Official Series Description


Lab Data Summary

Aggregate lab data for the BRYCAN soil series. This aggregation is based on all pedons with a current taxon name of BRYCAN, 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 BRYCAN were used in the calculation. Source: KSSL snapshot . Methods used to assemble the KSSL snapshot used by SoilWeb / SDE

There are insufficient data to create the lab data summary figure.


Water Balance

Monthly water balance estimated using a leaky-bucket style model for the BRYCAN 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 BRYCAN 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 BRYCAN 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 BRYCAN 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 BRYCAN 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 BRYCAN 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 BRYCAN 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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Soil series sharing subgroup-level classification with BRYCAN, 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 BRYCAN 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
Brycan association, moderately slopingBR8228507715k19xnm00719741:24000
Ring-Brycan association, moderately slopingRG7030507772k1crnm00719741:24000
Moreno-Brycan association, slopingMG14708375535dls1nm63019771:48000
Brycan silty clay loam, 3 to 25 percent slopesBS3799566571wynnm63619701:31680
Brycan loam, 3 to 25 percent slopesBR693566561wymnm63619701:31680
Moreno-Brycan association, slopingMR15077375704dlyhnm63819811:31680
Brycan loam, 1 to 3 percent slopesBe3702375670dlxdnm63819811:31680
Brycan loam, 3 to 8 percent slopesBf918375671dlxfnm63819811:31680
Brycan loam, 0 to 3 percent slopes6246972568342rrn5nm64819821:48000
Suposo-Brycan complex, 1 to 6 percent slopes2288994562301whwnm65019891:24000
Moreno-Brycan association, 3 to 15 percent slopesMR45129345842wl26nm6781:24000
Brycan-Emmons complex, 2 to 15 percent slopesWaC139828102352trcrut0131:24000
Brycan loam, 3 to 20 percent slopesDSB90414279391jxwkut0131:24000
Silas-Brycan loams1091836503682jx3tut61619831:24000
Brycan very fine sandy loam, 1 to 6 percent slopes252686504417jxwjut63619841:24000
Brycan very fine sandy loam, 6 to 15 percent slopes261395504418jxwkut63619841:24000
Mara-Longvalley-Brycan complex, 4 to 15 percent slopes44325125082122q7dyut6421:63360

Map of Series Extent

Approximate geographic distribution of the BRYCAN 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 .