Official Series Description


Lab Data Summary

Aggregate lab data for the PAULSON soil series. This aggregation is based on all pedons with a current taxon name of PAULSON, 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 PAULSON 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
43B91P012790WY023006Paulson5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties42.8802795,-110.7183304
43B69C0120S1969WY023007Paulson7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties42.7194443,-110.9955521

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the PAULSON 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 PAULSON 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 PAULSON 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 PAULSON 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 PAULSON 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 PAULSON 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 PAULSON 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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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 PAULSON, 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. WA-2012-05-11-50 | Star Valley Area - March 1976

    Generalized cross-section of Star Valley Area showing the relative position of the four soil associations: 1. Hobacker-Greyback-Leavittville association; 2. Turson-Dipman association; 3. Robana-Buckskin-Cowdrey association; and 4. Paulson-Lail-Stony rock land association (Soil Survey of Star Valley Area Wyoming-Idaho; Parts of Lincoln County, Wyoming, and Bonneville and Caribou Counties, Idaho; March 1976).

Map Units

Map units containing PAULSON 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
Paulson-Nielsen complex, 5 to 35 percent slopes3125314841782tlfid76919781:24000
Paulson silt loam, 4 to 12 percent slopes296178841752tlbid76919781:24000
Paulson silt loam, 12 to 30 percent slopes301292841772tldid76919781:24000
Paulson-Lail associationPL1271515271553x9wy62319711:20000
Paulson-Rockland complex, 30 to 60 percent slopesPKF582315271453x8wy62319711:20000
Paulson silty clay loam, 0 to 3 percent slopesPaA486815271953xfwy62319711:20000
Paulson-Osmund associationPO270615271653xbwy62319711:20000
Paulson-Robana association, hillyPRD216915271753xcwy62319711:20000
Paulson silty clay loam, 10 to 20 percent slopesPaD123515272253xjwy62319711:20000
Paulson silty clay loam, 3 to 6 percent slopesPaB50915272053xgwy62319711:20000
Paulson-Robana association, steepPRE43315271853xdwy62319711:20000
Paulson silty clay loam, 6 to 10 percent slopesPaC26215272153xhwy62319711:20000
Groomer-Paulson-Baird Hollow families, complex, 0 to 30 percent slopes462566152047536rwy66320121:24000
Clayburn-Paulson-Beavet complex, 2 to 15 percent slopes810231696852y0ybwy7231:24000
Davtone-Paulson, moist complex911130250352xdygwy7231:24000
Paulson-Amsden-Libeg, stony complex, 2 to 8 percent slopes632030250302xdy9wy7231:24000

Map of Series Extent

Approximate geographic distribution of the PAULSON 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 .