Official Series Description


Lab Data Summary

Aggregate lab data for the SAWDUST soil series. This aggregation is based on all pedons with a current taxon name of SAWDUST, 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 SAWDUST 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 SAWDUST 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 SAWDUST 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 SAWDUST 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 SAWDUST 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.

Click the image to view it full size.

Click the image to view it full size.

Click the image to view it full size.

Competing Series

Soil series competing with SAWDUST 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 SAWDUST 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 SAWDUST 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 SAWDUST, 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 SAWDUST 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
Rockerville-Sawdust-Rock outcrop complex, 9 to 60 percent slopesQ0660F1361924356492mrhbsd04719801:24000
Vanocker, dry-Sawdust-Rock outcrop complex, 40 to 80 percent slopesQ0678G34025171442mlhqsd04719801:24000
Sawdust-Vanocker, dry-Rockerville complex, 10 to 40 percent slopesQ0665E20625171322ml1tsd04719801:24000
Vanocker-Sawdust-Rock outcrop complex, warm, 40 to 80 percent slopesP542G1827681092s02wsd04719801:24000
Vanocker-Sawdust, moist-Rock outcrop complex, 40 to 80 percent slopesQ0589G2357123758302kr7psd08120071:24000
Hopdraw-Sawdust-Rock outcrop complex, moist, 40 to 80 percent slopesQ0530G37523758152kr76sd08120071:24000
Sawdust, moist-Vanocker-Rockerville, moist complex, 10 to 40 percent slopesQ0571E27423758202kr7csd08120071:24000
Vanocker-Sawdust, moist-Rock outcrop complex, 40 to 80 percent slopesQ0589G506225144792kr7psd60019741:24000
Sawdust, moist-Vanocker-Rockerville, moist complex, 10 to 40 percent slopesQ0571E152525142922kr7csd60019741:24000
Sawdust, moist-Rock outcrop complex, 40 to 80 percent slopesQ0591G27124801672p7tdsd60019741:24000
Vanocker, dry-Sawdust-Rock outcrop complex, 40 to 80 percent slopesQ0678G19025171432mlhqsd60019741:24000
Sawdust-Vanocker, dry-Rockerville complex, 10 to 40 percent slopesQ0665E17625171332ml1tsd60019741:24000
Rockerville-Sawdust-Rock outcrop complex, 9 to 60 percent slopesQ0660F13325171292mrhbsd60019741:24000
Hopdraw-Sawdust-Rock outcrop complex, moist, 40 to 80 percent slopesQ0530G8425142712kr76sd60019741:24000
Sawdust-Hopdraw-Rockerville complex, 10 to 40 percent slopesQ0664E5125171312ml1ssd60019741:24000
Sawdust-Vanocker, dry-Rockerville complex, 10 to 40 percent slopesQ0665E7560025866002ml1tsd60720111:24000
Hopdraw-Sawdust-Rock outcrop complex, 40 to 80 percent slopesQ0634G3114325866322krlnsd60720111:24000
Sawdust-Hopdraw-Rockerville complex, 10 to 40 percent slopesQ0664E2263925865322ml1ssd60720111:24000
Vanocker, dry-Sawdust-Rock outcrop complex, 40 to 80 percent slopesQ0678G2093025865002mlhqsd60720111:24000
Sawdust-Rock outcrop complex, 40 to 80 percent slopesQ0655G842125863932ml1nsd60720111:24000
Vanocker-Sawdust, moist-Rock outcrop complex, 40 to 80 percent slopesQ0589G564425865492kr7psd60720111:24000
Sawdust, moist-Rock outcrop complex, 40 to 80 percent slopesQ0591G197525866312p7tdsd60720111:24000
Sawdust, moist-Vanocker-Rockerville, moist complex, 10 to 40 percent slopesQ0571E167625865092kr7csd60720111:24000
Hopdraw-Sawdust-Rock outcrop complex, moist, 40 to 80 percent slopesQ0530G148325866082kr76sd60720111:24000
Sawdust, warm-Rock outcrop complex, 40 to 80 percent slopesP450G66927456802rxv9sd60720111:24000
Sawdust-Hopdraw-Rockerville complex, moist, 10 to 40 percent slopesQ0590E39825864952mhl9sd60720111:24000
Sawdust-Vanocker-Rockerville complex, warm, 10 to 40 percent slopesP452E34027456902rxvbsd60720111:24000
Schamber-Sawdust, warm-Rock outcrop complex, 40 to 80 percent slopesP456G30327456652rxvdsd60720111:24000
Sawdust family-Shawa family, calcareous association, 2 to 8 percent slopes240A1004512443k67fut6461:24000
Hopdraw-Sawdust-Rock outcrop complex, 40 to 80 percent slopesQ0634G201325169992krlnwy04519841:24000
Vanocker-Sawdust, moist-Rock outcrop complex, 40 to 80 percent slopesQ0589G142925145112kr7pwy04519841:24000
Vanocker, dry-Sawdust-Rock outcrop complex, 40 to 80 percent slopesQ0678G113625171422mlhqwy04519841:24000
Sawdust-Hopdraw-Rockerville complex, 10 to 40 percent slopesQ0664E76925171302ml1swy04519841:24000
Sawdust-Vanocker, dry-Rockerville complex, 10 to 40 percent slopesQ0665E825171342ml1twy04519841:24000
Sawdust-Weed-like-Cohagen-like complex, 3 to 55 percent slopes5C22335836731jyhwy6171:24000
Sawdust-Walstead-Repkie complex, 20 to 60 percent slopes591032030942zbstwy6291:24000

Map of Series Extent

Approximate geographic distribution of the SAWDUST 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 .