Official Series Description


Lab Data Summary

Aggregate lab data for the ANNALAKE soil series. This aggregation is based on all pedons with a current taxon name of ANNALAKE, 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 ANNALAKE 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
9200P0274S1999MI131002Annalake6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties46.8419456,-89.3249969
9201N0430S2000MI131005Annalake6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties46.8249969,-89.6598129
9201N0424S2000MI131038Annalake6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties46.9892426,-88.9795837
9202N0706S2001MI131004Annalake6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties46.9847527,-88.9404449
9203N0274S2002MI131012Annalake6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties46.7172203,-89.2084122
93B02N0152S2001MI053013Annalake6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties46.5664024,-90.3211212

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the ANNALAKE 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 ANNALAKE 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 ANNALAKE 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 ANNALAKE 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 ANNALAKE 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 ANNALAKE 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 ANNALAKE 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 ANNALAKE, 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-2010-09-10-04 | Gogebic County - 2010

    A typical pattern of soils and underlying material in the Gogebic-Wakefield-Cathro association (Soil Survey of Gogebic County, Michigan; 2010).

  2. MI-2010-09-10-15 | Ontonagon County -

    Typical pattern of soils and parent material in the Flintsteel-Big Iron-Watton association (Soil Survey of Ontonagon County, Michigan).

  3. MI-2010-09-10-20 | Ontonagon County -

    Typical pattern of soils and parent material in the Rockland-Moquah association (Soil Survey of Ontonagon County, Michigan).

Map Units

Map units containing ANNALAKE 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
Zimmerman-Annalake complex, 6 to 18 percent slopes85D59021903766d35mi00119931:20000
Annalake loamy very fine sand, 0 to 6 percent slopes36B49551903226d1fmi00119931:20000
Zimmerman-Annalake complex, 0 to 6 percent slopes85B27281903756d34mi00119931:20000
Annalake loamy very fine sand, 6 to 12 percent slopes36C23941903236d1gmi00119931:20000
Annalake loamy very fine sand, 0 to 6 percent slopes36B14401912756f15mi00719981:12000
Zimmerman-Annalake complex, 6 to 18 percent slopes85D9471913086f27mi00719981:12000
Annalake loamy very fine sand, 6 to 12 percent slopes36C2231912766f16mi00719981:12000
Annalake loamy fine sand, 6 to 12 percent slopes451C41913816f4lmi00719981:12000
Annalake-Gaastra-Champion complex, 1 to 6 percent slopes, extremely stony8091B79124507902n87rmi01319841:20000
Karlin, very deep water table-Annalake complex, 1 to 6 percent slopes8093B51924507922n87tmi01319841:20000
Annalake very fine sandy loam, 6 to 35 percent slopes, dissected8133D43224506672n83smi01319841:20000
Tonkey-Pleine-Annalake complex, 0 to 1 percent slopes680B412714563321kwfgmi05320071:24000
Annalake-Robago complex, 0 to 6 percent slopes686B345714563421kwfsmi05320071:24000
Chabeneau-Annalake complex, 0 to 6 percent slopes693B304914563531kwg4mi05320071:24000
Manido-Annalake complex, 1 to 6 percent slopes652B135214563221kwf4mi05320071:24000
Gogebic-Annalake complex, 1 to 6 percent slopes528B117514563161kwdymi05320071:24000
Annalake-Karlin complex, 6 to 18 percent slopes328C97914560741kw54mi05320071:24000
Annalake-Karlin complex, 1 to 6 percent slopes328B53814560731kw53mi05320071:24000
Annalake-Stutts-Arnheim, frequently flooded, complex, drainageway, 0 to 35 percent slopes694D51014563541kwg5mi05320071:24000
Gogebic-Annalake complex, 18 to 35 percent slopes528D40014563181kwf0mi05320071:24000
Annalake very fine sandy loam, 0 to 6 percent slopes648B14514562241kw9zmi05320071:24000
Gogebic-Annalake complex, 6 to 18 percent slopes528C12014563171kwdzmi05320071:24000
Annalake very fine sandy loam, 6 to 18 percent slopes648C7814562251kwb0mi05320071:24000
Karlin, very deep water table-Annalake complex, 1 to 6 percent slopes8093B61124862082pg38mi06119891:20000
Annalake-Gaastra-Champion complex, 1 to 6 percent slopes, extremely stony8091B27624836692pcgcmi06119891:20000
Zandi-Annalake complex, 1 to 6 percent slopes8158B12524847962pdmqmi06119891:20000
Zandi-Annalake complex, 6 to 18 percent slopes8158C724847972pdmrmi06119891:20000
Karlin, very deep water table-Annalake complex, 1 to 6 percent slopes8093B31424786122p667mi07119921:20000
Annalake-Gaastra-Champion complex, 1 to 6 percent slopes, extremely stony8091B4624786102p665mi07119921:20000
Annalake loamy fine sand, 0 to 6 percent slopes451B8011924046g6lmi11919971:12000
Annalake loamy fine sand, 6 to 12 percent slopes451C2231924036g6kmi11919971:12000
Annalake loam, 0 to 4 percent slopes14B801414563931kwhfmi13120071:24000
Zandi-Annalake complex, 1 to 6 percent slopes8158B174116748471t6tbmi13120071:24000
Annalake loam, 4 to 18 percent slopes14D67914563941kwhgmi13120071:24000
Zandi-Annalake complex, 6 to 18 percent slopes8158C48216748481t6tcmi13120071:24000
Annalake-Karlin complex, 1 to 6 percent slopes8328B13716749271t6wxmi13120071:24000
Annalake-Karlin complex, 6 to 18 percent slopes8328C10316749281t6wymi13120071:24000
Annalake loamy very fine sand, 0 to 6 percent slopes36B3241359834smi13520031:12000
Annalake-Totagatic, frequently flooded-Annanias complex, 0 to 8 percent slopes25B8417179231vnmwmi6061:12000
Annalake-Annanias-Arnheim, frequently flooded, complex, 0 to 57 percent slopes50E7023782172ktqpmi6061:12000
Annalake fine sandy loam, 2 to 6 percent slopes917B153814445131kh46wi00320061:12000
Annalake fine sandy loam, 6 to 15 percent slopes917C82414445141kh47wi00320061:12000
Annalake fine sandy loam, lake terrace, 2 to 6 percent slopes517B60814444371kh1rwi00320061:12000
Annalake fine sandy loam, lake terrace, 6 to 15 percent slopes517C32214444381kh1swi00320061:12000
Chabeneau-Annalake complex, 0 to 6 percent slopes5543B17717028801v4zmwi00320061:12000
Gogebic, very stony-Annalake complex, 0 to 6 percent slopes1451B17714445231kh4jwi00320061:12000
Gogebic, very stony-Annalake complex, 6 to 15 percent slopes1451C16914445241kh4kwi00320061:12000
Wakefield, stony-Annalake-Cathro complex, 0 to 18 percent slopes9020C612013839471hg3gwi00720051:12000
Springstead, stony-Annalake-Cathro complex, 0 to 6 percent slopes885B4272114743817j04wi00720051:12000
Wakefield, stony-Annalake-Cathro complex, 0 to 35 percent slopes9020D390813839481hg3hwi00720051:12000
Annalake fine sandy loam, lake terrace, 2 to 6 percent slopes517B894433599gk62wi00720051:12000
Annalake fine sandy loam, lake terrace, 6 to 15 percent slopes517C426433600gk63wi00720051:12000
Gogebic, very stony-Annalake complex, 0 to 6 percent slopes1451B414433555gk4nwi00720051:12000
Annalake fine sandy loam, 6 to 15 percent slopes917C40613839961hg51wi00720051:12000
Annalake fine sandy loam, 2 to 6 percent slopes917B40113839951hg50wi00720051:12000
Gogebic, very stony-Annalake complex, 6 to 15 percent slopes1451C296433556gk4pwi00720051:12000
Springstead, stony-Annalake-Cathro complex, 0 to 6 percent slopes885B312314826881lrvnwi03120051:12000
Newood, very stony-Annalake complex, 0 to 6 percent slopes451B2734781253v6yqwi03120051:12000
Newood, very stony-Annalake complex, 6 to 15 percent slopes451C2730781254v6yrwi03120051:12000
Annalake fine sandy loam, lake terrace, 2 to 6 percent slopes517B1164781309v70jwi03120051:12000
Annalake fine sandy loam, lake terrace, 6 to 15 percent slopes517C350781310v70kwi03120051:12000
Annalake fine sandy loam, 2 to 6 percent slopes917B291114954217l60wi03120051:12000
Annalake fine sandy loam, 6 to 15 percent slopes917C18114954317l61wi03120051:12000
Annalake fine sandy loam, 0 to 6 percent slopesAnB1919429990gffnwi03719951:12000
Annalake fine sandy loam, 6 to 15 percent slopesAnC404429991gffpwi03719951:12000
Chabeneau-Annalake complex, 0 to 6 percent slopes5543B140915321941nfcmwi05120061:12000
Annalake fine sandy loam, 2 to 6 percent slopes917B335782393v84hwi05120061:12000
Annalake fine sandy loam, lake terrace, 2 to 6 percent slopes517B317782177v7xjwi05120061:12000
Springstead, stony-Annalake-Cathro complex, 0 to 6 percent slopes885B23917012591v39bwi05120061:12000
Annalake fine sandy loam, lake terrace, 6 to 15 percent slopes517C144782178v7xkwi05120061:12000
Annalake fine sandy loam, 6 to 15 percent slopes917C9782394v84jwi05120061:12000
Annalake fine sandy loam, 0 to 6 percent slopesAnB215395778f8v1wi07819981:12000
Annalake fine sandy loam, 2 to 6 percent slopes917B1340627585p21pwi09920061:12000
Annalake fine sandy loam, 6 to 15 percent slopes917C353627586p21qwi09920061:12000
Annalake fine sandy loam, 2 to 6 percent slopes917B659625110nzgvwi10720061:12000
Annalake fine sandy loam, 6 to 15 percent slopes917C11813813181hccnwi10720061:12000
Annalake fine sandy loam, 2 to 6 percent slopes917B1521656076q0prwi11320061:12000
Annalake fine sandy loam, 6 to 15 percent slopes917C290656075q0pqwi11320061:12000

Map of Series Extent

Approximate geographic distribution of the ANNALAKE 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 .