Soil Data Explorer - SWANLAKE

Official Series Description

Lab Data Summary

Aggregate lab data for the SWANLAKE soil series. This aggregation is based on all pedons with a current taxon name of SWANLAKE, 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 SWANLAKE 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
103	UMN2103	S1975MN0332103	Swanlake	2	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	43.944416,-95.4358139
103	UMN2105	S1975MN0332105	Swanlake	2	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	43.9543877,-95.438736
103	UMN2792	S1978MN067150 (2792)	Swanlake	3	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	45.0629311,-95.2460632
103	UMN2816	S1979MN091014(2816)	Swanlake	3	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	43.7821503,-94.7517471

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the SWANLAKE 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 SWANLAKE 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 SWANLAKE 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 SWANLAKE 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 SWANLAKE 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 SWANLAKE 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 SWANLAKE 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 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 SWANLAKE, 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-2010-09-27-01 | Lac qui Parle County -

   Typical pattern of soils and underlying material in the Ves-Harps-Glencoe association (Soil Survey of Lac qui Parle County, Minnesota).

Map Units

Map units containing SWANLAKE 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
Reedslake-Swanlake complex, 3 to 12 percent slopes	L1213B	8	3111753	2y038	ia033	1978	1:15840
Clarion-Swanlake complex, 2 to 6 percent slopes	638B	1600	405612	2vvfb	ia063	1989	1:15840
Reedslake-Swanlake complex, 3 to 12 percent slopes	L1213B	40	3111756	2y038	ia081	1987	1:15840
Clarion-Swanlake complex, 2 to 6 percent slopes	638B	3330	408395	2vvfb	ia109	1980	1:15840
Clarion-Swanlake complex, 2 to 6 percent slopes	638B	319	410293	2vvfb	ia147	1973	1:15840
Clarion-Swanlake complex, 2 to 6 percent slopes	638B2	3164	412323	2vvfb	ia189	1984	1:15840
Reedslake-Swanlake complex, 3 to 12 percent slopes	L1213B	40	3111759	2y038	ia189	1984	1:15840
Clarion-Swanlake complex, 2 to 6 percent slopes	638B2	254	2398738	2vvfb	ia195	2012	1:12000
Reedslake-Swanlake complex, 3 to 12 percent slopes	L1213B	117	3111762	2y038	mn013	1975	1:12000
Amiret-Swanlake loams, 2 to 6 percent slopes	L223B	11849	2877271	2t3nk	mn015	1984	1:20000
Clarion-Swanlake complex, 2 to 6 percent slopes	921B2	2782	396315	2vvfb	mn015	1984	1:20000
Reedslake-Swanlake complex, 3 to 12 percent slopes	L1213B	17	3111765	2y038	mn019	1987	1:12000
Doland-Swanlake complex, 3 to 6 percent slopes, eroded	891B2	6735	396531	f9mb	mn023	1980	1:15840
Doland-Swanlake complex, 6 to 12 percent slopes, eroded	891C2	3698	396532	f9mc	mn023	1980	1:15840
Clarion-Swanlake complex, 2 to 6 percent slopes	L99B	11267	1596194	2vvfb	mn033	2008	1:12000
Amiret-Swanlake loams, 2 to 6 percent slopes	L223B	949	1590240	2t3nk	mn033	2008	1:12000
Swanlake-Round Lake complex, 2 to 6 percent slopes	L208B	751	1530023	1nc3l	mn033	2008	1:12000
Amiret-Swanlake-Round Lake complex, 2 to 6 percent slopes	L211B	428	1691090	1trq9	mn033	2008	1:12000
Annton-Swanlake, firm till, complex, 3 to 6 percent slopes	L248B	75	2406412	2ls26	mn033	2008	1:12000
Clarion-Swanlake complex, 2 to 6 percent slopes	887B	11811	397122	2vvfb	mn043	1989	1:20000
Swanlake-Terril complex, 18 to 40 percent slopes	1852F	892	397089	fb6b	mn043	1989	1:20000
Clarion-Swanlake complex, 2 to 6 percent slopes	921B	692	397890	2vvfb	mn047	1977	1:15840
Reedslake-Swanlake complex, 3 to 12 percent slopes	L1213B	267	3111772	2y038	mn047	1977	1:15840
Terril-Swanlake loams, 25 to 40 percent slopes	1852F	2225	398495	fcnp	mn063	1984	1:20000
Clarion-Swanlake loams, 12 to 18 percent slopes	887D	1505	398523	fcpl	mn063	1984	1:20000
Clarion-Swanlake loams, 6 to 12 percent slopes	887C	600	398522	fcpk	mn063	1984	1:20000
Amiret-Swanlake loams, 2 to 6 percent slopes	L223B	18582	2877270	2t3nk	mn067	1983	1:20000
Seaforth-Swanlake loams, 2 to 6 percent slopes	897B	5280	398731	fcx9	mn067	1983	1:20000
Swanlake-Ves loams, 6 to 12 percent slopes	954C	3030	398736	fcxg	mn067	1983	1:20000
Ves-Swanlake-Hawick complex, 2 to 6 percent slopes	999B	2165	398739	fcxk	mn067	1983	1:20000
Swanlake-Ves-Hawick complex, 6 to 12 percent slopes	999C	576	398740	fcxl	mn067	1983	1:20000
Swanlake-Ves loams, 12 to 18 percent slopes	954D	244	398737	fcxh	mn067	1983	1:20000
Amiret-Swanlake loams, 2 to 6 percent slopes	954B	36721	430365	2t3nk	mn073	1994	1:20000
Reedslake-Swanlake complex, 3 to 12 percent slopes	L1213B	45	3111775	2y038	mn079	1986	1:20000
Amiret-Round Lake-Swanlake complex, 2 to 6 percent slopes	L211B	33	1544631	1nv9t	mn081	2007	1:12000
Amiret-Swanlake loams, 2 to 6 percent slopes	L223B	16	1693183	2t3nk	mn081	2007	1:12000
Amiret-Swanlake loams, 2 to 6 percent slopes	421B2	22877	1859043	2t3nk	mn083	2008	1:12000
Annton-Swanlake, firm till complex, 3 to 6 percent slopes	L248B	2	2399982	2lkcs	mn083	2008	1:12000
Clarion-Swanlake complex, 2 to 6 percent slopes	887B	17403	399179	2vvfb	mn085	1993	1:20000
Reedslake-Swanlake complex, 3 to 12 percent slopes	L1213B	15	3111778	2y038	mn085	1993	1:20000
Clarion-Swanlake complex, 2 to 6 percent slopes	887B	47676	400062	2vvfb	mn091	1985	1:20000
Terril-Swanlake loams, 18 to 40 percent slopes	1852F	221	400033	ff89	mn091	1985	1:20000
Clarion-Swanlake complex, 2 to 6 percent slopes	887B	6056	436449	2vvfb	mn093	1996	1:20000
Reedslake-Swanlake complex, 3 to 12 percent slopes	L1213B	121	3111782	2y038	mn093	1996	1:20000
Annton-Swanlake, firm till complex, 3 to 6 percent slopes	L248B	1	2399059	2ljf0	mn101	2008	1:12000
Clarion-Swanlake complex, 2 to 6 percent slopes	921B	6898	400618	2vvfb	mn103	1990	1:20000
Reedslake-Swanlake complex, 3 to 12 percent slopes	L1213B	64	3111785	2y038	mn103	1990	1:20000
Amiret-Swanlake loams, 2 to 6 percent slopes	L223B	47305	2877272	2t3nk	mn127	2008	1:12000
Terril-Swanlake loams, 25 to 70 percent slopes	1852F	2856	2374065	2kpdr	mn127	2008	1:12000
Annton-Swanlake, firm till complex, 3 to 6 percent slopes	L248B	973	2399157	2ljj5	mn127	2008	1:12000
Amiret-Swanlake loams, 2 to 6 percent slopes	1355B	34374	436024	2t3nk	mn129	1995	1:20000
Clarion-Swanlake complex, 2 to 6 percent slopes	887B	29917	436125	2vvfb	mn129	1995	1:20000
Crooksford-Swanlake complex, 3 to 6 percent slopes	1371B	6010	436030	gmqh	mn129	1995	1:20000
Swanlake-Terril complex, 18 to 50 percent slopes	1242F	5283	436011	gmpw	mn129	1995	1:20000
Amiret-Swanlake-Hawick complex, 2 to 6 percent slopes	1386B	1704	436036	gmqp	mn129	1995	1:20000
Reedslake-Swanlake complex, 3 to 12 percent slopes	L1213B	71	3111788	2y038	mn131	1996	1:12000
Clarion-Swanlake complex, 2 to 6 percent slopes	887B	7241	431541	2vvfb	mn143	1991	1:20000
Swanlake-Lasa complex, 18 to 65 percent slopes	772F	933	431539	gh1m	mn143	1991	1:20000
Lester-Hawick-Swanlake complex, 6 to 12 percent slopes, eroded	944C2	384	431547	gh1w	mn143	1991	1:20000
Reedslake-Swanlake complex, 3 to 12 percent slopes	L1213B	205	3111791	2y038	mn143	1991	1:20000
Reedslake-Swanlake complex, 3 to 12 percent slopes	L1213B	87	3111794	2y038	mn147	1967	1:20000
Clarion-Swanlake complex, 2 to 6 percent slopes	L99B	367	455453	2vvfb	mn161	2001	1:12000
Reedslake-Swanlake complex, 3 to 12 percent slopes	L1213B	123	3111798	2y038	mn161	2001	1:12000
Clarion-Swanlake complex, 2 to 6 percent slopes	921B2	11815	428971	2vvfb	mn165	1987	1:20000
Amiret-Swanlake loams, 2 to 6 percent slopes	954B2	2516	428974	2t3nk	mn165	1987	1:20000
Reedslake-Swanlake complex, 3 to 12 percent slopes	L1213B	42	3111801	2y038	mn171	1998	1:12000
Amiret-Swanlake loams, 2 to 6 percent slopes	954B2	70626	1653642	2t3nk	mn173	1979	1:20000
Terril-Swanlake loams, 18 to 70 percent slopes	1852F	1764	1653570	1shnz	mn173	1979	1:20000

Map of Series Extent

Approximate geographic distribution of the SWANLAKE 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).