Official Series Description


Lab Data Summary

Aggregate lab data for the MANISTEE soil series. This aggregation is based on all pedons with a current taxon name of MANISTEE, 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 MANISTEE 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 MANISTEE 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 MANISTEE 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 MANISTEE 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 MANISTEE 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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Click the image to view it full size.

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

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Click the image to view it full size.

Competing Series

Soil series competing with MANISTEE 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 MANISTEE series and competing. Series are sorted according to hierarchical clustering of median values. Source: SSURGO map unit geometry and 1981-2010, 800m PRISM data .

There are insufficient data to create the annual climate figure.

Geomorphic description summaries for the MANISTEE 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 .

There are insufficient data to create the 2D hillslope position figure.

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

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

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

There are insufficient data to create the 3D flats position figure.

Soil series sharing subgroup-level classification with MANISTEE, 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-2012-02-06-10 | Chippewa County - February 1992

    Typical pattern of soils and parent material in the Pickford-Rudyard-Ontonagon association (Soil Survey of Chippewa County, Michigan; February 1992).

  2. MI-2012-02-06-12 | Chippewa County - February 1992

    Typical pattern of soils and parent material in the Fibre-Allendale-Pickford association (Soil Survey of Chippewa County, Michigan; February 1992).

  3. MI-2012-02-06-43 | Missaukee County - December 1985

    Pattern of soils and underlying material in the Nester-Kawkawlin-Manistee association (Soil Survey of Missaukee County, Michigan; December 1985).

Map Units

Map units containing MANISTEE 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
Manistee loamy sand, 6 to 12 percent slopes61C6651903486d28mi00119931:20000
Manistee loamy sand, 12 to 18 percent slopes61D1941903496d29mi00119931:20000
Manistee loamy sand, 25 to 45 percent slopes61F1591903506d2bmi00119931:20000
Manistee loamy sand, 0 to 2 percent slopesMdA641892016bw8mi01119641:20000
Manistee loamy sand, 2 to 6 percent slopesMdB471892026bw9mi01119641:20000
Kalkaska-Manistee sands, 0 to 6 percent slopes79B4519415168fy0jmi03319891:15840
Kalkaska-Manistee sands, 6 to 15 percent slopes79D1422415169fy0kmi03319891:15840
Manistee sand, 0 to 6 percent slopes117B1242415072fxxfmi03319891:15840
Manistee sand, 25 to 50 percent slopes117F240415074fxxhmi03319891:15840
Manistee sand, 6 to 15 percent slopes117D181415073fxxgmi03319891:15840
Manistee loamy sand, 0 to 6 percent slopesMeB6781893596c1cmi04719681:20000
Manistee sand, 0 to 4 percent slopesMdB5391898156cj2mi05119661:15840
Manistee-Ontonagon complex, dissected, 1 to 12 percent slopes58B714416139fz0vmi06119891:20000
Manistee sand, sandy substratum, 6 to 15 percent slopes117D64631305p5xpmi09520041:24000
Manistee sand, 0 to 6 percent slopes117B485416312fz6fmi09719941:20000
Manistee loamy sand, 0 to 6 percent slopes10B80681924066g6nmi11319831:15840
Manistee loamy sand, 6 to 12 percent slopes10C6471924076g6pmi11319831:15840
Manistee loamy sand, 0 to 6 percent slopes53B40131899336cmwmi12919871:15840
Nester-Manistee complex, 2 to 6 percent slopes82B32821899496cndmi12919871:15840
Nester-Manistee complex, 6 to 12 percent slopes82C23571899506cnfmi12919871:15840
Manistee loamy sand, 6 to 12 percent slopes53C10901899346cmxmi12919871:15840
Nester-Manistee complex, 12 to 18 percent slopes82D8431899516cngmi12919871:15840
Nester-Manistee complex, 18 to 35 percent slopes82E5471899526cnhmi12919871:15840
Manistee loamy sand, 12 to 18 percent slopes53D3201899356cmymi12919871:15840
Manistee loamy sand, 6 to 12 percent slopesMdC4001901016ct9mi13319661:15840
Manistee loamy sand, 2 to 6 percent slopesMdB3431901006ct8mi13319661:15840
Manistee loamy sand, 12 to 18 percent slopesMdD531901026ctbmi13319661:15840
Manistee-Montcalm loamy sands, 0 to 6 percent slopes26B83611907606dhkmi60019831:15840
Manistee-Montcalm loamy sands, 6 to 12 percent slopes26C30681907616dhlmi60019831:15840
Manistee-Kellogg-Ashwabay complex, 15 to 45 percent slopes813E98314444921kh3jwi00320061:12000
Manistee-Kellogg-Ashwabay complex, 15 to 45 percent slopes813E6119433314gjwwwi00720051:12000
Manistee fine sandy loam, 2 to 6 percent slopesMfB2129426212g9hswi00919701:20000
Manistee loamy fine sand, 2 to 6 percent slopesMeB1129426210g9hqwi00919701:20000
Manistee loamy fine sand, 6 to 14 percent slopes, erodedMeC2243426211g9hrwi00919701:20000
Manistee loamy sand, 2 to 6 percent slopesMeB622422252g5d1wi02919751:15840
Manistee-Kellogg-Ashwabay complex, 15 to 45 percent slopes813E403781488v769wi03120051:12000
Manistee-Kellogg-Ashwabay complex, 15 to 45 percent slopes813E14416977191tzm4wi05120061:12000
Manistee loamy fine sand, 2 to 6 percent slopesMeB276422331g5glwi06119781:15840
Manistee loamy sand, 2 to 6 percent slopesMeB1267422413g5k7wi07519871:20000
Manistee loamy fine sand, 2 to 6 percent slopesMeB1644422571g5qbwi08719751:15840
Manistee fine sandy loam, 2 to 6 percent slopesMfB732422573g5qdwi08719751:15840
Manistee loamy fine sand, 6 to 12 percent slopes, erodedMeC2274422572g5qcwi08719751:15840

Map of Series Extent

Approximate geographic distribution of the MANISTEE 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 .