Soil Data Explorer - WEINGART

Official Series Description

Lab Data Summary

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

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

Competing Series

Soil series competing with WEINGART 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 WEINGART 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 WEINGART 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 WEINGART, 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 WEINGART 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
Weingart silty clay, 2 to 8 percent slopes	15C	9437	342924	chv2	mt011	1992	1:24000
Orinoco-Weingart complex, 4 to 15 percent slopes	253D	7477	343046	chz0	mt011	1992	1:24000
Weingart silty clay loam, warm, 0 to 6 percent slopes	620C	311	343178	cj38	mt011	1992	1:24000
Weingart-Ivanell clay loams, 2 to 8 percent slopes	75C	14483	343663	cjlx	mt017	1995	1:24000
Delpoint-Weingart complex, 4 to 25 percent slopes	554E	4529	343538	cjgw	mt017	1995	1:24000
Abor-Weingart-Neldore complex, 2 to 15 percent slopes	959D	102	343800	2zg65	mt017	1995	1:24000
Pinehill-Weingart-Gerdrum complex, 0 to 6 percent slopes	993C	60	343834	cjsf	mt017	1995	1:24000
Weingart-Neldore complex, 4 to 25 perecent slopes	667E	32	343638	2xyn5	mt017	1995	1:24000
Weingart clay loam, 2 to 8 percent slopes	15C	6116	342104	cgzm	mt025	1991	1:24000
Orinoco-Weingart complex, 4 to 15 percent slopes	253D	651	342168	ch1p	mt025	1991	1:24000
Thebo-Weingart-Absher clays, 4 to 15 percent slopes	235	45546	342474	chck	mt027	1979	1:24000
Weingart-Gerdrum clay loams, 4 to 15 percent slopes	259	16828	342500	chdd	mt027	1979	1:24000
Weingart-Gerdrum clay loams, 0 to 4 percent slopes	258	3209	342499	chdc	mt027	1979	1:24000
Weingart-Absher clays, 0 to 4 percent slopes	260	2518	342502	chdg	mt027	1979	1:24000
Weingart very stony clay loam, 2 to 8 percent slopes	257	492	342498	chdb	mt027	1979	1:24000
Weingart clay, 2 to 8 percent slopes	95C	2973	342725	chmn	mt033	2002	1:24000
Weingart-Neldore complex, 4 to 25 perecent slopes	795E	1392	342727	2xyn5	mt033	2002	1:24000
Weingart, gullied-Niler, gullied-Rock outcrop, soft, complex, 2 to 25 percent slopes	796E	278	360659	d395	mt033	2002	1:24000
Weingart complex, 2 to 8 percent slopes	62C	3110	344020	cjzf	mt041	1994	1:24000
Creed-Weingart complex, 2 to 8 percent slopes	781C	1217	344264	ck79	mt051	1992	1:24000
Weingart clay, 2 to 8 percent slopes	155	2447	344355	ckb7	mt055	1981	1:24000
Weingart loam, 1 to 8 percent slopes	26A	1199	344536	cgjh	mt065	1996	1:24000
Weingart-Warhorse loams, 1 to 8 percent slopes	26B	214	344537	cgjj	mt065	1996	1:24000
Weingart silty clay loam, 1 to 8 percent slopes	91	12492	344764	ckrf	mt069	1989	1:24000
Weingart-Warhorse complex, 1 to 8 percent slopes	92	9668	344765	ckrg	mt069	1989	1:24000
Neldore-Weingart complex, 2 to 15 percent slopes	68	9262	344738	ckql	mt069	1989	1:24000
Tanna-Weingart complex, 2 to 8 percent slopes	76	5690	344747	ckqw	mt069	1989	1:24000
Abor-Weingart-Neldore complex, 2 to 15 percent slopes	3	3212	344862	2zg65	mt079	1986	1:24000
Pinelli-Weingart-Gerdrum complex, 0 to 6 percent slopes	105	1484	344781	ckrz	mt079	1986	1:24000
Neldore-Weingart-Kirby complex, 4 to 25 percent slopes	99	989	345055	cl1t	mt079	1986	1:24000
Megonot-Weingart-Delpoint complex, 0 to 4 percent slopes	141B	1647	346600	cmnn	mt615	1992	1:24000
Weingart loam, 1 to 8 percent slopes	26A	27	2513696	cgjh	mt624	2021	1:24000
Weingart-Assinniboine complex, 2 to 8 percent slopes	514B	2850	147840	4yv1	mt630	1991	1:24000
Megonot-Weingart complex, 8 to 35 percent slopes	149D	2240	147706	4ypq	mt630	1991	1:24000
Weingart clay loam, 2 to 8 percent slopes	614B	1316	147871	4yw1	mt630	1991	1:24000
Weingart-Musselshell complex, 2 to 8 percent slopes	714B	410	147897	4yww	mt630	1991	1:24000
Bascovy-Neldore-Weingart clays, 8 to 25 percent slopes	250E	33528	347648	cnrg	mt641	1994	1:24000
Sunburst-Bascovy-Weingart complex, 2 to 8 percent slopes	925C	15532	347810	cnxp	mt641	1994	1:24000
Weingart-Vaeda-Bascovy association, 4 to 25 percent slopes	1059E	9055	347567	cnnv	mt641	1994	1:24000
Weingart complex, 2 to 8 percent slopes	860C	6619	347790	cnx1	mt641	1994	1:24000
Kobase-Marvan-Weingart complex, 0 to 4 percent slopes	323B	904	347672	cns7	mt641	1994	1:24000
Weingart clay loam, 0 to 4 percent slopes	59B	490	347759	cnw1	mt641	1994	1:24000
Weingart-Niler-Rock outcrop complex, dissected, 2 to 25 percent slopes	196	11842	348026	cp4n	mt649	1985	1:24000
Weingart-Neldore complex, 4 to 25 perecent slopes	195	4701	348025	2xyn5	mt649	1985	1:24000
Weingart clay, 2 to 8 percent slopes	194	3185	348024	cp4l	mt649	1985	1:24000
Weingart-Warhorse loams, 1 to 8 percent slopes	26B	306	341667	cgjj	mt666	2008	1:24000
Weingart loam, 1 to 8 percent slopes	26A	288	341666	cgjh	mt666	2008	1:24000

Map of Series Extent

Approximate geographic distribution of the WEINGART 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).