Official Series Description


Lab Data Summary

Aggregate lab data for the BURBANK soil series. This aggregation is based on all pedons with a current taxon name of BURBANK, 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 BURBANK 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 BURBANK 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 BURBANK 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 BURBANK 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 BURBANK 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 BURBANK 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 BURBANK series and competing. Series are sorted according to hierarchical clustering of median values. Source: SSURGO map unit geometry and 1981-2010, 800m PRISM data .

Click the image to view it full size.

Geomorphic description summaries for the BURBANK 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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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 flats position figure.

Soil series sharing subgroup-level classification with BURBANK, 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. WA-2012-05-11-15 | Benton County Area - July 1971

    Cross section of Benton County, showing the relationship of elevation, precipitation, and major soil series (Soil Survey of Benton County Area, Washington; April 1980).

Map Units

Map units containing BURBANK 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
Burbank loamy fine sand, 2 to 5 percent slopes8B47176140021wnor64819771:24000
Burbank loamy fine sand, 5 to 12 percent slopes8C2106140121wpor64819771:24000
Burbank loamy fine sand, 0 to 5 percent slopes14B8604644532524or66719841:20000
Burbank loamy fine sand, 0 to 8 percent slopes71882699454rgv1wa01719981:12000
Burbank loamy fine sand, 8 to 25 percent slopes72507699455rgv2wa01719981:12000
Burbank loamy fine sand, 0 to 5 percent slopes43047717362dn2wa02119941:20000
Finley-Burbank-Starbuck complex, 0 to 10 percent slopes261019716962dlswa02119941:20000
Burbank gravelly loamy fine sand, 15 to 35 percent slopes6285718102dqgwa02119941:20000
Burbank loamy fine sand, 5 to 10 percent slopes5136717672dp2wa02119941:20000
Burbank loamy fine sand, 0 to 5 percent slopes26375856879829l9wa02519791:24000
Burbank stony loamy sand, 2 to 15 percent slopes2953946880129ldwa02519791:24000
Burbank loamy fine sand, 5 to 15 percent slopes2736186879929lbwa02519791:24000
Burbank very cobbly loamy sand, 0 to 15 percent slopes2820496880029lcwa02519791:24000
Burbank very bouldery loamy sand, 0 to 10 percent slopes3017346880329lgwa02519791:24000
Burbank loamy fine sand, 0 to 15 percent slopesBbC10397695082bb6wa60519651:20000
Burbank rocky loamy fine sand, basalt substratum, 0 to 30 percent slopesBfE7153695112bb9wa60519651:20000
Burbank loamy fine sand, basalt substratum, 0 to 30 percent slopesBdE4931695102bb8wa60519651:20000
Burbank loamy fine sand, 0 to 2 percent slopesBbA3940695072bb5wa60519651:20000
Burbank loamy fine sand, gravelly substratum, 0 to 2 percent slopesBlA1461695122bbbwa60519651:20000
Burbank rocky loamy fine sand, 30 to 65 percent slopesBkF1048695142bbdwa60519651:20000
Burbank loamy fine sand, 2 to 15 percent slopesBbD807695092bb7wa60519651:20000
Burbank loamy fine sand, gravelly substratum, 2 to 15 percent slopesBlD555695132bbcwa60519651:20000
Winchester-Burbank-Malaga complex, 30 to 60 percent slopes960441773512lh6wa63720081:24000
Sagehill-Burbank-Malaga complex, 30 to 60 percent slopes911356772912lf8wa63720081:24000
Winchester-Sagehill-Burbank complex, 5 to 30 percent slopes910183772902lf7wa63720081:24000
Winchester-Sagehill-Burbank complex, 5 to 30 percent slopes185502708542cqmwa68119941:24000
Sagehill-Burbank-Malaga complex, 30 to 60 percent slopes139363708052cp1wa68119941:24000
Burbank loamy fine sand, 0 to 5 percent slopes20610707652cmrwa68119941:24000

Map of Series Extent

Approximate geographic distribution of the BURBANK 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 .