Aggregate lab data for the HUMBARGER soil series. This aggregation is based on all pedons with a current taxon name of HUMBARGER, 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 HUMBARGER were used in the calculation. Source: KSSL snapshot (updated 2020-03-18). Methods used to assemble the KSSL snapshot used by SoilWeb / SDE
There are insufficient data to create the lab data summary figure.
Monthly water balance estimated using a leaky-bucket style model for the HUMBARGER 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 HUMBARGER series. Sketches are arranged according to their subgroup-level taxonomic structure. Source: SSURGO snapshot (updated 2024-10-24), parsed OSD records (updated 2025-02-20) and snapshot of SC database (updated 2025-02-20).
Select annual climate data summaries for the HUMBARGER series and siblings. Series are sorted according to hierarchical clustering of median values. Source: SSURGO map unit geometry and 1981-2010, 800m PRISM data (updated 2024-10-23).
Geomorphic description summaries for the HUMBARGER 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 (updated 2024-10-23).
There are insufficient data to create the 3D mountains figure.
Soil series competing with HUMBARGER share the same family level classification in Soil Taxonomy. Source: parsed OSD records (updated 2025-02-20) and snapshot of the SC database (updated 2025-02-20).
Select annual climate data summaries for the HUMBARGER series and competing. Series are sorted according to hierarchical clustering of median values. Source: SSURGO map unit geometry and 1981-2010, 800m PRISM data (updated 2024-10-23).
Geomorphic description summaries for the HUMBARGER 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 (updated 2024-10-23).
There are insufficient data to create the 3D mountains figure.
Soil series sharing subgroup-level classification with HUMBARGER, 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 (updated 2025-02-20).
Click a link below to display the diagram. Note that these diagrams may be from multiple survey areas.
Typical cross section of the Pawnee River drainage basin (Soil Survey of Finney County, Kansas; 1965).
Typical pattern of soils and parent material in the Holdrege-Uly-Penden association (Soil Survey of Graham County, Kansas; 1986).
Typical pattern of soils and parent material in the association (Soil Survey of Graham County, Kansas; 1986).
Relationships of soils in association 2 (Soil Survey of Grant County, Kansas; 1969).
Relationships of soils in association 3 (Soil Survey of Grant County, Kansas; 1969).
Distribution of the soils in the Muir-Carr-Humbarger association (Soil Survey of Republic County, Kansas; 1967).
Pattern of soils and parent material in the Armo-Heizer-Brownell association (Soil Survey of Trego County, Kansas; 1990).
Pattern of soils and parent material in the Penden-Armo association (Soil Survey of Trego County, Kansas; 1990).
Cross section of association 2 along White Woman Creek (Soil Survey of Wichita County, Kansas; 1965).
Relationship of soils to the landscape and to the common parent materials of Wichita County (Soil Survey of Wichita County, Kansas; 1965).
Relationship of soils and underlying material in the Plack-Berthoud association (Soil Survey of Dallam County, TX; 1975).
Map units containing HUMBARGER as a major component. Limited to 250 records.
Approximate geographic distribution of the HUMBARGER 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 (updated 2024-10-30).