Official Series Description


Lab Data Summary

Aggregate lab data for the CRYSTAL LAKE soil series. This aggregation is based on all pedons with a current taxon name of CRYSTAL LAKE, 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 CRYSTAL LAKE were used in the calculation. Source: KSSL snapshot . Methods used to assemble the KSSL snapshot used by SoilWeb / SDE

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Pedons used in the lab summary:

MLRALab IDPedon IDTaxonnameCINSSL / NASIS ReportsLink To SoilWeb GMap
9040A162575WI095008Crystal Laken/aPrimary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties45.3877792,-92.167778
90A84P0795S1982WI069001CRYSTAL LAKEn/aPrimary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties45.421094,-89.4900382
90BUMN2003S1975MN1632003Crystal Laken/aPrimary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties45.0836983,-92.8504333
9301N0450S2000MI053003Crystal Laken/aPrimary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties46.6515007,-90.003273

Water Balance

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

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Sibling Summary

Siblings are those soil series that occur together in map units, in this case with the CRYSTAL LAKE series. Sketches are arranged according to their subgroup-level taxonomic structure. Source: SSURGO snapshot , parsed OSD records and snapshot of SC database .

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Select annual climate data summaries for the CRYSTAL LAKE series and siblings. Series are sorted according to hierarchical clustering of median values. Source: SSURGO map unit geometry and 1981-2010, 800m PRISM data .

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Geomorphic description summaries for the CRYSTAL LAKE 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 .

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

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Competing Series

Soil series competing with CRYSTAL LAKE share the same family level classification in Soil Taxonomy. Source: parsed OSD records and snapshot of the SC database .

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Select annual climate data summaries for the CRYSTAL LAKE series and competing. Series are sorted according to hierarchical clustering of median values. Source: SSURGO map unit geometry and 1981-2010, 800m PRISM data .

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Geomorphic description summaries for the CRYSTAL LAKE 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 .

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Click the image to view it full size.

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

Click the image to view it full size.

Click the image to view it full size.

Soil series sharing subgroup-level classification with CRYSTAL LAKE, 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 .

Block Diagrams

No block diagrams are available.

Map Units

Map units containing CRYSTAL LAKE 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
Crystal Lake silt loam, 1 to 8 percent slopes449B675396865f9z3mn03719801:15840
Crystal Lake silt loam, 1 to 6 percent slopes367B4716772412ypbhmn12319781:15840
Crystal Lake silt loam, 0 to 3 percent slopes4493516772462ypbgmn12319781:15840
Crystal Lake silt loam, 1 to 6 percent slopes367B187516771062ypbhmn16319781:15840
Crystal Lake silt loam, 0 to 3 percent slopes449165716771112ypbgmn16319781:15840
Crystal Lake silt loam, 1 to 6 percent slopes3163B28814312922ypbhwi00519931:20000
Crystal Lake silt loam, 0 to 3 percent slopes3163A20904312912ypbgwi00519931:20000
Crystal Lake silt loam, 6 to 12 percent slopes3163C4654312812ypbjwi00519931:20000
Crystal Lake silt loam, 1 to 6 percent slopes3163B544352902ypbhwi01320041:12000
Crystal Lake silt loam, 0 to 3 percent slopes3163A304352892ypbgwi01320041:12000
Crystal Lake silt loam, 6 to 12 percent slopes3163C217845492ypbjwi01320041:12000
Crystal Lake silt loam, 0 to 3 percent slopes3163A22924215132ypbgwi01719851:15840
Crystal Lake silt loam, 1 to 6 percent slopes3163B12354215032ypbhwi01719851:15840
Crystal Lake silt loam, 6 to 12 percent slopes3163C7624215042ypbjwi01719851:15840
Crystal Lake silt loam, 1 to 6 percent slopes3163B3464318532ypbhwi01919941:20000
Crystal Lake silt loam, 1 to 6 percent slopes3163B4811495382ypbhwi03120051:12000
Crystal Lake silt loam, 1 to 6 percent slopes3163B49264210492ypbhwi06719831:20000
Crystal Lake silt loam, 1 to 6 percent slopes3163B21054316142ypbhwi06919931:20000
Crystal Lake silt loam, 6 to 12 percent slopes3163C5744316152ypbjwi06919931:20000
Crystal Lake silt loam, 1 to 6 percent slopes3163B22204211722ypbhwi09519781:15840
Crystal Lake silt loam, 0 to 3 percent slopes3163A13884211712ypbgwi09519781:15840
Crystal Lake silt loam, 6 to 12 percent slopes3163C3594211552ypbjwi09519781:15840
Crystal Lake-Newot, very stony-Pence complex, 15 to 35 percent slopes3864E238414827581lrxxwi09920061:12000
Crystal Lake-Freeon, very stony-Sconsin complex, 2 to 6 percent slopes3865B556627581p21kwi09920061:12000
Crystal Lake-Freeon, very stony-Antigo complex, 6 to 15 percent slopes3863C43914827561lrxvwi09920061:12000
Crystal Lake silt loam, 1 to 6 percent slopes3163B1406276092ypbhwi09920061:12000
Crystal Lake silt loam, 6 to 12 percent slopes3163C466276102ypbjwi09920061:12000
Crystal Lake silt loam, 12 to 20 percent slopes3163D186276112ypbkwi09920061:12000
Crystal Lake silt loam, 1 to 6 percent slopes3163B31996250242ypbhwi10720061:12000
Crystal Lake silt loam, 6 to 12 percent slopes3163C5196250252ypbjwi10720061:12000
Crystal Lake silt loam, 12 to 20 percent slopes3163D1166250262ypbkwi10720061:12000
Crystal Lake silt loam, 1 to 6 percent slopes3163B6846253512ypbhwi11320061:12000
Crystal Lake silt loam, 6 to 12 percent slopes3163C2226253522ypbjwi11320061:12000
Crystal Lake silt loam, 15 to 35 percent slopes3163E1086253542ypblwi11320061:12000
Crystal Lake-Freeon, very stony-Sconsin complex, 2 to 6 percent slopes3865B4204581189mhs1wi11920021:12000
Crystal Lake-Freeon, very stony-Newot, very stony complex, 10 to 20 percent slopes9087D3337435127glscwi11920021:12000
Crystal Lake silt loam, 1 to 6 percent slopes3163B31284210172ypbhwi11920021:12000
Crystal Lake-Freeon, very stony-Antigo complex, 6 to 15 percent slopes3863C2388579853mgcywi11920021:12000
Crystal Lake silt loam, 6 to 12 percent slopes3163C7274210182ypbjwi11920021:12000
Crystal Lake silt loam, 15 to 35 percent slopes3163E684210402ypblwi11920021:12000
Crystal Lake silt loam, 12 to 20 percent slopes3163D594210412ypbkwi11920021:12000
Crystal Lake silt loam, 1 to 6 percent slopes3163B20684354672ypbhwi12920021:12000
Crystal Lake silt loam, 0 to 3 percent slopes3163A6334354662ypbgwi12920021:12000
Crystal Lake silt loam, 6 to 12 percent slopes3163C3634354682ypbjwi12920021:12000
Crystal Lake silt loam, 15 to 35 percent slopes3163E116359882ypblwi12920021:12000

Map of Series Extent

Approximate geographic distribution of the CRYSTAL LAKE 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 .