Official Series Description


Lab Data Summary

Aggregate lab data for the ONAWA soil series. This aggregation is based on all pedons with a current taxon name of ONAWA, 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 ONAWA 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
107BM09165132009MO165013Onawa4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties39.5083333,-95.0825556
107B95P032694NE177015Onawa7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties41.4355545,-95.9602814
107B97P0032S1996IA193028Onawa7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties42.2329445,-96.2849731
107B09N1041S2009KS043001Onawa8Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties39.8174438,-94.9192505

Water Balance

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

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

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 ONAWA 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 ONAWA 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 ONAWA 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 ONAWA, 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-2010-09-02-23 | Monona County - 2003

    Typical pattern of soils and parent material in the Albaton-Percival-Sarpy and Albaton-Onawa-Forney associations (Soil Survey of Monona County, Iowa; 2003).

  2. MO-2012-02-06-01 | Atchison County - May 1994

    Typical pattern of soils and parent material in the Onawa-Paxico-Haynie association (Soil Survey of Atchison County, Missouri; May 1994).

  3. MO-2012-02-06-15 | Buchanan County - September 1989

    Pattern of soils and parent material in the Haynie-Onawa-Waldron association (Soil Survey of Buchanan County, Missouri; September 1989).

  4. NE-2012-02-10-04 | Cedar County - October 1985

    Typical pattern of soils in the Sarpy-Blake-Albaton association and the relationship of the soils to topography and parent material (Soil Survey of Cedar County, Nebraska; October 1985).

  5. NE-2012-02-13-67 | Nemaha County - December 1985

    Typical pattern of soils and parent material in the Monona-Ida and Onawa-Haynie-Albaton associations (Soil Survey of Nemaha County, Nebraska; December 1985).

  6. NE-2012-02-14-14 | Washington County - September 1964

    Soil pattern of the Luton-Volin and Albaton-Haynie associations (Soil Survey of Washington County, Nebraska; September 1964).

Map Units

Map units containing ONAWA 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
Onawa silty clay1463226406099fmkzia07119681:20000
Onawa silt loam145376406098fmkyia07119681:20000
Onawa silty clay1466066406735fn7hia08519711:15840
Onawa silt loam1451134406734fn7gia08519711:15840
Onawa silty clay, 0 to 2 percent slopes1463610409538fr4xia12919791:15840
Onawa silty clay, 0 to 2 percent slopes, rarely flooded1469899447347h0hkia13319941:12000
Onawa silty clay, 0 to 2 percent slopes, occasionally flooded11462546447404h0kdia13319941:12000
Onawa silt loam, 0 to 2 percent slopes, rarely flooded145797447346h0hjia13319941:12000
Onawa silt loam, 0 to 2 percent slopes, occasionally flooded1145197447403h0kcia13319941:12000
Onawa silty clay, 0 to 2 percent slopes1463790410445fs35ia15519861:15840
Onawa-Albaton complex, 0 to 2 percent slopes, rarely flooded31464079741626swqfia19320031:12000
Onawa silty clay, 0 to 2 percent slopes, occasionally flooded1146515401827fh45ia19320031:12000
Onawa and Waldron silty clay loams, occasionally flooded7760297114753841lj81ks00519981:24000
Haynie-Onawa complex, occasionally flooded7743182714753821lj7zks00519981:24000
Onawa loam, overwash, occasionally flooded776128614753851lj82ks00519981:24000
Onawa and Waldron silty clay loams, occasionally flooded77606687747178t2hjks04319771:24000
Onawa loamy fine sand, overwash, occasionally flooded77625237747179t2hkks04319771:24000
Haynie-Onawa complex, occasionally flooded77433596747160t2gyks04319771:24000
Onawa silty clay loam, occasionally flooded77633013186240520hzlks10319731:24000
Onawa soils, occasionally flooded, overwash77642038186240620hzmks10319731:24000
Onawa and Waldron silty clay loams, occasionally flooded7760620186240320hzjks10319731:24000
Haynie-Onawa complex, occasionally flooded7743154186240220hzhks10319731:24000
Onawa loam, overwash, occasionally flooded776135186240420hzkks10319731:24000
Onawa soils, occasionally flooded, overwash77642823186229420hw0ks20919731:24000
Onawa silty clay loam, occasionally flooded77632164186229320hvzks20919731:24000
Onawa silty clay, 0 to 2 percent slopes, rarely flooded13568706725284582qmv3mo00519881:24000
Onawa silty clay, 0 to 2 percent slopes, frequently flooded135671361902696z9b7mo00519881:24000
Onawa silty clay, 0 to 2 percent slopes, rarely flooded13568910225284572qmv3mo02119841:24000
Haynie-Onawa complex, 0 to 2 percent slopes, rarely flooded135301291887543yskfmo02119841:24000
Onawa silty clay, 0 to 2 percent slopes, rarely flooded1356812325284562qmv3mo16519821:24000
Onawa silty clay, occasionally flooded7880504357647d050ne01519761:20000
Onawa silty clay, occasionally flooded78803927427855gc6sne02119781:20000
Onawa silty clay, occasionally flooded7880202916914901ts46ne02519811:20000
Onawa silty clay, rarely flooded78832103427122gbg4ne02719821:20000
Onawa silty clay, occasionally flooded78805783426764gb2lne04319721:20000
Onawa silty clay, occasionally flooded78802330426694gb0bne05119751:20000
Onawa silty clay, rarely flooded788321922170692df1cne05119751:20000
Onawa silty clay, occasionally flooded7880184017109621vfdbne05520071:12000
Gilliam-Onawa complex, occasionally flooded848625617109431vfcqne05520071:12000
Onawa silty clay, occasionally flooded, wet776235125704782rmhwne10719891:20000
Onawa silty clay, rarely flooded788339849265xhqnne10719891:20000
Onawa silty clay, occasionally flooded7880469616916871tsbkne12719831:20000
Onawa silt loam, occasionally flooded787787016916861tsbjne12719831:20000
Onawa silt loam, overwash, occasionally flooded7878822193862dhg3ne12719831:20000
Onawa silty clay, occasionally flooded7880228916915481ts62ne13119791:20000
Onawa silt loam, overwash, occasionally flooded787866216915471ts61ne13119791:20000
Onawa silty clay, occasionally flooded7880130516910611trpcne14719671:20000
Onawa silty clay, occasionally flooded7880149817110251vfgcne15320071:12000
Onawa-Lossing silty clays, occasionally flooded7886107117110261vfgdne15320071:12000
Gilliam-Onawa complex, occasionally flooded848657817110081vfftne15320071:12000
Onawa silty clay, occasionally flooded78801517427742gc34ne17319661:20000
Onawa and Haynie soils, occasionally flooded7876645427741gc33ne17319661:20000
Onawa silty clay, occasionally flooded78803006395498f8k0ne17720001:12000
Onawa-Haynie complex, occasionally flooded78851803395515f8kkne17720001:12000
Onawa silty clay loam, occasionally flooded77631474395513f8khne17720001:12000
Onawa silty clay, occasionally flooded, wetS425A89126155892rmhwsd02319801:20000
Onawa fine sandy loam, overwashOh278355056cxgfsd02319801:20000
Onawa silty clay, 0 to 2 percent slopesOa3393445596gyp2sd02719951:24000
Haynie-Onawa-Blake complex, 0 to 2 percent slopesHo2280445579gynjsd02719951:24000
Onawa-Owego silty clays, 0 to 2 percent slopesOb646445597gyp3sd02719951:24000
Onawa silty clayOb6053453714h73ysd12719741:20000
Onawa silty clayOa1469418096g11zsd13519771:20000

Map of Series Extent

Approximate geographic distribution of the ONAWA 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 .