Official Series Description


Lab Data Summary

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

Competing Series

Soil series competing with BOLOBIN 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 BOLOBIN 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 BOLOBIN 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 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 BOLOBIN, 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 BOLOBIN 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
Bolobin-Anatone complex, 0 to 15 percent slopes5980AO622831207431t16bor60720181:24000
Klickson-Bolobin-Anatone complex, 30 to 60 percent slopes5728CO605531205341r1gpor60720181:24000
Bolobin-Melhorn-Fivebeaver complex, 30 to 60 percent slopes5990CO539631202321nvhmor60720181:24000
Bolobin-Nibolob-Bocker complex, eolian, 0 to 15 percent slopes4922AE372131204851r140or60720181:24000
Bolobin-Nibolob complex, 15 to 30 percent slopes5986BO270331205941r2nvor60720181:24000
Bolobin-Anatone complex, 15 to 30 percent slopes5980BO253831205881r2nhor60720181:24000
Klickson-Bolobin-Fivebit complex, 15 to 30 percent slopes4977BE1854312078920bmfor60720181:24000
Nibolob-Bolobin complex, 15 to 30 percent slopes5982BO106331205901r2nkor60720181:24000
Nibolob-Bolobin-Fivebeaver complex, 0 to 15 percent slopes5979AO70731205871r2ngor60720181:24000
Olot-Bolobin-Fivebeaver complex, 30 to 60 percent slopes5984CO52831205921r2nnor60720181:24000
Nibolob-Bolobin complex, depositional, 0 to 15 percent slopes4925AD50731204861r141or60720181:24000
Bolobin-Melhorn complex, 0 to 15 percent slopes4946AO45731204931r18xor60720181:24000
Bolobin-Fivebeaver-Larabee complex, 0 to 15 percent slopes5985AO25431205931r2nsor60720181:24000
Bolobin-Melhorn complex, depositional, 15 to 30 percent slopes4946BD5631204941r18yor60720181:24000
Klicker-Fivebeaver-Bolobin complex, 30 60 percent slopes5010CO1631205171r1b7or60720181:24000
Bolobin-Melhorn complex, 0 to 15 percent slopes4946AO107331223061r18xor62620181:24000
Bolobin-Nibolob-Bocker complex, eolian, 0 to 15 percent slopes4922AE96731222981r140or62620181:24000
Klicker-Fivebeaver-Bolobin complex, 30 60 percent slopes5010CO50231223331r1b7or62620181:24000
Bolobin-Melhorn complex, depositional, 15 to 30 percent slopes4946BD18531223071r18yor62620181:24000
Bolobin-Anatone complex, 0 to 15 percent slopes5980AO6131224891t16bor62620181:24000
Anatone-Bolobin complex, 0 to 15 percent slopes1829AE3431222251qzzzor62620181:24000
Klickson-Bolobin-Fivebit complex, 15 to 30 percent slopes4977BE31312251720bmfor62620181:24000
Klickson-Bolobin-Anatone complex, 30 to 60 percent slopes5728CO1231223481r1gpor62620181:24000
Bolobin-Anatone complex, 15 to 30 percent slopes5980BO1031223731r2nhor62620181:24000
Nibolob-Bolobin complex, depositional, 0 to 15 percent slopes4925AD931222991r141or62620181:24000
Bolobin-Anatone complex, 0 to 15 percent slopes5980AO1824868611t16bor63120181:24000
Bolobin-Anatone complex, 0 to 15 percent slopes5980AO62231215371t16bor64819771:24000
Klickson-Bolobin-Fivebit complex, 15 to 30 percent slopes4977BE360312153820bmfor64819771:24000
Bolobin-Nibolob-Bocker complex, eolian, 0 to 15 percent slopes4922AE26731215241r140or64819771:24000
Bolobin-Anatone complex, 15 to 30 percent slopes5980BO5431215321r2nhor64819771:24000
Bolobin-Anatone complex, 0 to 15 percent slopes5980AO13631146832ygdkwa62319701:20000
Bolobin-Anatone complex, 0 to 15 percent slopes5980AO185131144992ygdkwa71420181:24000

Map of Series Extent

Approximate geographic distribution of the BOLOBIN 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 .