Aggregate lab data for the PULLMAN soil series. This aggregation is based on all pedons with a current taxon name of PULLMAN, 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 PULLMAN were used in the calculation. Source: KSSL snapshot . Methods used to assemble the KSSL snapshot used by SoilWeb / SDE
Pedons used in the lab summary:
Monthly water balance estimated using a leaky-bucket style model for the PULLMAN 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.
Siblings are those soil series that occur together in map units, in this case with the PULLMAN series. Sketches are arranged according to their subgroup-level taxonomic structure. Source: SSURGO snapshot , parsed OSD records and snapshot of SC database .
Select annual climate data summaries for the PULLMAN series and siblings. Series are sorted according to hierarchical clustering of median values. Source: SSURGO map unit geometry and 1981-2010, 800m PRISM data .
Geomorphic description summaries for the PULLMAN 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 .
Soil series competing with PULLMAN share the same family level classification in Soil Taxonomy. Source: parsed OSD records and snapshot of the SC database .
Select annual climate data summaries for the PULLMAN series and competing. Series are sorted according to hierarchical clustering of median values. Source: SSURGO map unit geometry and 1981-2010, 800m PRISM data .
Geomorphic description summaries for the PULLMAN 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 .
Click a link below to display the diagram. Note that these diagrams may be from multiple survey areas.
Typical pattern of soils and parent material at Blanco Creek on the High Plains. Pullman soils are on gentle slopes at the top of the divide, and Mansker soils are in rolling areas leading to the stream channel (Soil Survey of Southwest Quay Area, New Mexico; May 1960).
Parent material and parent rock of most of the soils in Beaver County, and their position on the landscape (Soil Survey of Beaver County, Oklahoma; August 1962).
General relationship of the soils in Carson County (Soil Survey of Carson County, Texas).
Estacado-Pep (Soil Survey of Carson County, Texas).
A representative pattern of soils in one of the playas associated with the Pullman soil (Soil Survey of Carson County, Texas).
Pullman (Soil Survey of Carson County, Texas).
Typical pattern of soils in the Pullman general soil map unit (Soil Survey of Deaf Smith County, Texas; 2007).
Typical pattern of soils in the Pep-Estacado general soil map unit (Soil Survey of Deaf Smith County, Texas; 2007).
Typical pattern of soils in the Pep-Plemons general soil map unit (Soil Survey of Deaf Smith County, Texas; 2007).
Typical pattern of soils in the Pep-Berda-Bippus general soil map unit (Soil Survey of Deaf Smith County, Texas; 2007).
Typical pattern of soils in the Estacado-Pullman general soil map unit (Soil Survey of Deaf Smith County, Texas; 2007).
General relationship of the soils in Carson County (Soil Survey of Carson County, TX; 1962).
A representative pattern of soils in one of the playas of the Pullman-Randall soil association (Soil Survey of Carson County, TX; 1962).
Soil toposequence of playas (Soil Survey of Carson County, TX; 1962).
Soil toposequence of the escarpment separating the High Plains from the Rolling Plains (Soil Survey of Carson County, TX; 1962).
Topography and underlying material of the Mobeetie (3); Quay-Montoya-Vernon (8); and Mobeetie-Potter-Rough broken land (4) associations (Soil Survey of Deaf Smith County, TX; 1968).
Patterns of soils around a playa on the High Plains (Soil Survey of Deaf Smith County, TX; 1968).
Diagram showing typical locations of soil series and the underlying parent material (Soil Survey of Hansford County, TX; 1960).
Pattern of soils and underlying material in association 5 (Soil Survey of Lipscomb County, TX; 1975).
Relationship of soils in the Abilene-Mobeetie-Berda association to parent material and relief (Soil Survey of Wheeler County, TX; 1975).
Map units containing PULLMAN as a major component. Limited to 250 records.
Approximate geographic distribution of the PULLMAN 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 .