Official Series Description


Lab Data Summary

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

Soil series competing with CUBLAKE 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 CUBLAKE 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 CUBLAKE 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.

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

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

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Soil series sharing subgroup-level classification with CUBLAKE, 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 CUBLAKE 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
Cublake sand, 0 to 6 percent slopes26B24941903006d0qmi00119931:20000
Cublake sand, 0 to 6 percent slopes26B12101918096fldmi06919951:15840
Cublake sand, 0 to 6 percent slopes26B11451906976dfjmi07919981:12000
Cublake sand, 0 to 6 percent slopes26B2241352834kmi13520031:12000
Cublake sand, 0 to 6 percent slopes26B4511909766dqjmi14319991:12000
Cublake sand, 0 to 6 percent slopes219B16614570381kx57mi15320071:24000
Cublake-Croswell-Ashwabay complex, 0 to 6 percent slopes705B472014444771kh31wi00320061:12000
Cublake-Croswell-Ashwabay complex, 6 to 15 percent slopes705C103414444781kh32wi00320061:12000
Cublake-Keweenaw, stony complex, 0 to 6 percent slopes1385B26017116851vg4nwi00320061:12000
Cublake loamy sand, 0 to 3 percent slopes905A2116019001qrx6wi00320061:12000
Cublake-Croswell-Ashwabay complex, 0 to 6 percent slopes705B19726433296gjw9wi00720051:12000
Cublake-Croswell-Ashwabay complex, 6 to 15 percent slopes705C9731433299gjwdwi00720051:12000
Cublake-Keweenaw, stony, complex, 0 to 6 percent slopes1385B1111114744017j06wi00720051:12000
Cublake loamy sand, 0 to 3 percent slopes905A1639781521v77cwi03120051:12000
Cublake-Croswell-Ashwabay complex, 0 to 6 percent slopes705B147214876501ly0qwi03120051:12000
Cublake loamy sand, 0 to 3 percent slopesCuA1571429996gffvwi03719951:12000
Cublake loamy sand, 0 to 4 percent slopesCuA8154298352tnxtwi04119951:12000
Cublake-Croswell-Ashwabay complex, 0 to 6 percent slopes705B184616977081tzlswi05120061:12000
Cublake-Croswell-Ashwabay complex, 6 to 15 percent slopes705C130516977091tzltwi05120061:12000
Cublake loamy sand, 0 to 4 percent slopes905A56117012652tnxtwi05120061:12000
Cublake-Keweenaw, stony complex, 0 to 6 percent slopes1385B7417012381v38nwi05120061:12000
Cublake loamy sand, 0 to 4 percent slopesCsB66744316132tnxtwi06919931:20000
Cublake loamy sand, 0 to 4 percent slopesCsA50604210822tnxtwi08519881:20000
Cublake loamy sand, 0 to 4 percent slopes905A2176398992tnxtwi09920061:12000
Cublake loamy sand, 0 to 3 percent slopes905A957626799p17bwi11320061:12000
Cublake loamy sand, 0 to 4 percent slopesCsA25184212332tnxtwi12519851:20000
Cublake loamy sand, 0 to 3 percent slopes905A214448525h1qkwi12920021:12000

Map of Series Extent

Approximate geographic distribution of the CUBLAKE 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 .