Official Series Description


Lab Data Summary

Aggregate lab data for the ARNHEIM soil series. This aggregation is based on all pedons with a current taxon name of ARNHEIM, 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 ARNHEIM 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.

Pedons used in the lab summary:

MLRALab IDPedon IDTaxonnameCINSSL / NASIS ReportsLink To SoilWeb GMap
9205N0186S2004MI131014Arnheim6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties46.7191963,-89.2081757
n/aRO-0361958-OH141-036Arnheim2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Propertiesn/a
n/aHY-0611967-OH071-061Arnheim4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Propertiesn/a

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the ARNHEIM 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 ARNHEIM 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 ARNHEIM 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 ARNHEIM 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 ARNHEIM 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 ARNHEIM 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 ARNHEIM 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 ARNHEIM, 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-2010-09-10-20 | Ontonagon County -

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

  2. MI-2012-02-06-18 | Houghton County Area - October 1991

    Diagrammatic cross section of Houghton County showing the topography, elevation, general soil texture, landforms, and dominant soils and their drainage class (Soil Survey of Houghton County Area, Michigan; October 1991).

Map Units

Map units containing ARNHEIM 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
Arnheim mucky silt loam736821415016fxvmmi01319841:20000
Bowstring-Arnheim complex, 0 to 1 percent slopes, frequently flooded8054123924418762myz6mi01319841:20000
Bowstring-Arnheim complex, 0 to 1 percent slopes, frequently flooded3031400414560321kw3smi05320071:24000
Rockland-Arnheim, frequently flooded, complex, 0 to 70 percent slopes285F998814563571kwg8mi05320071:24000
Moquah-Arnheim complex, 0 to 3 percent slopes, frequently flooded230B448014563791kwgzmi05320071:24000
Cathro-Arnheim, frequently flooded, complex, 0 to 1 percent slopes382195714560831kw5fmi05320071:24000
Annalake-Stutts-Arnheim, frequently flooded, complex, drainageway, 0 to 35 percent slopes694D51014563541kwg5mi05320071:24000
Sturgeon-Arnheim-Pelkie complex137A7173416076fyytmi06119891:20000
Arnheim silt loam372089416128fz0hmi06119891:20000
Bowstring-Arnheim complex, 0 to 1 percent slopes, frequently flooded8054163824834202pc6bmi06119891:20000
Moquah-Arnheim complex, 0 to 3 percent slopes, frequently flooded63B10725660331kwkrmi06119891:20000
Bowstring-Arnheim complex, 0 to 1 percent slopes, frequently flooded303262824525152nb1dmi07119921:20000
Arnheim-Moquah complex, 0 to 3 percent slopes247398415463fyb1mi10919851:20000
Arnheim silt loam655571899416cn4mi12919871:15840
Moquah-Arnheim complex, 0 to 3 percent slopes, frequently flooded63B520714564651kwkrmi13120071:24000
Bowstring-Arnheim complex, 0 to 1 percent slopes, frequently flooded8079211416748101t6s4mi13120071:24000
Ubly-Moquah, frequently flooded-Arnheim, frequently flooded, complex, 0 to 60 percent slopes157F137214565971kwq0mi13120071:24000
Arnheim mucky silt loam, 0 to 1 percent slopes, frequently flooded16A103314563981kwhlmi13120071:24000
Cathro-Arnheim, frequently flooded, complex, 0 to 1 percent slopes838243416749461t6xjmi13120071:24000
Rockland-Arnheim, frequently flooded, complex, 0 to 70 percent slopes8285F27716748871t6vmmi13120071:24000
Pelkie, occasionally flooded-Arnheim, frequently flooded complex, 0 to 4 percent slopes490B484514569911kx3qmi15320071:24000
Arnheim-Sturgeon-Pelkie complex, 0 to 3 percent slopes158A1171800773vw8dmi60520041:24000
Cathro, Lupton, and Arnheim soils, drainageway, 0 to 4 percent slopes, frequently flooded36A700317179841vnpvmi6061:12000
Arnheim-Totagatic-Sturgeon complex, 0 to 6 percent slopes, frequently flooded24A32317179221vnmvmi6061:12000
Annalake-Annanias-Arnheim, frequently flooded, complex, 0 to 57 percent slopes50E7023782172ktqpmi6061:12000
Bowstring-Arnheim complex, 0 to 1 percent slopes, frequently flooded5374A141317028731v4zdwi00320061:12000
Arnheim mucky silt loam, 0 to 1 percent slopes, frequently flooded5A110014443571kgz5wi00320061:12000
Moquah-Arnheim complex, 0 to 3 percent slopes, frequently flooded5504A60517116971vg51wi00320061:12000
Arnheim mucky silt loam, 0 to 1 percent slopes, frequently flooded5A4213433671gk8dwi00720051:12000
Arnheim mucky silt loam, 0 to 1 percent slopes, frequently flooded5A212314826841lrvjwi03120051:12000
Bowstring-Arnheim complex, 0 to 1 percent slopes, frequently flooded5374A1481717024451v4jlwi05120061:12000
Rockland-Arnheim, frequently flooded complex, 0 to 70 percent slopes5285F293517023661v4g1wi05120061:12000
Moquah-Arnheim complex, 0 to 3 percent slopes, frequently flooded5504A231917116961vg50wi05120061:12000
Arnheim mucky silt loam, 0 to 1 percent slopes, frequently flooded5A418781906v7mswi05120061:12000
Arnheim silt loam, 0 to 1 percent slopesAr18605422375g5j0wi07519871:20000

Map of Series Extent

Approximate geographic distribution of the ARNHEIM 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 .