Official Series Description


Lab Data Summary

Aggregate lab data for the KASSON soil series. This aggregation is based on all pedons with a current taxon name of KASSON, 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 KASSON 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
10405N02672004IA017007Kasson7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties42.6684723,-92.5408859
10440A171970MN039002Kasson7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties43.9455566,-92.8305588
104UMN1276S1963MN0491276Kasson2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties44.1974924,-92.8931299
104UMN1098S1966MN1311098Kasson2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties44.3408203,-93.1138763
104UMN3109S1979MN0993109Kasson2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties43.7366371,-92.7798462
104UMN3385S1980MN099133Kasson3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties43.8432503,-92.8714905
10485P0408S1984IA105024Kasson5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties42.0705556,-91.1694444

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the KASSON 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 KASSON 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 KASSON 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 KASSON 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 KASSON 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 KASSON 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 KASSON 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 KASSON, 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. IA-2010-09-09-28 | Winneshiek County - 2007

    Typical pattern of soils and parent material in the Winneshiek-Marlean association (Soil Survey of Winneshiek County, Iowa; 2007).

  2. IA-2010-09-09-29 | Winneshiek County - 2007

    Typical pattern of soils and parent material in the Kasson-Floyd association (Soil Survey of Winneshiek County, Iowa; 2007).

  3. MN-2012-02-06-01 | Olmsted County - March 1980

    Pattern of soils and underlying material in the Readlyn-Maxfield-Kenyon association (Soil Survey of Olmsted County, Minnesota; March 1980).

Map Units

Map units containing KASSON 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
Kasson loam, 2 to 5 percent slopes582B405116895822xl3ria01720081:12000
Kasson loam, 5 to 9 percent slopes582C45216895832xl3sia01720081:12000
Kasson loam, 2 to 5 percent slopes582B2724793082xl3ria03719891:15840
Kasson loam, 5 to 9 percent slopes582C924793222xl3sia03719891:15840
Kasson loam, 5 to 9 percent slopes, eroded582C2224793232xl3tia03719891:15840
Kasson loam, 2 to 5 percent slopes582B7124753532xl3ria06519751:15840
Kasson loam, 2 to 5 percent slopes582B960314291102xl3ria19120051:12000
Kasson loam, 5 to 9 percent slopes582C509714291112xl3sia19120051:12000
Kasson loam, 5 to 9 percent slopes, eroded582C2247014291122xl3tia19120051:12000
Kasson silt loam, 2 to 6 percent slopesM506B197587848112xl3xmn03920051:12000
Bassett-Kasson complex, 6 to 12 percent slopes, erodedM523C2199413849872sj9dmn03920051:12000
Kasson silt loam, 0 to 1 percent slopesKa1030622167482xl3wmn04520081:12000
Kasson silt loam, 2 to 6 percent slopesKb668822167492xl3xmn04520081:12000
Kasson silt loam, 1 to 4 percent slopes24B2763978342xl3vmn04719771:15840
Kasson silt loam, 2 to 6 percent slopesM506B1984816707292xl3xmn04920071:12000
Bassett-Kasson complex, 6 to 12 percent slopes, erodedM523C21027717116432sj9dmn04920071:12000
Kasson silt loam, 1 to 4 percent slopes24B74144004412xl3vmn09919861:15840
Kasson silt loam, 1 to 4 percent slopes2447964007302xl3vmn10919771:15840
Kasson silt loam, 1 to 4 percent slopes2411574296252xl3vmn13119961:12000
Kasson silt loam24176429021gdfdmn16919871:20000
Kasson silt loam, 2 to 6 percent slopes866B345916986151v0k1wi09320061:12000

Map of Series Extent

Approximate geographic distribution of the KASSON 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 .