Soil Data Explorer - WERNER

Official Series Description

Lab Data Summary

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

There are insufficient data to create the annual climate figure.

Geomorphic description summaries for the WERNER 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 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 WERNER, 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

Click a link below to display the diagram. Note that these diagrams may be from multiple survey areas.

1. ND-2012-02-08-29 | McIntosh County - 2001

   Typical pattern of soils and underlying materials in the Amor-Arnegard-Werner association (Soil Survey of McIntosh County, North Dakota; 2001).

Map Units

Map units containing WERNER 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
Werner-Amor-Arnegard loams, 9 to 50 percent slopes	E2651F	13285	2661744	2r8lh	nd015	1967	1:20000
Werner-Chama-Sen silt loams, 9 to 15 percent slopes	E2747D	10500	2661727	2r6tt	nd015	1967	1:20000
Sen-Werner complex, 9 to 15 percent slopes	C964D	7779	2564197	2q83f	nd015	1967	1:20000
Werner-Amor-Arnegard loams, 9 to 50 percent slopes	C962F	2729	2596905	2q83c	nd015	1967	1:20000
Sen-Werner complex, 6 to 9 percent slopes	C964C	218	2564183	2q73l	nd015	1967	1:20000
Sen-Werner loams, 6 to 9 percent slopes	E2765C	108	2661740	2r8l0	nd015	1967	1:20000
Amor-Werner loams, 9 to 15 percent slopes	E2607D	23	2661738	2r4hx	nd015	1967	1:20000
Amor-Werner-Farnuf loams, 6 to 9 percent slopes	E2609C	3	2661739	2r4hy	nd015	1967	1:20000
Werner-Amor-Arnegard loams, 9 to 50 percent slopes	E2651F	2890	2758481	2r8lh	nd025	1981	1:20000
Amor-Werner loams, 6 to 15 percent slopes, very stony	E2998D	1670	2707214	2r6tp	nd025	1981	1:20000
Werner-Chama-Sen silt loams, 9 to 15 percent slopes	E2747D	282	2758482	2r6tt	nd025	1981	1:20000
Amor-Werner loams, 9 to 15 percent slopes	E2607D	164	2758479	2r4hx	nd025	1981	1:20000
Amor-Werner-Farnuf loams, 6 to 9 percent slopes	E2609C	51	2758480	2r4hy	nd025	1981	1:20000
Werner-Amor-Arnegard loams, 9 to 50 percent slopes	E2651F	43221	2661841	2r8lh	nd029	1979	1:20000
Amor-Werner loams, 3 to 6 percent slopes	E2607B	26075	2661836	2r4hw	nd029	1979	1:20000
Amor-Werner loams, 9 to 15 percent slopes	E2607D	12634	2661837	2r4hx	nd029	1979	1:20000
Werner-Amor loams, 9 to 15 percent slopes	E2611D	7889	2661839	2r4hz	nd029	1979	1:20000
Amor-Werner-Farnuf loams, 6 to 9 percent slopes	E2609C	6174	2661838	2r4hy	nd029	1979	1:20000
Reeder-Werner loams, 9 to 15 percent slopes	E2641D	1420	2661840	2r8lf	nd029	1979	1:20000
Amor-Werner loams, 9 to 15 percent slopes	C903D	1404	2596835	2q53v	nd029	1979	1:20000
Amor-Werner loams, 6 to 15 percent slopes, very stony	E2998D	578	2661817	2r6tp	nd029	1979	1:20000
Werner-Amor-Arnegard loams, 9 to 50 percent slopes	C962F	463	2595828	2q83c	nd029	1979	1:20000
Amor-Werner-Farnuf loams, 6 to 9 percent slopes	E2609C	6686	2661892	2r4hy	nd047	1992	1:20000
Amor-Werner loams, 9 to 15 percent slopes	E2607D	6453	2661891	2r4hx	nd047	1992	1:20000
Amor-Werner loams, 3 to 6 percent slopes	E2607B	5259	2661890	2r4hw	nd047	1992	1:20000
Amor-Werner loams, 9 to 15 percent slopes	C903D	1558	2566520	2q53v	nd047	1992	1:20000
Werner-Amor-Arnegard loams, 9 to 50 percent slopes	E2651F	1256	2661893	2r8lh	nd047	1992	1:20000
Werner-Amor-Arnegard loams, 9 to 50 percent slopes	C962F	630	2566543	2q83c	nd047	1992	1:20000
Werner-Amor-Arnegard loams, 9 to 50 percent slopes	E2651F	1673	2662028	2r8lh	nd051	1992	1:24000
Amor-Werner loams, 9 to 15 percent slopes	C903D	1448	2566610	2q53v	nd051	1992	1:24000
Amor-Werner-Farnuf loams, 6 to 9 percent slopes	E2609C	1431	2662027	2r4hy	nd051	1992	1:24000
Amor-Werner loams, 9 to 15 percent slopes	E2607D	1428	2662026	2r4hx	nd051	1992	1:24000
Amor-Werner loams, 3 to 6 percent slopes	E2607B	1132	2662025	2r4hw	nd051	1992	1:24000
Werner-Amor-Arnegard loams, 9 to 50 percent slopes	C962F	74	2566629	2q83c	nd051	1992	1:24000
Amor-Werner loams, 6 to 15 percent slopes, very stony	E2998D	27	2662016	2r6tp	nd051	1992	1:24000
Reeder-Werner loams, 6 to 9 percent slopes	E2641C	1484	2715078	d346	nd053	2003	1:24000
Werner-Amor-Arnegard loams, 9 to 50 percent slopes	E2651F	25682	2662496	2r8lh	nd055	1974	1:20000
Zahl-Werner complex, 15 to 35 percent slopes	C966F	4883	2566720	2q73f	nd055	1974	1:20000
Dogtooth-Janesburg-Werner complex, 3 to 25 percent slopes	C593E	6	2567157	2q6md	nd055	1974	1:20000
Werner-Amor-Arnegard loams, 9 to 50 percent slopes	E2651F	64016	2699388	2r8lh	nd057	1976	1:20000
Werner-Chama-Sen silt loams, 9 to 15 percent slopes	E2747D	18915	2699389	2r6tt	nd057	1976	1:20000
Amor-Werner-Farnuf loams, 6 to 9 percent slopes	E2609C	10075	2699238	2r4hy	nd057	1976	1:20000
Amor-Werner loams, 9 to 15 percent slopes	E2607D	4810	2755726	2r4hx	nd057	1976	1:20000
Werner-Amor-Arnegard loams, 9 to 50 percent slopes	E2651F	985	2759673	2r8lh	nd059	1998	1:20000
Werner-Chama-Sen silt loams, 9 to 15 percent slopes	E2747D	162	2759674	2r6tt	nd059	1998	1:20000
Dogtooth-Janesburg-Werner complex, 3 to 25 percent slopes	C593E	2520	2566775	2q6md	nd061	1988	1:24000
Werner-Amor-Zahl loams, 25 to 60 percent slopes	C908F	675	2597015	2q6lr	nd061	1988	1:24000
Amor-Zahl-Werner loams, 9 to 25 percent slopes	C906E	59	2567103	2q1nq	nd061	1988	1:24000
Werner-Amor-Arnegard loams, 9 to 50 percent slopes	E2651F	37878	2525947	2r8lh	nd065	1971	1:20000
Werner-Chama-Sen silt loams, 9 to 15 percent slopes	E2747D	17288	2525948	2r6tt	nd065	1971	1:20000
Amor-Werner-Farnuf loams, 6 to 9 percent slopes	E2609C	9920	2525946	2r4hy	nd065	1971	1:20000
Morton-Werner silt loams, 6 to 9 percent slopes	E2933C	5688	2525955	2r6v2	nd065	1971	1:20000
Sen-Werner loams, 6 to 9 percent slopes	E2765C	1628	2525950	2r8l0	nd065	1971	1:20000
Amor-Werner loams, 9 to 15 percent slopes	E2607D	1171	2525945	2r4hx	nd065	1971	1:20000
Amor-Werner loams, 6 to 15 percent slopes, very stony	E2998D	512	2525957	2r6tp	nd065	1971	1:20000
Morton-Werner silt loams, 9 to 15 percent slopes	E2933D	269	2525956	2r6v3	nd065	1971	1:20000
Sen-Werner loams, 3 to 6 percent slopes	E2765B	123	2525949	2qz90	nd065	1971	1:20000
Amor-Zahl-Werner loams, 9 to 25 percent slopes	C906E	3952	2567029	2q1nq	nd105	1993	1:24000
Werner-Amor-Zahl loams, 25 to 60 percent slopes	C908F	1735	2567037	2q6lr	nd105	1993	1:24000
Watrous-Werner loams, 2 to 6 percent slopes	WaB	4165	355811	cy7s	sd063	1984	1:24000
Werner-Watrous loams, 2 to 9 percent slopes	WeC	3938	355814	cy7w	sd063	1984	1:24000
Amor-Werner loams, 2 to 6 percent slopes	AeB	3838	355711	cy4k	sd063	1984	1:24000
Werner-Reva complex, 3 to 9 percent slopes	WdC	482	355813	cy7v	sd063	1984	1:24000

Map of Series Extent

Approximate geographic distribution of the WERNER 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).