Official Series Description


Lab Data Summary

Aggregate lab data for the TOTAGATIC soil series. This aggregation is based on all pedons with a current taxon name of TOTAGATIC, 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 TOTAGATIC 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
91B98P0250S1997WI129001Totagatic6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties46.0744438,-91.9697189

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the TOTAGATIC 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 TOTAGATIC 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 TOTAGATIC 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 TOTAGATIC 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 TOTAGATIC 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 TOTAGATIC series and competing. Series are sorted according to hierarchical clustering of median values. Source: SSURGO map unit geometry and 1981-2010, 800m PRISM data .

There are insufficient data to create the annual climate figure.

Geomorphic description summaries for the TOTAGATIC 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 .

There are insufficient data to create the 2D hillslope position figure.

There are insufficient data to create the 3D hills figure.

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 TOTAGATIC, 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 TOTAGATIC 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
Arnheim-Totagatic-Sturgeon complex, 0 to 6 percent slopes, frequently flooded24A32317179221vnmvmi6061:12000
Annalake-Totagatic, frequently flooded-Annanias complex, 0 to 8 percent slopes25B8417179231vnmwmi6061:12000
Lougee-Totagatic-Bowstring complex, 0 to 1 percent slopes, frequently floodedD89A1535727326572ndrfmn03520091:24000
Graycalm-Totagatic, frequently flooded complex, 0 to 35 percent slopes2-11D247927326622p6v0mn03520091:24000
Fordum, Totagatic, and Bowstring soils, 0 to 1 percent slopes, frequently flooded9050A840614445571kh5mwi00320061:12000
Fordum, Totagatic, and Bowstring soils, 0 to 1 percent slopes, frequently flooded9050A330913839491hg3jwi00720051:12000
Totagatic-Bowstring-Ausable complex, 0 to 2 percent slopes, frequently flooded3A236114740017hyxwi00720051:12000
Totagatic-Bowstring-Ausable complex, 0 to 2 percent slopes, frequently flooded3A5891816923wf2cwi01320041:12000
Totagatic-Winterfield complex, 0 to 2 percent slopes, frequently flooded64A3282816926wf2gwi01320041:12000
Winterfield-Totagatic complex, 0 to 2 percent slopes, frequently flooded706A1571816940wf2xwi01320041:12000
Totagatic-Bowstring-Ausable complex, 0 to 2 percent slopes, frequently flooded3A274313859931hj7gwi03120051:12000
Totagatic-Winterfield complex, 0 to 2 percent slopes, frequently flooded64A932781071v6rvwi03120051:12000
Winterfield-Totagatic complex, 0 to 2 percent slopes, frequently flooded706A771781442v74twi03120051:12000
Totagatic-Bowstring-Ausable complex, 0 to 2 percent slopes, frequently flooded3A154416883061tnthwi05120061:12000
Fordum, Totagatic, and Bowstring soils, 0 to 1 percent slopes, frequently flooded9050A10117012611v39dwi05120061:12000
Totagatic-Bowstring-Ausable complex, 0 to 2 percent slopes, frequently flooded3A69324276962mh6swi09519781:15840
Totagatic-Winterfield complex, 0 to 2 percent slopes, frequently flooded64A51524276922mh6nwi09519781:15840
Fordum, Totagatic, and Bowstring soils, 0 to 1 percent slopes, frequently flooded9050A604713957401hvcwwi09920061:12000
Fordum, Totagatic, and Bowstring soils, 0 to 1 percent slopes, frequently flooded9050A761913861081hjc5wi11320061:12000
Totagatic-Bowstring-Ausable complex, 0 to 2 percent slopes, frequently flooded3A628625335nzq3wi11320061:12000
Totagatic-Bowstring-Ausable complex, 0 to 2 percent slopes, frequently flooded3A3257449064h28ywi12920021:12000
Totagatic-Winterfield complex, 0 to 2 percent slopes, frequently flooded64A1012435469gm4dwi12920021:12000
Winterfield-Totagatic complex, 0 to 2 percent slopes, frequently flooded706A72433550gk4hwi12920021:12000

Map of Series Extent

Approximate geographic distribution of the TOTAGATIC 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 .