Soil Data Explorer - OLDWOLF

Official Series Description

Lab Data Summary

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

Water Balance

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

Competing Series

Soil series competing with OLDWOLF 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 OLDWOLF 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 OLDWOLF 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.

Soil series sharing subgroup-level classification with OLDWOLF, 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 OLDWOLF 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
Deekay-Oldwolf loams, 0 to 6 percent slopes	134	111	1387742	1hl1w	mt643	1967	1:20000
Oldwolf loam, 2 to 10 percent slopes	P296C	3538	2745725	2rvfw	wy011	1978	1:24000
Deekay-Oldwolf loams, 6 to 15 percent slopes	221	219	780124	2wlqc	wy011	1978	1:24000
Oldwolf-Xema complex, 3 to 15 percent slopes	P302D	90	2745726	2rvfz	wy011	1978	1:24000
Deekay-Oldwolf loams, 0 to 6 percent slopes	220	78	780120	2wlq9	wy011	1978	1:24000
Oldwolf-Fairburn loams, 6 to 15 percent slopes	P300D	52	2768180	2rvfy	wy011	1978	1:24000
Oldwolf-Fairburn loams, 3 to 15 percent slopes	230	18	780145	2yrz0	wy011	1978	1:24000
Oldwolf loam, 2 to 10 percent slopes	P296C	2045	2745975	2rvfw	wy045	1984	1:24000
Oldwolf-Cambria, moist loams, 2 to 10 percent slopes	P298C	110	2745976	2rvfx	wy045	1984	1:24000
Oldwolf-Xema complex, 3 to 15 percent slopes	P302D	101	2745978	2rvfz	wy045	1984	1:24000
Oldwolf-Fairburn loams, 6 to 15 percent slopes	P300D	70	2745977	2rvfy	wy045	1984	1:24000
Deekay-Oldwolf loams, 0 to 6 percent slopes	134	16292	349819	2wlq9	wy605	1995	1:24000
Ziggy-Ucross-Oldwolf loams, 3 to 15 percent slopes	250	15628	349951	2yryj	wy605	1995	1:24000
Deekay-Oldwolf loams, 6 to 15 percent slopes	135	14117	349820	2wlqc	wy605	1995	1:24000
Deekay-Oldwolf loams, 0 to 6 percent slopes	134	42380	817523	2wlq9	wy705	2003	1:24000
Deekay-Oldwolf loams, 6 to 15 percent slopes	135	13854	817525	2wlqc	wy705	2003	1:24000
Oldwolf-Fairburn loams, 3 to 15 percent slopes	299	12909	817566	2yrz0	wy705	2003	1:24000
Ziggy-Ucross-Oldwolf loams, 3 to 15 percent slopes	250	1365	817616	2yryj	wy705	2003	1:24000
Deekay-Oldwolf loams, 6 to 15 percent slopes	736	2213	1384630	2wlqc	wy719	2013	1:24000

Map of Series Extent

Approximate geographic distribution of the OLDWOLF 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).