Official Series Description


Lab Data Summary

Aggregate lab data for the NORMANNA soil series. This aggregation is based on all pedons with a current taxon name of NORMANNA, 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 NORMANNA 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
93AUMN2634S1978MN1372634Normanna3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties46.8070068,-92.2705078
93A14N0995S2014MN137026Normanna7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties46.932029,-92.19611

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the NORMANNA 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 NORMANNA 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 NORMANNA 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 NORMANNA 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 NORMANNA 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 NORMANNA 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 NORMANNA 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 NORMANNA, 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 NORMANNA 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
Ahmeek-Normanna-Canosia complex, 0 to 18 percent slopes21C501383963452wcmrmn01719731:20000
Normanna-Greysolon complex, 2 to 8 percent slopes, very rockyA1-40B1250727745672rmzcmn03120131:24000
Ahmeek-Normanna-Mesaba, stony complex, 4 to 18 percent slopes, very rockyA1-41D965627745042rmzfmn03120131:24000
Normanna, clayey substratum-Badriver, colluvial mantle complex, 3 to 18 percent slopes, very rockyC1071D641227745452t217mn03120131:24000
Normanna-Canosia-Hermantown complex, 0 to 8 percent slopesA3-30B638627746842rmzpmn03120131:24000
Greysolon-Normanna-Giese, rubbly complex, 0 to 8 percent slopes, very rockyA2-40B214627745782rn03mn03120131:24000
Ahmeek-Normanna-Canosia complex, 0 to 18 percent slopesA3-31D173727745242wcmrmn03120131:24000
Normanna-Giese, depressional complex, 0 to 8 percent slopes, pittedA3-41B38427747212rmztmn03120131:24000
Normanna-Aldenlake-Canosia complex, 0 to 8 percent slopesF2-40B25829437472rn29mn03120131:24000
Normanna-Fluvaquents, frequently flooded-Rock outcrop complex, 0 to 8 percent slopesE1-9B14527746362rn1bmn03120131:24000
Normanna-Hermantown complex, 1 to 8 percent slopesA3-22B7527745882rmznmn03120131:24000
Ahmeek-Normanna-Cathro, depressional complex 0 to 25 percent slopes, pittedA3-42D7329437402rmzvmn03120131:24000
Normanna-Canosia-Hermantown complex, 0 to 8 percent slopesA3-30B3751927421252yz7ymn07520131:24000
Ahmeek-Normanna-Mesaba, stony complex, 4 to 18 percent slopes, very rockyA1-41D2012227421172rmzfmn07520131:24000
Ahmeek-Normanna-Canosia complex, 0 to 18 percent slopesA3-31D1750027421262yz88mn07520131:24000
Aldenlake-Ahmeek complex, 8 to 18 percent slopesF2-41D1684227422252yz82mn07520131:24000
Normanna-Aldenlake-Canosia complex, 0 to 8 percent slopesF2-40B1143927422242zw3zmn07520131:24000
Normanna-Greysolon complex, 2 to 8 percent slopes, very rockyA1-40B1054127421152rmzcmn07520131:24000
Ahmeek-Normanna-Cathro, depressional complex 0 to 25 percent slopes, pittedA3-42D766127421292rmzvmn07520131:24000
Normanna-Giese, depressional complex, 0 to 8 percent slopesA3-41B720927421302zw3vmn07520131:24000
Normanna-Hermantown complex, 1 to 8 percent slopesA3-22B648327421242yz89mn07520131:24000
Greysolon-Normanna-Giese, rubbly complex, 0 to 8 percent slopes, very rockyA2-40B220127421372rn03mn07520131:24000
Normanna, clayey substratum-Badriver, colluvial mantle complex, 3 to 18 percent slopes, very rockyC1071D24227421722t217mn07520131:24000
Normanna-Fluvaquents, frequently flooded-Rock outcrop complex, 0 to 8 percent slopesE1-9B11327421812rn1bmn07520131:24000
Normanna-Canosia-Hermantown complex, 0 to 8 percent slopesF137B41706449574h2tdmn61520071:24000
Ahmeek-Normanna-Canosia complex, 0 to 18 percent slopesF138D272154495752wcmrmn61520071:24000
Normanna-Giese, depressional, complex, pitted, 0 to 8 percent slopesF140B9848449577h2thmn61520071:24000
Ahmeek-Normanna-Cathro, depressional, complex, pitted, 0 to 25 percent slopesF141D8986449578h2tjmn61520071:24000
Urban land-Normanna-Canosia complex, 0 to 8 percent slopesF158B367514249001jtqjmn61520071:24000
Normanna-Aldenlake-Canosia complex, 0 to 8 percent slopesF143B2385449580h2tlmn61520071:24000
Urban land-Ahmeek-Normanna complex, 3 to 18 percent slopesF159D118314248991jtqhmn61520071:24000
Urban land-Greysolon-Normanna-Rock outcrop complex, 1 to 20 percent slopesF119B27014248981jtqgmn61520071:24000
Normanna-Canosia-Hermantown complex, 0 to 8 percent slopesF137B1976317158511vlh1mn61920091:24000
Normanna-Aldenlake-Canosia complex, 0 to 8 percent slopesF143B941317158571vlh7mn61920091:24000
Ahmeek-Normanna-Canosia complex, 0 to 18 percent slopesF138D650817158522wcmrmn61920091:24000
Normanna-Giese, depressional, complex, pitted, 0 to 8 percent slopesF140B366117158541vlh4mn61920091:24000
Ahmeek-Normanna-Cathro, depressional, complex, pitted, 0 to 25 percent slopesF141D198317158551vlh5mn61920091:24000

Map of Series Extent

Approximate geographic distribution of the NORMANNA 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 .