719851:20000
Antler-Wyard loams, 0 to 2 percent slopesI504A1013524945731tbnhnd01719831:20000
Antler-Mustinka complex, 0 to 2 percent slopesI397A38724945712wfh0nd01719831:20000
Antler clay loam, 0 to 2 percent slopesI405A33224945672mbq5nd01719831:20000
Antler silty clay loam, moderately saline, 0 to 2 percent slopesI477A6624945701tbm5nd01719831:20000
Antler silt loam, 0 to 2 percent slopesI156A3066126425762mb9gnd03519801:20000
Antler-Mustinka silt loams, 0 to 2 percent slopesI199A2958026425692l6w9nd03519801:20000
Antler silty clay loam, moderately saline, 0 to 2 percent slopesI477A2485726425201tbm5nd03519801:20000
Antler, moderately saline-Mustinka silty clay loams, 0 to 2 percent slopesI157A450726425772mb9hnd03519801:20000
Antler clay loam, moderately saline, 0 to 2 percent slopesI563A726425882mbmcnd03519801:20000
Antler clay loam, 0 to 2 percent slopesI405A326430292mbq5nd06719721:20000
Antler-Mustinka complex, 0 to 2 percent slopesI397A3165024945722wfh0nd07720051:12000
Antler clay loam, 0 to 2 percent slopesI405A461824945682mbq5nd07720051:12000
Antler silt loam, 0 to 2 percent slopesI156A70426411222mb9gnd07720051:12000
Antler-Winger silt loams, 0 to 2 percent slopesI613A1326409952mdc6nd07720051:12000
Antler clay loam, 0 to 2 percent slopesI405A243626414202mbq5nd09119911:20000
Antler clay loam, moderately saline, 0 to 2 percent slopesI563A141326414142mbmcnd09119911:20000
Antler, moderately saline-Mustinka silty clay loams, 0 to 2 percent slopesI157A526414092mb9hnd09119911:20000
Antler-Mustinka complex, 0 to 2 percent slopesI397A1476026424542wfh0nd09719741:20000
Antler-Mustinka silt loams, 0 to 2 percent slopesI199A347326424532l6w9nd09719741:20000
Antler, moderately saline-Mustinka clay loams, 0 to 2 percent slopesI197A196026424552l6wcnd09719741:20000
Antler clay loam, 0 to 2 percent slopesI405A1924945692mbq5nd09719741:20000
Antler clay loam, 0 to 2 percent slopesI405A136626429202mbq5nd09919671:20000
Antler clay loam, 0 to 2 percent slopes, very stonyI391A60626428882mb9fnd09919671:20000
Antler silt loam, 0 to 2 percent slopesI156A274528002132mb9gsd10919771:20000
Antler-Winger silt loams, 0 to 2 percent slopesI613A123628002212mdc6sd10919771:20000
Antler-Mustinka silt loams, 0 to 2 percent slopesI199A95328002122l6w9sd10919771:20000
Antler-Mustinka complex, 0 to 2 percent slopesI397A728001862wfh0sd10919771:20000
Antler clay loam, 0 to 2 percent slopesI405A128001852mbq5sd10919771:20000

Map of Series Extent

Approximate geographic distribution of the ANTLER 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 .