Soil Data Explorer - WYNONA

Official Series Description

Lab Data Summary

Aggregate lab data for the WYNONA soil series. This aggregation is based on all pedons with a current taxon name of WYNONA, 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 WYNONA 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 WYNONA 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 WYNONA series. Sketches are arranged according to their subgroup-level taxonomic structure. Source: SSURGO snapshot (updated 2024-02-21), parsed OSD records (updated 2023-10-02) and snapshot of SC database (updated 2023-10-02).

Select annual climate data summaries for the WYNONA 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 2023-10-09).

Geomorphic description summaries for the WYNONA 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 2023-10-04).

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

Competing Series

Soil series competing with WYNONA share the same family level classification in Soil Taxonomy. Source: parsed OSD records (updated 2023-10-02) and snapshot of the SC database (updated 2023-10-02).

Select annual climate data summaries for the WYNONA 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 2023-10-09).

Geomorphic description summaries for the WYNONA 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 2023-10-04).

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 WYNONA, 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 2023-10-02).

Block Diagrams

No block diagrams are available.

Map Units

Map units containing WYNONA 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
Wynona silt loam, occasionally flooded	8390	42	792107	vl7v	ks091	1976	1:24000
Wynona silt loam, occasionally flooded	8390	16	1468946	1l9kc	ks121	1979	1:24000
Dela and Wynona soils, 0 to 1 percent slopes, frequently flooded	Ra	24757	571610	m5t1	ok029	1969	1:24000
Wynona silt loam, 0 to 1 percent slopes, occasionally flooded	La	14614	571604	m5sv	ok029	1969	1:24000
Wynona silty clay loam, 0 to 1 percent slopes, occasionally flooded	Lc	7909	571605	m5sw	ok029	1969	1:24000
Wynona clay loam, 0 to 1 percent slopes, occasionally flooded	Vd	7708	571658	m5vl	ok063	1965	1:24000
Wynona silty clay loam, 0 to 1 percent slopes, occasionally flooded	Wa	13496	106605	2w221	ok105	1975	1:24000
Wynona silt loam, 0 to 1 percent slopes, occasionally flooded	WynA	1570	384222	2w220	ok107	1996	1:24000
Wynona silty clay loam, 0 to 1 percent slopes, occasionally flooded	70	16099	623465	2w221	ok113	1975	1:24000
Wynona-Urban land complex, 0 to 1 percent slopes, occasionally flooded	WyUA	8	1427103	1jx0l	ok113	1975	1:24000
Wynona silty clay loam, 0 to 1 percent slopes, frequently flooded	Ka	1029	106631	3kyq	ok115	1961	1:24000
Wynona silty clay loam, 0 to 1 percent slopes, occasionally flooded	Ar	2466	384599	dx6f	ok123	1967	1:24000
Wynona silt loam, 0 to 1 percent slopes, occasionally flooded	50	1773	384839	2w220	ok133	1976	1:24000
Wynona silty clay loam, 0 to 1 percent slopes, occasionally flooded	53	13005	106737	2w221	ok143	1975	1:12000
Wynona-Urban land complex, 0 to 1 percent slopes, occasionally flooded	54	1669	106738	3l25	ok143	1975	1:12000

Map of Series Extent

Approximate geographic distribution of the WYNONA 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 2023-10-04).