Official Series Description


Lab Data Summary

Aggregate lab data for the MARQUETTE soil series. This aggregation is based on all pedons with a current taxon name of MARQUETTE, 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 MARQUETTE 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
56UMN1261S1971MN0691261Marquette2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties48.78265,-96.5150833
57UMN4471S1990MN029815 (4471)Marquette2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties47.5615997,-95.3426208
57UMN4472S1990MN029816 (4472)Marquette2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties47.5589981,-95.3438339
91BUMN4513S1991MN141162 (4513)Marquette3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties45.3728676,-93.564003

Water Balance

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

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 MARQUETTE, 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-2010-09-10-08 | Roseau County -

    Relationship of soils, underlying materials, and landforms in the Karstad-Markey-Corliss association (Soil Survey of Roseau County, Minnesota).

Map Units

Map units containing MARQUETTE 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
Marquette loamy sand, 6 to 12 percent slopes2038C110125204622t4svmn00719911:24000
Marquette loamy sand, 1 to 6 percent slopes2038B101925204612t4swmn00719911:24000
Marquette loamy sand, 1 to 6 percent slopes2038B88026036352t4swmn02919931:20000
Marquette loamy sand, 6 to 12 percent slopes2038C3526036342t4svmn02919931:20000
Marquette loamy sand, 2 to 9 percent slopesI78B265279842321bxcmn06920071:12000
Karlstad-Marquette loamy sands, 0 to 8 percent slopesI80B8279842821bxjmn06920071:12000
Marquette loamy sand, 1 to 6 percent slopes242B10383988752t4swmn07719891:24000
Marquette loamy sand, 6 to 12 percent slopes242D2483988762t4svmn07719891:24000
Marquette loamy sand, 1 to 6 percent slopes242B20703571322t4swmn08919941:20000
Marquette loamy sand, 2 to 9 percent slopesI78B212279896021bxcmn08919941:20000
Marquette loamy sand, 2 to 9 percent slopesI78B612279970021bxcmn11919961:20000
Marquette loamy sand, 9 to 30 percent slopesI78D47127997332ql29mn11919961:20000
Karlstad-Marquette complex, 0 to 8 percent slopes1327B2325394806f7tpmn13519991:24000
Marquette loamy sand, 1 to 6 percent slopes242B21313948452t4swmn13519991:24000
Karlstad-Marquette loamy sands, 0 to 8 percent slopesI80B1320279984521bxjmn13519991:24000
Marquette loamy sand, 2 to 9 percent slopesI78B240279984021bxcmn13519991:24000

Map of Series Extent

Approximate geographic distribution of the MARQUETTE 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 .