Soil Data Explorer - CHEQUAMEGON

Official Series Description

Lab Data Summary

Aggregate lab data for the CHEQUAMEGON soil series. This aggregation is based on all pedons with a current taxon name of CHEQUAMEGON, 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 CHEQUAMEGON 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
90A	01N1031	S2000WI099003	Chequamegon	6	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	45.5097198,-90.0798264

Water Balance

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

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

Soil series sharing subgroup-level classification with CHEQUAMEGON, 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 CHEQUAMEGON 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
Chequamegon silt loam, 2 to 6 percent slopes, very stony	750B	14536	1292278	1dcqd	wi099	2006	1:12000
Chequamegon silt loam, 6 to 15 percent slopes, very stony	750C	5903	1292279	1dcqf	wi099	2006	1:12000
Chequamegon, very stony-Sconsin complex, 2 to 6 percent slopes	1345B	1499	1598761	1qnmy	wi099	2006	1:12000
Chequamegon silt loam, 15 to 30 percent slopes, very stony	750D	390	1292280	1dcqg	wi099	2006	1:12000
Chequamegon silt loam, 2 to 6 percent slopes, very stony	750B	9657	1381312	1hccg	wi107	2006	1:12000
Chequamegon silt loam, 6 to 15 percent slopes, very stony	750C	2371	1381315	1hcck	wi107	2006	1:12000
Chequamegon, very stony-Sconsin complex, 2 to 6 percent slopes	1345B	459	1385296	1hhhz	wi107	2006	1:12000
Chequamegon silt loam, 15 to 30 percent slopes, very stony	750D	122	1381316	1hccl	wi107	2006	1:12000
Chequamegon silt loam, 2 to 6 percent slopes, very stony	750B	29371	1386093	1hjbp	wi113	2006	1:12000
Chequamegon silt loam, 6 to 15 percent slopes, very stony	750C	11069	1386092	1hjbn	wi113	2006	1:12000
Chequamegon, very stony-Sconsin complex, 2 to 6 percent slopes	1345B	1517	1669959	1t1qn	wi113	2006	1:12000
Chequamegon silt loam, 15 to 30 percent slopes, very stony	750D	224	1386091	1hjbm	wi113	2006	1:12000

Map of Series Extent

Approximate geographic distribution of the CHEQUAMEGON 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).