Official Series Description


Lab Data Summary

Aggregate lab data for the BREKO soil series. This aggregation is based on all pedons with a current taxon name of BREKO, 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 BREKO 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
2973C0056S1973NV009003Breko8Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties37.539669,-117.4942474

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the BREKO 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 BREKO 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 BREKO 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 BREKO 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 BREKO 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 BREKO 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 BREKO 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 flats position figure.

Soil series sharing subgroup-level classification with BREKO, 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

No block diagrams are available.

Map Units

Map units containing BREKO 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
Breko-Crunker associaton607010477477004j0c7nv77419851:24000
Breko-Wiskiflat association MLRA 29607252864770062whm0nv77419851:24000
Handpah-Breko-Crunker association60813680477008j0ccnv77419851:24000
Handpah-Breko association60822220477009j0cdnv77419851:24000
Breko gravelly sandy loam, 2 to 8 percent slopes60732123477007j0cbnv77419851:24000
Breko stony loamy sand, 4 to 15 percent slopes6071933477005j0c8nv77419851:24000
Belted-Breko association1326472476755j036nv77419851:24000
Breko-Yody association69826622158232dcr5nv77820131:24000
Biken-Breko association12433510480208j3plnv78019901:24000
Molion-Unsel-Breko association5502285480519j40mnv78019901:24000
Breko-Yody association9822015480652j44xnv78019901:24000
Breko-Armespan association9811490480651j44wnv78019901:24000
Nyala-Breko-Unsel association6211195480549j41lnv78019901:24000
Breko-Veet-Handpah association30806386480899j4dwnv78319911:24000
Tomel-Breko-Wardenot association29617056469230hr8gnv78519951:24000
Breko-Veet association20905857469088hr3wnv78519951:24000
Handpah-Breko-Veet association79215047485149j8tznv79619841:63360
Handpah-Tomel-Breko association7941539485151j8v1nv79619841:63360
Terlco-Breko association4301714477645j10xnv79919911:24000
Breko-Wiskiflat association MLRA 2918011394776112whm0nv79919911:24000
Breko, dry-Wiskiflat association181923477612j0zvnv79919911:24000
Breko-Checkett families-Rock outcrop complex, 30 to 70 percent slopes118581642mj7nut6491:24000

Map of Series Extent

Approximate geographic distribution of the BREKO 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 .