Soil Data Explorer - WINTONER

Official Series Description

Lab Data Summary

Aggregate lab data for the WINTONER soil series. This aggregation is based on all pedons with a current taxon name of WINTONER, 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 WINTONER were used in the calculation. Source: KSSL snapshot (updated 2020-03-18). 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 WINTONER 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 WINTONER series. Sketches are arranged according to their subgroup-level taxonomic structure. Source: SSURGO snapshot (updated 2024-02-21), parsed OSD records (updated 2023-10-06) and snapshot of SC database (updated 2023-10-02).

Select annual climate data summaries for the WINTONER 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 WINTONER 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).

Competing Series

Soil series competing with WINTONER share the same family level classification in Soil Taxonomy. Source: parsed OSD records (updated 2023-10-06) and snapshot of the SC database (updated 2023-10-02).

Select annual climate data summaries for the WINTONER 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 WINTONER 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 3D flats position figure.

Soil series sharing subgroup-level classification with WINTONER, 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 WINTONER 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
Inville-Wintoner families complex, 2 to 15 percent slopes.	146	22735	470367	hsg4	ca702	1984	1:24000
Belzar-Wintoner, pumice overburden families complex, 2 to 15 percent slopes.	104	16469	470325	hsds	ca702	1984	1:24000
Belzar-Wintoner, pumice overburden, families, 15 to 50 percent slopes.	105	13490	470326	hsdt	ca702	1984	1:24000
Inville-Wintoner families association, 30 to 50 percent slopes.	147	8323	470368	hsg5	ca702	1984	1:24000
Merkel-Wintoner families complex, 50 to 80 percent slopes.	194	4044	470792	hswv	ca707	1983	1:24000
Wintoner-Jayar families complex, 20 to 50 percent slopes.	350	2759	470948	ht1w	ca707	1983	1:24000
Inville-Wintoner families complex, 0 to 35 percent slopes.	36	39399	471009	ht3v	ca708	1984	1:24000
Wintoner family-Aquolls-Patio family association, 0 to 15 percent slopes.	121	14811	471094	ht6l	ca708	1984	1:24000
Wintoner-Trojan-De Masters families association, 0 to 15 percent slopes.	122	8395	471095	ht6m	ca708	1984	1:24000
De Masters family-Lithic Haplxerolls-Wintoner family association, 0 to 35 percent slopes.	18	6903	470991	ht38	ca708	1984	1:24000
Inville-Klicker-Wintoner families association, 0 to 35 percent slopes.	30	5987	471003	ht3n	ca708	1984	1:24000
Inville-Klicker-Wintoner families association, 35 to 50 percent slopes.	31	4207	471004	ht3p	ca708	1984	1:24000
Inville-Wintoner families complex, 35 to 50 percent slopes.	37	4008	471010	ht3w	ca708	1984	1:24000
Wintoner-Yallani families complex, 0 to 35 percent slopes.	123	2610	471096	ht6n	ca708	1984	1:24000
Trojan-Klicker-Wintoner families association, 0 to 35 percent slopes.	109	311	471082	ht66	ca708	1984	1:24000
Inville-Wintoner families complex, 35 to 50 percent slopes.	L37	52	1546123	1nwvy	ca713	1984	1:24000
Wintoner-Tallac families complex, 15 to 40 percent slop es	199	19926	465073	hlyc	ca731	1981	1:24000
Wintoner family, 5 to 35 percent slopes	197	14796	465071	hly9	ca731	1981	1:24000
Gerle, deep-Wintoner families complex, 5 to 35 percent slopes	120	12155	464996	hlvw	ca731	1981	1:24000
Gerle, deep-Wintoner families complex, 35 to 50 percent slopes	121	5337	464997	hlvx	ca731	1981	1:24000
Wintoner-Inville families complex, 15 to 40 percent slo pes	198	1406	465072	hlyb	ca731	1981	1:24000
Wintoner silt loam, 3 to 8 percent slopes	WnB	595	73412	2gd4	wa607	1969	1:20000
Wintoner silt loam, 8 to 15 percent slopes	WnC	332	73413	2gd5	wa607	1969	1:20000
Wintoner silt loam, 0 to 3 percent slopes	WnA	298	73411	2gd3	wa607	1969	1:20000

Map of Series Extent

Approximate geographic distribution of the WINTONER 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).