Official Series Description


Lab Data Summary

Aggregate lab data for the EKALAKA soil series. This aggregation is based on all pedons with a current taxon name of EKALAKA, 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 EKALAKA 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
5440A021464ND011006Ekalaka7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties46.0444444,-103.0094444
5481ND03701081ND037010Ekalaka4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties46.3305556,-101.1030556
58D40A137664ND011007Ekalaka7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties45.995,-103.9766667

Water Balance

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

Click the image to view it full size.

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.

Competing Series

Soil series competing with EKALAKA 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 EKALAKA 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 EKALAKA 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.

There are insufficient data to create the 3D flats position figure.

Soil series sharing subgroup-level classification with EKALAKA, 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-2010-09-27-16 | Morton County - 2002

    Typical pattern of soils and underlying materials in the Ekalaka-Lakota-Vebar-Desart association (Soil Survey of Morton County, North Dakota; 2002).

  2. ND-2012-02-08-05 | Grant County - September 1988

    Typical pattern of soils and parent material in the Ekalaka-Desart-Lemert association (Soil Survey of Grant County, North Dakota; September 1988).

  3. SD-2012-03-15-08 | Corson County - July 1995

    Pattern of soils and parent material in the Vebar association (Soil Survey of Corson County, SD; 1995).

Map Units

Map units containing EKALAKA 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
Ekalaka-Yegen fine sandy loams, 0 to 6 percent slopesE1231B369925257322r4h9nd00119831:20000
Ekalaka-Lakota fine sandy loams, 0 to 6 percent slopesE1239B472755642cdkpnd00119831:20000
Ekalaka-Parshall-Desart fine sandy loams, 0 to 6 percent slopesE1247B156117151741vzsqnd00719981:24000
Desart-Ekalaka-Telfer complex, 0 to 6 percent slopesE1227B142758430cdk7nd00719981:24000
Desart-Ekalaka-Telfer complex, 0 to 6 percent slopesE1227B89942563546cdk7nd01119691:20000
Ekalaka-Desart fine sandy loams, 0 to 6 percent slopesEdB850199281812b3dnd01119691:20000
Blown-out land-Ladner-Ekalaka complex, 0 to 15 percent slopesBk613499279112b2jnd01119691:20000
Ekalaka-Zeona-Ladner loamy fine sands, 0 to 6 percent slopesEmB593699282012b3gnd01119691:20000
Ekalaka-Seroco-Lakota loamy fine sands, 0 to 6 percent slopesE1237B402125635492r4hcnd01119691:20000
Ekalaka-Ladner complex, 6 to 15 percent slopesElC146099281912b3fnd01119691:20000
Beisigl, severely eroded-Lakota-Ekalaka complex, 0 to 15 percent slopesE1249D48825635242r4hfnd01119691:20000
Ekalaka-Lakota fine sandy loams, 0 to 6 percent slopesE1239B72758448cdkpnd01119691:20000
Ekalaka-Yegen fine sandy loams, 0 to 6 percent slopesE1231B90227071962r4h9nd02519811:20000
Ekalaka-Yegen fine sandy loams, 0 to 6 percent slopesE1231B59926618332r4h9nd02919791:20000
Desart-Ekalaka-Telfer complex, 0 to 6 percent slopesE1227B79202525865cdk7nd03719851:20000
Ekalaka-Lakota fine sandy loams, 0 to 6 percent slopesE1239B65552525866cdkpnd03719851:20000
Lakota-Ekalaka-Sham, high precipitation, gullied complex, 0 to 9 percent slopesE1243C10952759639cdkxnd03719851:20000
Rhoades-Daglum-Ekalaka fine sandy loams, 0 to 9 percent slopesE0457C272759631cdp6nd03719851:20000
Ekalaka-Yegen fine sandy loams, 0 to 6 percent slopesE1231B127596382r4h9nd03719851:20000
Ekalaka-Yegen fine sandy loams, 0 to 6 percent slopesE1231B71625257912r4h9nd04119861:20000
Desart-Janesburg-Ekalaka complex, 0 to 6 percent slopesE1228B4602715050d33xnd05320031:24000
Ekalaka-Lakota fine sandy loams, 0 to 6 percent slopesE1239B115632699162cdkpnd05919981:20000
Lakota-Ekalaka-Sham, high precipitation, gullied complex, 0 to 9 percent slopesE1243C63452699176cdkxnd05919981:20000
Desart-Ekalaka-Telfer complex, 0 to 6 percent slopesE1227B57172699160cdk7nd05919981:20000
Rhoades-Daglum-Ekalaka fine sandy loams, 0 to 9 percent slopesE0457C44122699202cdp6nd05919981:20000
Ekalaka-Lakota fine sandy loams, 0 to 6 percent slopesE1239B275232699081cdkpnd08519921:24000
Desart-Ekalaka-Telfer complex, 0 to 6 percent slopesE1227B224902699077cdk7nd08519921:24000
Lakota-Ekalaka-Sham, high precipitation, gullied complex, 0 to 9 percent slopesE1243C191342699100cdkxnd08519921:24000
Ekalaka-Yegen fine sandy loams, 0 to 6 percent slopesE1231B186727073942r4h9nd08719741:20000
Desart-Ekalaka-Telfer complex, 0 to 6 percent slopesE1227B18632707393cdk7nd08719741:20000
Ekalaka-Parshall-Desart fine sandy loams, 0 to 6 percent slopesE1247B41017134961vzsqnd08919651:20000
Ekalaka very fine sandy loam, 0 to 6 percent slopesEkA2089356154cylvsd03119861:24000
Telfer-Ekalaka complex, 0 to 6 percent slopesTeB1420356219cynysd03119861:24000
Glenross-Ekalaka fine sandy loamsGk1146356164cym5sd03119861:24000
Ekalaka-Parshall complex, 0 to 6 percent slopesEpB1045356155cylwsd03119861:24000
Ekalaka fine sandy loam, 0 to 6 percent slopesEkA5773354188cwkfsd04119721:24000
Parshall-Ekalaka fine sandy loamsPe2114354220cwlgsd04119721:24000
Ekalaka fine sandy loam, 6 to 9 percent slopesEkC956354189cwkgsd04119721:24000

Map of Series Extent

Approximate geographic distribution of the EKALAKA 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 .