Official Series Description


Lab Data Summary

Aggregate lab data for the ISLANDLAKE soil series. This aggregation is based on all pedons with a current taxon name of ISLANDLAKE, 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 ISLANDLAKE 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
94A93P0805S1992MI079035Islandlake6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties44.7315389,-84.86635

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the ISLANDLAKE 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 ISLANDLAKE 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 ISLANDLAKE 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 ISLANDLAKE 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 ISLANDLAKE 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 ISLANDLAKE 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 ISLANDLAKE 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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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 ISLANDLAKE, 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).

Map Units

Map units containing ISLANDLAKE 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
Islandlake sand, 6 to 15 percent slopes319D277714554701kvjnmi00320071:24000
Islandlake sand, 15 to 35 percent slopes319E155514554711kvjpmi00320071:24000
Islandlake sand, 0 to 6 percent slopes, burned312B124114554571kvj7mi00320071:24000
Islandlake sand, 0 to 6 percent slopes319B90114554691kvjmmi00320071:24000
Islandlake-McMillan complex, 15 to 35 percent slopes296E62014554301kvhcmi00320071:24000
Islandlake sand, 35 to 60 percent slopes319F50814554721kvjqmi00320071:24000
Islandlake-McMillan complex, 6 to 15 percent slopes296D33814554291kvhbmi00320071:24000
Islandlake sand, 6 to 15 percent slopes, burned312D32314554581kvj8mi00320071:24000
Islandlake sand, 0 to 6 percent slopes, very deep water table318B26814554671kvjkmi00320071:24000
Islandlake sand, 6 to 15 percent slopes, very deep water table318D7114554681kvjlmi00320071:24000
Islandlake loamy sand, 0 to 6 percent slopesIslaaB577031559182ytjbmi00919761:15840
Islandlake sand, 0 to 6 percent slopesIslabB112931559192ytj3mi00919761:15840
Islandlake sand, 6 to 18 percent slopesIslabD19331559202ytj4mi00919761:15840
Islandlake sand, 18 to 35 percent slopesIslabE11531559212ytj5mi00919761:15840
Islandlake loamy sand, 1 to 6 percent slopes8129B261425660312pdjcmi01319841:20000
McMillan-Islandlake complex, 6 to 18 percent slopes319C161514560581kw4mmi05320071:24000
McMillan-Islandlake complex, 35 to 55 percent slopes319E18514560601kw4pmi05320071:24000
McMillan-Islandlake complex, 18 to 35 percent slopes319D16314560591kw4nmi05320071:24000
Islandlake loamy sand, 1 to 6 percent slopes8129B299424846922pdjcmi06119891:20000
Islandlake loamy sand, 6 to 18 percent slopes8129C1824846932pdjdmi06119891:20000
Islandlake loamy sand, 0 to 6 percent slopes402B323401906526dd2mi07919981:12000
Islandlake sand, 0 to 6 percent slopes338B123741906446dctmi07919981:12000
Islandlake-Blue Lake complex, 0 to 6 percent slopes366B100311906496dczmi07919981:12000
Islandlake sand, 12 to 18 percent slopes338D85081906466dcwmi07919981:12000
Islandlake sand, 18 to 35 percent slopes338E72201906476dcxmi07919981:12000
Islandlake sand, 6 to 12 percent slopes338C68471906456dcvmi07919981:12000
Islandlake-Blue Lake complex, 6 to 12 percent slopes366C50551906506dd0mi07919981:12000
Islandlake-Southwells complex, 0 to 6 percent slopes457B50231906916dfbmi07919981:12000
Islandlake-Southwells complex, 6 to 12 percent slopes457C38591906926dfcmi07919981:12000
Islandlake-Blue Lake complex, 12 to 18 percent slopes366D33281906936dfdmi07919981:12000
Islandlake-Southwells complex, 12 to 18 percent slopes457D27531906906df9mi07919981:12000
Islandlake-Blue Lake complex, 18 to 35 percent slopes366E16181906946dffmi07919981:12000
Islandlake-Southwells complex, 18 to 35 percent slopes457E11861906896df8mi07919981:12000
Islandlake loamy sand, 6 to 12 percent slopes402C10171907116dfzmi07919981:12000
Islandlake-Menominee sands, 12 to 18 percent slopes458D3361906886df7mi07919981:12000
Islandlake sand, 6 to 18 percent slopesIslabD3731870392ytj4mi07919981:12000
Islandlake loamy sand, 1 to 6 percent slopes8129B76016748371t6t0mi13120071:24000
McMillan-Islandlake complex, 6 to 18 percent slopes8319C35516749181t6wmmi13120071:24000
Islandlake loamy sand, 6 to 18 percent slopes8129C19816748381t6t1mi13120071:24000
McMillan-Islandlake complex, 18 to 35 percent slopes8319D14016749191t6wnmi13120071:24000
Islandlake sand, 0 to 6 percent slopes338B165520903970j6mi13520031:12000
Islandlake sand, 6 to 18 percent slopes507D1151628151p2mymi13520031:12000
Islandlake-Blue Lake sands, 6 to 18 percent slopes508D1035628149p2mwmi13520031:12000
Islandlake-Blue Lake sands, 0 to 6 percent slopes508B811628150p2mxmi13520031:12000
Islandlake sand, 18 to 35 percent slopes338E273628152p2mzmi13520031:12000
Islandlake-Blue Lake sands, 18 to 35 percent slopes508E166628148p2mvmi13520031:12000
Islandlake loamy sand, 0 to 6 percent slopes402B68811914956f88mi13719981:12000
Islandlake sand, 0 to 6 percent slopes338B54691914756f7mmi13719981:12000
Islandlake sand, 6 to 12 percent slopes338C9871914766f7nmi13719981:12000
Islandlake loamy sand, 6 to 12 percent slopes402C6811914966f89mi13719981:12000
Islandlake sand, 12 to 18 percent slopes338D1791915496fb0mi13719981:12000
Islandlake loamy sand, 12 to 18 percent slopes402D1011915466f9xmi13719981:12000
Islandlake sand, 6 to 18 percent slopesIslabD3331870482ytj4mi13719981:12000
Islandlake sand, 6 to 15 percent slopes549D147915380891nmhsmi15320071:24000
Islandlake sand, 0 to 6 percent slopes549B75015380901nmhtmi15320071:24000
Islandlake sand, 6 to 15 percent slopes, burned558D42315380561nmgqmi15320071:24000
Islandlake-McMillan complex, 0 to 6 percent slopes527B41514569701kx31mi15320071:24000
Islandlake-McMillan complex, 15 to 35 percent slopes527E40414569711kx32mi15320071:24000
Islandlake sand, 0 to 6 percent slopes, burned558B38615380571nmgrmi15320071:24000
Islandlake-McMillan complex, 6 to 15 percent slopes527D38414569721kx33mi15320071:24000
Islandlake sand, 15 to 35 percent slopes549E15315380881nmhrmi15320071:24000
Islandlake sand, 0 to 6 percent slopes, very deep water table560B14115380721nmh7mi15320071:24000

Map of Series Extent

Approximate geographic distribution of the ISLANDLAKE 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 .