Official Series Description


Lab Data Summary

Aggregate lab data for the QUAM soil series. This aggregation is based on all pedons with a current taxon name of QUAM, 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 QUAM 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
102AUMN1175S1970MN0511175Quam3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties45.980793,-95.9708557
102AUMN1225S1971MN0831225Quam3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties44.3529968,-95.8935013
102AUMN2263S1976MN0272263Quam3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties46.8039627,-96.2747726
102AUMN3261S1980MN1013261Quam2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties44.1800117,-95.6830902
91AUMN2021S1975MN0272021Quam3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties46.653453,-96.217348

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the QUAM 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 QUAM 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 QUAM 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 QUAM 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.

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

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Competing Series

Soil series competing with QUAM 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 QUAM 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 QUAM 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.

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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 QUAM, 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. MN-2010-09-08-04 | Becker County - 1998

    Typical pattern of soils and parent material in the Formdale-Langhei-Flom association (Soil Survey of Becker County, Minnesota; 1998).

  2. MN-2010-09-08-19 | Otter Tail County - 2001

    Typical pattern of soils and parent material in the Barnes-Langhei-Lakepark association (Soil Survey of Otter Tail County, Minnesota; 2001).

  3. MN-2010-09-08-20 | Otter Tail County - 2001

    Typical pattern of soils and parent material in the Chapett-Sisseton-Friberg association (Soil Survey of Otter Tail County, Minnesota; 2001).

  4. MN-2010-09-08-22 | Otter Tail County - 2001

    Typical pattern of soils and parent material in the Forman-Buse-Peever association (Soil Survey of Otter Tail County, Minnesota; 2001).

  5. MN-2010-09-10-15 | Swift County -

    Tara-Doland-Buse association (Soil Survey of Swift County, Minnesota).

  6. MN-2010-09-10-16 | Swift County -

    Bearden-Rondell association (Soil Survey of Swift County, Minnesota).

Map Units

Map units containing QUAM 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
Quam family, 0 to 5 percent slopes.1729617470393hsgzca70219841:24000
Quam and Cathro soils, 0 to 1 percent slopes, frequently pondedJ130A869731825122yw5bmn00519941:20000
Quam-Cathro-Lakepark complex, 0 to2 percent slopes, frequently pondedJ132A454431825062yw53mn00519941:20000
Quam, Cathro, and Urness soils, frequently ponded, 0 to 1 percent slopes122727823974452w8fgmn00519941:20000
Quam silty clay loam, 0 to 1 percent slopes, occasionally pondedJ131A270431825052yw52mn00519941:20000
Flom-Quam silty clay loams, 0 to 1 percent slopes, occasionally pondedJ116A166931825132yw5cmn00519941:20000
Aazdahl-Quam-Lakepark complex, 0 to 4 percent slopesJ112B149631825092yw57mn00519941:20000
Quam silty clay loam, occasionally ponded, 0 to 1 percent slopes34411573975162vv68mn00519941:20000
Flom-Aazdahl-Quam complex, 0 to 4 percent slopesJ114B36231825112yw59mn00519941:20000
Quam and Cathro soils, 0 to 1 percent slopes, frequently pondedJ130A1104231825302yw5bmn01119901:20000
Quam silty clay loam, 0 to 1 percent slopes, occasionally pondedJ131A374031825232yw52mn01119901:20000
Flom-Quam silty clay loams, 0 to 1 percent slopes, occasionally pondedJ116A152331825312yw5cmn01119901:20000
Flom-Aazdahl-Quam complex, 0 to 4 percent slopesJ114B56031825292yw59mn01119901:20000
Quam-Cathro-Lakepark complex, 0 to2 percent slopes, frequently pondedJ132A45731825242yw53mn01119901:20000
Aazdahl-Quam-Lakepark complex, 0 to 4 percent slopesJ112B33631825272yw57mn01119901:20000
Bearden-Quam, depressional, complex, 0 to 2 percent slopesJ51A8866424230572mbd4mn02319801:15840
Colvin-Quam complex, depressional, 0 to 1 percent slopesJ260A2393724230702mbdkmn02319801:15840
Spicer-Quam silty clay loams18022828396496f9l6mn02319801:15840
Quam, Cathro, and Urness soils, frequently ponded, 0 to 1 percent slopesJ43A118930264492w8fgmn02319801:15840
Glyndon-Quam silty clay loams8811118396529f9m8mn02319801:15840
Quam silty clay loam, occasionally ponded, 0 to 1 percent slopesJ17A102024230362vv68mn02319801:15840
Quam, Cathro, and Urness soils, frequently ponded, 0 to 1 percent slopes105591133569362w8fgmn02719801:20000
Quam silty clay loam, occasionally ponded, 0 to 1 percent slopes34431613569622vv68mn02719801:20000
Quam silt loam3442129396842f9ycmn03719801:15840
Quam silt loam, ponded1824866396794f9wtmn03719801:15840
Quam silty clay loam, occasionally ponded, 0 to 1 percent slopesQu134513973152vv68mn04119701:12000
Quam, Cathro, and Urness soils, frequently ponded, 0 to 1 percent slopesMh73543972962w8fgmn04119701:12000
Quam and Cathro soils, 0 to 1 percent slopes, frequently pondedJ130A1275231825482yw5bmn05119741:20000
Quam silty clay loam, 0 to 1 percent slopes, occasionally pondedJ131A561431825412yw52mn05119741:20000
Flom-Quam silty clay loams, 0 to 1 percent slopes, occasionally pondedJ116A490431825492yw5cmn05119741:20000
Quam-Cathro-Lakepark complex, 0 to2 percent slopes, frequently pondedJ132A363831825422yw53mn05119741:20000
Quam, Cathro, and Urness soils, frequently ponded, 0 to 1 percent slopes105329363980212w8fgmn05119741:20000
Aazdahl-Quam-Lakepark complex, 0 to 4 percent slopesJ112B141031825452yw57mn05119741:20000
Quam silty clay loam, occasionally ponded, 0 to 1 percent slopes3445793980412vv68mn05119741:20000
Flom-Aazdahl-Quam complex, 0 to 4 percent slopesJ114B32231825472yw59mn05119741:20000
Quam mucky silty clay loam, depressional, MLRA 90, 0 to 1 percent slopesC21A29516734691t5cwmn06520061:12000
Quam, Cathro, and Urness soils, frequently ponded, 0 to 1 percent slopesJ43A739430264502w8fgmn06719831:20000
Quam silty clay loam, occasionally ponded, 0 to 1 percent slopesJ17A110528844312vv68mn06719831:20000
Quam silty clay loam, occasionally ponded, 0 to 1 percent slopes34447304303002vv68mn07319941:20000
Quam silty clay loam, depressional, 0 to 1 percent slopesJ17A1746114951317l52mn08120071:12000
Quam silty clay loam, depressional, 0 to 1 percent slopesJ17A414862191lwjkmn08320081:12000
Quam, Cathro, and Urness soils, frequently ponded, 0 to 1 percent slopes180470713992122w8fgmn08719921:20000
Quam silty clay loam, occasionally ponded, 0 to 1 percent slopes3448583992272vv68mn08719921:20000
Quam mucky silty clay loam, depressional, MLRA 90, 0 to 1 percent slopesC21A89216763701t8dgmn09520061:12000
Quam silty clay loam, depressional, 0 to 1 percent slopesJ17A591114951517l54mn10120081:12000
Quam, Cathro, and Urness soils, frequently ponded, 0 to 1 percent slopesMh10743572522w8fgmn10719701:20000
Quam, Cathro, and Urness soils, frequently ponded, 0 to 1 percent slopes1227125704355712w8fgmn11119961:20000
Quam and Cathro soils, 0 to 1 percent slopes, frequently pondedJ130A809331825662yw5bmn11119961:20000
Quam silty clay loam, occasionally ponded, 0 to 1 percent slopes123949374355772vv68mn11119961:20000
Flom-Quam silty clay loams, 0 to 1 percent slopes, occasionally pondedJ116A293531825672yw5cmn11119961:20000
Quam silty clay loam, 0 to 1 percent slopes, occasionally pondedJ131A276431825592yw52mn11119961:20000
Quam-Cathro-Lakepark complex, 0 to2 percent slopes, frequently pondedJ132A255331825602yw53mn11119961:20000
Aazdahl-Quam-Lakepark complex, 0 to 4 percent slopesJ112B201531825632yw57mn11119961:20000
Flom-Aazdahl-Quam complex, 0 to 4 percent slopesJ114B66031825652yw59mn11119961:20000
Quam, Cathro, and Urness soils, frequently ponded, 0 to 1 percent slopes1055199629474172w8fgmn11919961:20000
Quam, Cathro, and Urness soils, frequently ponded, 0 to 1 percent slopesMk58404013712w8fgmn12119681:20000
Quam silty clay loam, occasionally ponded, 0 to 1 percent slopesJ17A31114013502vv68mn12119681:20000
Quam and Cathro soils, 0 to 1 percent slopes, frequently pondedJ130A43131825842yw5bmn12119681:20000
Flom-Quam silty clay loams, 0 to 1 percent slopes, occasionally pondedJ116A17331825852yw5cmn12119681:20000
Aazdahl-Quam-Lakepark complex, 0 to 4 percent slopesJ112B11931825812yw57mn12119681:20000
Quam silty clay loam, 0 to 1 percent slopes, occasionally pondedJ131A11031825772yw52mn12119681:20000
Quam-Cathro-Lakepark complex, 0 to2 percent slopes, frequently pondedJ132A9431825782yw53mn12119681:20000
Flom-Aazdahl-Quam complex, 0 to 4 percent slopesJ114B2631825832yw59mn12119681:20000
Quam silty clay loam, occasionally ponded, 0 to 1 percent slopes11451584280732vv68mn14519801:15840
Quam, Cathro, and Urness soils, frequently ponded, 0 to 1 percent slopes105533004280702w8fgmn14519801:15840
Quam and Cathro soils, 0 to 1 percent slopes, frequently pondedJ130A970031826022yw5bmn14919661:15840
Quam silty clay loam, 0 to 1 percent slopes, occasionally pondedJ131A626331825952yw52mn14919661:15840
Flom-Quam silty clay loams, 0 to 1 percent slopes, occasionally pondedJ116A442231826032yw5cmn14919661:15840
Quam-Cathro-Lakepark complex, 0 to2 percent slopes, frequently pondedJ132A165631825962yw53mn14919661:15840
Quam, Cathro, and Urness soils, frequently ponded, 0 to 1 percent slopesMh10934283562w8fgmn14919661:15840
Aazdahl-Quam-Lakepark complex, 0 to 4 percent slopesJ112B92731825992yw57mn14919661:15840
Flom-Aazdahl-Quam complex, 0 to 4 percent slopesJ114B31531826012yw59mn14919661:15840
Bearden-Quam, depressional, complex, 0 to 2 percent slopesJ51A58936434839glh2mn15120001:12000
Quam silty clay loam, occasionally ponded, 0 to 1 percent slopesJ17A63284347942vv68mn15120001:12000
Quam, Cathro, and Urness soils, frequently ponded, 0 to 1 percent slopesJ43A45804348282w8fgmn15120001:12000
Quam and Cathro soils, 0 to 1 percent slopes, frequently pondedJ130A557831826202yw5bmn15519861:20000
Flom-Quam silty clay loams, 0 to 1 percent slopes, occasionally pondedJ116A80931826212yw5cmn15519861:20000
Quam silty clay loam, 0 to 1 percent slopes, occasionally pondedJ131A79931826132yw52mn15519861:20000
Quam-Cathro-Lakepark complex, 0 to2 percent slopes, frequently pondedJ132A76531826142yw53mn15519861:20000
Quam silty clay loam, ponded1940404357347czvbmn15519861:20000
Flom-Aazdahl-Quam complex, 0 to 4 percent slopesJ114B18531826192yw59mn15519861:20000
Quam silty clay loam, occasionally ponded, 0 to 1 percent slopes3441273573592vv68mn15519861:20000
Aazdahl-Quam-Lakepark complex, 0 to 4 percent slopesJ112B8431826172yw57mn15519861:20000
Quam, Cathro, and Urness soils, frequently ponded, 0 to 1 percent slopes10555483573902w8fgmn16719851:20000
Quam silty clay loam, occasionally ponded, 0 to 1 percent slopes3442553573932vv68mn16719851:20000
Quam silty clay loam, 0 to 1 percent slopes, occasionally pondedJ131A131826272yw52mn16719851:20000

Map of Series Extent

Approximate geographic distribution of the QUAM 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 .