Official Series Description


Lab Data Summary

Aggregate lab data for the DANAHER soil series. This aggregation is based on all pedons with a current taxon name of DANAHER, 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 DANAHER 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 DANAHER 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 DANAHER 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 DANAHER 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 DANAHER 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 flats position figure.

Competing Series

Soil series competing with DANAHER 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 DANAHER series and competing. Series are sorted according to hierarchical clustering of median values. Source: SSURGO map unit geometry and 1981-2010, 800m PRISM data .

Click the image to view it full size.

Geomorphic description summaries for the DANAHER 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 hills figure.

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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 DANAHER, 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 DANAHER 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
Danaher-Loberg complex, 15 to 35 percent slopes387E122185957420f18mt60520071:24000
Danaher loam, 4 to 15 percent slopes87D46185956320f0xmt60520071:24000
Danaher-Loberg complex, 15 to 35 percent slopes387E4941547525610mt61620031:24000
Danaher loam, 4 to 15 percent slopes87D16615512656f2mt61620031:24000
Danaher loam, 15 to 35 percent slopes87E4815512756f3mt61620031:24000
Danaher-Loberg complex, 15 to 35 percent slopes387E20381443674v70mt62119971:24000
Danaher-Loberg-Elve complex, 15 to 35 percent slopes487E9431444524v9rmt62119971:24000
Danaher-Loberg-Elve complex, 8 to 15 percent slopes487D9281444514v9qmt62119971:24000
Danaher-Loberg complex, 8 to 15 percent slopes387D8241443664v6zmt62119971:24000
Danaher loam, 4 to 15 percent slopes87D5911446304vhhmt62119971:24000
Danaher loam, 15 to 35 percent slopes87E1421446314vhjmt62119971:24000
Danaher-Loberg complex, 35 to 60 percent slopes387F931443684v71mt62119971:24000
Danaher, stony-Loberg, very stony complex, 15 to 45 percent slopes792E880155729571jmt62219971:24000
Danaher, stony-Loberg, very stony complex, 8 to 15 percent slopes792D508155728571hmt62219971:24000
Loberg, very stony-Danaher, stony complex, 15 to 45 percent slopes396E46315545456rnmt62219971:24000
Loberg-Worock-Danaher families, complex, moderately steep old moraines22UC2516914941050gpmt63520061:24000
Loberg-Worock-Danaher families, complex, unstable moderately steep old moraines22UCD220614941150gqmt63520061:24000
Danaher-Loberg complex, 15 to 35 percent slopes387E100617029441v51pmt63520061:24000
Loberg-Danaher-Elvick families, complex, low relief mountain slopes and ridges75DCD67114953250lmmt63520061:24000
Danaher-Loberg-Elve complex, 15 to 35 percent slopes487E35317029631v529mt63520061:24000
Danaher loam, 4 to 15 percent slopes87D29317029871v532mt63520061:24000
Danaher-Loberg-Elve complex, 8 to 15 percent slopes487D12417029621v528mt63520061:24000
Danaher-Timberlin complex, 25 to 60 percent slopes407F618149968511pmt63920001:24000
Tongue River-Danaher loams, 15 to 35 percent slopes358E5481499165100mt63920001:24000
Danaher-Loberg complex, 15 to 35 percent slopes387E11861457044wm4mt64419951:24000
Danaher loam, 4 to 15 percent slopes87D6901459434wvvmt64419951:24000
Danaher loam, 15 to 35 percent slopes87E6081459444wvwmt64419951:24000
Rocko-Danaher-Mollet loams, 4 to 35 percent slopes5528E2088699257rgmpmt6691:24000

Map of Series Extent

Approximate geographic distribution of the DANAHER 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 .