Official Series Description


Lab Data Summary

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

There are insufficient data to create the lab data summary figure.


Water Balance

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

Click the image to view it full size.

Geomorphic description summaries for the BLUE 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.

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

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Soil series sharing subgroup-level classification with BLUE 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

Click a link below to display the diagram. Note that these diagrams may be from multiple survey areas.

  1. MI-2010-09-07-07 | Kalkaska County - 2005

    Typical pattern of soils and parent material in the Islandlake-Blue Lake-Morganlake, sandy substratum, general soil map unit (Soil Survey of Kalkaska County, Michigan; 2005).

  2. MI-2010-09-07-22 | Montmorency County - 2003

    Typical pattern of soils and underlying material in the Algonquin-Negwegon-Springport association (Soil Survey of Montmorency County, Michigan; 2003).

  3. MI-2010-09-07-25 | Montmorency County - 2003

    Typical pattern of soils and underlying material in the Lupton-Tawas and Mancelona-Millersburg-Blue Lake associations (Soil Survey of Montmorency County, Michigan; 2003).

  4. MI-2010-09-07-27 | Otsego County - 2004

    Typical pattern of soils and parent material in the Kalkaska-Blue Lake-Rubicon association. Depth is indicated in inches (Soil Survey of Otsego County, Michigan; 2004).

  5. MI-2012-02-06-07 | Cheboygan County - September 1991

    Typical pattern of soils and parent material in the Grayling-Rubicon and Cheboygan-Blue Lake associations (Soil Survey of Cheboygan County, Michigan; September 1991).

  6. MI-2012-02-06-08 | Cheboygan County - September 1991

    Typical pattern of soils and parent material in the Cheboygan-Blue Lake and Tawas-Lupton associations (Soil Survey of Cheboygan County, Michigan; September 1991).

  7. MI-2012-03-22-01 | Cheboygan County - September 1991

    Typical pattern of soils and parent material in the Grayling-Rubicon and Cheboygan-Blue Lake associations (Soil Survey of Cheboygan County, MI; 1991).

  8. MI-2012-03-22-02 | Cheboygan County - September 1991

    Typical pattern of soils and parent material in the Cheboygan-Blue Lake and Tawas-Lupton associations (Soil Survey of Cheboygan County, MI; 1991).

Map Units

Map units containing BLUE 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
Garlic-Blue Lake-Voelker complex, 8 to 35 percent slopes, dissected76E550014552991kvc4mi00320071:24000
Kalkaska-Blue Lake complex, 8 to 35 percent slopes, dissected254E414314554031kvghmi00320071:24000
Kalkaska-Blue Lake complex, 6 to 15 percent slopes214D335814553611kvf4mi00320071:24000
Steuben-Blue Lake-Kalkaska complex, 6 to 15 percent slopes284D280314554221kvh3mi00320071:24000
Steuben-Blue Lake-Kalkaska complex, 1 to 6 percent slopes284B252514554211kvh2mi00320071:24000
Garlic-Blue Lake-Voelker complex, 1 to 12 percent slopes, dissected76C238714552981kvc3mi00320071:24000
Kalkaska-Blue Lake complex, 15 to 70 percent slopes, dissected254F206814554041kvgjmi00320071:24000
Kalkaska-Blue Lake complex, 1 to 6 percent slopes214B189314553601kvf3mi00320071:24000
Kalkaska-Blue Lake complex, 15 to 35 percent slopes214E146414553621kvf5mi00320071:24000
Garlic-Blue Lake-Voelker complex, 6 to 15 percent slopes77D102714553021kvc7mi00320071:24000
Kalkaska-Blue Lake complex, 1 to 12 percent slopes, dissected254C77614554021kvggmi00320071:24000
Garlic-Blue Lake-Voelker complex, 15 to 60 percent slopes, dissected76F74414553001kvc5mi00320071:24000
Garlic-Blue Lake-Voelker complex, 1 to 6 percent slopes77B66014553011kvc6mi00320071:24000
Steuben-Blue Lake-Kalkaska complex, 15 to 35 percent slopes284E57014554231kvh4mi00320071:24000
Garlic-Blue Lake-Voelker complex, 15 to 35 percent slopes77E19114553031kvc8mi00320071:24000
Blue Lake loamy sand, 0 to 6 percent slopes, deep water table, burned315B16414554621kvjdmi00320071:24000
Blue Lake loamy sand, 0 to 6 percent slopes, burned316B16214554631kvjfmi00320071:24000
Blue Lake loamy sand, 0 to 6 percent slopes, very deep water table, burned314B4814554611kvjcmi00320071:24000
Blue Lake loamy sand, 6 to 15 percent slopes, burned316D1414554641kvjgmi00320071:24000
Morganlake-Ossineke, sandy substratum-Blue Lake complex, 0 to 6 percent slopes424B471913786f4hmi00719981:12000
Blue Lake sand, 18 to 35 percent slopes350E51913736f4bmi00719981:12000
Allendale-Dorval-Blue Lake complex, 0 to 6 percent slopes361B51913756f4dmi00719981:12000
Morganlake-Ossineke, sandy substratum-Blue Lake complex, 6 to 12 percent slopes424C41913796f4jmi00719981:12000
Kalkaska-Blue Lake sands, 18 to 35 percent slopesKlkbaE3722731559292ytjnmi00919761:15840
Kalkaska-Blue Lake sands, 6 to 18 percent slopesKlkbaD2927431558872ytjmmi00919761:15840
Kalkaska-Blue Lake sands, 0 to 6 percent slopesKlkbaB2532931559272ytjlmi00919761:15840
Emmet-Blue Lake loamy sands, 18 to 35 percent slopesEmtblE1267431559042ytjsmi00919761:15840
Emmet-Blue Lake loamy sands, 2 to 6 percent slopesEmtblB1113531559012ytjpmi00919761:15840
Emmet-Blue Lake loamy sands, 6 to 12 percent slopesEmtblC680031559022ytjqmi00919761:15840
Emmet-Blue Lake loamy sands, lake moderated, 18 to 35 percent slopesEmtlmE636631559082ytk7mi00919761:15840
Emmet-Blue Lake loamy sands, 12 to 18 percent slopesEmtblD504731559032ytjrmi00919761:15840
Emmet-Blue Lake loamy sands, lake moderated, 12 to 18 percent slopesEmtlmD326131559072ytk6mi00919761:15840
Emmet-Blue Lake loamy sands, lake moderated, 2 to 6 percent slopesEmtlmB323231559052ytk4mi00919761:15840
Emmet-Blue Lake loamy sands, lake moderated, 6 to 12 percent slopesEmtlmC321831559062ytk5mi00919761:15840
Blue Lake loamy sand, 0 to 6 percent slopesBluaaB91831558862ythsmi00919761:15840
Blue Lake-Kalkaska association, undulatingBKB14731904046d42mi02919701:15840
Blue Lake loamy sand, 0 to 6 percent slopesBlB11251904066d44mi02919701:15840
Emmet-Blue Lake loamy sands, 18 to 35 percent slopesEmtblE67131560192ytjsmi02919701:15840
Blue Lake-Kalkaska association, rollingBKC6301904056d43mi02919701:15840
Blue Lake loamy sand, 6 to 12 percent slopesBlC4661904076d45mi02919701:15840
Blue Lake loamy sand, 18 to 50 percent slopesBlF4091904096d47mi02919701:15840
Blue Lake loamy sand, 12 to 18 percent slopesBlD2211904086d46mi02919701:15840
Emmet-Blue Lake loamy sands, 2 to 6 percent slopesEmtblB20231560162ytjpmi02919701:15840
Emmet-Blue Lake loamy sands, 6 to 12 percent slopesEmtblC20231560172ytjqmi02919701:15840
Emmet-Blue Lake loamy sands, lake moderated, 18 to 35 percent slopesEmtlmE17931560242ytk7mi02919701:15840
Kalkaska-Blue Lake sands, 18 to 35 percent slopesKlkbaE15631870312ytjnmi02919701:15840
Emmet-Blue Lake loamy sands, lake moderated, 6 to 12 percent slopesEmtlmC9731560222ytk5mi02919701:15840
Emmet-Blue Lake loamy sands, 12 to 18 percent slopesEmtblD9431560182ytjrmi02919701:15840
Emmet-Blue Lake loamy sands, lake moderated, 12 to 18 percent slopesEmtlmD8331560232ytk6mi02919701:15840
Kalkaska-Blue Lake sands, 0 to 6 percent slopesKlkbaB7131560292ytjlmi02919701:15840
Emmet-Blue Lake loamy sands, lake moderated, 2 to 6 percent slopesEmtlmB6931560202ytk4mi02919701:15840
Kalkaska-Blue Lake sands, 6 to 18 percent slopesKlkbaD4531560212ytjmmi02919701:15840
Blue Lake loamy sand, 0 to 6 percent slopes18B145611905396d8fmi03119881:15840
Blue Lake loamy sand, 6 to 12 percent slopes18C90181905406d8gmi03119881:15840
Blue Lake loamy sand, 12 to 30 percent slopes18D86701905416d8hmi03119881:15840
Blue Lake loamy sand, 30 to 50 percent slopes18F21161905426d8jmi03119881:15840
Blue Lake loamy sand, 0 to 6 percent slopes52B68451897246cf4mi03919931:15840
Blue Lake loamy sand, 6 to 18 percent slopes52D4051897256cf5mi03919931:15840
Blue Lake sand, 0 to 6 percent slopesBlB136115880171q9gcmi04119691:24000
Blue Lake sand, 6 to 18 percent slopesBlD25515880181q9gdmi04119691:24000
Blue Lake sand, 18 to 40 percent slopesBlE2015880191q9gfmi04119691:24000
Blue Lake loamy sand, 0 to 6 percent slopesBlB310801893096bzrmi04719681:20000
Blue Lake loamy sand, 6 to 12 percent slopesBlC223601893106bzsmi04719681:20000
Blue Lake loamy sand, 25 to 60 percent slopesBlF171281893136bzwmi04719681:20000
Blue Lake loamy sand, 18 to 25 percent slopesBlE166791893126bzvmi04719681:20000
Blue Lake loamy sand, 12 to 18 percent slopesBlD58391893116bztmi04719681:20000
Kalkaska-Blue Lake loamy sands, 0 to 6 percent slopesKbB12451893486c10mi04719681:20000
Islandlake-Blue Lake complex, 0 to 6 percent slopes366B100311906496dczmi07919981:12000
Islandlake-Blue Lake complex, 6 to 12 percent slopes366C50551906506dd0mi07919981:12000
Islandlake-Blue Lake complex, 12 to 18 percent slopes366D33281906936dfdmi07919981:12000
Morganlake, sandy substratum-Woodman-Blue Lake complex, 1 to 6 percent slopes467B25711907236dgcmi07919981:12000
Islandlake-Blue Lake complex, 18 to 35 percent slopes366E16181906946dffmi07919981:12000
Morganlake, sandy substratum-Woodman-Blue Lake complex, 6 to 12 percent slopes467C11581907246dgdmi07919981:12000
Kalkaska-Blue Lake sands, 0 to 6 percent slopesKlkbaB111931870412ytjlmi07919981:12000
Kalkaska-Blue Lake sands, 18 to 35 percent slopesKlkbaE40731870422ytjnmi07919981:12000
Kalkaska-Blue Lake sands, 6 to 18 percent slopesKlkbaD37531870372ytjmmi07919981:12000
Mancelona-Blue Lake complex, 0 to 6 percent slopes471B2821907286dgjmi07919981:12000
Mancelona-Millersburg-Blue Lake complex, 6 to 18 percent slopes363D64011922596g1xmi11919971:12000
Allendale-Dorval-Blue Lake complex, 0 to 6 percent slopes361B42181922556g1smi11919971:12000
Morganlake-Ossineke, sandy substratum-Blue Lake complex, 0 to 6 percent slopes424B40101924006g6gmi11919971:12000
Mancelona-Millersburg-Blue Lake complex, 8 to 35 percent slopes, dissected364E25481922606g1ymi11919971:12000
Blue Lake sand, 0 to 6 percent slopes350B25251922446g1fmi11919971:12000
Morganlake-Ossineke, sandy substratum-Blue Lake complex, 6 to 12 percent slopes424C22831924016g6hmi11919971:12000
Blue Lake sand, 6 to 18 percent slopes350D17711922456g1gmi11919971:12000
Menominee-Bamfield, sandy substratum-Blue Lake complex, 12 to 18 percent slopes399D15101921706fz1mi11919971:12000
Millersburg-Blue Lake complex, 0 to 6 percent slopes450B11421923016g38mi11919971:12000
Millersburg-Blue Lake complex, 6 to 18 percent slopes450D10321923026g39mi11919971:12000
Millersburg-Blue Lake complex, 18 to 35 percent slopes450E7271923036g3bmi11919971:12000
Mancelona-Ossineke-Blue Lake complex, 0 to 6 percent slopes353B4791922496g1lmi11919971:12000
Menominee-Bamfield, sandy substratum-Blue Lake complex, 18 to 70 percent slopes, dissected400F4751923986g6dmi11919971:12000
Mancelona-Blue Lake sands, 15 to 70 percent slopes, dissected354F4691922526g1pmi11919971:12000
Blue Lake sand, 18 to 35 percent slopes350E2401922466g1hmi11919971:12000
Blue Lake loamy sand, 6 to 12 percent slopesBlC22841899886cpnmi13319661:15840
Blue Lake loamy sand, 2 to 6 percent slopesBlB16971899876cpmmi13319661:15840
Blue Lake loamy sand, 12 to 18 percent slopesBlD11751899896cppmi13319661:15840
Blue Lake loamy sand, 18 to 25 percent slopesBlE4631899906cpqmi13319661:15840
Blue Lake loamy sand, 0 to 2 percent slopesBlA3301899866cplmi13319661:15840
Islandlake-Blue Lake sands, 6 to 18 percent slopes508D1035628149p2mwmi13520031:12000
Morganlake-Ossineke, sandy substratum-Blue Lake complex, 6 to 12 percent slopes424C829628170p2nkmi13520031:12000
Islandlake-Blue Lake sands, 0 to 6 percent slopes508B811628150p2mxmi13520031:12000
Morganlake-Ossineke, sandy substratum-Blue Lake complex, 0 to 6 percent slopes424B692628171p2nlmi13520031:12000
Menominee-Bamfield, sandy substratum-Blue Lake complex, 12 to 18 percent slopes399D195628161p2n8mi13520031:12000
Islandlake-Blue Lake sands, 18 to 35 percent slopes508E166628148p2mvmi13520031:12000
Menominee-Bamfield, sandy substratum-Blue Lake complex, 18 to 70 percent slopes, dissected400F128628172p2nmmi13520031:12000
Blue Lake loamy sand, 0 to 6 percent slopes52B235841915066f8mmi13719981:12000
Blue Lake loamy sand, 6 to 18 percent slopes52D186231915076f8nmi13719981:12000
Blue Lake loamy sand, 8 to 50 percent slopes, dissected365F128551914846f7xmi13719981:12000
Menominee-Bamfield, sandy substratum-Blue Lake complex, 18 to 70 percent slopes, dissected400F27521914936f86mi13719981:12000
Menominee-Bamfield, sandy substratum-Blue Lake complex, 12 to 18 percent slopes399D22891914926f85mi13719981:12000
Blue Lake loamy sand, 18 to 35 percent slopes52E21151915086f8pmi13719981:12000
Morganlake-Ossineke, sandy substratum-Blue Lake complex, 0 to 6 percent slopes424B18171914976f8bmi13719981:12000
Morganlake-0ssineke, sandy substratum,-Blue Lake complex, 6 to 12 percent slopes424C14691914986f8cmi13719981:12000
Mancelona-Blue Lake sands, 15 to 70 percent slopes, dissected354F14081915536fb4mi13719981:12000
Kalkaska-Blue Lake sands, 6 to 18 percent slopesKlkbaD12631870472ytjmmi13719981:12000
Kalkaska-Blue Lake sands, 18 to 35 percent slopesKlkbaE9231870512ytjnmi13719981:12000
Blue Lake sand, 6 to 18 percent slopes350D261915426f9smi13719981:12000
Kalkaska-Blue Lake sands, 0 to 6 percent slopesKlkbaB1031870502ytjlmi13719981:12000

Map of Series Extent

Approximate geographic distribution of the BLUE 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 .