Official Series Description


Lab Data Summary

Aggregate lab data for the KENT soil series. This aggregation is based on all pedons with a current taxon name of KENT, 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 KENT 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
94A40A1894S1970MI051001Kent7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties44.0811119,-84.457962
94C40A1898S1970MI031001Kent7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties45.6149979,-84.4646301
9840A1901S1970MI107001Kent7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties43.7488899,-85.5205002

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the KENT 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 KENT 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 KENT 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 KENT 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.

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

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Competing Series

Soil series competing with KENT 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 KENT 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 KENT 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.

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

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Soil series sharing subgroup-level classification with KENT, 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 KENT 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
Kent loam, 6 to 12 percent slopesKnC1021891936bw0mi01119641:20000
Kent loam, 2 to 6 percent slopesKnB851891926bvzmi01119641:20000
Kent loam, 0 to 2 percent slopesKnA681891916bvymi01119641:20000
Kent soils, 12 to 18 percent slopesKkD8718800669mqmi06719651:15840
Kent soils, 2 to 6 percent slopesKkB8218800469mnmi06719651:15840
Kent silty clay, 6 to 12 percent slopes, severely erodedKlC32818800369mmmi06719651:15840
Kent soils, 6 to 12 percent slopesKkC1918800569mpmi06719651:15840
Kent sandy loam, 2 to 6 percent slopes25B8351917986fl1mi06919951:15840
Kent sandy loam, 6 to 12 percent slopes25C4281917996fl2mi06919951:15840
Kent silt loam, 25 to 45 percent slopesKtE34018735668yrmi12119661:15840
Kent sandy loam, 2 to 6 percent slopes25B61431898986clrmi12919871:15840
Kent loam, 2 to 6 percent slopes, eroded25B218351898996clsmi12919871:15840
Kent-Selkirk complex, 0 to 6 percent slopes85B8761899566cnmmi12919871:15840
Kent sandy loam, 6 to 12 percent slopes25C7521899006cltmi12919871:15840
Kent loam, 6 to 12 percent slopes, eroded25C25811899016clvmi12919871:15840
Kent sandy loam, 12 to 18 percent slopes25D1981899026clwmi12919871:15840
Kent loam, 2 to 6 percent slopesKtB6961900826cspmi13319661:15840
Kent loam, 6 to 12 percent slopes, moderately erodedKtC24131900846csrmi13319661:15840
Kent loam, 6 to 12 percent slopesKtC3931900836csqmi13319661:15840
Kent loam, 12 to 18 percent slopes, moderately erodedKtD21781900866cstmi13319661:15840
Kent loam, 12 to 18 percent slopesKtD1051900856cssmi13319661:15840
Kent sandy loam, 6 to 12 percent slopes25C2491914646f78mi13719981:12000
Kent sandy loam, 2 to 6 percent slopes25B1991914636f77mi13719981:12000

Map of Series Extent

Approximate geographic distribution of the KENT 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 .