Official Series Description


Lab Data Summary

Aggregate lab data for the HOWCAN soil series. This aggregation is based on all pedons with a current taxon name of HOWCAN, 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 HOWCAN 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 HOWCAN 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 HOWCAN 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 HOWCAN 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 HOWCAN 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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There are insufficient data to create the 3D flats position figure.

Competing Series

Soil series competing with HOWCAN 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 HOWCAN 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 HOWCAN 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 the image to view it full size.

Click the image to view it full size.

Click the image to view it full size.

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There are insufficient data to create the 3D flats position figure.

Soil series sharing subgroup-level classification with HOWCAN, 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 HOWCAN 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
Howcan-Hagenbarth-Hutchley complex, 5 to 60 percent slopes93-CL5005631736052smpid7031:24000
Bradshaw-Klug, very stony surface-Howcan, stony surface, complex, 5 to 55 percent slopes127AT1192832390082ztdnid7031:24000
Shakespeare-Howcan, stony surface, families, complex, 20 to 60 percent slopes127AU533731756452z447id7031:24000
Howcan-Zeebar-Hutchley association, 15 to 60 percent slopes39-B255731736222n6mid7031:24000
Zeebar-Parvis-Howcan association, 15 to 60 percent slopes141-B100831736212n5gid7031:24000
Soen-Justesen-Howcan complex, 4 to 35 percent slopes204-CL11231736172sghid7031:24000
Howcan-Searla complex, 12 to 55 percent slopes17113716131701r4mrid70819871:24000
Cloudless-Hades-Howcan complex, 12 to 20 percent slopes397926198902v07sid7131:24000
Cloudless-Hades-Howcan complex, 12 to 20 percent slopes39356531635672v07sid71419971:24000
Shakespeare-Howcan, stony surface, families, complex, 20 to 60 percent slopes127AU33124352z447id7201:24000
Howcan family-Cloudless family, complex, 20 to 50 percent slopes127CQ332044630mrcid7201:24000
Howcan-Parkay family-Lag family, complex, 10 to 50 percent slopes12411332043930mr1id7201:24000
Howcan-Searla complex, 12 to 55 percent slopes17171424100262lwtsid72120091:24000
Howcan-Searla complex, 4 to 12 percent slopes1706424100252lwtrid72120091:24000
Howcan-Hagenbarth-Hutchley complex, 5 to 60 percent slopes9323562832562smpid75219991:24000
Howcan family-Cloudless family, complex, 20 to 50 percent slopes127CQ6075331244930mrcid75219991:24000
Bradshaw-Klug, very stony surface-Howcan, stony surface, complex, 5 to 55 percent slopes127AT425932390562ztdnid75219991:24000
Howcan-Parkay family-Lag family, complex, 10 to 50 percent slopes124111499331244430mr1id75219991:24000
Soen-Justesen-Howcan complex, 4 to 35 percent slopes2041330830952sghid75219991:24000
Shakespeare-Howcan, stony surface, families, complex, 20 to 60 percent slopes127AU102632390652z447id75219991:24000
Howcan-Zeebar-Hutchley association, 15 to 60 percent slopes3919495790072n6mid76319981:24000
Hagenbarth-Howcan-Jonda association, 5 to 45 percent slopes354341790032n6hid76319981:24000
Zeebar-Parvis-Howcan association, 15 to 60 percent slopes1412078789712n5gid76319981:24000
Howcan-Hutchley-Rock outcrop complex, 15 to 60 percent slopes381856790062n6lid76319981:24000
Shakespeare-Howcan, stony surface, families, complex, 20 to 60 percent slopes127AU90532390862z447id76319981:24000
Howcan-Zeebar-Hutchley association, 15 to 60 percent slopes205014870531lxdgid78019981:24000
Howcan gravelly loam, 15 to 35 percent north slopes7004116824821352p9vwor6451:24000

Map of Series Extent

Approximate geographic distribution of the HOWCAN 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 .