Official Series Description


Lab Data Summary

Aggregate lab data for the TELL soil series. This aggregation is based on all pedons with a current taxon name of TELL, 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 TELL were used in the calculation. Source: KSSL snapshot . Methods used to assemble the KSSL snapshot used by SoilWeb / SDE

Click the image to view it full size.

Pedons used in the lab summary:

MLRALab IDPedon IDTaxonnameCINSSL / NASIS ReportsLink To SoilWeb GMap
108B82IL0110361982IL011036Tell1Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties41.5458271,-89.7476624

Water Balance

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

Click the image to view it full size.



Click the image to view it full size.

Sibling Summary

Siblings are those soil series that occur together in map units, in this case with the TELL series. Sketches are arranged according to their subgroup-level taxonomic structure. Source: SSURGO snapshot , parsed OSD records and snapshot of SC database .

Click the image to view it full size.

Select annual climate data summaries for the TELL series and siblings. 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 TELL 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 .

Click the image to view it full size.

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.

Competing Series

Soil series competing with TELL share the same family level classification in Soil Taxonomy. Source: parsed OSD records and snapshot of the SC database .

Click the image to view it full size.

Select annual climate data summaries for the TELL 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 TELL 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 .

Click the image to view it full size.

Click the image to view it full size.

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 TELL, 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-2011-06-01-08 | Louisa County - 1980

    Pattern of soils and parent material in the Downs-Fayette association (Soil Survey of Louisa County, Iowa; 1980).

  2. WI-2012-03-22-02 | Buffalo County - March 1962

    Soil associations and relief in Buffalo County. 1. Silty soils of the rolling limestone uplands and Steep stony and rocky land: Dubuque, Fayette, Steep stony and rocky land. 2. Loamy soils of the rolling to hilly sandstone uplands: Gale, Hixton. 3. Sandy soils of the rolling to hilly sandstone uplands: Boone, Hixton. 4. Sandy soils of stream terraces: Sparta, Plainfield. 5. Silty soils of stream terraces: Bertrand, Richwood. 6. Loamy terrace soils underlain by sand on stream terraces: Meridian, Tell. 7. Wet organic and mineral soils of bottom lands: Peat and Muck, Ettrick, Wallkill. 8. Soils of overflow bottom lands: Loamy alluvial lands, Marsh (Soil Survey of Bayfield County, WI; 1961).

  3. WI-2012-03-22-05 | Crawford County - December 1961

    Landscape showing relationships among soils of the bottom lands of Crawford County (Soil Survey of Crawford County, WI; 1961).

  4. WI-2012-03-23-31 | Richland County - March 1959

    Soil landscape of Richland County showing relationships among major soil series (Courtesy Wis. Geol. and Nat. Hist. Survey) (Soil Survey of Richland County, WI; 1959).

Map Units

Map units containing TELL 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
Fayette-Chelsea-Tell complex, 9 to 18 percent slopes293E110813971022thl7ia03120081:12000
Fayette-Chelsea-Tell complex, 5 to 9 percent slopes293C56113971012thl4ia03120081:12000
Fayette-Chelsea-Tell complex, 18 to 40 percent slopes293G37913971032thlbia03120081:12000
Tell silt loam, 2 to 5 percent slopes353B582404409fktgia04519781:15840
Tell silt loam, 5 to 9 percent slopes353C345404410fkthia04519781:15840
Tell silt loam, 0 to 2 percent slopes353300404408fktfia04519781:15840
Tell silt loam, 2 to 5 percent slopes353B272405035flgnia05519841:15840
Fayette-Chelsea-Tell complex, 18 to 40 percent slopes293G170811443842thlbia09520051:12000
Fayette-Chelsea-Tell complex, 9 to 14 percent slopes, eroded293D2125411443802thl6ia09520051:12000
Fayette-Chelsea-Tell complex, 14 to 18 percent slopes, eroded293E2120211443872thl9ia09520051:12000
Fayette-Chelsea-Tell complex, 9 to 14 percent slopes293D8884528642thl5ia09520051:12000
Fayette-Chelsea-Tell complex, 5 to 9 percent slopes293C7674528632thl4ia09520051:12000
Fayette-Chelsea-Tell complex, 14 to 18 percent slopes293E5784528662thl8ia09520051:12000
Tell silt loam, 5 to 9 percent slopes, moderately eroded353C2193114447517dxkia09520051:12000
Tell silt loam, 2 to 5 percent slopes353B138114447317dxhia09520051:12000
Tell silt loam, 5 to 9 percent slopes353C135114447617dxlia09520051:12000
Tell silt loam, 9 to 14 percent slopes, moderately eroded353D285114447417dxjia09520051:12000
Douds-Alvin-Tell Complex, 18 to 60 percent slopesS154G1803408432fq07ia11119761:15840
Tell silt loam, 2 to 5 percent slopes353B620408616fq65ia11319701:15840
Tell silt loam, 5 to 9 percent slopes, moderately eroded353C2217408617fq66ia11319701:15840
Tell silt loam, 9 to 14 percent slopes, moderately eroded353D2425408768fqc2ia11519841:15840
Tell silt loam, 5 to 9 percent slopes, moderately eroded353C2171408767fqc1ia11519841:15840
Tell silt loam, 2 to 5 percent slopes565B587186275920jc0il01120071:12000
Tell silt loam, 0 to 2 percent slopes565A431186275820jbzil01120071:12000
Tell silt loam, 5 to 10 percent slopes, eroded565C232186276020jc1il01120071:12000
Tell silt loam, 5 to 10 percent slopes, eroded565C21264867757y3z5il01520051:12000
Tell silt loam, 10 to 18 percent slopes, eroded565D21196796098vqdlil01520051:12000
Tell-Lamont complex, 18 to 35 percent slopes, eroded952F2948905338zd2gil01520051:12000
Tell silt loam, 10 to 18 percent slopes, severely eroded565D3596901207z7s6il01520051:12000
Tell silt loam, 18 to 35 percent slopes, eroded565F2584901213z7sdil01520051:12000
Tell-Lamont complex, 10 to 18 percent slopes, eroded952D2583902724z9c4il01520051:12000
Tell-Lamont complex, 5 to 10 percent slopes, eroded952C2527902719z9bzil01520051:12000
Tell-Lamont complex, 10 to 18 percent slopes, severely eroded952D3304902727z9c7il01520051:12000
Tell silt loam, 2 to 5 percent slopes565B242867756y3z4il01520051:12000
Oakville-Tell complex, 7 to 15 percent slopes917D436324483986s1il07320011:12000
Tell silt loam, 2 to 5 percent slopes565B204024479786qpil07320011:12000
Oakville-Tell complex, 1 to 7 percent slopes917B194824483786rzil07320011:12000
Tell silt loam, 5 to 10 percent slopes, eroded565C2143524479886qqil07320011:12000
Tell silt loam 0 to 2 percent slopes565A55524479686qnil07320011:12000
Oakville-Tell complex, 10 to 18 percent slopes, eroded917D226724484086s2il07320011:12000
Oakville-Tell complex, 5 to 10 percent slopes, eroded917C23824483886s0il07320011:12000
Tell silt loam, 2 to 5 percent slopes565B424194957923fpnil08519901:12000
Tell silt loam, 5 to 10 percent slopes, eroded565C2314194958023fppil08519901:12000
Oakville-Tell complex, 5 to 10 percent slopes, eroded917C212041987516ntbil16120021:12000
Oakville-Tell complex, 10 to 18 percent slopes, eroded917D210651987526ntcil16120021:12000
Tell silt loam, 5 to 10 percent slopes, eroded565C23075793083vm8bil19520031:12000
Oakville-Tell complex, 5 to 10 percent slopes, eroded917C22585793098vm8til19520031:12000
Tell silt loam, 10 to 18 percent slopes, eroded565D22033793084vm8cil19520031:12000
Oakville-Tell complex, 10 to 18 percent slopes, eroded917D21497793099vm8vil19520031:12000
Tell silt loam, 2 to 5 percent slopes565B837793082vm89il19520031:12000
Tell silt loam, 0 to 2 percent slopesThA25422164372ddczmn15720081:12000
Tell silt loam, 2 to 6 percent slopesThB16522164382ddd0mn15720081:12000
Tell silt loam, 0 to 3 percent slopesTeA611422966g642wi00119781:20000
Tell silt loam, 1 to 6 percent slopesTeB680421599g4pzwi01719851:15840
Tell silt loam, 2 to 6 percent slopesTeB1245421839g4yqwi03519741:12000
Tell silt loam, 0 to 2 percent slopesTeA591421838g4ypwi03519741:12000
Tell silt loam, 2 to 6 percent slopes, moderately erodedTcB21321425381g8mzwi04519691:12000
Tell silt loam, 0 to 2 percent slopesTcA625425380g8mywi04519691:12000
Tell silt loam, 6 to 12 percent slopes, moderately erodedTcC2211425382g8n0wi04519691:12000
Tell silt loam, 2 to 6 percent slopes, moderately erodedTeB233424727g7ywwi04919601:20000
Tell silt loam, 2 to 6 percent slopesTeB1275423218g6d6wi11119771:15840
Tell silt loam, 6 to 12 percent slopes, erodedTeC2807423219g6d7wi11119771:15840
Tell silt loam, 12 to 20 percent slopes, erodedTeD2382423220g6d8wi11119771:15840
Tell silt loam, 0 to 2 percent slopesTeA230423217g6d5wi11119771:15840

Map of Series Extent

Approximate geographic distribution of the TELL 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 .