Official Series Description


Lab Data Summary

Aggregate lab data for the KNOCO soil series. This aggregation is based on all pedons with a current taxon name of KNOCO, 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 KNOCO 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
78B03N078303TX155OO2KNOCO8Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties34.0269432,-99.8755569
78C88P090788OK151002Knoco7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties36.9055557,-98.8166656

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the KNOCO 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 KNOCO 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 KNOCO 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 KNOCO 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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There are insufficient data to create the 3D flats position figure.

Competing Series

Soil series competing with KNOCO 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 KNOCO 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 KNOCO 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.

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 KNOCO, 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. OK-2010-09-29-18 | Woods County - 2003

    Typical pattern of soils and underlying material in the Burford-Knoco-Vernon general soil map unit (Soil Survey of Woods County, Oklahoma; 2003).

  2. OK-2012-02-16-42 | Harmon County - September 1984

    Typical pattern of soils and underlying material in the Tillman-Vernon map unit (Soil Survey of Harmon County, Oklahoma; September 1984).

  3. OK-2012-02-16-43 | Harmon County - September 1984

    Typical pattern of soils and underlying material in the Knoco-Vernon-Cornick map unit (Soil Survey of Harmon County, Oklahoma; September 1984).

  4. TX-2010-11-03-49 | King County - 2007

    Typical pattern of the Westill-Tilvern and Talpa-Knoco general soil map units (Soil Survey of King County, Texas; 2007).

  5. TX-2012-03-19-10 | Archer County - April 1995

    Typical pattern of soils and parent material in the Bluegrove-Jolly-Weswind general soil map unit (Soil Survey of Archer County, TX; 1995).

  6. TX-2012-03-19-11 | Archer County - April 1995

    Typical pattern of soils and parent material in the Kamay-Deandale general soil map unit (Soil Survey of Archer County, TX; 1995).

  7. TX-2012-03-19-12 | Archer County - April 1995

    Typical pattern of soils and parent material in the Vernon-Knoco general soil map unit (Soil Survey of Archer County, TX; 1995).

Map Units

Map units containing KNOCO 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
Knoco-Rock outcrop complex, 15 to 80 percent slopes54333432213824941hdllks00719731:24000
Vernon-Knoco complex, 1 to 5 percent slopes64442025813825281hdmpks00719731:24000
Knoco-Cornick-Rock outcrop complex, 2 to 20 percent slopes3232733381669dt4xok00919781:24000
Knoco-Rock outcrop complex, 20 to 40 percent slopes3310880381670dt4yok00919781:24000
Knoco-Badland complex, dry, 1 to 12 percent slopes545513816882t014ok00919781:24000
Vernon-Knoco complex, cool, 1 to 12 percent slopes6032413817002t02fok00919781:24000
Knoco-Badland complex, 5 to 15 percent slopesVr29857381783dt8lok01119651:24000
Knoco-Rock outcrop complex, 20 to 40 percent slopesRo11665381767dt82ok01119651:24000
Vernon-Knoco complex, 3 to 12 percent slopesVeD12053819272t027ok01519671:24000
Vernon-Knoco complex, 3 to 12 percent slopesVeD418983822092t027ok03119651:24000
Vernon-Knoco complex, 3 to 12 percent slopesVsE468563822542t027ok03319611:24000
Treadway, Beckman, occasionally flooded, and Knoco soils, 0 to 3 percent slopesTs4021382251dtrpok03319611:24000
Knoco-Badland complex, 1 to 12 percent slopesRg3083822462t015ok03319611:24000
Knoco soils and Rock outcrop, 12 to 40 percent slopesKcRG21062648171prgrok05520051:24000
Vernon-Knoco complex, cool, 1 to 12 percent slopesVeKE129096481872t02fok05520051:24000
Knoco-Badland complex, dry, 1 to 12 percent slopesKoBE127376481702t014ok05520051:24000
Knoco, Rock outcrop, and Cottonwood soils, 2 to 20 percent slopesKRCF7230754293t9x1ok05520051:24000
Spikebox-Knoco-Rock outcrop complex, 12 to 40 percent slopesSKRG1321755322tbz7ok05520051:24000
Vernon-Knoco complex, cool, 1 to 12 percent slopes65175619755012t02fok05719821:24000
Knoco, Rock outcrop, and Cottonwood soils, 2 to 20 percent slopesKRCF1391597546711r1pok05719821:24000
Knoco-Badland complex, dry, 1 to 12 percent slopesKoBE111369754662t014ok05719821:24000
Knoco soils and Rock outcrop, 12 to 40 percent slopesKcRG199297546811r1qok05719821:24000
Knoco-Aspermont complex, 3 to 12 percent slopes, gulliedKnAE4122597546511r1mok05719821:24000
Knoco soils and Rock outcrop, 12 to 40 percent slopesKcRG5599392384f59kok06520001:24000
Vernon-Knoco complex, cool, 1 to 12 percent slopesVeKE46303924102t02fok06520001:24000
Knoco-Badland complex, dry, 1 to 12 percent slopesKoBE35123923832t014ok06520001:24000
Vernon-Knoco complex, 3 to 12 percent slopesVsE195153834942t027ok07519731:24000
Vernon-Knoco-Badland complex, 2 to 12 percent slopesVrE1801383493dw1rok07519731:24000
Knoco-Cornick-Rock outcrop complex, 2 to 20 percent slopesVp19085383874dwg1ok09319651:24000
Knoco-Badland complex, 1 to 3 percent slopesVnB15853383873dwg0ok09319651:24000
Knoco-Rock outcrop complex, 20 to 40 percent slopesRo9781383857dwfhok09319651:24000
Vernon-Knoco complex, 3 to 12 percent slopesVmE352713849862t027ok14119681:24000
Knoco-Badland complex, 1 to 12 percent slopesBv12823849372t015ok14119681:24000
Vernon-Knoco-Badland complex, 2 to 12 percent slopes491032385035dxnhok14919761:24000
Vernon-Knoco complex, 1 to 12 percent slopesVeKE34659385244dxw7ok15119951:24000
Knoco-Badland complex, 12 to 40 percent slopesKnBG32699385206dxv0ok15119951:24000
Knoco-Badland complex, 1 to 12 percent slopesKoBE12527385207dxv1ok15119951:24000
Vernon-Knoco complex, 3 to 5 percent slopes, erodedVeKC210584385243dxw6ok15119951:24000
Vernon-Knoco complex, 5 to 12 percent slopesVcD33498385308dxy9ok15319611:24000
Knoco-Cottonwood-Rock outcrop complex, 2 to 20 percent slopesVp30131385310dxycok15319611:24000
Knoco-Rock outcrop complex, 20 to 40 percent slopesRb6274385299dxy0ok15319611:24000
Vernon-Knoco complex, 3 to 12 percent slopesVkD265303624512t027tx00919861:24000
Knoco-Vernon complex, 3 to 45 percent slopes, extremely boulderyKvE22209362438d54ktx00919861:24000
Knoco-Vernon complex, 3 to 12 percent slopesKvD151113624372t028tx00919861:24000
Latom-Knoco complex, 3 to 20 percent slopesVlD16463624522wt75tx00919861:24000
Weymouth-Knoco complexWf32792362502d56mtx01119631:20000
Knoco-Vernon complex, 3 to 12 percent slopesOvD761233627282t028tx02319711:24000
Knoco-Badland complex, 1 to 12 percent slopesBoC121233627002t015tx02319711:24000
Vernon-Knoco complex, dry, 1 to 12 percent slopesVe190783629792t02dtx03319701:24000
Knoco silty clayBa2156362941d5nstx03319701:24000
Knoco-Vernon complex, 3 to 20 percent slopesKvE882962335f6m8tx03319701:24000
Knoco-Badland complex, dry, 1 to 12 percent slopesVe384303638532t014tx07519611:20000
Knoco-Burson complexVx11529363854d6m7tx07519611:20000
Knoco-Weymouth clay loams, 3 to 5 percent slopesVcC1158363852d6m5tx07519611:20000
Nebgen-Knoco complex, 3 to 25 percent slopes418188363895d6nktx07719771:24000
Knoco-Vernon complex, 3 to 12 percent slopes2825403638802t028tx07719771:24000
Knoco-Badland complex, dry, 1 to 12 percent slopesOb439903646072t014tx10119691:20000
Badland and Knoco soils, dry, 2 to 20 percent slopesBo313223645742vt7ztx10119691:20000
Knoco, Talpa, and Vernon soilsOt19693364608d7dktx10119691:20000
Knoco-Latom complex, 3 to 45 percent slopesVb125273647462wt74tx10719641:20000
Knoco clay, 8 to 25 percent slopesBa3945364699d7hhtx10719641:20000
Knoco-Vernon complex, 3 to 20 percent slopesKvE1868393646f6m8tx11520041:24000
Vernon-Knoco complex, dry, 1 to 12 percent slopesVb86263658162t02dtx15119641:24000
Knoco-Latom complex, 3 to 45 percent slopesTv84193658142wt74tx15119641:24000
Knoco clay, 5 to 40 percent slopesBa3854365780d8mctx15119641:24000
Cottonwood-Knoco complex, 3 to 20 percent slopesCKF3674431561692t02btx15520211:24000
Knoco-Badland complex, 1 to 12 percent slopesKnBF3522231561222t015tx15520211:24000
Knoco-Talpa complex, 5 to 30 percent slopes, very boulderyKTG3218131009551lh4ztx15520211:24000
Talpa-Knoco complex, 5 to 30 percent slopesTKF136723100958f7dftx15520211:24000
Vernon-Knoco complex, 3 to 12 percent slopesVKD1362331561652t027tx15520211:24000
Vernon-Knoco complex, cool, 1 to 12 percent slopesVKcD983131009132t02ftx15520211:24000
Spikebox-Knoco-Rock outcrop complex, 5 to 30 percent slopesSKRG401531010501lh55tx15520211:24000
Badland and Knoco soils, dry, 2 to 20 percent slopesBKF299031009112vt7ztx15520211:24000
Cottonwood-Knoco complex, 3 to 20 percent slopesCt317503671312t02btx19719651:20000
Knoco-Badland complex, dry, 1 to 12 percent slopesVr218103671722t014tx19719651:20000
Weymouth and Knoco clay loams, 3 to 8 percent slopesWvD4939367174db2btx19719651:20000
Talpa-Knoco complexTc4150367165db21tx19719651:20000
Glenrio-Knoco complex, 3 to 12 percent slopesGkD2293367434dbbqtx20519731:24000
Knoco complexVr13170367538dbg2tx20719601:20000
Vernon-Knoco complex, dry, 1 to 12 percent slopesVx169093918612t02dtx22719651:24000
Knoco-Vernon complex, 3 to 12 percent slopesBv77633682262t028tx25319661:20000
Cottonwood-Knoco complex, 3 to 20 percent slopesCKF778713686332t02btx26919991:31680
Talpa-Knoco-Rock outcrop complex, 5 to 30 percent slopesTKG61278368611dckptx26919991:31680
Vernon-Knoco complex, cool, 1 to 12 percent slopesKVD253563685912t02ftx26919991:31680
Badland and Knoco soils, dry, 2 to 20 percent slopesBKF155993685902vt7ztx26919991:31680
Knoco-Badland complex, 1 to 12 percent slopes181004393687182t015tx27519751:24000
Cottonwood-Knoco complex, 3 to 20 percent slopes10377163687102t02btx27519751:24000
Knoco-Vernon complex, 3 to 12 percent slopes39172193687412t028tx27519751:24000
Vernon-Knoco complex, dry, 1 to 12 percent slopesVx309353707492t02dtx33519651:20000
Vernon-Knoco complex, 5 to 25 percent slopes, severely eroded407536370787dftwtx33719751:24000
Knoco clay, 1 to 8 percent slopes153923370982dg15tx35319791:24000
Burson-Knoco-Rock outcrop association, steepBKG229883124136dg59tx35919781:24000
Knoco-Badland association, rollingKBE141873124142dg5htx35919781:24000
Vernon-Knoco complex, cool, 1 to 12 percent slopesVWF1385531242392t02ftx37519741:24000
Knoco-Badland association, rollingKBE41353124217dgdjtx37519741:24000
Knoco-Quinlan-Burson association, 5 to 50 percent slopesKQB10418371416dgh5tx38119991:24000
Vernon-Knoco complex, dry, 1 to 12 percent slopesVd82763720412t02dtx41519661:24000
Knoco-Badland complex, dry, 1 to 12 percent slopesOB527773722922t014tx43319701:24000
Cottonwood-Knoco complex, 3 to 20 percent slopesCt438083722682t02btx43319701:24000
Knoco-Badland complex, 1 to 12 percent slopesObE102083915342t015tx44119711:20000
Knoco-Vernon complex, 3 to 12 percent slopes, very boulderyKrE1651372691dht9tx44719911:24000
Vernon-Knoco complex, 3 to 12 percent slopesVoD137083733952t027tx48519721:20000
Knoco clay, 3 to 15 percent slopesOwE8970373379djjhtx48519721:20000
Latom-Knoco complex, 3 to 20 percent slopesLaE10623733642wt75tx48519721:20000
Knoco stony clay, 5 to 30 percent slopesOsF869373378djjgtx48519721:20000
Knoco-Badland complex, 1 to 12 percent slopesVx374383734522t015tx48719601:20000
Knoco-Vernon complex, 3 to 12 percent slopesKvE80373737612t028tx50320031:24000
Knoco-Vernon complex, 3 to 45 percent slopes, extremely boulderyKvG466777724v38wtx50320031:24000

Map of Series Extent

Approximate geographic distribution of the KNOCO 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 .