Official Series Description


Lab Data Summary

Aggregate lab data for the PLANO soil series. This aggregation is based on all pedons with a current taxon name of PLANO, 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 PLANO 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
108A60IL0370011960IL037001Plano2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties41.7918172,-88.8748862
108A60IL0370021960IL037002Plano2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties41.9120995,-88.8842283
108A84IL0190031984IL019003Plano2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties40.0694444,-88.22
108A84IL0390031984IL039003Plano2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties40.1003111,-89.0646306
108A84P035083IL183013aPlano6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties39.9833662,-87.8333561
108A82P0044S1981IL115048PLANO6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties39.8369446,-88.8047256
108B77IL0730151977IL073015Plano1Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties41.4291113,-89.9028258
95B40A1543S1953WI027022Plano4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties43.3800011,-88.7422256
95B40A1585S1962WI021002Plano7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties43.3033333,-89.331665
95B40A1586S1962WI025002Plano7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties43.1969452,-89.3763885

Water Balance

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

Click the image to view it full size.

Click the image to view it full size.

Soil series sharing subgroup-level classification with PLANO, 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-2010-09-01-48 | Mason County - 1995

    Typical pattern of soils and parent material in the Elburn-Plano-Thorp association (Soil Survey of Mason County, Illinois; 1995).

  2. IL-2010-09-01-73 | Stark County - 1996

    Typical pattern of soils and parent material in the Elburn-Plano and Catlin-Flanagan associations (Soil Survey of Stark County, Illinois; 1996).

  3. IL-2010-09-01-85 | Woodford County - 1999

    Typical pattern of soils and parent material in the Alvin-Coloma-Jasper association (Soil Survey of Woodford County, Illinois; 1999).

  4. 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).

  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-2011-08-04-23 | Henry County - 1984

    Pattern of soils in the Plano-Elburn association (Soil Survey of Henry County, Illinois; 1984).

  7. IL-2011-08-04-26 | Henry County - 1984

    Pattern of soils in the Sawmill-Radford association (Soil Survey of Henry County, Illinois; 1984).

  8. IL-2011-08-04-64 | Mason County - 1995

    Typical pattern of soils and parent material in the Elburn-Plano-Thorp association (Soil Survey of Mason County, Illinois; 1995).

Map Units

Map units containing PLANO 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
Plano silty clay loam, 0 to 2 percent slopes, rarely flooded12759223775812kt25ia01720081:12000
Plano silt loam, 2 to 5 percent slopes199B23191997912tjwvil00720061:12000
Plano silt loam, 0 to 2 percent slopes199A15251997902tjwsil00720061:12000
Plano silt loam, 5 to 10 percent slopes, eroded199C27213953562tjwxil00720061:12000
Plano silt loam, 0 to 2 percent slopes199A4938186271120j9gil01120071:12000
Plano silt loam, 2 to 5 percent slopes199B3900186271220j9hil01120071:12000
Plano silt loam, 2 to 5 percent slopes, eroded199B22632186271320j9jil01120071:12000
Plano silt loam, 5 to 10 percent slopes, eroded199C21061186271420j9kil01120071:12000
Plano silt loam, 0 to 2 percent slopes199A738869315y5lfil03920051:12000
Plano silt loam, 2 to 5 percent slopes, eroded199B2628869316y5lgil03920051:12000
Plano silt loam, sandy substratum, 2 to 5 percent slopes748B50415989751qnvvil03920051:12000
Plano silt loam, 0 to 2 percent slopes, rarely flooded7199A47515977451qml5il03920051:12000
Plano silt loam, 2 to 5 percent slopes, rarely flooded7199B47015977461qml6il03920051:12000
Plano silt loam, sandy substratum, 0 to 2 percent slopes748A8616022241qs7nil03920051:12000
Plano silt loam, 2 to 5 percent slopes199B3532002086qbbil04120041:12000
Plano silt loam, 2 to 5 percent slopes199B325843555x9sgil04519971:12000
Plano silt loam, 2 to 5 percent slopes199B628615644nnmhil05719971:12000
Plano silt loam, 0 to 2 percent slopes199A435211621736hil05919661:20000
Plano silt loam, 2 to 4 percent slopes199B88211622736jil05919661:20000
Plano silt loam, 2 to 5 percent slopes199B802224466486ldil07320011:12000
Plano silt loam, 0 to 2 percent slopes199A238924466386lcil07320011:12000
Plano silt loam, 5 to 10 percent slopes, eroded199C2126524466586lfil07320011:12000
Plano silt loam, 0 to 2 percent slopes199A2666638751pfnwil09320071:12000
Plano silt loam, 2 to 5 percent slopes199B436638752pfnxil09320071:12000
Plano silt loam, 5 to 10 percent slopes, eroded199C254638753pfnyil09320071:12000
Plano silt loam, 2 to 5 percent slopes199B1022813862121hjgjil09920061:12000
Plano silt loam, 5 to 10 percent slopes, eroded199C2292713862131hjgkil09920061:12000
Plano silt loam, 0 to 2 percent slopes199A10442634068v2zil09920061:12000
Plano silt loam, 5 to 10 percent slopes, eroded199C243313874951hksxil10320041:12000
Plano silt loam, 0 to 2 percent slopes199A1006215960351qkt0il10720061:12000
Plano silt loam, sandy substratum, 2 to 5 percent slopes748B593316006271qql4il10720061:12000
Plano silt loam, 2 to 5 percent slopes199B316115960381qkt3il10720061:12000
Plano silt loam, sandy substratum, 0 to 2 percent slopes748A228216006261qql3il10720061:12000
Plano silt loam, sandy substratum, 5 to 10 percent slopes, eroded748C2200416006281qql5il10720061:12000
Plano silt loam, 5 to 10 percent slopes, eroded199C2126315960391qkt4il10720061:12000
Plano silt loam, 0 to 2 percent slopes, rarely flooded7199A86615960371qkt2il10720061:12000
Plano silt loam, 2 to 5 percent slopes199B50581990886p56il11320001:12000
Plano silt loam, 0 to 2 percent slopes199A24261990876p55il11320001:12000
Plano silt loam, 2 to 5 percent slopes, eroded199B2271957356kp1il11320001:12000
Plano silt loam, 2 to 5 percent slopes, rarely flooded7199B326488902rlv4il11320001:12000
Plano silt loam, 2 to 5 percent slopes199B38731913943227m3il11520071:12000
Plano silt loam, 0 to 2 percent slopes199A17171913942227m2il11520071:12000
Plano silt loam, 5 to 10 percent slopes, eroded199C23441913944227m4il11520071:12000
Plano silt loam, 2 to 5 percent slopes, rarely flooded7199B2841913990227nmil11520071:12000
Plano silt loam, 0 to 2 percent slopes199A145118210463hbil12319971:15840
Plano silt loam, 2 to 5 percent slopes199B116418210563hcil12319971:15840
Plano silt loam, 0 to 2 percent slopes199A27041777685yzgil12519891:15840
Plano silt loam, 2 to 5 percent slopes199B5241777695yzhil12519891:15840
Plano silt loam, sandy substratum, 0 to 2 percent slopes748A14725179742qhc1il12519891:15840
Plano silt loam, 0 to 2 percent slopes, rarely flooded7199A4225185942qhcnil12519891:15840
Plano silt loam, 0 to 2 percent slopes199A553614045521j4k4il12920051:12000
Plano silt loam, 2 to 5 percent slopes199B194414045541j4k6il12920051:12000
Plano silt loam, 2 to 5 percent slopes199B21224496486x2il13120001:12000
Plano silt loam, 5 to 10 percent slopes, eroded199C215524496586x3il13120001:12000
Plano silt loam, 2 to 5 percent slopes199B109212085582tjwvil14120051:12000
Plano silt loam, 0 to 2 percent slopes199A71402085572tjwsil14120051:12000
Plano silt loam, 5 to 10 percent slopes, eroded199C231662085592tjwxil14120051:12000
Plano silt loam, 2 to 5 percent slopes199B158920896770fwil14319861:15840
Plano silt loam, 2 to 5 percent slopes, eroded199B21599194970223ftmil14720091:12000
Plano silt loam, 2 to 5 percent slopes199B156517228211vtqwil14720091:12000
Plano silt loam, 0 to 2 percent slopes199A851993076pd8il16719991:12000
Plano silt loam, 2 to 5 percent slopes199B701993086pd9il16719991:12000
Plano silt loam, 2 to 5 percent slopes199B347917907060bgil17519921:15840
Plano silt loam, 0 to 2 percent slopes199A322717909460c7il17519921:15840
Plano silt loam, 2 to 5 percent slopes, eroded199B2166817907160bhil17519921:15840
Plano silt loam, 2 to 5 percent slopes, rarely flooded7199B11125423882r1zdil17519921:15840
Plano silt loam, 0 to 2 percent slopes, rarely flooded7199A3825423872r1zcil17519921:15840
Plano silt loam, 2 to 5 percent slopes199B607615919882tjwvil17720061:12000
Plano silt loam, 5 to 10 percent slopes, eroded199C2356215919902tjwxil17720061:12000
Plano silt loam, 0 to 2 percent slopes199A17881791622tjwsil17720061:12000
Plano silt loam, 2 to 5 percent slopes199B192517936660n0il17919911:15840
Plano silt loam, 0 to 2 percent slopes199A183217936560mzil17919911:15840
Plano silt loam, 0 to 2 percent slopes, rarely flooded7199A63825097882qgxkil17919911:15840
Plano silt loam, 2 to 5 percent slopes, rarely flooded7199B14225097892qgxlil17919911:15840
Plano silt loam, 2 to 5 percent slopes199B199716010451qr0mil18320061:12000
Plano silt loam, 2 to 5 percent slopes199B86921739822tjwvil20119971:12000
Plano silt loam, 0 to 2 percent slopes199A31421739812tjwsil20119971:12000
Plano silt loam, 5 to 10 percent slopes, eroded199C212801739832tjwxil20119971:12000
Plano silt loam, 0 to 2 percent slopes199A32822160662dd00il20320081:12000
Plano silt loam, 2 to 5 percent slopes199B10922160682dd02il20320081:12000
Plano silt loam, 0 to 2 percent slopesPlA4961604535cyxin16519771:20000
Plano silt loam, till substratum, 2 to 6 percent slopesPnB322584233332tjwtwi02119721:15840
Plano silt loam, till substratum, 0 to 2 percent slopesPnA94274233322tjwrwi02119721:15840
Plano silt loam, till substratum, 6 to 12 percent slopes, erodedPnC227044233342tjwwwi02119721:15840
Plano silt loam, till substratum, 2 to 6 percent slopesPnB383317535572tjwtwi02519721:15840
Plano silt loam, gravelly substratum, 2 to 6 percent slopesPoB77917535602tjwzwi02519721:15840
Plano silt loam, till substratum, 0 to 2 percent slopesPnA73247535562tjwrwi02519721:15840
Plano silt loam, gravelly substratum, 0 to 2 percent slopesPoA54487535592tjwywi02519721:15840
Plano silt loam, till substratum, 6 to 12 percent slopes, erodedPnC221907535582tjwwwi02519721:15840
Plano silt loam, gravelly substratum, 6 to 12 percent slopes, erodedPoC2254753561t94fwi02519721:15840
Plano silt loam, moderately well drained, 0 to 3 percent slopesPtA14086423636g6tpwi02719761:15840
Plano silt loam, till substratum, 2 to 6 percent slopesPsB79104236352tjwtwi02719761:15840
Plano silt loam, till substratum, 0 to 2 percent slopesPsA71604236342tjwrwi02719761:15840
Plano silt loam, till substratum, 2 to 6 percent slopesPsB105154255462tjwtwi03919671:15840
Plano silt loam, till substratum, 0 to 2 percent slopesPsA68714255452tjwrwi03919671:15840
Plano fine sandy loam, sandy variant, 2 to 6 percent slopesPuB328425548g8tcwi03919671:15840
Plano silt loam, 2 to 6 percent slopes, erodedPsB2214425547g8tbwi03919671:15840
Plano silt loam, till substratum, 0 to 2 percent slopesPnA141854237362tjwrwi04719741:20000
Plano silt loam, till substratum, 2 to 6 percent slopesPnB84664237372tjwtwi04719741:20000
Plano silt loam, gravelly substratum, 0 to 2 percent slopesPt48032686992tjwywi05920231:15840
Plano silt loam, gravelly substratum, 0 to 2 percent slopesPt16034032682tjwywi10120231:15840
Plano silt loam, gravelly substratum, 0 to 2 percent slopesPmA376364263612tjwywi10519701:20000
Plano silt loam, gravelly substratum, 2 to 6 percent slopesPmB70704263622tjwzwi10519701:20000
Plano silt loam, till substratum, 2 to 6 percent slopesPlB60084263592tjwtwi10519701:20000
Plano silt loam, till substratum, 0 to 2 percent slopesPlA41334263582tjwrwi10519701:20000
Plano loam, loamy variant, 2 to 6 percent slopesPnB1752426364g9npwi10519701:20000
Plano loam, loamy variant, 0 to 2 percent slopesPnA1414426363g9nnwi10519701:20000
Plano silt loam, till substratum, 6 to 12 percent slopes, erodedPlC22664263602tjwwwi10519701:20000
Plano silt loam, gravelly substratum, 0 to 2 percent slopesPtA230844256672tjwywi12719671:15840
Plano silt loam, till substratum, 2 to 6 percent slopesPsB121274256652tjwtwi12719671:15840
Plano silt loam, till substratum, 0 to 2 percent slopesPsA71054256642tjwrwi12719671:15840
Plano silt loam, gravelly substratum, 2 to 6 percent slopesPtB40714256682tjwzwi12719671:15840
Plano silt loam, till substratum, 6 to 12 percent slopes, erodedPsC8774256662tjwwwi12719671:15840
Plano silt loam, gravelly substratum, 6 to 12 percent slopes, erodedPtC253425669g8y8wi12719671:15840
Plano silt loam, till substratum, 2 to 6 percent slopesPsB13184228212tjwtwi13919771:20000

Map of Series Extent

Approximate geographic distribution of the PLANO 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 .