Soil Data Explorer - SPRINGLAKE

Official Series Description

Lab Data Summary

Aggregate lab data for the SPRINGLAKE soil series. This aggregation is based on all pedons with a current taxon name of SPRINGLAKE, 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 SPRINGLAKE 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
94B	91P0130	90MI097002	Springlake	5	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	46.181385,-85.2174301

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the SPRINGLAKE 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 SPRINGLAKE 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 SPRINGLAKE 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 SPRINGLAKE 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 SPRINGLAKE 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 SPRINGLAKE 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 SPRINGLAKE 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 SPRINGLAKE, 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 SPRINGLAKE 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
Springlake-Kalkaska sands, 0 to 6 percent slopes	SrlkaB	31894	3155939	2ytjd	mi009	1976	1:15840
Springlake-Kalkaska sands, 6 to 18 percent slopes	SrlkaD	2528	3155940	2ytjf	mi009	1976	1:15840
Springlake-Kalkaska sands, 18 to 35 percent slopes	SrlkaE	2179	3155941	2ytjg	mi009	1976	1:15840
Springlake-Kalkaska sands, 0 to 6 percent slopes	SrlkaB	65	3187033	2ytjd	mi029	1970	1:15840
Springlake sand, 0 to 6 percent slopes	EaB	590	1588044	1q9h7	mi041	1969	1:24000
Springlake sand, 0 to 6 percent slopes	454B	6478	190677	6ddw	mi079	1998	1:12000
Springlake-Kalkaska sands, 0 to 6 percent slopes	SrlkaB	1226	3187044	2ytjd	mi079	1998	1:12000
Springlake sand, 6 to 12 percent slopes	454C	679	190709	6dfx	mi079	1998	1:12000
Springlake sand, 18 to 35 percent slopes	454E	649	190716	6dg4	mi079	1998	1:12000
Springlake sand, 12 to 18 percent slopes	454D	335	190720	6dg8	mi079	1998	1:12000
Springlake-Kalkaska sands, 18 to 35 percent slopes	SrlkaE	49	3187046	2ytjg	mi079	1998	1:12000
Springlake-Kalkaska sands, 6 to 18 percent slopes	SrlkaD	17	3187045	2ytjf	mi079	1998	1:12000
Springlake loamy coarse sand, 0 to 6 percent slopes	24B	523	627473	p1y2	mi095	2004	1:24000
Springlake loamy coarse sand, 0 to 6 percent slopes	24B	12041	416380	fz8m	mi097	1994	1:20000
Springlake loamy coarse sand, 6 to 15 percent slopes	24D	2065	416381	fz8n	mi097	1994	1:20000
Springlake loamy coarse sand, 15 to 35 percent slopes	24E	628	416382	fz8p	mi097	1994	1:20000
Springlake-Kalkaska sands, 0 to 6 percent slopes	SrlkaB	164	3187054	2ytjd	mi137	1998	1:12000
Springlake-Kalkaska sands, 18 to 35 percent slopes	SrlkaE	3	3187055	2ytjg	mi137	1998	1:12000
Springlake loamy sand, 0 to 6 percent slopes	355B	3029	1457007	1kx47	mi153	2007	1:24000

Map of Series Extent

Approximate geographic distribution of the SPRINGLAKE 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).