Official Series Description


Lab Data Summary

Aggregate lab data for the SHODDY soil series. This aggregation is based on all pedons with a current taxon name of SHODDY, 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 SHODDY 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 SHODDY 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 SHODDY 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 SHODDY 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 SHODDY 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 SHODDY 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 SHODDY 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 SHODDY 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 SHODDY, 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 SHODDY 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
Cabbart-Shoddy-Amesha complex, 8 to 15 percent slopes191D1971475934yl2mt60919711:24000
Cabbart-Shoddy-Amesha complex, 15 to 45 percent slopes191E1601475944yl3mt60919711:24000
Bronec-Shoddy-Amesha complex, 15 to 35 percent slopes273E1041476054ylgmt60919711:24000
Shoddy silty clay loam, 2 to 8 percent slopes83C211475784yklmt60919711:24000
Amesha-Crago-Shoddy complex, 4 to 15 percent slopes114D181475834ykrmt60919711:24000
Walbert-Shoddy-Cabbart complex, 2 to 15 percent slopes851D161476264ym4mt60919711:24000
Shoddy silty clay loam, 8 to 15 percent slopes83D111476624yn9mt60919711:24000
Cabbart-Shoddy-Amesha complex, 2 to 8 percent slopes191C71475924yl1mt60919711:24000
Bronec-Shoddy-Amesha complex, 4 to 15 percent slopes273D21476044ylfmt60919711:24000
Polaris, stony-Dyce-Shoddy complex, 8 to 45 percent slopes76F62691883043216gbmt61220111:24000
Polaris stony-Shody-Badland complex, 15 to 45 percent slopes176F254924099872lwsjmt61220111:24000
Dyce, very bouldery-Shoddy, extremely stony-Bronec complex, 15 to 35 percent slopes, landslides420E79424263222mfsgmt61220111:24000
Bronec-Shoddy-Amesha complex, 15 to 35 percent slopes273E4678150998523xmt62719981:24000
Cabbart-Shoddy-Amesha complex, 15 to 45 percent slopes191E254415076251w9mt62719981:24000
Walbert-Shoddy-Cabbart complex, 15 to 35 percent slopes851F119415152952p1mt62719981:24000
Amesha-Crago-Shoddy complex, 15 to 45 percent slopes114E116215050051lvmt62719981:24000
Walbert-Shoddy-Cabbart complex, 2 to 15 percent slopes851D107715152852p0mt62719981:24000
Cabbart-Shoddy-Amesha complex, 8 to 15 percent slopes191D75415076151w8mt62719981:24000
Bronec-Shoddy-Amesha complex, 4 to 15 percent slopes273D686150997523wmt62719981:24000
Shoddy-Cabbart-Kobarter complex, 4 to 25 percent slopes831E33115152152nsmt62719981:24000
Shoddy silty clay loam, 8 to 15 percent slopes83D26615152552nxmt62719981:24000
Cabbart-Shoddy-Amesha complex, 2 to 8 percent slopes191C22415076051w7mt62719981:24000
Amesha-Crago-Shoddy complex, 4 to 15 percent slopes114D21415049951ltmt62719981:24000
Shoddy silty clay loam, 2 to 8 percent slopes83C21015152452nwmt62719981:24000
Shoddy-Rock outcrop-Delpoint complex, 2 to 25 percent slopes832E13415152252ntmt62719981:24000
Shoddy parachannery silty clay loam, 10 to 35 percent slopes425300025314482qmghwy6301:24000

Map of Series Extent

Approximate geographic distribution of the SHODDY 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 .