Official Series Description


Lab Data Summary

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

There are insufficient data to create the 2D hillslope position figure.

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

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

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 BUKREEK, 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 BUKREEK 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
Bukreek loam, 0 to 1 percent slopesBukA3667732282rhnjok05520051:24000
Bukreek loam, 1 to 3 percent slopesAcB56943632642rhnktx04519721:20000
Bukreek loam, 0 to 1 percent slopesAcA31373632632rhnjtx04519721:20000
Bukreek loam, 1 to 3 percent slopesBuB139823645762rhnktx10119691:20000
Bukreek loam, 0 to 1 percent slopesBuA128533645752rhnjtx10119691:20000
Bukreek loam, 3 to 5 percent slopesBuC16333645772y7bktx10119691:20000
Bukreek loam, 1 to 3 percent slopesOmB3099391939f4v6tx17919651:20000
Bukreek loam, 3 to 5 percent slopesOmC2603391940f4v7tx17919651:20000
Bukreek loam, 0 to 1 percent slopesOmA363391938f4v5tx17919651:20000
Bukreek loam, 1 to 3 percent slopesDuB20326367558dbgqtx21119671:20000
Bukreek loam, 3 to 5 percent slopesDuC12001367559dbgrtx21119671:20000
Bukreek loam, 0 to 1 percent slopesDuA1169367557dbgptx21119671:20000
Bukreek fine sandy loam, moist, 0 to 1 percent slopesCbA25783682272y7bjtx25319661:20000
Bukreek loam, 0 to 1 percent slopesAcA88193707132rhnjtx33519651:20000
Bukreek loam, 1 to 3 percent slopesAcB75523707142rhnktx33519651:20000
Bukreek loam, 1 to 3 percent slopesBuB44023708542rhnktx34519721:24000
Bukreek loam, 0 to 1 percent slopesBuA26523708532rhnjtx34519721:24000
Bukreek loam, 0 to 1 percent slopesAcA172253717632rhnjtx39919651:20000
Bukreek loam, 1 to 3 percent slopesAcB63653717642rhnktx39919651:20000
Bukreek loam, 1 to 3 percent slopesBuB30843722602rhnktx43319701:24000
Bukreek loam, gravelly substratum, 1 to 3 percent slopesBvB1048372262dhcgtx43319701:24000
Bukreek loam, gravelly substratum, 0 to 1 percent slopesBvA879372261dhcftx43319701:24000
Bukreek loam, 0 to 1 percent slopesBuA8023722592rhnjtx43319701:24000

Map of Series Extent

Approximate geographic distribution of the BUKREEK 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 .