Official Series Description


Lab Data Summary

Aggregate lab data for the OXWALL soil series. This aggregation is based on all pedons with a current taxon name of OXWALL, 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 OXWALL 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
998P0237S1997OR023027OXWALL6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties44.416111,-118.8280563

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the OXWALL 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 OXWALL 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 OXWALL 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 OXWALL 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 OXWALL 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 OXWALL 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 OXWALL 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 OXWALL, 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. OR-2010-09-29-11 | Lake County, Southern Part - 1999

    Soil-landscape relationships in Goose Lake Valley. Goose Lake and Lakeview soils on basin floor, Drew soils on middle terraces, Salisbury and Oxwall soils on high terraces, and Booth soils on hills (Soil Survey of Lake County, Oregon, Southern Part; 1999).

  2. OR-2012-05-10-20 | Lake County, Southern Part - 1999

    Soil-landscape relationships in Goose Lake Valley. Goose Lake and Lakeview soils on basin floor, Drews soils on middle terraces, Salisbury and Oxwall soils on high terraces, and Booth soils on hills (Soil Survey of Lake County Oregon, Southern Part; 1999).

Map Units

Map units containing OXWALL 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
Oxwall gravelly loam, 0 to 5 percent slopes189or47189941221rhcca70319831:24000
Oxwall very cobbly silty clay loam, 1 to 4 percent slopes650A87893426220nk2bor6271:24000
Oxwall-Oxbow complex, 4 to 10 percent slopes653B560934262472st5sor6271:24000
Oxwall gravelly loam, 1 to 4 percent slopes190B36913426284vykwor6271:24000
Oxwall-Belshaw complex, 10 to 30 percent north slopes656D131434294932st5tor6271:24000
Zweygardt-Oxwall complex, 2 to 15 percent slopes652E10743429542nk3qor6271:24000
Oxwall-Oxbow-Zweygardt complex, 0 to 30 percent slopes654D97534295582lhpbor6271:24000
Oxwall-Belshaw complex, 30 to 50 percent north slopes656E89534295622sz65or6271:24000
Oxwall-Starkey complex, 30 to 50 percent south slopes628E66134319722sz61or6271:24000
Oxwall-Balder-Belshaw complex, 10 to 30 percent slopes658D61234319962wj7xor6271:24000
Belshaw-Plaiden-Oxwall complex, 2 to 20 percent slopes650C29434321192wj7wor6271:24000
Oxwall-Starkey complex, 10 to 30 percent south slopes628D25034321252sz60or6271:24000
Oxwall-Rubble land complex, disturbed, 0 to 10 percent slopes629B13434321742sz62or6271:24000
Oxwall gravelly loam, 0 to 5 percent slopes189B8681489021jdvwor63619911:24000
Oxwall-Salisbury complex, 0 to 5 percent slopes190B3343489024jdvzor63619911:24000
Drews-Oxwall complex, 0 to 5 percent slopes75B417489437jf99or63619911:24000

Map of Series Extent

Approximate geographic distribution of the OXWALL 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 .