Official Series Description


Lab Data Summary

Aggregate lab data for the KENDALL soil series. This aggregation is based on all pedons with a current taxon name of KENDALL, 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 KENDALL 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
108A84P087284IL183005aKendall6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties40.1147536,-87.8305783
111DCA84051984IN015005Kendall2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties40.6755028,-86.4452056
114B72IL0770011972IL077001Kendall4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties37.8268621,-89.3316669

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the KENDALL 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 KENDALL 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 KENDALL 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 KENDALL 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 KENDALL 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 KENDALL 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 KENDALL 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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Click the image to view it full size.

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

Click the image to view it full size.

Click the image to view it full size.

Soil series sharing subgroup-level classification with KENDALL, 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. IL-2010-09-01-05 | Edgar County - 2002

    Typical pattern of soils and parent material in the Camden-Starks association (Soil Survey of Edgar County, Illinois; 2002).

  2. IL-2010-09-24-01 | Christian County -

    Typical pattern of soils and underlying material in the Elburn-Drummer-Camden association (Soil Survey of Christian County, Illinois).

  3. IL-2010-09-24-06 | Christian County -

    Typical pattern of soils and underlying material in the Middletown-Alvin-Broadwell association (Soil Survey of Christian County, Illinois).

  4. IL-2011-06-01-06 | Brown County - 1988

    Typical cross section showing the relationship of parent material to soils in Brown County (Soil Survey of Brown County, Illinois; 1988).

  5. IL-2011-08-03-10 | Christian County - 1994

    Typical pattern of soils and parent material in the Elburn-Drummer-Camden association (Soil Survey of Christian County, Illinois; 1994).

  6. IL-2011-08-03-14 | Christian County - 1994

    Typical pattern of soils and parent material in the Middletown-Alvin-Broadwell association (Soil Survey of Christian County, Illinois; 1994).

Map Units

Map units containing KENDALL 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
Kendall silt loam, 1 to 5 percent slopes242B13741738535tx5il00519811:12000
Kendall silt loam, 0 to 2 percent slopes242A75041015766132znil00720061:12000
Kendall silt loam, 0 to 2 percent slopes, rarely flooded7242A67326041582rbfkil00919841:12000
Kendall silt loam, 0 to 2 percent slopes242A3521729515sz2il00919841:12000
Kendall silt loam, 0 to 2 percent slopes, rarely flooded7242A2825186112qj6cil01319861:15840
Kendall silt loam, 0 to 2 percent slopes242A144124300084vqil01919991:12000
Kendall silt loam, 0 to 2 percent slopes242A12662617618scxil02119991:12000
Kendall silt loam, 0 to 2 percent slopes, rarely flooded7242A7322617838sdmil02119991:12000
Kendall silt loam, 0 to 2 percent slopes, rarely flooded7242A14415986871qnkkil03920051:12000
Kendall silt loam, 0 to 2 percent slopes242A14272002066qb8il04120041:12000
Kendall silt loam, 0 to 2 percent slopes242A1640843559x9slil04519971:12000
Kendall silt loam, 0 to 2 percent slopes242A575615645nnmjil05719971:12000
Kendall silt loam, 0 to 2 percent slopes242A738211720739pil06119681:15840
Kendall silt loam, 0 to 2 percent slopes, rarely flooded7242A23426041112r796il06719931:15840
Kendall silt loam, 0 to 2 percent slopes, rarely flooded7242A215752687t877il08320021:12000
Kendall silt loam, 0 to 2 percent slopes242A15627153393k4il08920001:12000
Kendall silt loam, 0 to 2 percent slopes242A337186888120qqhil09320071:12000
Kendall silt loam, 0 to 2 percent slopes242A14662634528v4gil09920061:12000
Kendall silt loam, 0 to 2 percent slopes, rarely flooded7242A8617215021vscbil13520071:12000
Kendall silt loam, 2 to 5 percent slopes, rarely flooded7242B16816721301t3zpil13719841:15840
Kendall silt loam, 0 to 2 percent slopes242A95713989151hyp9il14120051:12000
Kendall silt loam, 0 to 2 percent slopes242A3331914021227pmil14720091:12000
Kendall silt loam, 0 to 2 percent slopes, rarely flooded7242A19614907nmvqil14920011:12000
Kendall silt loam, 0 to 2 percent slopes, rarely flooded7242A9241993806pgmil16719991:12000
Kendall silt loam, 0 to 2 percent slopes242A2541993116pddil16719991:12000
Kendall silt loam, 0 to 2 percent slopes242A5572020686s8bil16920001:12000
Kendall silt loam, 0 to 2 percent slopes, rarely flooded7242A4082022566sgdil16920001:12000
Kendall silt loam, 2 to 5 percent slopes, rarely flooded7242B29325421032qrd9il17119841:12000
Kendall silt loam, 0 to 2 percent slopes242A9925423242qzhzil17519921:15840
Kendall silt loam, 0 to 2 percent slopes242A78117919260gdil17720061:12000
Kendall silt loam, 2 to 5 percent slopes242B31117919360gfil17720061:12000
Kendall silt loam, 0 to 2 percent slopes242A338216131851r4n7il18320061:12000
Kendall silt loam, 0 to 2 percent slopes242A25781739935v1pil20119971:12000
Kendall-Fincastle silt loams, 0 to 1 percent slopesKgA98171651775jw9in01519871:15840
Kendall silt loam, 0 to 1 percent slopesKfA15271651765jw8in01519871:15840
Kendall silt loam, 0 to 3 percent slopesKlA571423170g6bnwi11119771:15840
Kendall silt loam, 0 to 3 percent slopesKlA686423896g732wi11719741:15840
Kendall silt loam, 1 to 3 percent slopesKlA4926425632g8x2wi12719671:15840
Kendall silt loam, 1 to 3 percent slopesKlA3784425742g90mwi13119671:15840
Kendall silt loam, 1 to 3 percent slopesKlA12693403404g94hwi13320231:15840

Map of Series Extent

Approximate geographic distribution of the KENDALL 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 .