Official Series Description


Lab Data Summary

Aggregate lab data for the MINNEWAUKAN soil series. This aggregation is based on all pedons with a current taxon name of MINNEWAUKAN, 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 MINNEWAUKAN 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 MINNEWAUKAN 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 MINNEWAUKAN 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 MINNEWAUKAN 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 MINNEWAUKAN 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 MINNEWAUKAN 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 MINNEWAUKAN 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 MINNEWAUKAN 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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There are insufficient data to create the 3D mountains figure.

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Click the image to view it full size.

Soil series sharing subgroup-level classification with MINNEWAUKAN, 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. ND-2010-09-27-13 | Morton County - 2002

    Typical pattern of soils and underlying materials in the Havrelon-Mckeen-Lohler association (Soil Survey of Morton County, North Dakota; 2002).

  2. ND-2012-02-08-46 | Ramsey County - August 1986

    Typical pattern of soils and underlying material in the Lallie-Mauvais-Wamduska association (Soil Survey of Ramsey County, North Dakota; August 1986).

Map Units

Map units containing MINNEWAUKAN 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
Minnewaukan soils83783839312tbgid76519751:24000
Minnewaukan fine sandy loam, 0 to 2 percent slopes, frequently floodedE4043A188432567491vzvtmt08319731:24000
Minnewaukan loamy fine sand, 0 to 2 percent slopesG426A38325736112q5cnnd00319881:20000
Minnewaukan loamy fine sand, 0 to 2 percent slopesF426A344425876642q553nd0051:12000
Minnewaukan loamy fine sand, 0 to 2 percent slopesG426A30425737772q5cnnd0051:12000
Mauvais-Minnewaukan, saline complex, 0 to 6 percent slopesF428B14725876492q556nd0051:12000
Minnewaukan fine sandy loam, 0 to 2 percent slopes, frequently floodedE4043A33426617141vzvtnd01519671:20000
Minnewaukan-Stirum complex, 0 to 2 percent slopesC320A3525956522q4x9nd01519671:20000
Minnewaukan loamy fine sand, 0 to 2 percent slopesG426A133825763072q5cnnd0271:12000
Minnewaukan fine sandy loam, 0 to 2 percent slopes, frequently floodedE4043A56526618001vzvtnd02919791:20000
Lallie, saline-Minnewaukan complex, 0 to 2 percent slopesG446A71425764492q5n3nd03119901:20000
Minnewaukan loamy fine sand, 0 to 2 percent slopesG426A61725764482q5cnnd03119901:20000
Lallie, saline-Minnewaukan complex, 0 to 2 percent slopesG446A18125766302q5n3nd03919911:24000
Minnewaukan-Stirum complex, 0 to 2 percent slopesC320A1276725644132q4x9nd04319851:20000
Minnewaukan-Stirum complex, 0 to 2 percent slopesC320A1325967072q4x9nd04719921:20000
Minnewaukan fine sandy loam, 0 to 2 percent slopes, frequently floodedE4043A204632567161vzvtnd05320031:24000
Minnewaukan fine sandy loam, 0 to 2 percent slopes, frequently floodedE4043A5032567551vzvtnd05719761:20000
Minnewaukan fine sandy loam, 0 to 2 percent slopes, frequently floodedE4043A50226991891vzvtnd05919981:20000
Minnewaukan loamy fine sand, 0 to 2 percent slopesF426A114825873382q553nd0631:12000
Minnewaukan loamy fine sand, 0 to 2 percent slopesG426A38925773302q5cnnd0631:12000
Lallie, saline-Minnewaukan complex, 0 to 2 percent slopesG446A9525773322q5n3nd0631:12000
Minnewaukan fine sandy loam, 0 to 2 percent slopes, frequently floodedE4043A58632567171vzvtnd06519711:20000
Mauvais-Minnewaukan, saline complex, 0 to 6 percent slopesF428B453225872122q556nd06919751:20000
Mauvais-Minnewaukan, saline complex, 0 to 6 percent slopesG428B306925823152q5mvnd06919751:20000
Minnewaukan loamy fine sand, 0 to 2 percent slopesG426A6225823172q5cnnd06919751:20000
Minnewaukan loamy fine sand, 0 to 2 percent slopesF426A3025872242q553nd06919751:20000
Minnewaukan loamy fine sand, 0 to 2 percent slopesF426A68125871282q553nd07119841:12000
Mauvais-Minnewaukan, saline complex, 0 to 6 percent slopesF428B3225880682q556nd07919901:24000
Minnewaukan loamy fine sand, 0 to 2 percent slopesG426A15625819892q5cnnd08319901:20000
Minnewaukan fine sandy loam, 0 to 2 percent slopes, frequently floodedE4043A7127160051vzvtnd08919651:20000
Minnewaukan loamy fine sand, 0 to 2 percent slopesG426A36125813802q5cnnd09319901:24000
Minnewaukan fine sandy loam, 0 to 2 percent slopes, frequently floodedE4043A1526625481vzvtnd10519931:24000
Minnewaukan loamy sand, 0 to 3 percent slopesMw65418786g1s7sd01119951:24000
Minnewaukan loamy sandMw1344417762g0q6sd02519921:20000
Minnewaukan loamy sand, occasionally ponded, 0 to 3 percent slopesZ201A104927652522qkm8sd02920061:12000
Minnewaukan loamy sandMw509417110g015sd03719921:20000
Minnewaukan loamy sand, occasionally ponded, 0 to 3 percent slopesZ201A18227129802qkm8sd03919921:20000
Minnewaukan loamy sand, occasionally ponded, 0 to 3 percent slopesZ201A4127129082qkm8sd05119771:20000
Minnewaukan loamy sandMn370417294g073sd05719921:20000
Minnewaukan loamy sand, occasionally ponded, 0 to 3 percent slopesZ201A29127653532qkm8sd05719921:20000
Minnewaukan loamy sandMw651417498g0fpsd07719921:20000
Minnewaukan loamy sandSa120416512fzdwsd07919671:20000
Minnewaukan loamy sandSa432416601fzhrsd09119701:20000
Minnewaukan loamy sandSb603417869g0tnsd10919771:20000
Minnewaukan loamy sand, occasionally ponded, 0 to 3 percent slopesZ201A1527128012qkm8sd10919771:20000

Map of Series Extent

Approximate geographic distribution of the MINNEWAUKAN 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 .