Soil Data Explorer - SCHAFFENAKER

Official Series Description

Lab Data Summary

Aggregate lab data for the SCHAFFENAKER soil series. This aggregation is based on all pedons with a current taxon name of SCHAFFENAKER, 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 SCHAFFENAKER were used in the calculation. Source: KSSL snapshot (updated 2020-03-13). Methods used to assemble the KSSL snapshot used by SoilWeb / SDE

There are insufficient data to create the lab data summary figure.

Pedons used in the lab summary:

MLRA	Lab ID	Pedon ID	Taxonname	CI	NSSL / NASIS Reports	Link To SoilWeb GMap
n/a	RC-014	1968-OH139-014	Schaffenaker	4	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	n/a

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the SCHAFFENAKER 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.

Sibling Summary

Siblings are those soil series that occur together in map units, in this case with the SCHAFFENAKER series. Sketches are arranged according to their subgroup-level taxonomic structure. Source: SSURGO snapshot (updated 2024-10-24), parsed OSD records (updated 2024-10-23) and snapshot of SC database (updated 2024-10-23).

Select annual climate data summaries for the SCHAFFENAKER series and siblings. Series are sorted according to hierarchical clustering of median values. Source: SSURGO map unit geometry and 1981-2010, 800m PRISM data (updated 2024-10-23).

Geomorphic description summaries for the SCHAFFENAKER 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 (updated 2024-10-23).

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 SCHAFFENAKER share the same family level classification in Soil Taxonomy. Source: parsed OSD records (updated 2024-10-23) and snapshot of the SC database (updated 2024-10-23).

Select annual climate data summaries for the SCHAFFENAKER series and competing. Series are sorted according to hierarchical clustering of median values. Source: SSURGO map unit geometry and 1981-2010, 800m PRISM data (updated 2024-10-23).

Geomorphic description summaries for the SCHAFFENAKER 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 (updated 2024-10-23).

There are insufficient data to create the 3D mountains figure.

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

Soil series sharing subgroup-level classification with SCHAFFENAKER, 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 (updated 2024-10-23).

Block Diagrams

No block diagrams are available.

Map Units

Map units containing SCHAFFENAKER 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
Schaffenaker loamy sand, 10 to 40 percent slopes	ScE	400	288196	9nwn	oh005	1976	1:15840
Schaffenaker loamy sand, 12 to 25 percent slopes	SaD	2	1592662	1qg96	oh005	1976	1:15840
Schaffenaker loamy sand, 12 to 25 percent slopes	SaD	16	2108994	28sl2	oh031	1996	1:15840
Schaffenaker very bouldery loamy sand, 25 to 60 percent slopes	SbF	13	2108995	28sl3	oh031	1996	1:15840
Schaffenaker loamy sand, 12 to 25 percent slopes	ScD	85	286933	9mkx	oh075	1989	1:15840
Schaffenaker loamy sand, 12 to 25 percent slopes	ScD	1125	614625	nmkm	oh083	1983	1:15840
Schaffenaker very bouldery loamy sand, 25 to 60 percent slopes	SdF	604	614626	nmkn	oh083	1983	1:15840
Schaffenaker loamy sand, 25 to 70 percent slopes	ScF	252	288388	9p2v	oh103	1974	1:15840
Schaffenaker loamy sand, 18 to 40 percent slopes	SaE	1026	170802	5qqr	oh139	1971	1:15840
Schaffenaker loamy sand, 12 to 18 percent slopes	SaD	802	170801	5qqq	oh139	1971	1:15840
Schaffenaker loamy sand, 2 to 12 percent slopes	SaC	392	170800	5qqp	oh139	1971	1:15840
Schaffenaker loamy sand, 10 to 40 percent slopes	SbE	2	1406555	1j6mr	oh139	1971	1:15840
Schaffenaker loamy sand, 8 to 15 percent slopes	32C	280	2481042	2p8qm	va045	2010	1:24000
Schaffenaker very stony loamy sand, 7 to 25 percent slopes	37D	219	521111	kh81	va069	1983	1:15840
Schaffenaker very stony loamy sand, 25 to 65 percent slopes	37E	144	521112	kh82	va069	1983	1:15840
Schaffenaker-Vanderlip loamy sands, 35 to 65 percent slopes, very bouldery	SnF	688	555739	ln92	wv065	2003	1:24000
Schaffenaker-Rock outcrop complex, 35 to 65 percent slopes, rubbly	SkF	421	555740	ln93	wv065	2003	1:24000
Schaffenaker-Vanderlip loamy sands, 15 to 35 percent slopes, very bouldery	SnE	83	555724	ln8l	wv065	2003	1:24000
Schaffenaker loamy sand, 3 to 15 percent slopes, very bouldery	ShC	34	555723	ln8k	wv065	2003	1:24000
Schaffenaker very stony loamy sand, 15 to 35 percent slopes	ShE	9345	555980	lnjv	wv608	1973	1:20000
Schaffenaker very stony loamy sand, 35 to 65 percent slopes	ShF	8643	555981	lnjw	wv608	1973	1:20000
Schaffenaker very stony loamy sand, 3 to 15 percent slopes	ShC	3829	555979	lnjt	wv608	1973	1:20000
Schaffenaker-Drall stony loamy sands, 15 to 35 percent slopes	ShE	5261	515962	k9wy	wv628	1980	1:20000
Schaffenaker-Drall stony loamy sands, 35 to 65 percent slopes	ShF	4056	515963	k9wz	wv628	1980	1:20000
Schaffenaker-Drall stony loamy sands, 3 to 15 percent slopes	ShC	1864	515961	k9wx	wv628	1980	1:20000
Schaffenaker-Drall extremely cobbly loamy sands, 15 to 35 percent slopes, extremely bouldery	SfEb	191	3244705	2zf80	wv628	1980	1:20000
Schaffenaker-Drall extremely cobbly loamy sands, 8 to 15 percent slopes, extremely bouldery	SfCb	94	3244704	2zf7z	wv628	1980	1:20000
Schaffenaker-Drall extremely cobbly loamy sands, 0 to 8 percent slopes, extremely bouldery	SfBb	48	3244703	2zf7y	wv628	1980	1:20000
Schaffenaker-Rock outcrop complex, 25 to 65 percent slopes, extremely stony	SrFs	37	3244707	2zf82	wv628	1980	1:20000
Schaffenaker-Drall complex, 0 to 8 percent slopes, very stony	SdBs	22	3244702	2zf7x	wv628	1980	1:20000
Schaffenaker-Drall very cobbly loamy sands, 25 to 65 percent slopes, very stony	SnFs	15	3244706	2zf81	wv628	1980	1:20000

Map of Series Extent

Approximate geographic distribution of the SCHAFFENAKER 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 (updated 2024-10-30).