Soil Data Explorer - WYARNO

Official Series Description

Lab Data Summary

Aggregate lab data for the WYARNO soil series. This aggregation is based on all pedons with a current taxon name of WYARNO, 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 WYARNO 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 WYARNO 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 WYARNO 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 WYARNO 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 WYARNO 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 WYARNO 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 WYARNO 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 WYARNO 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 WYARNO, 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 WYARNO 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
Wyarno clay loam, 2 to 6 percent slopes	211	2202	349299	cqgq	wy011	1978	1:24000
Wyarno clay loam, 6 to 10 percent slopes	212	2132	349300	cqgr	wy011	1978	1:24000
Wyarno clay loam, 0 to 2 percent slopes	210	816	349298	cqgp	wy011	1978	1:24000
Wyarno-Ulm clay loams, 0 to 6 percent slopes	246	1268	349946	cr4l	wy605	1995	1:24000
Limon-Cadoma association	LO	9204	350877	cs3m	wy619	1971	1:24000
Absted-Wyarno complex, sloping	ADC	8156	350805	cs19	wy619	1971	1:24000
Wyarno-Limon association	WO	6475	350965	cs6g	wy619	1971	1:24000
Samsil-Renohill association	SE	2893	350924	cs54	wy619	1971	1:24000
Absted-Wyarno complex, gently sloping	ADB	2210	350804	cs18	wy619	1971	1:24000
Ulm-Wyarno association	UW	1890	350957	cs66	wy619	1971	1:24000
Wyarno clay loam, 0 to 3 percent slopes	WnA	1284	350967	cs6j	wy619	1971	1:24000
Wyarno clay loam, 3 to 6 percent slopes	WnB	905	350968	2wlqp	wy619	1971	1:24000
Wyarno-Stoneham association	WY	759	350966	cs6h	wy619	1971	1:24000
Wyarno-Ulm clay loams, 0 to 6 percent slopes	246	15	817253	wff0	wy619	1971	1:24000
Wyarno clay loam, 3 to 6 percent slopes	313	3360	361010	2wlqp	wy633	1987	1:24000
Wyarno clay loam, 0 to 3 percent slopes	309	3346	2494802	1t4p1	wy633	1987	1:24000
Renohill, moist-Wyarno association, 6 to 9 percent slopes	240	2973	360991	d3mw	wy633	1987	1:24000
Wyarno clay loam, dry, 0 to 3 percent slopes	312	2066	361011	d3nj	wy633	1987	1:24000
Wyarno clay loam, 6 to 9 percent slopes	311	2045	361012	d3nk	wy633	1987	1:24000
Wyarno clay loam, moist, 3 to 6 percent slopes	310	1973	361013	2wlqr	wy633	1987	1:24000
Urban land-Wyarno-Nuncho complex, 0 to 3 percent slopes	296	1047	361027	d3p1	wy633	1987	1:24000
Wyarno clay loam, dry, 6 to 9 percent slopes	314	840	361009	d3ng	wy633	1987	1:24000
Wyarno clay loam, 0 to 3 percent slopes	670	529	1672792	1t4p1	wy719	2013	1:24000
Wyarno clay loam, moist, 3 to 6 percent slopes	680	8	1905111	2wlqr	wy719	2013	1:24000

Map of Series Extent

Approximate geographic distribution of the WYARNO 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).