Soil Data Explorer - SVERDRUP

Official Series Description

Lab Data Summary

Aggregate lab data for the SVERDRUP soil series. This aggregation is based on all pedons with a current taxon name of SVERDRUP, 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 SVERDRUP 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
102A	87P0576	87MN051001	Sverdrup	7	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	45.9963875,-95.8713913
102A	87P0577	87MN051001A	Sverdrup	6	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	45.9963875,-95.8686142
102A	87P0578	87MN051001B	Sverdrup	6	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	45.998333,-95.8713913
102A	87P0580	87MN051001D	Sverdrup	6	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	45.9972229,-95.8702774
102A	UMN1078	S1970MN1171078	Sverdrup	3	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	44.0872955,-96.1459122
102A	UMN1111	S1970MN1171111	Sverdrup	3	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	44.1874847,-96.4272079
102A	UMN1937	S1975MN1731937	Sverdrup	2	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	44.767198,-96.298592
102A	UMN3260	S1979MN1013260	Sverdrup	2	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	44.0542831,-95.8069534
102A	87P0579	S1987MN051001C	Sverdrup	6	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	45.998333,-95.8686142
91A	UMN1751	S1974MN0271751	Sverdrup	3	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	46.7174644,-96.1891251

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the SVERDRUP 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 SVERDRUP 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 SVERDRUP 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 SVERDRUP 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 SVERDRUP 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 SVERDRUP 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 SVERDRUP 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 SVERDRUP, 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. MN-2010-09-08-21 | Otter Tail County - 2001

   Typical pattern of soils and parent material in the Arvilla-Sverdrup-Sandberg association (Soil Survey of Otter Tail County, Minnesota; 2001).

Map Units

Map units containing SVERDRUP 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
Sverdrup-Abbeylake complex, 1 to 6 percent slopes	1125B	1049	397410	fbjp	mn005	1994	1:20000
Sverdrup-Abbeylake complex, 6 to 12 percent slopes	1125C	235	397411	fbjq	mn005	1994	1:20000
Sverdrup sandy loam, 2 to 6 percent slopes	127B	2463	396055	2thb1	mn011	1990	1:20000
Sverdrup sandy loam, 2 to 6 percent slopes	J7B	1560	2423029	2thb1	mn023	1980	1:15840
Sverdrup sandy loam, 6 to 12 percent slopes	127C	544	396493	2thb3	mn023	1980	1:15840
Sverdrup sandy loam, 0 to 2 percent slopes	J7A	500	2423028	2th9y	mn023	1980	1:15840
Sverdrup sandy loam, 2 to 6 percent slopes	127B	2898	356937	2thb1	mn027	1980	1:20000
Sioux-Sverdrup complex, 6 to 18 percent slopes	892C	1650	357016	czhn	mn027	1980	1:20000
Sverdrup sandy loam, 6 to 12 percent slopes	127C	1067	356938	2thb3	mn027	1980	1:20000
Sioux-Sverdrup complex, 1 to 6 percent slopes	892B	557	357015	czhm	mn027	1980	1:20000
Sverdrup sandy loam, 0 to 2 percent slopes	SpA	3627	397326	2th9y	mn041	1970	1:12000
Sverdrup sandy loam, 2 to 6 percent slopes	SpB	3217	397327	2thb1	mn041	1970	1:12000
Sverdrup loam, thick solum, 0 to 3 percent slopes	SvA	1400	397329	fbg2	mn041	1970	1:12000
Sverdrup sandy loam, 6 to 12 percent slopes	SpC	575	397328	2thb3	mn041	1970	1:12000
Sverdrup sandy loam, 2 to 6 percent slopes	127B	2712	398023	2thb1	mn051	1974	1:20000
Sverdrup sandy loam, 2 to 6 percent slopes	27B	586	398683	2thb1	mn067	1983	1:20000
Sverdrup sandy loam, 2 to 6 percent slopes	127B	8218	430222	2thb1	mn073	1994	1:20000
Sverdrup sandy loam, 0 to 2 percent slopes	127A	1468	430221	2th9y	mn073	1994	1:20000
Sverdrup sandy loam, 6 to 12 percent slopes	127C	611	430223	2thb3	mn073	1994	1:20000
Sverdrup sandy loam, 2 to 6 percent slopes	J7B	597	991447	2thb1	mn081	2007	1:12000
Sverdrup sandy loam, 2 to 6 percent slopes	J7B	991	1486202	2thb1	mn083	2008	1:12000
Sverdrup sandy loam, 0 to 2 percent slopes	J7A	220	1486242	2th9y	mn083	2008	1:12000
Sverdrup sandy loam, 2 to 6 percent slopes	127B	1688	399210	2thb1	mn087	1992	1:20000
Sverdrup sandy loam, 2 to 6 percent slopes	J7B	1345	1147606	2thb1	mn101	2008	1:12000
Sverdrup sandy loam, 6 to 12 percent slopes	127C	362	1859424	20dwf	mn101	2008	1:12000
Sverdrup sandy loam, 0 to 2 percent slopes	J7A	253	1147605	2th9y	mn101	2008	1:12000
Sverdrup sandy loam, 0 to 2 percent slopes	SnA	854	357266	2th9y	mn107	1970	1:20000
Sverdrup sandy loam, 2 to 6 percent slopes	SnC	637	357267	2thb1	mn107	1970	1:20000
Sverdrup sandy loam, 2 to 6 percent slopes	127B	4068	435595	2thb1	mn111	1996	1:20000
Sverdrup-Sandberg complex, 2 to 6 percent slopes	1221B	3488	435569	gm7m	mn111	1996	1:20000
Sandberg-Sverdrup complex, 6 to 12 percent slopes	1219C	3276	435568	gm7l	mn111	1996	1:20000
Sverdrup sandy loam, 0 to 2 percent slopes	127A	1264	435594	2th9y	mn111	1996	1:20000
Sverdrup sandy loam, 6 to 12 percent slopes	127C	1217	435596	2thb3	mn111	1996	1:20000
Corliss-Sverdrup complex, 12 to 20 percent slopes	1277D	959	435593	gm8d	mn111	1996	1:20000
Sverdrup sandy loam, 2 to 6 percent slopes	J7B	643	780529	2thb1	mn117	2005	1:12000
Sverdrup sandy loam, 0 to 2 percent slopes	J7A	224	780528	2th9y	mn117	2005	1:12000
Sverdrup sandy loam, 2 to 6 percent slopes	J7B	4320	401404	2thb1	mn121	1968	1:20000
Sverdrup sandy loam, 0 to 2 percent slopes	J7A	2832	401406	2th9y	mn121	1968	1:20000
Sverdrup sandy loam, 6 to 12 percent slopes	SyC2	1208	401405	2thb3	mn121	1968	1:20000
Sverdrup sandy loam, Sandy Outwash, 0 to 2 percent slopes	327A	9185	428121	2thb0	mn145	1980	1:15840
Sverdrup sandy loam, Sandy Outwash, 2 to 6 percent slopes	327B	7566	428122	2thb2	mn145	1980	1:15840
Sverdrup sandy loam, 0 to 2 percent slopes	SwA	908	428377	2th9y	mn149	1966	1:15840
Sverdrup sandy loam, 2 to 6 percent slopes	SwB	211	428378	2thb1	mn149	1966	1:15840
Sverdrup sandy loam, 2 to 6 percent slopes	J7B	5076	434770	2thb1	mn151	2000	1:12000
Sverdrup sandy loam, 0 to 2 percent slopes	J7A	1590	434769	2th9y	mn151	2000	1:12000
Sverdrup sandy loam, Sandy Outwash, 0 to 2 percent slopes	127A	3625	428497	2thb0	mn153	1985	1:20000
Sverdrup sandy loam, Sandy Outwash, 2 to 6 percent slopes	127B	2172	428498	2thb2	mn153	1985	1:20000
Sverdrup sandy loam, 6 to 12 percent slopes	127C	150	1653563	1shnr	mn173	1979	1:20000
Sverdrup sandy loam, 0 to 2 percent slopes	J7A	92	1481701	2th9y	mn173	1979	1:20000
Sverdrup sandy loam, 2 to 6 percent slopes	J7B	70	1481702	2thb1	mn173	1979	1:20000
Sverdrup sandy loam, 2 to 6 percent slopes	SwB	5421	417877	2thb1	sd109	1977	1:20000
Sverdrup sandy loam, 0 to 2 percent slopes	SwA	2450	417876	2th9y	sd109	1977	1:20000

Map of Series Extent

Approximate geographic distribution of the SVERDRUP 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).