Soil Data Explorer - WINTERFIELD

Official Series Description

Lab Data Summary

Aggregate lab data for the WINTERFIELD soil series. This aggregation is based on all pedons with a current taxon name of WINTERFIELD, 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 WINTERFIELD were used in the calculation. Source: KSSL snapshot (updated 2020-03-18). Methods used to assemble the KSSL snapshot used by SoilWeb / SDE

Pedons used in the lab summary:

MLRA	Lab ID	Pedon ID	Taxonname	CI	NSSL / NASIS Reports	Link To SoilWeb GMap
88	UMN2553	S1978MN0612553	Winterfield	3	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	47.1573944,-93.4137268

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the WINTERFIELD 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 WINTERFIELD 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 WINTERFIELD 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 WINTERFIELD 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 WINTERFIELD 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 WINTERFIELD 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 WINTERFIELD 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 mountains figure.

Soil series sharing subgroup-level classification with WINTERFIELD, 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 WINTERFIELD 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
Winterfield fine sandy loam	70	851	415013	fxvj	mi013	1984	1:20000
Winterfield-Evart complex	Wn	5182	189652	6cbt	mi035	1977	1:15840
Evart-Winterfield association	EW	2360	189778	6cgw	mi051	1966	1:15840
Winterfield loamy sand, 0 to 2 percent slopes	406A	1304	191852	6fms	mi069	1995	1:15840
Winterfield loamy sand, rarely flooded, 0 to 2 percent slopes	406A	155	190727	6dgh	mi079	1998	1:12000
Winterfield loamy fine sand, 0 to 3 percent slopes	69A	173	190932	6dp3	mi141	1989	1:15840
Winterfield sand	34	1839	190768	6dht	mi600	1983	1:15840
Pengilly-Winterfield association	872	838	432979	gjk2	mn001	1996	1:20000
Fordum-Winterfield complex, 0 to 2 percent slopes, frequently flooded	Fo	183	885885	yqty	mn003	1972	1:15840
Fordum-Winterfield complex, 0 to 2 percent slopes, frequently flooded	1011A	2519	1899594	21rp7	mn009	2007	1:12000
Fordum-Winterfield complex, 0 to 4 percent slopes, flooded	1011A	377	2732687	2slnc	mn035	2009	1:24000
Fordum-Winterfield complex, 0 to 2 percent slopes, frequently flooded	D19A	466	451585	h4x8	mn053	2001	1:12000
Pengilly-Winterfield association	872	20509	398481	fcn7	mn061	1982	1:24000
Fordum-Winterfield complex, 0 to 2 percent slopes, frequently flooded	1011A	622	1676335	1t8cb	mn095	2006	1:12000
Fordum-Winterfield complex	1946	9973	400358	ffls	mn097	1987	1:20000
Winterfield loamy fine sand, 1 to 3 percent slopes, occasionally flooded	I832A	1392	2799745	2sw9t	mn119	1996	1:20000
Fordum-Winterfield complex, 0 to 2 percent slopes, frequently flooded	1946	5324	431467	ggz9	mn141	1994	1:15840
Fordum-Winterfield complex, 0 to 2 percent slopes, frequently flooded	1946	390	435090	glr5	mn171	1998	1:12000
Winterfield-Evart complex, river valleys, 0 to 3 percent slopes, frequently flooded	WiEvA	7187	3053867	2xk6s	wi001	1978	1:20000
Winterfield-Fordum complex, river valleys, 0 to 3 percent slopes, frequently flooded	WiFoA	4768	3053866	2xk6r	wi001	1978	1:20000
Pelkie-Winterfield loamy fine sands, river valleys, 0 to 3 percent slopes, occasionally flooded	PeWiA	2180	3182114	2xvsg	wi001	1978	1:20000
Totagatic-Winterfield complex, 0 to 2 percent slopes, frequently flooded	64A	3282	816926	wf2g	wi013	2004	1:12000
Winterfield-Totagatic complex, 0 to 2 percent slopes, frequently flooded	706A	1571	816940	wf2x	wi013	2004	1:12000
Pelkie-Winterfield loamy fine sands, river valleys, 0 to 3 percent slopes, occasionally flooded	PeWiA	893	431913	2xvsg	wi019	1994	1:20000
Winterfield-Fordum complex, river valleys, 0 to 3 percent slopes, frequently flooded	WiFoA	386	3053868	2xk6r	wi019	1994	1:20000
Winterfield-Evart complex, river valleys, 0 to 3 percent slopes, frequently flooded	WiEvA	61	3182040	2xk6s	wi021	1972	1:15840
Pelkie-Winterfield loamy fine sands, river valleys, 0 to 3 percent slopes, occasionally flooded	PeWiA	48	3182039	2xvsg	wi021	1972	1:15840
Winterfield-Fordum complex, river valleys, 0 to 3 percent slopes, frequently flooded	WiFoA	47	3182041	2xk6r	wi021	1972	1:15840
Totagatic-Winterfield complex, 0 to 2 percent slopes, frequently flooded	64A	932	781071	v6rv	wi031	2005	1:12000
Winterfield-Totagatic complex, 0 to 2 percent slopes, frequently flooded	706A	771	781442	v74t	wi031	2005	1:12000
Pelkie-Winterfield loamy fine sands, river valleys, 0 to 3 percent slopes, occasionally flooded	PeWiA	1394	3099885	2xvsg	wi035	1974	1:15840
Winterfield-Fordum complex, river valleys, 0 to 3 percent slopes, frequently flooded	WiFoA	1086	3182132	2xk6r	wi035	1974	1:15840
Winterfield-Evart complex, river valleys, 0 to 3 percent slopes, frequently flooded	WiEvA	119	3182131	2xk6s	wi035	1974	1:15840
Winterfield-Fordum complex, river valleys, 0 to 3 percent slopes, frequently flooded	WiFoA	704	3053872	2xk6r	wi053	1994	1:20000
Pelkie-Winterfield loamy fine sands, river valleys, 0 to 3 percent slopes, occasionally flooded	PeWiA	145	3182137	2xvsg	wi053	1994	1:20000
Winterfield-Fordum complex, river valleys, 0 to 3 percent slopes, frequently flooded	WiFoA	13266	2561524	2xk6r	wi057	1987	1:15840
Pelkie-Winterfield loamy fine sands, river valleys, 0 to 3 percent slopes, occasionally flooded	PeWiA	372	3182148	2xvsg	wi057	1987	1:15840
Winterfield-Evart complex, river valleys, 0 to 3 percent slopes, frequently flooded	WiEvA	40	3182151	2xk6s	wi057	1987	1:15840
Winterfield fine sandy loam, 0 to 2 percent slopes	Wf	8406	422524	g5nt	wi083	1985	1:15840
Totagatic-Winterfield complex, 0 to 2 percent slopes, frequently flooded	64A	515	2427692	2mh6n	wi095	1978	1:15840
Winterfield-Fordum complex, river valleys, 0 to 3 percent slopes, frequently flooded	WiFoA	5115	3053878	2xk6r	wi097	1972	1:20000
Winterfield-Evart complex, river valleys, 0 to 3 percent slopes, frequently flooded	WiEvA	1295	3053877	2xk6s	wi097	1972	1:20000
Pelkie-Winterfield loamy fine sands, river valleys, 0 to 3 percent slopes, occasionally flooded	PeWiA	506	3182163	2xvsg	wi097	1972	1:20000
Winterfield-Fordum complex, river valleys, 0 to 3 percent slopes, frequently flooded	WiFoA	239	3182097	2xk6r	wi111	1977	1:15840
Winterfield-Evart complex, river valleys, 0 to 3 percent slopes, frequently flooded	WiEvA	96	3182172	2xk6s	wi111	1977	1:15840
Pelkie-Winterfield loamy fine sands, river valleys, 0 to 3 percent slopes, occasionally flooded	PeWiA	6	3182170	2xvsg	wi111	1977	1:15840
Totagatic-Winterfield complex, 0 to 2 percent slopes, frequently flooded	64A	1012	435469	gm4d	wi129	2002	1:12000
Winterfield-Totagatic complex, 0 to 2 percent slopes, frequently flooded	706A	72	433550	gk4h	wi129	2002	1:12000
Winterfield-Evart complex, river valleys, 0 to 3 percent slopes, frequently flooded	WiEvA	222	3182174	2xk6s	wi137	1986	1:20000
Winterfield-Fordum complex, river valleys, 0 to 3 percent slopes, frequently flooded	WiFoA	7287	3053879	2xk6r	wi141	1971	1:20000
Winterfield-Evart complex, river valleys, 0 to 3 percent slopes, frequently flooded	WiEvA	1788	3053880	2xk6s	wi141	1971	1:20000
Pelkie-Winterfield loamy fine sands, river valleys, 0 to 3 percent slopes, occasionally flooded	PeWiA	1547	3182201	2xvsg	wi141	1971	1:20000

Map of Series Extent

Approximate geographic distribution of the WINTERFIELD 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).