Official Series Description


Lab Data Summary

Aggregate lab data for the WALDRON soil series. This aggregation is based on all pedons with a current taxon name of WALDRON, 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 WALDRON 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
107BM87195261987MO195026mWaldron3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties39.2536125,-93.4225006
115B85P01781984MO027001Waldron7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.6641655,-91.8899994
115B85P04451984MO027002Waldron7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.6699982,-91.7791672
115B85P04461984MO027003Waldron7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.6280556,-91.8925018
115BM88073071988MO073007Waldron3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.9672203,-92.3450012
115B90P04231989MO183010Waldron7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.8588905,-90.194725
115B90P04301989MO183013Waldron6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.8630562,-90.1702805
115B90P04361989MO183019Waldron6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.8661118,-90.2016678
115B90P04391989MO183022Waldron6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.8669434,-90.1994476
115B90P04401989MO183023Waldron6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.8672218,-90.1991653
115BM90051171990MO051017Waldron4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.9672644,-92.3451678
115BM90053261990MO053026Waldron4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.9672203,-92.3450012
115BM90053441990MO053044Waldron4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.9672203,-92.3450012
115BM90053451990MO053045Waldron4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties39.0343056,-92.9231667
115BM90099111990MO099011Waldron4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.3814417,-90.3542695
115BM90151071995MO151059Waldron3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.6933802,-91.6834793
115BM90151371995MO151066Waldron3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.6764359,-91.7776489
115BM97051151997MO051121Waldron4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.65808,-92.2805215
115BM97051191997MO051125Waldron4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.6094302,-92.2126699
115BM03219082003MO219008Waldron4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.6047444,-90.9962778
115BM07027292007MO027029WALDRON4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.614,-91.95125
115BM07027302007MO027030WALDRON4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.6372778,-91.9259722
115BM07027352007MO027035WALDRON4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.6665556,-91.8785556
115BM07183022007MO183002WALDRON4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.6015833,-90.7981389

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the WALDRON 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 WALDRON 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 WALDRON 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 WALDRON 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 hills figure.

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

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Click the image to view it full size.

Competing Series

Soil series competing with WALDRON 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 WALDRON 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 WALDRON 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 WALDRON, 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. 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).

Map Units

Map units containing WALDRON 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 and Waldron silty clay loams, occasionally flooded7760297114753841lj81ks00519981:24000
Onawa and Waldron silty clay loams, occasionally flooded77606687747178t2hjks04319771:24000
Onawa and Waldron silty clay loams, occasionally flooded7760620186240320hzjks10319731:24000
Waldron silty clay loam, 0 to 2 percent slopes, rarely flooded135914471887580yslmmo02119841:24000
Waldron silty clay, 0 to 2 percent slopes, frequently flooded661176225716892qpb2mo03119781:24000
Waldron silty clay loam, 0 to 2 percent slopes, occasionally flooded660061088025334882qp87mo03319881:24000
Haynie-Waldron complex, 0 to 2 percent slopes, occasionally flooded13532466925283902qmtnmo04119921:24000
Haynie-Waldron complex, 0 to 2 percent slopes, frequently flooded135313812888511ytknmo04119921:24000
Waldron silty clay, loamy substratum, 0 to 2 percent slopes, occasionally flooded661113014888504ytkfmo04119921:24000
Waldron silty clay loam, 0 to 2 percent slopes, occasionally flooded6600674725334912qp87mo04719821:24000
Waldron silty clay loam, 0 to 2 percent slopes, frequently flooded66052811574253m8k9mo09920001:24000
Waldron silty clay loam, 0 to 2 percent slopes, occasionally flooded66006221525334892qp87mo10719701:24000
Haynie-Waldron complex, 0 to 2 percent slopes, occasionally flooded1353214025283892qmtnmo10719701:24000
Waldron silty clay, 0 to 2 percent slopes, occasionally flooded66112255325337972qp9zmo15719831:24000
Haynie-Waldron complex, 0 to 2 percent slopes, occasionally flooded13532202425283872qmtnmo15719831:24000
Waldron silty clay, 0 to 2 percent slopes, frequently flooded66117183325338102qpb2mo15719831:24000
Haynie-Waldron complex, 0 to 2 percent slopes, frequently flooded6611872017226491vtkbmo15719831:24000
Waldron silty clay loam, 0 to 2 percent slopes, occasionally flooded66006315525334902qp87mo16519821:24000
Waldron silty clay loam, 0 to 2 percent slopes, occasionally flooded66006947625334872qp87mo17719791:24000
Waldron silty clay, 0 to 2 percent slopes, frequently flooded661172025338092qpb2mo18619821:24000
Waldron silty clay, 0 to 2 percent slopes, occasionally flooded661121116425337982qp9zmo19519891:24000
Haynie-Waldron complex, 0 to 2 percent slopes, occasionally flooded13532526525283882qmtnmo19519891:24000

Map of Series Extent

Approximate geographic distribution of the WALDRON 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 .