Official Series Description


Lab Data Summary

Aggregate lab data for the ECKLEY soil series. This aggregation is based on all pedons with a current taxon name of ECKLEY, 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 ECKLEY 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
7283P0431S1981NE007002Eckley5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties41.4438896,-103.7988892
n/a00P0765S2000CO123001Eckley6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Propertiesn/a

Water Balance

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

Soil series sharing subgroup-level classification with ECKLEY, 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. CO-2011-05-27-12 | Phillips County - 1971

    Typical landscape of the Rago-Platner-Kuma association showing the major soils and the minor Wages, Eckley, and Dix soils (Soil Survey of Phillips County, Colorado; 1971).

Map Units

Map units containing ECKLEY 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
Ascalon-Eckley complex, 5 to 20 percent slopes53229943403557co01719851:24000
Eckley-Wages complex, 4 to 20 percent slopes22128839681337r0co06319961:24000
Ascalon-Eckley loams, 1 to 5 percent slopes810839679737qhco06319961:24000
Dix-Eckley complex, 5 to 25 percent slopes25186809450535bkco07519741:24000
Julesburg-Eckley complex, 3 to 9 percent slopes4976409453135cdco07519741:24000
Altvan-Eckley sandy loams, 3 to 5 percent slopes453479452135c2co07519741:24000
Altvan-Eckley sandy loams, 5 to 9 percent slopes548359453235cfco07519741:24000
Wages-Eckley-Dix complex, 5 to 25 percent slopesWeE81459479135msco09519711:20000
Platner-Eckley association, 3 to 5 percent slopesPeC6949478235mhco09519711:20000
Eckley-Chappell complex, 9 to 20 percent slopesEcE333099493335scco11519691:15840
Eckley-Orsa gravelly sandy loams, 5 to 15 percent slopes2046099498035twco12119821:24000
Eckley gravelly sandy loam, 3 to 7 percent slopes1527609505735xcco12519761:24000
Eckley-Dix-Blakeland complex, 6 to 20 percent slopes2689999511735z9co61719801:24000
Eckley sandy clay loam, 6 to 9 percent slopes2514769511635z8co61719801:24000
Eckley sandy clay loam, 0 to 6 percent slopes2413329511535z7co61719801:24000
Eckley gravelly sandy loam, 3 to 30 percent slopes1577853216924791tt53ne00719881:20000
Altvan-Eckley complex, 3 to 9 percent slopes1508633816924552x2x5ne00719881:20000
Eckley and Altvan soils, 9 to 50 percent slopes15781922281422dskkne00719881:20000
Altvan-Eckley-Satanta complex, 3 to 9 percent slopes150927922196962dhs3ne03319891:20000
Altvan-Eckley complex, 3 to 9 percent slopes150825522196792x2x5ne03319891:20000
Altvan-Eckley-Tassel complex, 3 to 9 percent slopes151011322196802dhrlne03319891:20000
Eckley and Altvan soils, 9 to 50 percent slopes15781922196812dhrmne03319891:20000
Altvan-Eckley-Satanta complex, 3 to 9 percent slopes15091963116987951v0qvne04920001:24000
Altvan-Eckley-Satanta complex, 3 to 9 percent slopes15096222195782dhn9ne10119901:20000
Altvan-Eckley complex, 3 to 9 percent slopes15086005816925322x2x5ne10520041:24000
Eckley and Altvan soils, 9 to 50 percent slopes15781750516925421tt74ne10520041:24000
Altvan-Eckley-Tassel complex, 3 to 9 percent slopes15101477616925341tt6wne10520041:24000
Altvan-Eckley-Satanta complex, 3 to 9 percent slopes1509322195712dhn2ne13519871:20000
Schamber-Eckley complex, 9 to 40 percent slopesSmE5541355153cxkksd04719801:24000
Eckley loam, 0 to 9 percent slopesEaC1684355104cxhzsd04719801:24000
Schamber-Eckley complex, 9 to 40 percent slopesP454E94727331562rxvcsd04719801:24000
Eckley loam, 0 to 9 percent slopesP118C20227331282qt2lsd04719801:24000

Map of Series Extent

Approximate geographic distribution of the ECKLEY 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 .