Official Series Description


Lab Data Summary

Aggregate lab data for the BRACE soil series. This aggregation is based on all pedons with a current taxon name of BRACE, 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 BRACE 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
2303N032702OR025005Brace6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties43.4102821,-119.6311646

Water Balance

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

Soil series competing with BRACE 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 BRACE 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 BRACE 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 BRACE, 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-2010-09-29-08 | Lake County, Southern Part - 1999

    Soil-landform relationships on grass- and shrub-covered tablelands and mountains (Soil Survey of Lake County, Oregon, Southern Part; 1999).

  2. OR-2012-05-10-17 | Lake County, Southern Part - 1999

    Soil-landform relationships on grass- and shrub-covered tablelands and mountains (Soil Survey of Lake County Oregon, Southern Part; 1999).

Map Units

Map units containing BRACE 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
Larioscamp-Dishpan-Brace loams, 1 to 12 percent slopes9326463486298jb11id67519921:24000
Brace-Freshwater complex, 1 to 15 percent slopes2315376486152j9wbid67519921:24000
Raz-Brace complex, 2 to 20 percent slopes, harney area, mlra 232725597664906822wzsbor62819971:24000
Raz-Brace complex, low precipitation, 2 to 20 percent slopes27362443490683jglhor62819971:24000
Brace-Vergas complex, 2 to 20 percent slopes4713274490857jgs3or62819971:24000
Brace-Coztur-Rock outcrop complex, 2 to 20 percent slopes4613175490854jgs0or62819971:24000
Raz-Brace complex, high precipitation, 2 to 20 percent slopes53818792516900381tqmcor63520061:24000
Raz-Brace complex, low precipitation, 2 to 20 percent slopes53913106316900391tqmdor63520061:24000
Raz-Brace complex, 2 to 10 percent slopes537702316900371tqmbor63520061:24000
Brace-Foleylake complex, 2 to 15 percent slopes231394816897421tq9tor63520061:24000
Raz-Brace complex, overblown, 2 to 20 percent slopes540269016900401tqmfor63520061:24000
Brace-Raz complex, 2 to 15 percent slopes29C61022489163jf0gor63619911:24000
Raz-Brace complex, 2 to 20 percent slopes, south lake area, mlra 23219D173684890682wzscor63619911:24000
Brace-Coglin complex, 2 to 15 percent slopes28C5526489160jf0cor63619911:24000
Raz-Brace complex, overblown, 2 to 15 percent slopes220C1463489073jdxkor63619911:24000
Fertaline-Brace complex, 0 to 8 percent slopes50171634127222652vsb0or6451:24000

Map of Series Extent

Approximate geographic distribution of the BRACE 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 .