Official Series Description


Lab Data Summary

Aggregate lab data for the RHONE soil series. This aggregation is based on all pedons with a current taxon name of RHONE, 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 RHONE 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 RHONE 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 RHONE 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 RHONE 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 RHONE 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 RHONE 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 RHONE 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 RHONE 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.

Click the image to view it full size.

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 RHONE, 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-2011-05-31-02 | Rio Blanco Area - 1982

    Typical pattern of soils in general map unit 11 (Soil Survey of Rio Blanco Area, Colorado; 1982).

  2. CO-2012-05-09-07 | Rio Blanco County Area - May 1982

    Typical pattern of soils in general map unit 11 (Soil Survey of Rio Blanco County Area, Colorado; May 1982).

Map Units

Map units containing RHONE 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
Leaps-Rhone families, complex, 10 to 35 percent slopes, landslides5830600509358k30xco6471:24000
Parachute-Irigul-Rhone association, 25 to 50 percent slopes MLRA 48A1783265095432w4z7co66019941:24000
Parachute-Irigul-Rhone association, 25 to 50 percent slopes MLRA 48A56910804967192w4z7co68219861:24000
Parachute-Rhone loams, 5 to 30 percent slopes579598496720jnw7co68219861:24000
Parachute-Rhone loams, 5 to 30 percent slopes5338100496796jnypco68319771:24000
Rhone loam, 5 to 30 percent slopes607800496804jnyyco68319771:24000
Rhone loam, 30 to 70 percent slopes615300496805jnyzco68319771:24000
Jerry-Thornburgh-Rhone complex, 8 to 65 percent slopes626448496906jp27co68419841:24000
Rhone-Northwater-Lamphier loams, 3 to 50 percent slopes1005277496823jnzkco68419841:24000
Gothic-Rhone-Namela complex, 5 to 25 percent slopes493267496891jp1rco68419841:24000
Hapgood-Rhone-Quander loams, 20 to 65 percent slopes572364496900jp21co68419841:24000
Gothic-Rhone-Namela complex, 25 to 65 percent slopes50904496893jp1tco68419841:24000
Jerry-Thornburgh-Rhone complex, 8 to 65 percent slopes4540164496996jp54co68519791:24000
Parachute-Rhone loams, 5 to 30 percent slopes5912979497011jp5mco68519791:24000
Blakabin-Rhone-Waybe complex, 5 to 50 percent slopes912357497045jp6qco68519791:24000
Rhone loam, 30 to 75 percent slopes7611623497030jp67co68519791:24000
Rhone-Northwater-Lamphier loams, 3 to 50 percent slopes779316497031jp68co68519791:24000
Rhone family-Mult family, very stony complex, 2 to 8 percent slopes208C1117791265vkcput6511:24000

Map of Series Extent

Approximate geographic distribution of the RHONE 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 .