Official Series Description


Lab Data Summary

Aggregate lab data for the KYBURZ soil series. This aggregation is based on all pedons with a current taxon name of KYBURZ, 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 KYBURZ 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 KYBURZ 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 KYBURZ 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 KYBURZ 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 KYBURZ 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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Click the image to view it full size.

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

Competing Series

Soil series competing with KYBURZ 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 KYBURZ series and competing. Series are sorted according to hierarchical clustering of median values. Source: SSURGO map unit geometry and 1981-2010, 800m PRISM data .

There are insufficient data to create the annual climate figure.

Geomorphic description summaries for the KYBURZ 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.

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 KYBURZ, 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 KYBURZ 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
Aldi-Kyburz-Rock outcrop complex, 30 to 75 percent slopesKRG80832330912zmrhca61419671:24000
Rock outcrop-Franktown-Kyburz complex, 50 to 75 percent slopesRAG41532331052zmrqca61419671:24000
Trojan-Sattley-Kyburz complex, 30 to 50 percent slopesTTF40932331232zms0ca61419671:24000
Kyburz-Trojan complex, 9 to 30 percent slopesFUE25032330652zmr3ca61419671:24000
Kyburz-Aldi complex, 2 to 30 percent slopesKME20732330852zmrdca61419671:24000
Kyburz-Aldi complex, 30 to 50 percent slopesKMF18632330872zmrfca61419671:24000
Delleker-Kyburz-Trojan complex, 2 to 30 percent slopesDLE9832330632zmr2ca61419671:24000
Kyburz-Rock outcrop-Trojan complex, 2 to 30 percent slopesKRE4832330892zmrgca61419671:24000
Kyburz-Trojan complex, 30 to 50 percent slopesFUF2932330672zmr4ca61419671:24000
Aldi-Kyburz-Rock outcrop complex, 30 to 75 percent slopesKRG1849132330902zmrhca71919821:24000
Kyburz-Trojan complex, 9 to 30 percent slopesFUE1548232330642zmr3ca71919821:24000
Kyburz-Aldi complex, 2 to 30 percent slopesKME1147932330842zmrdca71919821:24000
Kyburz-Trojan complex, 30 to 50 percent slopesFUF1066532330662zmr4ca71919821:24000
Kyburz-Aldi complex, 30 to 50 percent slopesKMF970132330862zmrfca71919821:24000
Aldi-Kyburz complex, 2 to 30 percent slopesARE9694464608hlgcca71919821:24000
Rock outcrop-Franktown-Kyburz complex, 50 to 75 percent slopesRAG599832331042zmrqca71919821:24000
Kyburz-Rock outcrop-Trojan complex, 30 to 50 percent slopesKRF4975464725hll4ca71919821:24000
Kyburz-Rock outcrop-Trojan complex, 2 to 30 percent slopesKRE472732330882zmrgca71919821:24000
Trojan-Sattley-Kyburz complex, 30 to 50 percent slopesTTF369232331222zms0ca71919821:24000
Kyburz-Trojan-Sierraville complex, 2 to 9 percent slopesFUC3243464663hlj4ca71919821:24000
Aldi variant-Kyburz-Jorge variant complex, 2 to 30 percent slopesCRE2601464628hlh0ca71919821:24000
Sierraville-Trojan-Kyburz complex, 2 to 30 percent slopesSIE2534464793hlnbca71919821:24000
Jorge variant-Kyburz complex, 2 to 30 percent slopesXXE2390464844hlpzca71919821:24000
Aldi-Aquolls-Kyburz complex, 2 to 9 percent slopesKPC2368464723hll2ca71919821:24000
Trojan-Sattley-Kyburz complex, 2 to 30 percent slopesTTE2345464813hlnzca71919821:24000
Delleker-Kyburz-Trojan complex, 2 to 30 percent slopesDLE169232330622zmr2ca71919821:24000
Kyburz-Trojan complex, 2 to 30 percent slopes, alteredFUE51611464665hlj6ca71919821:24000
Kyburz-Aldi complex, 30 to 50 percent slopes, erodedKMF21591464722hll1ca71919821:24000
Kyburz-Aldi variant-Jorge variant complex, 2 to 30 percent slopesXCE1540464840hlpvca71919821:24000
Aldi-Kyburz-Rock outcrop comlex, 30 to 75 percent slopes, erodedKRG21093464728hll7ca71919821:24000
Kyburz-Aldi variant-Jorge variant complex, 30 to 50 percent slopesXCF946464841hlpwca71919821:24000
Jorge variant-Kyburz complex, 30 to 50 percent slopesXXF865464845hlq0ca71919821:24000
Kyburz loam, 2 to 9 percent slopesULC783464820hlp6ca71919821:24000
Cinder land-Sierraville-Kyburz complex, 30 to 50 percent slopesCIF741464621hlgsca71919821:24000
Kyburz-Rock outcrop-Trojan complex, 30 to 50 percent slopes, erodedKRF2610464726hll5ca71919821:24000
Aldi variant-Kyburz-Jorge variant complex, 30 to 50 percent slopesCRF537464629hlh1ca71919821:24000
Kyburz-Aldi complex, 2 to 30 percent slopes, alteredKME5440464720hlkzca71919821:24000
Kyburz-Trojan-Aquolls complex, 2 to 30 percent slopesKVE282464729hll8ca71919821:24000
Kyburz-Trojan complex, 30 to 50 percent slopes, terracedFUF656464667hlj8ca71919821:24000

Map of Series Extent

Approximate geographic distribution of the KYBURZ 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 .