Official Series Description


Lab Data Summary

Aggregate lab data for the PENROSE soil series. This aggregation is based on all pedons with a current taxon name of PENROSE, 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 PENROSE 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
67B97P029396CO628024PENROSE7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties37.3364444,-103.1846667
67B97P058696CO628025Penrose7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties37.1991667,-103.6088889

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the PENROSE 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 PENROSE 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 PENROSE 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 PENROSE 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 PENROSE 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 PENROSE series and competing. Series are sorted according to hierarchical clustering of median values. Source: SSURGO map unit geometry and 1981-2010, 800m PRISM data .

There are insufficient data to create the annual climate figure.

Geomorphic description summaries for the PENROSE 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 .

There are insufficient data to create the 2D hillslope position figure.

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

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

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 PENROSE, 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-2011-05-27-01 | Bent County - 1971

    Representative pattern of soils and underlying materials in associations 3 (Soil Survey of Bent County, Colorado; 1971).

  2. CO-2011-05-27-02 | Bent County - 1971

    Representative pattern of soils and underlying materials in association 3 (Soil Survey of Bent County, Colorado; 1971).

  3. CO-2011-05-27-07 | Otero County - 1972

    Volney-Olney-Dwyer association; part of Minnequa-Penrose soil association in background (Soil Survey of Otero County, Colorado; 1972).

  4. CO-2011-05-27-08 | Otero County - 1972

    Minnequa-Penrose association (Soil Survey of Otero County, Colorado; 1972).

  5. CO-2011-05-27-11 | Otero County - 1972

    Cross section of Otero County showing relief, drainage, and relation of soils to underlying geologic formations (Soil Survey of Otero County, Colorado; 1972).

  6. CO-2011-05-27-18 | Prowers County - 1966

    Main soils and underlying materials in soil association 8 (Soil Survey of Prowers County, Colorado; 1966).

  7. CO-2011-05-27-19 | Prowers County - 1966

    Cross sections showing relationships of the soils to the landscape and to the underlying geologic formations in Prowers County. The upper cross section shows relationships in the western part of the county, and the lower shows those in the eastern part of the county (Soil Survey of Prowers County, Colorado; 1966).

  8. NM-2012-02-14-01 | Harding County - November 1973

    Typical pattern of soils in association 2 in the northwestern part of the county (Soil Survey of Harding County, New Mexico; November 1973).

Map Units

Map units containing PENROSE 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
Penrose channery loam, 1 to 15 percent slopesPeD502227665282rgr9co00919661:20000
Penrose channery loamPe2796942093510co00919661:20000
Penrose-Midway-Rock outcrop complex, 10 to 45 percent slopesPeF29524976552pd2nco00919661:20000
Penrose-Minnequa complex, 1 to 15 percent slopesMpC1722727665332rgr8co01119651:15840
Penrose channery loam, 1 to 15 percent slopesPcD1685727665292rgr9co01119651:15840
Penrose-Minnequa complex, 1 to 15 percent slopes, dryPM767427665322rgrbco01119651:15840
Penrose-Midway-Rock outcrop complex, 10 to 45 percent slopesPeF277424842672pd2nco01119651:15840
Penrose channery loam, 1 to 15 percent slopesPeE6376226111622rgr9co08919661:15840
Penrose-Midway-Rock outcrop complex, 10 to 45 percent slopesPeF1018824976542pd2nco08919661:15840
Penrose-Rock outcrop complexPk24319486735q7co09919631:15840
Penrose channery loam, 1 to 15 percent slopesPeD179927665302rgr9co09919631:15840
Penrose loam, 1 to 5 percent slopesPaC3939486635q6co09919631:15840
Penrose-Manvel complex, 3 to 45 percent slopes642223954273699co62519751:24000
Penrose-Midway-Rock outcrop complex, 10 to 45 percent slopesPrF74175955282pd2nco62619741:24000
Penrose-Minnequa complex, 1 to 15 percent slopesPmE6222927665342rgr8co62619741:24000
Penrose-Minnequa complex, 1 to 15 percent slopes, dryPM5251027665352rgrbco62619741:24000
Penrose-Minnequa complex, 1 to 15 percent slopesPM1209827665742rgr8co62719801:24000
Penrose channery loam, 1 to 15 percent slopesPeD1103827665702rgr9co62719801:24000
Shingle-Penrose complex, 2 to 15 percent slopesShD646051054353jq4co62820081:24000
Penrose channery loam, 1 to 15 percent slopesPeD5712027665312rgr9co62820081:24000
Penrose-Midway-Rock outcrop complex, 10 to 45 percent slopesPeF3952924992522pd2nco62820081:24000
Penrose-Minnequa complex, 1 to 15 percent slopesPM686827665362rgr8co62820081:24000
Penrose loam, moist, 2 to 15 percent slopesPnD37521054093jp9co62820081:24000
Penrose-Minnequa complex, 1 to 15 percent slopes831303026111272rgr8co63719861:24000
Penrose-Midway-Rock outcrop complex, 10 to 45 percent slopes8463244983542pd2nco63719861:24000
Penrose-Rock land complex, 10 to 20 percent slopes27941474115233517p33ks05519621:24000
Minnequa-Penrose silt loams, 5 to 15 percent slopes169717791115053717m73ks10919621:24000
Shingle-Penrose-Rock outcrop complex, 15 to 40 percent slopesSnE27162355154cxklsd04719801:24000
Fairburn-Penrose, moist-Rock outcrop complex, 15 to 40 percent slopesP126E30027331572rvdbsd04719801:24000
Penrose-Rock outcrop complex, 9 to 60 percent slopesPdF29662580952cyjssd60620111:24000
Minnequa-Penrose complex, 6 to 9 percent slopesMrC15732580932cyj4sd60620111:24000

Map of Series Extent

Approximate geographic distribution of the PENROSE 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 .