Official Series Description


Lab Data Summary

Aggregate lab data for the BLUECANYON soil series. This aggregation is based on all pedons with a current taxon name of BLUECANYON, 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 BLUECANYON 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 BLUECANYON 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 BLUECANYON 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 BLUECANYON 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 BLUECANYON 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 terrace figure.

There are insufficient data to create the 3D flats position figure.

Competing Series

Soil series competing with BLUECANYON 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 BLUECANYON 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 BLUECANYON 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 .

Click the image to view it full size.

Click the image to view it full size.

Click the image to view it full size.

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

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Soil series sharing subgroup-level classification with BLUECANYON, 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 BLUECANYON 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
Bluecanyon-Ironside complex, 30 to 60 percent south slopes7709CS11925939371sgd0or60419881:24000
Bluecanyon-Analulu complex, 30 to 60 percent slopes7759CO7731206471sgfsor60720181:24000
Bluecanyon-Ironside complex, sandstone substratum, 15 to 30 percent slopes2013BO7331204261r00sor60720181:24000
Bluecanyon-Ironside complex, 30 to 60 percent south slopes7709CS5031206271sgd0or60720181:24000
Bluecanyon-Analulu complex, 15 to 30 percent slopes7759BO4431206461sgfror60720181:24000
Vogel-Ironside-Bluecanyon complex, 30 to 60 percent slopes7731CO4331202621q70cor60720181:24000
Bluecanyon-Analulu complex, 60 to 90 percent slopes7759DO3431206481sgftor60720181:24000
Vogel-Ironside-Bluecanyon complex, 15 to 30 percent slopes7731BO1431207841v6m0or60720181:24000
Porch-Wintercanyon-Bluecanyon complex, 20 to 50 percent slopes7817CO1371933854612xj8lor62620181:24000
Wintercanyon-Bluecanyon-Porch complex, 20 to 50 percent slopes7816CO1226433854602xj8jor62620181:24000
Bluecanyon-Wintercanyon-Porch complex, 2 to 20 percent slopes7815NO915533854592xj8kor62620181:24000
Bluecanyon-Ironside complex, 30 to 60 percent south slopes7709CS309031224121sgd0or62620181:24000
Bluecanyon-Analulu complex, 60 to 90 percent slopes7759DO146731224311sgftor62620181:24000
Bluecanyon-Ironside-Rock outcrop complex, 60 to 90 percent south slopes7778DS123631224341sgh0or62620181:24000
Bluecanyon-Ironside complex, 0 to 15 percent slopes7709AO78631224101sgcxor62620181:24000
Bluecanyon-Ironside complex, 15 to 30 percent slopes7709BO51431224111sgczor62620181:24000
Vogel-Bluecanyon complex, 0 to 15 percent slopes7304AO8731223781sg92or62620181:24000
Prag-Bluecanyon-Bocker complex, 20 to 50 percent north slopes4325NO5433854092w6bcor62620181:24000
Bluecanyon-Analulu complex, 15 to 30 percent slopes7759BO4531224301sgfror62620181:24000
Vogel-Ironside-Bluecanyon complex, 30 to 60 percent slopes7731CO3931221131q70cor62620181:24000
Bluecanyon-Ruddley complex, 20 to 50 percent north slopes4326NO2233854102sz69or62620181:24000
Bluecanyon-Prag-Bocker complex, 2 to 20 percent slopes4325AO633854082w6bbor62620181:24000
Prag-Bluecanyon-Bocker complex, 20 to 50 percent north slopes245E299134263122w6bcor6271:24000
Bluecanyon-Prag-Bocker complex, 2 to 20 percent slopes245C274534263292w6bbor6271:24000
Fopiano-Bluecanyon-Powellbutte complex, 2 to 20 percent slopes239C153234294472qczfor6271:24000
Bluecanyon-Prag-Bocker complex, 20 to 50 percent south slopes246E65134319742sz6bor6271:24000
Bluecanyon-Wintercanyon-Porch complex, 2 to 20 percent slopes7815NO13534318482xj8kor6271:24000
Vogel-Bluecanyon complex, 0 to 15 percent slopes7304AO12134318991sg92or6271:24000
Wintercanyon-Bluecanyon-Porch complex, 20 to 50 percent slopes7816CO10534318472xj8jor6271:24000
Porch-Wintercanyon-Bluecanyon complex, 20 to 50 percent slopes7817CO2134318492xj8lor6271:24000
Bluecanyon-Ironside complex, 30 to 60 percent south slopes7709CS496824374771sgd0or63120181:24000
Vogel-Ironside-Bluecanyon complex, 30 to 60 percent slopes7731CO203824374881q70cor63120181:24000
Bluecanyon-Ironside complex, 15 to 30 percent slopes7709BO182324374761sgczor63120181:24000
Bluecanyon-Analulu complex, 15 to 30 percent slopes7759BO105424868941sgfror63120181:24000
Vogel-Ironside-Bluecanyon complex, 15 to 30 percent slopes7731BO56624374871v6m0or63120181:24000
Bluecanyon-Ironside-Rock outcrop complex, 60 to 90 percent south slopes7778DS5724375041sgh0or63120181:24000
Bluecanyon-Ironside complex, 0 to 15 percent slopes7709AO3324374751sgcxor63120181:24000
Vogel-Bluecanyon complex, 0 to 15 percent slopes7304AO724868651sg92or63120181:24000
Ironside, south-Bluecanyon-Ironside complex, 2 to 45 percent slopes90361111130270322xf36or6451:24000
Lostbasin-Bluecanyon complex, 15 to 60 percent south slopes9039981931156412yggmor6451:24000
Ironside-Bluecanyon complex, 15 to 60 percent south slopes9029201927222742sf34or6451:24000
Hondu-Bluecanyon complex, 30 to 60 percent slopes903266227222772sf31or6451:24000
Ironside-Bluecanyon-Scratchpost complex, 12 to 45 percent slopes903762530270332xf37or6451:24000
Bluecanyon-Ironside complex, sandstone substratum, 15 to 30 percent slopes2013BO3931215201r00sor64819771:24000
Analulu-Slicklog-Bluecanyon complex, 30 to 60 percent south slopes545847732v6mor67019991:24000

Map of Series Extent

Approximate geographic distribution of the BLUECANYON 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 .