Official Series Description


Lab Data Summary

Aggregate lab data for the DULUTH soil series. This aggregation is based on all pedons with a current taxon name of DULUTH, 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 DULUTH 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
88UMN2571S1978MN137031 (2571)Duluth2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties47.4832191,-92.684967
88UMN2799S1978MN137035 (2799)Duluth2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties47.4595299,-92.7610626
88UMN2798S1978MN137036 (2798)Duluth2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties47.4654007,-92.7630692
88UMN2572S1978MN137044 (2572)Duluth2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties46.9898186,-92.5765228
8897P0221S1996MN137529Duluthn/aPrimary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties46.8883324,-92.6416702
90A40A171268MN017004Duluth6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties46.5166664,-92.5999985
90AUMN1081S1969MN0011081Duluth2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties46.5508232,-93.4254837
90AUMN2058S1975MN0012058Duluth2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties46.5214767,-93.6844788
90AUMN2927S1978MN0012927Duluth3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties46.5802841,-93.1798935
90AUMN3629S1982MN001008 (3629)Duluth2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties46.6489105,-93.0698624
90A97P0269S1994MN095045Duluth6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties46.1791649,-93.8016663
90BUMN1568S1972MN1631568Duluth2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties45.2525902,-92.8499069
90B40A1757S1974MN163007DULUTH7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties45.1705475,-92.8968735
92UMN2998S1979MN137052 (2998)Duluth2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties46.8948402,-92.0067368

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the DULUTH 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 DULUTH 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 DULUTH 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 DULUTH 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 DULUTH 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 DULUTH 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 DULUTH 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 DULUTH, 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

No block diagrams are available.

Map Units

Map units containing DULUTH 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
Duluth fine sandy loam, 1 to 6 percent slopes504B25707432922gjh7mn00119961:20000
Duluth fine sandy loam, 6 to 12 percent slopes504C11087432923gjh8mn00119961:20000
Duluth fine sandy loam, 12 to 25 percent slopes504E3465432924gjh9mn00119961:20000
Duluth very fine sandy loam, 2 to 12 percent slopes504C44318396369f9g3mn01719731:20000
Duluth very fine sandy loam, 0 to 2 percent slopes50410264396368f9g2mn01719731:20000
Duluth very fine sandy loam, 12 to 25 percent slopes504E3368396370f9g4mn01719731:20000
Duluth very fine sandy loam, 25 to 35 percent slopes504G726396371f9g5mn01719731:20000
Duluth-Sanburn-Cathro complex, pitted, 0 to 15 percent slopesC45C242216763911t8f4mn09520061:12000
Duluth-Sanburn-Cathro complex, pitted, 0 to 35 percent slopesC45E174516763921t8f5mn09520061:12000
Duluth loam, 8 to 15 percent slopesC43C86916763881t8f1mn09520061:12000
Duluth loam, 15 to 25 percent slopesC43E58916763891t8f2mn09520061:12000
Duluth silt loam, 6 to 12 percent slopes504C21816772651t9bbmn12319781:15840
Duluth silt loam, 12 to 25 percent slopes504D17316772661t9bcmn12319781:15840
Duluth silt loam, 1 to 6 percent slopes504B6816772641t9b9mn12319781:15840
Duluth silt loam, 1 to 6 percent slopes504B142816771291t95ymn16319781:15840
Duluth silt loam, 6 to 12 percent slopes504C138316771301t95zmn16319781:15840
Duluth silt loam, 12 to 25 percent slopes504D76216771311t960mn16319781:15840
Duluth-Culver-Cathro, depressional, complex, 0 to 18 percent slopesB128D2658449538h2s7mn61520071:24000
Duluth-Duluth, coarse substratum-Ellsburg complex, 0 to 18 percent slopesB130D1998449540h2s9mn61520071:24000
Duluth-Culver complex, 3 to 18 percent slopesB126D1493449535h2s4mn61520071:24000
Dinham-Duluth complex, 8 to 18 percent slopesB150D1350435333gm00mn61520071:24000
Duluth-Duluth, coarse substratum complex, 18 to 45 percent slopesB131F283449542h2scmn61520071:24000
Duluth silt loam, 18 to 45 percent slopesB126E231449536h2s5mn61520071:24000
Duluth-Culver-Cathro, depressional, complex, 0 to 18 percent slopesB128D677917157391vlcfmn61920091:24000
Duluth-Culver complex, 3 to 18 percent slopesB126D506117157361vlcbmn61920091:24000
Duluth silt loam, 18 to 45 percent slopesB126E206717157371vlccmn61920091:24000
Duluth-Duluth, coarse substratum-Ellsburg complex, 0 to 18 percent slopesB130D167817157411vlchmn61920091:24000
Duluth-Duluth, coarse substratum, complex, 18 to 45 percent slopesB131F109717157421vlcjmn61920091:24000
Dinham-Duluth complex, 8 to 18 percent slopesB150D44717157471vlcpmn61920091:24000

Map of Series Extent

Approximate geographic distribution of the DULUTH 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 .