Official Series Description


Lab Data Summary

Aggregate lab data for the HANGMANS soil series. This aggregation is based on all pedons with a current taxon name of HANGMANS, 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 HANGMANS 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 HANGMANS 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 HANGMANS 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 HANGMANS 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 HANGMANS 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 HANGMANS 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 HANGMANS 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 HANGMANS 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 HANGMANS, 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 HANGMANS 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
Blackleaf, stony-Hangmans-Rock outcrop complex, 15 to 45 percent290F2498797991vscnmt61220111:24000
Hangmans-Galbreth-Rock outcrop complex, 20 to 75 percent slopes, very stony552433583012w7jvwy6171:24000
Hangmans-Dunlap-like-Marthaspeak complex, 20 to 40 percent slopes544631708632wxmbwy6171:24000
Hangmans-Galbreth-Rock outcrop complex, 20 to 75 percent slopes, very stony552429119202w7jvwy6291:24000
Rencot-Amalia-like, stony-Hangmans complex, 25 to 50 percent slopes450431709592z1zpwy6291:24000
Hangmans-Dunlap-like-Marthaspeak complex, 20 to 40 percent slopes544629690852wxmbwy6291:24000
Hangmans-Tyzut-like complex, 15 to 50 percent slopes440532090442zdq8wy6291:24000
Hangmans, stony-Spudbar, very bouldery-Birney complex, 15 to 35 percent slopes440832090542zdqlwy6291:24000
Rencot-Amalia-like, stony-Hangmans complex, 25 to 50 percent slopes450432505222z1zpwy65620081:24000
Hangmans-Duffymont-Rock outcrop complex, 15 to 45 percent slopes -- draft8603202028434362tsbfwy7231:24000
Hangmans, extremely stony-Delpoint-Montsweet complex, 4 to 15 percent slopes412032225042ztmgwy7371:24000
Bonhigh-Hangmans-Snakerattle family, complex, 2 to 8 percent slopes412132225052ztmhwy7371:24000
Hangmans-Cabbart-Hawkdepth complex, 2 to 25 percent slopes4240322251230j6zwy7371:24000
Hawkdepth-Hangmans-Bonhigh family, complex, 4 to 25 percent slopes431232224332zjtvwy7371:24000
Hangmans-Delphill-Rangecreek complex, 15 to 35 percent slopes411332223302ztm2wy7371:24000
Hangmans-Birney-Hawksell families, complex, 8 to 15 percent slopes411232223312ztm3wy7371:24000
Sheecal family-Hangmans complex, 8 to 35 percent slopes411032223332ztm5wy7371:24000
Hangmans, extremely stony surface-Figuore, very stony surface-Lonna, very stony surface, complex, 2 to 15 percent slopes4506322236130j9kwy7371:24000
Yamacall family-Hangmans-Lodore complex, 2 to 8 percent slopes431332224352zjtwwy7371:24000
Lonna family-Craighigh, rubbly surface-Hangmans, rubbly surface, complex, 15 to 35 percent slopes431432224362zjtzwy7371:24000
Hangmans-Hawkdepth-Rock outcrop complex, 10 to 30 percent slopes431632224382zjtywy7371:24000
Hangmans-Hawksell complex, 8 to 60 percent slopes4230322244230j6nwy7371:24000
Yawdim-Hangmans-Birney family, complex, 20 to 60 percent slopes4231322244330j6pwy7371:24000
Hangmans-Coyoteflats-Bonhigh family, complex, 2 to 8 percent slopes34321271426119442qstmwy7371:24000

Map of Series Extent

Approximate geographic distribution of the HANGMANS 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 .