Official Series Description


Lab Data Summary

Aggregate lab data for the RAGO soil series. This aggregation is based on all pedons with a current taxon name of RAGO, 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 RAGO 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
67B90P003289CO063273Rago7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties39.5388908,-102.9946747
67B89P056089CO063273ARago4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties39.538887,-102.9941635
7290P078190CO095001Rago7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties40.6044388,-102.2054901
7240A3909S1954CO063003Rago5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties39.1288872,-102.2975006
n/a02N0412S2001CO075003Rago7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Propertiesn/a

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the RAGO 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 RAGO 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 RAGO 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 RAGO 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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Competing Series

Soil series competing with RAGO 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 RAGO 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 RAGO 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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There are insufficient data to create the 3D flats position figure.

Soil series sharing subgroup-level classification with RAGO, 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).

  2. CO-2011-05-27-13 | Phillips County - 1971

    Cross section of Phillips County showing relationship of major soils to parent materials (Soil Survey of Phillips County, Colorado; 1971).

Map Units

Map units containing RAGO 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
Rago silt loam, dry, 0 to 1 percent slopesRaA884942752zcs1co01119651:15840
Rago-Weld silt loams, 0 to 2 percent slopes71203019686437snco06319961:24000
Rago silt loam, 0 to 2 percent slopes, occasionally flooded70131219686337smco06319961:24000
Rago silt loam, 0 to 2 percent slopes, rarely flooded175144461052563jjcco07320011:24000
Rago silt loam, dry, 0 to 2 percent slopes, rarely flooded1766841052573jjdco07320011:24000
Rago loam, 0 to 3 percent slopes9275749945792tlq2co07519741:24000
Platner-Rago-Dacono loams91255309457835dxco07519741:24000
Rago clay loam, 0 to 2 percent slopes931471945802tlq5co07519741:24000
Rago loam, 0 to 3 percent slopesRa44501104602tlq2co08719651:24000
Rago and Kuma loamsRa1794269478435mkco09519711:20000
Rago and kuma silt loams, 0 to 3 percent slopesRaB776749495435t1co11519691:15840
Rago and kuma silt loams, 3 to 5 percent slopesRaC20929495535t2co11519691:15840
Rago silt loam, 0 to 2 percent slopes5895427950212tlq4co12119821:24000
Rago clay loam, occasional overflow, 0 to 2 percent slopes591172950222tlq6co12119821:24000
Rago loam, 0 to 3 percent slopes373592630403242tlq2co12519761:24000
Rago clay loam, occasional overflow, 0 to 2 percent slopes384551950822tlq6co12519761:24000
Muzzler family, stony-Rago family association, 15 to 60 percent slopes1112386512363k64vut6461:24000
Rago family, 1 to 25 percent slopes374612512394k65vut6461:24000

Map of Series Extent

Approximate geographic distribution of the RAGO 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 .