Official Series Description


Lab Data Summary

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

Competing Series

Soil series competing with COMODORE 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 COMODORE 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 COMODORE 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.

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

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

Soil series sharing subgroup-level classification with COMODORE, 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-2011-05-31-04 | Saguache County Area - 1984

    Pattern of soils in the Dune land map unit and soils in the Comodore-Uracca-Rock outcrop map (Soil Survey of Saguache County Area, Colorado; 1984).

Map Units

Map units containing COMODORE 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
Comodore-Uracca-Rock outcrop complex, 5 to 65 percent slopesCuF3124014290941jz2tco02320091:24000
Comodore extremely rocky loam, 40 to 150 percent slopesCmF3786498530jqrmco63219681:24000
Comodore-Rock outcrop complex, 40 to 65 percent slopes1324621498443jqntco63319811:24000
Comodore very stony loam, 25 to 65 percent slopes129047498442jqnsco63319811:24000
Comodore family-Rock outcrop complex, 35 to 65 percent slopes625S9940500967jt97co6341:24000
Comodore family-Transfer complex, 40 to 65 percent slopes410S769500949jt8nco6341:24000
Comodore-Rock outcrop-Toothaker complex, 5 to 50 percent slopes43323431068552rb2sco6481:24000
Comodore-Rock outcrop association, 35 to 60 percent slopes1201257724538122ncd7co66419871:24000
Comodore very stony clay loam, 5 to 35 percent slopes1191159924538112ncd6co66419871:24000
Midfork family-Comodore complex6241600503756jx66ut61619831:24000
Comodore-Datino variant complex208796503710jx4qut61619831:24000
Beje-Comodore complex6426503753jx63ut61619831:24000
Comodore-Rock outcrop complex, 15 to 40 percent slopes3913830504432jxx0ut63619841:24000
Tolman family, dry-Comodore family-Rock outcrop complex, 15 to 45 percent slopes2625801512469k688ut6461:24000
Rock outcrop-Comodore family, moist complex, 20 to 60 percent slopes222125512372k654ut6461:24000
Comodore family, stony-Rock outcrop complex, 15 to 40 percent slopes129625212nzl4ut6491:24000
Comodore-Toothaker complex, 5 to 50 percent slopes4321562226178302rb2rwy6301:24000
Comodore-Rock outcrop-Toothaker complex, 5 to 50 percent slopes433901026178312rb2swy6301:24000

Map of Series Extent

Approximate geographic distribution of the COMODORE 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 .