Official Series Description


Lab Data Summary

Aggregate lab data for the CERRO soil series. This aggregation is based on all pedons with a current taxon name of CERRO, 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 CERRO 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 CERRO 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 CERRO 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 CERRO 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 CERRO 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 CERRO 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 CERRO 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 CERRO 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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Soil series sharing subgroup-level classification with CERRO, 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

No block diagrams are available.

Map Units

Map units containing CERRO 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
Cerro family, 5 to 25 percent slopes3501B874762966tlxtco6451:24000
Cerro-Herm complex, 15 to 40 percent slopesGM11787331283630gvcco6541:24000
Cerro-Herm complex, 15 to 40 percent slopes1175276509464k34bco66019941:24000
Cerro-Herm complex, 0 to 15 percent slopes1161561509463k349co66019941:24000
Cerro silty clay loam, 12 to 25 percent slopes115116509462k348co66019941:24000
Cerro-Bendire complex, 3 to 30 percent slopes9313529908441vkf7co66019941:24000
Cerro-Swansonlake complex, 1 to 45 percent slopes928322129909402kmn3co66219681:24000
Cerro-Curecanti, extremely stony complex, 15 to 60 percent slopes9879302990852vw1qco66219681:24000
Cerro, very stony-Curecanti, extremely stony complex, 3 to 35 percent slopes96761299086517pbsco66219681:24000
Cerro-Bendire complex, 3 to 30 percent slopes9311229908451vkf7co66219681:24000
Cerro-Curecanti, extremely stony complex, 15 to 60 percent slopes9877462990877vw1qco67419981:24000
Cerro, very stony-Curecanti, extremely stony complex, 3 to 35 percent slopes967646299086617pbsco67419981:24000
Cerro-Curecanti, extremely stony complex, 15 to 60 percent slopes987362927476vw1qco67519861:24000
Kubler-Delson-Cerro families complex, 3 to 15 percent slopes2456717510588k49lco67619831:24000
Cerro-Swansonlake complex, 1 to 45 percent slopes928625529909462kmn3co67619831:24000
Cerro-Curecanti, extremely stony complex, 15 to 60 percent slopes98712082990954vw1qco67619831:24000
Cerro, very stony-Curecanti, extremely stony complex, 3 to 35 percent slopes96730133115257317pbsco67720181:24000
Cerro-Swansonlake complex, 1 to 45 percent slopes9282853323723712kmn3co67720181:24000
Cerro-Curecanti, extremely stony complex, 15 to 60 percent slopes98724869800566vw1qco67720181:24000
Cerro, extremely stony-Shermap-Curecanti complex, 3 to 25 percent slopes9411439916133091r4s7co67720181:24000
Curecanti, extremely stony-Cerro complex, 25 to 55 percent slopes847N572229908312x5lwco67720181:24000
Cerro-Bendire complex, 3 to 30 percent slopes931259517148341vkf7co67720181:24000
Cerro clay loam, 5 to 35 percent slopes9842458804236vzw3co67720181:24000
Shermap-Cerro complex, 3 to 30 percent slopes932109617148351vkf8co67720181:24000
Cerro stony loam, 10 to 35 percent slopes227799496598jnr9co67919761:24000
Cerro loam, 6 to 12 percent slopes214153496597jnr8co67919761:24000
Cerro loam, 1 to 6 percent slopes202807496596jnr7co67919761:24000
Emmons-Cerro-Pagoda complex, 5 to 30 percent slopes, very stony335359496694jnvdco68219861:24000
Cerro silty clay loam, 6 to 12 percent slopes192887496678jntwco68219861:24000
Cerro silty clay loam, 12 to 25 percent slopes201439496680jntyco68219861:24000
Cerro silty clay loam, 2 to 6 percent slopes18520496677jntvco68219861:24000

Map of Series Extent

Approximate geographic distribution of the CERRO 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 .