Official Series Description


Lab Data Summary

Aggregate lab data for the ZUMBRO soil series. This aggregation is based on all pedons with a current taxon name of ZUMBRO, 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 ZUMBRO 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
104UMN1158S1970MN0491158Zumbro3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties44.5467796,-92.7673645

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the ZUMBRO 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 ZUMBRO 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 ZUMBRO 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 ZUMBRO 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 ZUMBRO 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 ZUMBRO 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 ZUMBRO 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 ZUMBRO, 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 ZUMBRO 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
Zumbro sandy loam, 1 to 6 percent slopes, occasionally flooded8349B41023786952kv73il00119971:12000
Zumbro sandy loam, 1 to 6 percent slopes, occasionally flooded8349B10991752135wb1il06719931:15840
Zumbro sandy loam, 1 to 6 percent slopes, occasionally flooded8349B1586614908nmvril14920011:12000
Zumbro sandy loam, 1 to 4 percent slopes, rarely flooded7349B8910793133vm9yil19520031:12000
Zumbro loamy sand495326396297f9csmn01519841:20000
Zumbro loamy fine sand18151163396791f9wqmn03719801:15840
Zumbro fine sandy loam495936396871f9z9mn03719801:15840
Ankeny-Zumbro complex, 0 to 3 percent slopes, occasionally floodedN622A191516758831t7wrmn04920071:12000
Du Page-Zumbro complex, occasionally flooded883460430350gft8mn07319941:20000
Havelock-Zumbro complex, 0 to 3 percent slopes, frequently floodedL243A1423998032lk60mn08320081:12000
Havelock-Zumbro complex, 0 to 3 percent slopes, frequently floodedL243A1823990612ljf2mn10120081:12000
Zumbro loamy sand495627400811fg2dmn10919771:15840
Havelock-Zumbro complex, 0 to 3 percent slopes, frequently floodedL243A649923991552ljj3mn12720081:12000
Zumbro loamy fine sandZb116122164612dddrmn15720081:12000
Zumbro-Calco complex1867106716535711shp0mn17319791:20000
Zumbro-Du Page complex88333716536371shr4mn17319791:20000

Map of Series Extent

Approximate geographic distribution of the ZUMBRO 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 .