Soil Data Explorer - VIENNA

Official Series Description

Lab Data Summary

Aggregate lab data for the VIENNA soil series. This aggregation is based on all pedons with a current taxon name of VIENNA, 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 VIENNA were used in the calculation. Source: KSSL snapshot (updated 2020-03-13). 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
102A	40A2472	S1958SD029004	Vienna	7	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	44.8650017,-97.026947
102A	UMN1091	S1970MN1171091	Vienna	3	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	43.995079,-96.1117935
102A	UMN1312	S1971MN1171312	Vienna	4	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	44.0538673,-96.2938919
102A	UMN1315	S1971MN1171315	Vienna	5	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	44.0909157,-96.1257095
102A	UMN3202	S1979MN1013202	Vienna	3	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	43.9408875,-96.0513992

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the VIENNA 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 VIENNA 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 VIENNA 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 VIENNA 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 VIENNA 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 VIENNA 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 VIENNA 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.

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

Soil series sharing subgroup-level classification with VIENNA, 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

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

1. SD-2010-11-01-02 | Brookings County - 2004

   Typical pattern of soils and parent material in the Kranzburg-Brookings association (Soil Survey of Brookings County, South Dakota; 2004).

2. SD-2010-11-01-04 | Brookings County - 2004

   Typical pattern of soils and parent material in the Buse-Barnes-Lamoure association (Soil Survey of Brookings County, South Dakota; 2004).

3. SD-2010-11-01-09 | Hamlin County - 2003

   Typical pattern of soils and underlying material in the Kranzburg-Brookings association (Soil Survey of Hamlin County, South Dakota; 2003).

4. SD-2012-03-15-02 | Codington County - December 1966

   Diagram showing the relative position of the major soils in association 3 (Soil Survey of Codington County, SD; 1966).

5. SD-2012-03-15-04 | Codington County - December 1966

   Diagram showing the relative position of the major soils in association 6 in the valley of the Big Sioux River (Soil Survey of Codington County, SD; 1966).

6. SD-2012-03-15-27 | Deuel County - November 1997

   Typical pattern of soils and parent material in the Kranzburg-Brookings association (Soil Survey of Deuel County, SD; 1997).

Map Units

Map units containing VIENNA 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
Vienna silty clay loam, 3 to 6 percent slopes	J86B	3424	991443	128p1	mn081	2007	1:12000
Buse-Vienna complex, 6 to 12 percent slopes, moderately eroded	J92C2	1565	991444	128p2	mn081	2007	1:12000
Vienna-Brookings complex, 1 to 6 percent slopes	J79B	1186	991442	2wkpx	mn081	2007	1:12000
Vienna-Brookings complex, 1 to 6 percent slopes	J79B	3978	988905	2wkpx	mn101	2008	1:12000
Vienna silty clay loam, 3 to 6 percent slopes	J86B	2061	988906	12616	mn101	2008	1:12000
Buse-Vienna complex, 6 to 12 percent slopes, moderately eroded	J92C2	234	988888	1260m	mn101	2008	1:12000
Vienna silty clay loam, 3 to 6 percent slopes	J86B	10995	780671	v6by	mn117	2005	1:12000
Vienna-Brookings complex, 1 to 6 percent slopes	J79B	3789	780668	2wkpx	mn117	2005	1:12000
Buse-Vienna complex, 6 to 12 percent slopes, moderately eroded	J92C2	3692	780287	v5yk	mn117	2005	1:12000
Vienna-Brookings complex, 1 to 6 percent slopes	VbB	12908	418818	2wkpx	sd011	1995	1:24000
Vienna-Brookings complex, 0 to 2 percent slopes	VbA	9686	418817	2wkpw	sd011	1995	1:24000
Vienna-Buse complex, 6 to 9 percent slopes	VnC	5008	418820	g1tb	sd011	1995	1:24000
Vienna-Buse complex, 2 to 6 percent slopes	VnB	1219	418819	g1t9	sd011	1995	1:24000
Vienna-Brookings complex, 1 to 6 percent slopes	Z192B	28105	2765246	2wkpx	sd029	2006	1:12000
Vienna-Brookings complex, 0 to 2 percent slopes	Z192A	19321	2765245	2wkpw	sd029	2006	1:12000
Vienna-Barnes-Forestville loams, 1 to 6 percent slopes	Z199B	3861	3333632	2wkrj	sd029	2006	1:12000
Vienna-Buse complex, coteau, 6 to 9 percent slopes	Z193C	2284	2765247	2qkm3	sd029	2006	1:12000
Vienna-Forestville loams, coteau, 0 to 2 percent slopes	Z198A	757	2765250	2qkm6	sd029	2006	1:12000
Vienna-Brookings complex, 1 to 6 percent slopes	VoB	2082	417142	2wkpx	sd037	1992	1:20000
Vienna-Brookings complex, 0 to 2 percent slopes	VoA	510	417141	2wkpw	sd037	1992	1:20000
Vienna-Brookings complex, 1 to 6 percent slopes	VtB	22547	416911	2wkpx	sd039	1992	1:20000
Vienna-Brookings complex, 0 to 2 percent slopes	VrA	7437	416910	2wkpw	sd039	1992	1:20000
Vienna-Barnes-Forestville loams, 1 to 6 percent slopes	VzB	5379	3333633	2wkrj	sd039	1992	1:20000
Vienna-Buse complex, 6 to 9 percent slopes	VwC	3109	416912	fzts	sd039	1992	1:20000
Vienna-Forestville loams, 0 to 2 percent slopes	VzA	113	1670164	1t1y8	sd039	1992	1:20000
Vienna-Forestville loams, coteau, 0 to 2 percent slopes	Z198A	1	2712979	2qkm6	sd039	1992	1:20000
Vienna-Brookings complex, 1 to 6 percent slopes	Z192B	13515	2712902	2wkpx	sd051	1977	1:20000
Vienna-Brookings complex, 0 to 2 percent slopes	Z192A	10027	2712901	2wkpw	sd051	1977	1:20000
Vienna-Barnes-Forestville loams, 1 to 6 percent slopes	Z199B	8420	3333634	2wkrj	sd051	1977	1:20000
Vienna-Forestville loams, coteau, 0 to 2 percent slopes	Z198A	1086	2712906	2qkm6	sd051	1977	1:20000
Vienna-Buse complex, coteau, 6 to 9 percent slopes	Z193C	977	2712903	2qkm3	sd051	1977	1:20000
Vienna-Brookings complex, 1 to 6 percent slopes	VbB	17531	417319	2wkpx	sd057	1992	1:20000
Vienna-Brookings complex, 0 to 2 percent slopes	VbA	5074	417318	2wkpw	sd057	1992	1:20000
Vienna-Buse complex, 6 to 9 percent slopes	VnC	2052	417321	g07z	sd057	1992	1:20000
Barnes-Vienna complex, 0 to 2 percent slopes	BnA	459	3333637	2yyjd	sd057	1992	1:20000
Vienna-Brookings complex, 1 to 6 percent slopes	VbB	2204	417521	2wkpx	sd077	1992	1:20000
Vienna-Brookings complex, 0 to 2 percent slopes	VbA	834	417520	2wkpw	sd077	1992	1:20000
Kranzburg-Vienna silt loams, 6 to 9 percent slopes	G790C	903	2799376	2sd5s	sd091	1970	1:20000
Vienna-Brookings complex, 1 to 6 percent slopes	Z192B	8683	2712797	2wkpx	sd109	1977	1:20000
Vienna-Barnes-Forestville loams, 1 to 6 percent slopes	Z199B	3262	3333635	2wkrj	sd109	1977	1:20000
Vienna-Brookings complex, 0 to 2 percent slopes	Z192A	2978	2712796	2wkpw	sd109	1977	1:20000
Vienna-Buse complex, coteau, 6 to 9 percent slopes	Z193C	838	2712798	2qkm3	sd109	1977	1:20000
Vienna, very stony-Barnes, very stony-Forestville loams, 1 to 6 percent slopes	Z298B	256	3333636	2yyj8	sd109	1977	1:20000
Vienna-Forestville loams, coteau, 0 to 2 percent slopes	Z198A	54	2712799	2qkm6	sd109	1977	1:20000

Map of Series Extent

Approximate geographic distribution of the VIENNA 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).