Official Series Description


Lab Data Summary

Aggregate lab data for the MOQUAH soil series. This aggregation is based on all pedons with a current taxon name of MOQUAH, 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 MOQUAH 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
9200P0275S1999MI131003Moquah6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties46.8419456,-89.3249969
9203N0268S2002MI131006Moquah7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties46.7196121,-89.2061996
9203N0272S2002MI131010Moquah6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties46.8219414,-88.968956
93B02N0153S2001MI053016Moquah7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties46.5122032,-89.9819717

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the MOQUAH 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 MOQUAH 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 MOQUAH 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 MOQUAH 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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Click the image to view it full size.

Competing Series

Soil series competing with MOQUAH 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 MOQUAH 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 MOQUAH 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 MOQUAH, 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-2010-09-10-14 | Ontonagon County -

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

Map Units

Map units containing MOQUAH 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
Moquah silt loam, 0 to 3 percent slopes43A1850414980fxtgmi01319841:20000
Moquah-Arnheim complex, 0 to 3 percent slopes, frequently flooded230B448014563791kwgzmi05320071:24000
Moquah loam, 0 to 3 percent slopes, occasionally flooded8230B54624850002pdv9mi06119891:20000
Moquah-Arnheim complex, 0 to 3 percent slopes, frequently flooded63B10725660331kwkrmi06119891:20000
Moquah-Pelkie complex, 1 to 8 percent slopes, frequently flooded8077B5124861632pg1tmi06119891:20000
Miskoaki-Moquah, frequently flooded-Watton complex, 0 to 50 percent slopes8139E2725660351kwp2mi06119891:20000
Loggerhead-Ubly-Moquah, frequently flooded complex, 0 to 35 percent slopes8285D324848092pdn4mi06119891:20000
Arnheim-Moquah complex, 0 to 3 percent slopes247398415463fyb1mi10919851:20000
Rockland-Moquah, frequently flooded-Watton complex, 0 to 70 percent slopes125F1638214565521kwnkmi13120071:24000
Rockland-Moquah, frequently flooded, complex, 0 to 70 percent slopes169F1357714566101kwqfmi13120071:24000
Moquah loam, 0 to 3 percent slopes, occasionally flooded119A721014565421kwn7mi13120071:24000
Rockland-Negwegon-Moquah, frequently flooded, complex, 0 to 35 percent slopes170E562914566111kwqgmi13120071:24000
Moquah-Arnheim complex, 0 to 3 percent slopes, frequently flooded63B520714564651kwkrmi13120071:24000
Miskoaki-Moquah, frequently flooded-Watton complex, 0 to 50 percent slopes139E349114565681kwp2mi13120071:24000
Loggerhead-Ubly-Moquah, frequently flooded, complex, 0 to 35 percent slopes8285D174716748861t6vlmi13120071:24000
Ubly-Moquah, frequently flooded-Arnheim, frequently flooded, complex, 0 to 60 percent slopes157F137214565971kwq0mi13120071:24000
Gogebic-Moquah, frequently flooded, complex, 0 to 55 percent slopes, very rocky8367E50416749381t6x8mi13120071:24000
Moquah-Pelkie complex, 1 to 8 percent slopes, frequently flooded8077C27116748091t6s3mi13120071:24000
Moquah fine sandy loam, 0 to 3 percent slopes, frequently flooded6A820514443581kgz6wi00320061:12000
Moquah-Arnheim complex, 0 to 3 percent slopes, frequently flooded5504A60517116971vg51wi00320061:12000
Moquah fine sandy loam, 0 to 3 percent slopes, frequently flooded6A3543433739gkblwi00720051:12000
Moquah fine sandy loam, 0 to 3 percent slopes, frequently flooded6A289014826851lrvkwi03120051:12000
Moquah-Arnheim complex, 0 to 3 percent slopes, frequently flooded5504A231917116961vg50wi05120061:12000
Moquah fine sandy loam, 0 to 3 percent slopes, frequently flooded6A179781907v7mtwi05120061:12000
Moquah fine sandy loam, 0 to 2 percent slopesMt2259422425g5kmwi07519871:20000

Map of Series Extent

Approximate geographic distribution of the MOQUAH 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 .