Official Series Description


Lab Data Summary

Aggregate lab data for the ONARGA soil series. This aggregation is based on all pedons with a current taxon name of ONARGA, 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 ONARGA 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
108A78IL1030161978IL103016Onarga1Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties41.6233794,-89.4016426
108B84IL1250081984IL125008Onarga2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties40.2091444,-89.8756333
108B85IL1250571985IL125057Onarga2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties40.4066556,-89.7179111
115APS75011975IN129001Onarga3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties37.9287722,-87.9894944
115APS75031975IN129003Onarga3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties37.9521444,-87.9767
115C67IL0610051967IL061005Onarga6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties39.4786153,-90.5807618
115C79IL1710081979IL171008Onarga1Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties39.6156997,-90.5128765
115C80IL0090291980IL009029Onarga2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties39.8606327,-90.5989964
115C80IL1710301980IL171030Onarga1Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties39.7609395,-90.5884209
115C84IL1250051984IL125005Onarga2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties40.3127111,-89.8967444
115C84IL1250091984IL125009Onarga2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties40.2748139,-89.9885417
115C85IL1250041985IL125004Onarga2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties40.3124472,-89.9754028
115C85IL1250391985IL125039Onarga2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties40.3215528,-89.7960889
115C85IL1250441985IL125044Onarga2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties40.3117972,-89.9755556
115C85IL1250461985IL125046Onarga2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties40.3545917,-89.8197111

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the ONARGA 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 ONARGA 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 ONARGA 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 ONARGA 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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Competing Series

Soil series competing with ONARGA 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 ONARGA series and competing. 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 ONARGA 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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There are insufficient data to create the 3D hills figure.

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.

Soil series sharing subgroup-level classification with ONARGA, 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-2010-09-01-45 | Mason County - 1995

    Typical pattern of soils and parent material in the Onarga-Dakota-Sparta association (Soil Survey of Mason County, Illinois; 1995).

  2. IL-2010-09-01-46 | Mason County - 1995

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

  3. IL-2010-09-01-47 | Mason County - 1995

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

  4. 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).

  5. IL-2010-09-01-49 | Mason County - 1995

    Typical pattern of soils and parent material in the Broadwell-Edgington-Pillot association (Soil Survey of Mason County, Illinois; 1995).

  6. IL-2011-06-01-06 | Brown County - 1988

    Typical cross section showing the relationship of parent material to soils in Brown County (Soil Survey of Brown County, Illinois; 1988).

  7. IL-2011-08-04-60 | Mason County - 1995

    Typical pattern of soils and parent material in the Sparta-Plainfield-Ade association (Soil Survey of Mason County, Illinois; 1995).

  8. IL-2011-08-04-61 | Mason County - 1995

    Typical pattern of soils and parent material in the Onarga-Dakota-Sparta association (Soil Survey of Mason County, Illinois; 1995).

  9. IL-2011-08-04-62 | Mason County - 1995

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

  10. 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).

  11. IL-2011-08-04-65 | Mason County - 1995

    Typical pattern of soils and parent material in the Broadwell-Edgington-Pillot association (Soil Survey of Mason County, Illinois; 1995).

Map Units

Map units containing ONARGA 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
Onarga loam, 0 to 2 percent slopes, rarely flooded7150A4431729445syvil00919841:12000
Onarga sandy loam, 2 to 5 percent slopes150B29024296284thil01919991:12000
Onarga fine sandy loam, 2 to 5 percent slopes150B1611983306ncril05320011:12000
Onarga fine sandy loam, 2 to 5 percent slopes150B370615642nnmfil05719971:12000
Onarga fine sandy loam, 1 to 4 percent slopes190B305211619736fil05919661:20000
Onarga fine sandy loam, 4 to 10 percent slopes190C115211620736gil05919661:20000
Onarga sandy loam, 0 to 2 percent slopes, rarely flooded7150A661211724739til06119681:15840
Onarga fine sandy loam, 2 to 5 percent slopes150B60761755495wnwil07519801:15840
Onarga fine sandy loam, 2 to 5 percent slopes150B143098045511x7lil09120031:12000
Onarga fine sandy loam, 0 to 2 percent slopes150A12402631678tv8il09120031:12000
Onarga fine sandy loam, 2 to 5 percent slopes150B13551769305y3fil10519911:15840
Onarga fine sandy loam, 5 to 10 percent slopes150C1831769315y3gil10519911:15840
Broadwell-Onarga complex, 2 to 5 percent slopes827B162215960861qkvnil10720061:12000
Broadwell-Onarga complex, 2 to 5 percent slopes, eroded827B245215960881qkvqil10720061:12000
Broadwell-Onarga complex, 0 to 2 percent slopes827A16415960831qkvkil10720061:12000
Onarga sandy loam, 0 to 2 percent slopes, rarely flooded7150A5511989066nzbil11920011:12000
Onarga sandy loam, 0 to 2 percent slopes150A51018208463gpil12319971:15840
Onarga sandy loam, 5 to 10 percent slopes150C46518208663gril12319971:15840
Onarga sandy loam, 0 to 2 percent slopes150A156831777585yz4il12519891:15840
Onarga sandy loam, 2 to 5 percent slopes150B71211777595yz5il12519891:15840
Onarga sandy loam, 5 to 10 percent slopes, eroded150C225341777605yz6il12519891:15840
Broadwell-Onarga complex, 2 to 5 percent slopes827B4925179762qhc3il12519891:15840
Onarga sandy loam, 2 to 5 percent slopes, rarely flooded7150B4425185912qhckil12519891:15840
Onarga sandy loam, 0 to 2 percent slopes, rarely flooded7150A4225179902qgxhil12519891:15840
Broadwell-Onarga complex, 2 to 5 percent slopes827B181614088501j90sil12920051:12000
Broadwell-Onarga complex, 5 to 10 percent slopes, eroded827C279414088511j90til12920051:12000
Onarga sandy loam, 2 to 5 percent slopes150B10316721161t3z7il13719841:15840
Onarga fine sandy loam, 2 to 5 percent slopes, rarely flooded7150B3025421862qvkgil13719841:15840
Onarga fine sandy loam, 2 to 5 percent slopes, rarely flooded7150B65825421002qrd6il17119841:12000
Onarga sandy loam, 2 to 5 percent slopes150B29125420692qrc4il17119841:12000
Onarga sandy loam, 0 to 2 percent slopes150A789417935960msil17919911:15840
Onarga sandy loam, 2 to 5 percent slopes150B520317936060mtil17919911:15840
Onarga sandy loam, 0 to 2 percent slopes, rarely flooded7150A27425097862qgxhil17919911:15840
Broadwell-Onarga complex, 2 to 5 percent slopes827B1425088182q7yril17919911:15840
Onarga fine sandy loam, 2 to 5 percent slopes150B86616127471r463il18320061:12000
Onarga fine sandy loam, 5 to 10 percent slopes, eroded150C219016127481r464il18320061:12000
Onarga fine sandy loam, 2 to 5 percent slopes150B10772624138t1yil19720021:12000
Onarga fine sandy loam 5 to 10 percent slopes, eroded150C2179617101nq4hil19720021:12000
Onarga fine sandy loam, moderately wet, 2 to 6 percent slopes, erodedOnB29931636975hbkin11119901:15840
Onarga fine sandy loam, moderately wet, 0 to 2 percent slopesOnA9311636945hbgin11119901:15840
Onarga fine sandy loam, till substratum, 2 to 6 percent slopes, erodedOpB27081637045hbsin11119901:15840
Onarga fine sandy loam, 0 to 2 percent slopes, rarely floodedOnA7391599005cd2in12919781:15840

Map of Series Extent

Approximate geographic distribution of the ONARGA 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 .