Official Series Description


Lab Data Summary

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

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

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Click the image to view it full size.

Soil series sharing subgroup-level classification with PULTNEY, 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-2011-05-27-18 | Prowers County - 1966

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

  2. 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).

Map Units

Map units containing PULTNEY 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
Pultney loam, 1 to 9 percent slopesPuC1560942742zcs0co01119651:15840
Kim-Pultney complex, 1 to 9 percent slopes26220594314354dco01719851:24000
Singerton-Pultney complex, 1 to 10 percent slopes322873494442358jco06119771:24000
Pultney loam, 1 to 5 percent slopesPuC36999487035qbco09919631:15840
Spearfish-Pultney association, hillySSd16686346145cm5zmt60719701:24000
Spearfish-Rock outcrop complex, very steepSSb8646346143cm5xmt60719701:24000
Pultney-Neville association, undulatingPO6455346098cm4gmt60719701:24000
Spearfish-Pultney association, rollingSSc5130346144cm5ymt60719701:24000
Rock outcrop-Pultney complex, very steepRP1316346113cm4ymt60719701:24000
Rock outcrop-Tassel-Pultney complex, 5 to 40 percent slopes4892022015223553dtwy6031:24000
Hiland-Pultney-Zigweid-like complex, 3 to 10 percent slopes532431368572ypntwy6291:24000
Renohill-Hilight-Pultney complex, 15 to 55 percent slopes542931332462ynm5wy6291:24000
Begay-Pultney complex, 6 to 20 percent slopes532229119692y4yrwy6291:24000

Map of Series Extent

Approximate geographic distribution of the PULTNEY 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 .