Official Series Description


Lab Data Summary

Aggregate lab data for the HOBNAIL soil series. This aggregation is based on all pedons with a current taxon name of HOBNAIL, 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 HOBNAIL 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 HOBNAIL 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 HOBNAIL series. Sketches are arranged according to their subgroup-level taxonomic structure. Source: SSURGO snapshot , parsed OSD records and snapshot of SC database .

There are insufficient data to create the sibling sketch figure.

Select annual climate data summaries for the HOBNAIL 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 HOBNAIL 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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Click the image to view it full size.

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.

Competing Series

Soil series competing with HOBNAIL 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 HOBNAIL 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 HOBNAIL 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 HOBNAIL, 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

No block diagrams are available.

Map Units

Map units containing HOBNAIL 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
Hobnail-Threebear complex, 5 to 25 percent slopesHm3js795250118654nzid05720131:24000
Hobnail ashy silt loam, 15 to 35 percent slopesHb5j173250206454nvid05720131:24000
Hobnail-Threebear complex, 5 to 25 percent slopes362658515344954nzid60819941:24000
Hobnail ashy silt loam, 15 to 35 percent slopes322508115344554nvid60819941:24000
Hobnail silt loam, very strongly acid, 15 to 35 percent slopes, eroded3599715344854nyid60819941:24000
Hobnail ashy silt loam, 15 to 40 percent slopes1hn6f92027430481hn6fid60819941:24000
Hobnail silt loam, strongly acid, 15 to 35 percent slopes3488315344754nxid60819941:24000
Hobnail-Threebear complex, 5 to 30 percent slopes1hn8761727430541hn87id60819941:24000
Hobnail silt loam, moderately acid, 15 to 35 percent slopes3336515344654nwid60819941:24000
Hobnail-Threebear silt loams, extremely acid, 5 to 15 percent slopes, severely eroded3726515345054p0id60819941:24000
Hobnail-Threebear complex, warm, 5 to 35 percent slopes1hn886027430581hn88id60819941:24000
Hobnail ashy silt loam, 15 to 40 percent slopes913204513898051hn6fid62020131:24000
Hobnail-Threebear complex, 5 to 30 percent slopes500161013898611hn87id62020131:24000
Hobnail-Threebear complex, warm, 5 to 35 percent slopes501148713898621hn88id62020131:24000
Hobnail ashy silt loam, 15 to 35 percent slopes54nv81285097154nvid6701:24000
Hobnail-Threebear complex, 5 to 25 percent slopes54nz73285097254nzid6701:24000

Map of Series Extent

Approximate geographic distribution of the HOBNAIL 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 .