Official Series Description


Lab Data Summary

Aggregate lab data for the CHANNAHON soil series. This aggregation is based on all pedons with a current taxon name of CHANNAHON, 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 CHANNAHON 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 CHANNAHON 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 CHANNAHON 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 CHANNAHON 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 CHANNAHON 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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Click the image to view it full size.

Competing Series

Soil series competing with CHANNAHON 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 CHANNAHON 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 CHANNAHON 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 CHANNAHON, 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

Click a link below to display the diagram. Note that these diagrams may be from multiple survey areas.

  1. MN-2012-02-06-02 | Olmsted County - March 1980

    Pattern of soils and underlying material in the Rockton-Channahon-Atkinson association (Soil Survey of Olmsted County, Minnesota; March 1980).

Map Units

Map units containing CHANNAHON 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
Channahon silt loam, 0 to 2 percent slopes315A16716074611qyplil02320061:12000
Channahon silt loam, 0 to 2 percent slopes315A64915409131nqfwil06320051:12000
Channahon silt loam, 2 to 4 percent slopes315B374114401617dfril06320051:12000
Channahon silt loam, 4 to 6 percent slopes, eroded315C218815409141nqfxil06320051:12000
Channahon-Hesch fine sandy loams, 0 to 2 percent slopes817A11415474801ny8qil06320051:12000
Channahon-Hesch fine sandy loams, 2 to 6 percent slopes817B4415474811ny8ril06320051:12000
Channahon silt loam, 0 to 2 percent slopes315A11902631928tw2il09120031:12000
Channahon silt loam, 2 to 4 percent slopes315B7612631938tw3il09120031:12000
Channahon silt loam, 4 to 6 percent slopes, eroded315C2759881431257lil09120031:12000
Channahon-Hesch fine sandy loams, 2 to 6 percent slopes817B162514160581jjj9il09920061:12000
Channahon-Hesch fine sandy loams, 0 to 2 percent slopes817A133914160571jjj8il09920061:12000
Channahon silt loam, 2 to 4 percent slopes315B4892634888v5mil09920061:12000
Channahon silt loam, 0 to 2 percent slopes315A1454618708nrtbil19720021:12000
Channahon silt loam, 2 to 4 percent slopes315B922618709nrtcil19720021:12000
Channahon silt loam, 4 to 6 percent slopes, eroded315C2381618710nrtdil19720021:12000
Channahon loam, 0 to 3 percent slopes45A66818725268vdmi11519801:15840
Channahon-Emeline-Rockton complex, 25 to 50 percent slopesN575F171613849771hh5pmn03920051:12000
Channahon loam, 6 to 12 percent slopes472C7151400783fg1hmn10919771:15840
Channahon loam, 1 to 6 percent slopes472B5290400782fg1gmn10919771:15840
Channahon silt loam, 12 to 18 percent slopes472D86916771261t95vmn16319781:15840
Channahon silt loam, 6 to 12 percent slopes472C55316771251t95tmn16319781:15840
Channahon silt loam, 1 to 6 percent slopes472B27516771241t95smn16319781:15840
Channahon-Biglick complex, 6 to 12 percent slopesChC62644377pmjcoh06319971:12000
Channahon silt loam, 0 to 2 percent slopesCnA19801699715pvyoh14719781:15840
Channahon silt loam, 2 to 6 percent slopesCnB11901699725pvzoh14719781:15840
Channahon loam, 2 to 6 percent slopesCnB18933268469g609wi01520231:15840
Channahon loam, 6 to 12 percent slopesCnC10473268470g60bwi01520231:15840
Channahon silt loam, 12 to 30 percent slopes, erodedCaE22910423266g6frwi02119721:15840
Channahon silt loam, 6 to 12 percent slopes, erodedCaC21799423265g6fqwi02119721:15840
Channahon silt loam, 2 to 6 percent slopesCaB869423264g6fpwi02119721:15840
Channahon silt loam, 1 to 6 percent slopesCdB1236423557g6r4wi02719761:15840
Channahon silt loam, 6 to 12 percent slopes, erodedCdC2753423558g6r5wi02719761:15840
Rock outcrop-Channahon complex, 5 to 30 percent slopesRcE643423638g6trwi02719761:15840
Channahon silt loam, 12 to 25 percent slopes, erodedCdD2458423559g6r6wi02719761:15840
Channahon loam, 2 to 6 percent slopesCnB5173268600g609wi07120231:15840
Channahon loam, 6 to 12 percent slopesCnC4283268599g60bwi07120231:15840
Channahon silt loam, 2 to 6 percent slopesCnB437422541g5pcwi08719751:15840

Map of Series Extent

Approximate geographic distribution of the CHANNAHON 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 .