Official Series Description


Lab Data Summary

Aggregate lab data for the KONAWA soil series. This aggregation is based on all pedons with a current taxon name of KONAWA, 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 KONAWA 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
10694P081394KS103002Konawa5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.9824982,-95.1494446
118B73-OK-32-173-OK063-32-1Konawa3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties35.0771417,-96.0810917
84A73-OK-57-1573-OK113-57-15Konawa3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties36.1936639,-96.2170333
84A75-OK-63-175-OK125-63-1Konawa4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties34.9546444,-96.8272444
84A80-OK-49-2080-OK049-49-20Konawa4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties34.836575,-96.96755
84A80-OK-49-2180-OK049-49-21Konawa4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties34.8366833,-96.9677278
84B76-OK-48-476-OK095-48-4Konawa4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties33.8554306,-96.7657611

Water Balance

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

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 KONAWA 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 KONAWA series and competing. Series are sorted according to hierarchical clustering of median values. Source: SSURGO map unit geometry and 1981-2010, 800m PRISM data .

There are insufficient data to create the annual climate figure.

Geomorphic description summaries for the KONAWA 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 .

There are insufficient data to create the 2D hillslope position figure.

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

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 KONAWA, 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-2010-09-29-04 | Logan County - 2006

    Typical pattern of soils and underlying material in the Dougherty-Konawa-Derby general soil map unit (Soil Survey of Logan County, Oklahoma; 2006).

  2. OK-2010-09-29-10 | Noble County - 2005

    Typical pattern of soils and underlying material in the Teller-Konawa general soil map unit (Soil Survey of Noble County, Oklahoma; 2005).

  3. OK-2012-02-16-15 | Comanche County - August 1967

    Topography and underlying material of major soils in northeastern part of county (Soil Survey of Comanche County, Oklahoma; August 1967).

  4. OK-2012-02-16-50 | Hughes County - December 1968

    Typical pattern of soils in associations 4 and 5 (Soil Survey of Hughes County, Oklahoma; December 1968).

  5. OK-2012-02-17-17 | Okmulgee County - May 1968

    Relationship of the Taloka and Choteau soils (upper right) to the soils of the Dennis-Bates-Parsons, Collinsville-Talihina, Hector-Hartsells, Konawa-Stidham, and Verdigris-Lightning-Pulaski associations. (The Deep Fork River is also known as the Deep Fork Canadian River) (Soil Survey of Okmulgee County, Oklahoma; May 1968).

  6. OK-2012-02-17-30 | Payne County - April 1987

    Typical pattern of soils and underlying material in the Norge-Teller-Konawa map unit (Soil Survey of Payne County, Oklahoma; April 1987).

  7. OK-2012-02-17-31 | Payne County - April 1987

    Typical pattern of soils and underlying material in the Konawa-Dougherty-Derby map unit (Soil Survey of Payne Oklahoma; April 1987).

Map Units

Map units containing KONAWA 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
Konawa fine sandy loam, 8 to 12 percent slopes728233914734951lg93ks17719661:24000
Konawa loamy fine sand, 3 to 8 percent slopesKoC107963817352tq7gok01119651:24000
Konawa loamy fine sand, 0 to 3 percent slopesKoB58473817342tq7fok01119651:24000
Dougherty-Konawa loamy fine sands association and 0 to 3 percent slopesDoB1166638188130g72ok01519671:24000
Konawa loamy fine sand, 1 to 5 percent slopes, erodedKoC26538381894dtd5ok01519671:24000
Konawa loamy fine sand, 3 to 8 percent slopes, severely erodedKsD314703818952tq7jok01519671:24000
Konawa loamy fine sand, 3 to 8 percent slopesKwD68143819562tq7gok01719721:24000
Konawa fine sandy loam, 3 to 5 percent slopesGdC34123819432tq7dok01719721:24000
Konawa fine sandy loam, 3 to 8 percent slopes, severely erodedGdD325313819462tq7nok01719721:24000
Konawa fine sandy loam, 5 to 8 percent slopesGdD2153381945dtftok01719721:24000
Konawa fine sandy loam, 3 to 8 percent slopes, erodedGdC214513819442tq7lok01719721:24000
Konawa fine sandy loam, 1 to 3 percent slopesGdB11953819422tq7cok01719721:24000
Konawa fine sandy loam, 0 to 1 percent slopes213590382004dthqok01919771:24000
Konawa fine sandy loam, 1 to 3 percent slopes2220393820052tq7cok01919771:24000
Konawa fine sandy loam, 8 to 20 percent slopes231257382006dthsok01919771:24000
Dougherty-Konawa complex, 3 to 8 percent slopes11779382084dtl9ok02719841:24000
Konawa loamy fine sand, 3 to 8 percent slopesKoC60463821832tq7gok03119651:24000
Konawa loamy fine sand, 3 to 8 percent slopes, severely erodedKnB343403821812tq7jok03119651:24000
Konawa loamy fine sand, 3 to 8 percent slopes, erodedKoC239813821842tq7hok03119651:24000
Konawa loamy fine sand, 0 to 3 percent slopesKoB17543821822tq7fok03119651:24000
Konawa and Gasil soils, 5 to 8 percent slopesDh7791382281dtsnok03719521:24000
Konawa-Gullied land complex, 3 to 8 percent slopesBd68923822672tq7kok03719521:24000
Konawa and Gasil soils, 3 to 5 percent slopesDf6571382279dtslok03719521:24000
Konawa and Gasil soils, 1 to 3 percent slopesDg1108382280dtsmok03719521:24000
Konawa fine sandy loam, 3 to 8 percent slopes, eroded3938213825712tq7lok04919821:24000
Konawa loamy fine sand, 3 to 8 percent slopes, gullied361789382568dv2xok04919821:24000
Konawa loamy fine sand, 3 to 8 percent slopes3417143825662tq7gok04919821:24000
Konawa loamy fine sand, 3 to 8 percent slopes, eroded3515083825672tq7hok04919821:24000
Konawa fine sandy loam, 5 to 8 percent slopes40970382573dv32ok04919821:24000
Konawa fine sandy loam, 1 to 3 percent slopes389313825702tq7cok04919821:24000
Konawa loamy fine sand, 8 to 20 percent slopes37542382569dv2yok04919821:24000
Konawa loamy fine sand, 0 to 3 percent slopes18117543826362tq7fok05119751:24000
Konawa-Stephenville complex, 3 to 8 percent slopes, severely eroded199669382637dv54ok05119751:24000
Konawa fine sandy loam, 1 to 3 percent slopes335086383297dvvfok06919761:24000
Konawa fine sandy loam, 0 to 1 percent slopes322719383296dvvdok06919761:24000
Konawa loamy fine sand, 3 to 8 percent slopes, severely erodedKoD358263835142tq7jok08119661:24000
Konawa loamy fine sand, 0 to 3 percent slopesKoB52033835132tq7fok08119661:24000
Konawa loamy fine sand, 0 to 3 percent slopesKonB41103836352tq7fok08319941:12000
Konawa loamy fine sand, 3 to 8 percent slopes, erodedKonD239943836362tq7hok08319941:12000
Konawa loamy fine sand, 3 to 8 percent slopes2345283837792tq7gok08719761:24000
Konawa loamy fine sand, 0 to 3 percent slopes2219213837782tq7fok08719761:24000
Konawa-Gullied land complex, 3 to 8 percent slopes241363837802tq7kok08719761:24000
Konawa fine sandy loam, 3 to 8 percent slopes, gullied199057383893dwgnok09519781:24000
Konawa fine sandy loam, 1 to 5 percent slopes, eroded187354383892dwgmok09519781:24000
Konawa fine sandy loam, 1 to 3 percent slopes171383383891dwglok09519781:24000
Konawa fine sandy loam, 0 to 3 percent slopes401324383947dwjdok09919821:24000
Bastrop and Konawa soils, 3 to 8 percent slopes, gullied5581383957dwjqok09919821:24000
Konawa fine sandy loam, 3 to 8 percent slopesKowD815384072dwnfok10319941:24000
Konawa fine sandy loam, 1 to 3 percent slopesKowB4673840712tq7cok10319941:24000
Konawa-Gullied land complex, 3 to 12 percent slopesKoGE44166384174dwrqok10719961:24000
Konawa fine sandy loam, 3 to 8 percent slopes, erodedKowD229263841772tq7lok10719961:24000
Konawa fine sandy loam, 3 to 5 percent slopesKowC14253841762tq7dok10719961:24000
Konawa fine sandy loam, 0 to 3 percent slopesKowB886384175dwrrok10719961:24000
Konawa fine sandy loam, 3 to 8 percent slopesKowD3636384315dwx8ok10919961:12000
Konawa-Urban land complex, 1 to 8 percent slopesKwUD2868384320dwxfok10919961:12000
Konawa fine sandy loam, 1 to 3 percent slopesKowB27293843142tq7cok10919961:12000
Konawa fine sandy loam, 3 to 8 percent slopes, erodedKowD226983843162tq7lok10919961:12000
Konawa fine sandy loam, 3 to 8 percent slopes, gulliedKowD45033843172tq7mok10919961:12000
Konawa loamy fine sand, 3 to 8 percent slopes, eroded2819386234232tq7hok11319751:24000
Konawa fine sandy loam, 3 to 8 percent slopes, erodedKowC2320516759712tq7lok11720071:24000
Konawa-Gullied land complex, 3 to 8 percent slopesKoGD464116759772tq7kok11720071:24000
Konawa fine sandy loam, 1 to 3 percent slopesKowB60616773472tq7cok11720071:24000
Konawa and Teller soils, 3 to 8 percent slopes, eroded5910086384558dx53ok11919831:24000
Konawa fine sandy loam, 1 to 3 percent slopes2459453845202tq7cok11919831:24000
Konawa loamy fine sand, 5 to 8 percent slopes235144384519dx3vok11919831:24000
Konawa loamy fine sand, 3 to 5 percent slopes, gullied753515384576dx5pok11919831:24000
Konawa fine sandy loam, 3 to 5 percent slopes2218163845182tq7dok11919831:24000
Konawa loamy fine sand, 3 to 8 percent slopes, severely erodedKtD3108353846352tq7jok12319671:24000
Konawa loamy fine sand, 3 to 8 percent slopesKsD72413846332tq7gok12319671:24000
Konawa loamy fine sand, 3 to 8 percent slopes, erodedKsD266233846342tq7hok12319671:24000
Konawa fine sandy loam, 1 to 3 percent slopesKoB24353846312tq7cok12319671:24000
Konawa fine sandy loam, 3 to 5 percent slopesKoC11283846322tq7dok12319671:24000
Konawa fine sandy loam, 0 to 1 percent slopesKoA643384630dx7fok12319671:24000
Konawa fine sandy loam, 3 to 8 percent slopes, severely eroded26146423846862tq7nok12519751:24000
Konawa fine sandy loam, 3 to 5 percent slopes2582213846852tq7dok12519751:24000
Konawa loamy fine sand, 3 to 8 percent slopes2371013846832tq7gok12519751:24000
Konawa fine sandy loam, 1 to 3 percent slopes2442843846842tq7cok12519751:24000
Konawa fine sandy loam, 3 to 8 percent slopes, eroded23114013848092tq7lok13319761:24000
Konawa fine sandy loam, 3 to 8 percent slopes, gullied2486913848102tq7mok13319761:24000
Konawa fine sandy loam, 3 to 5 percent slopes2259523848082tq7dok13319761:24000
Konawa fine sandy loam, 1 to 3 percent slopes2128293848072tq7cok13319761:24000
Dougherty and Konawa soils, 3 to 8 percent slopesDoC4656384858dxgsok13719601:24000
Dougherty-Konawa loamy fine sands association and 0 to 3 percent slopesDoB146438485730g72ok13719601:24000
Konawa and Dougherty soils, 1 to 5 percent slopes, erodedDuB2354384859dxgtok13719601:24000
Konawa fine sandy loam, 5 to 8 percent slopesKoD945365531d8cbtx14719891:24000
Konawa loamy fine sand, 3 to 8 percent slopesKoC4652374485dkp5tx61219731:20000
Konawa loamy fine sand, 1 to 3 percent slopesKoB1090374484dkp4tx61219731:20000

Map of Series Extent

Approximate geographic distribution of the KONAWA 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 .