Official Series Description


Lab Data Summary

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

Soil series competing with KILBURN 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 KILBURN 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 KILBURN 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 terrace figure.

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

Soil series sharing subgroup-level classification with KILBURN, 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 KILBURN 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
Olete-Kilburn-Etsel families complex, 50 to 80 percent slopes420af1432562681hm79ca69620161:24000
Bairs-Kilburn family complex, 8 to 30 percent slopes125bo405322291102dtksca73219981:24000
Kilburn family, 5 to 30 percent slopes.3482839471461htlfca73219981:24000
Kilburn family-Watterson-Watterson wet association, 4 to 30 percent slopes227bo190022291532dtm5ca73219981:24000
Kilburn-Nanamkin families association, 5 to 15 percent slopes.3551868471468htlnca73219981:24000
Kilburn-Nanamkin families association, 15 to 30 percent slopes.356912471469htlpca73219981:24000
Kilburn family-Watterson association, 4 to 15 percent slopes226bo39122291522dtm4ca73219981:24000
Kilburn family-Watterson-Xerofluvents association, 0 to 8 percent slopes228bo29922291542dtm6ca73219981:24000
Bairs-Kilburn family complex, 8 to 30 percent slopes125bo36122300492dvk2ca74019961:24000
Kilburn family-Watterson-Watterson wet association, 4 to 30 percent slopes227bo19922300532dvk6ca74019961:24000
Kilburn family, 5 to 30 percent slopes.348iw6222300302dvjgca74019961:24000
Kilburn-Wrentham-Supan families association, 30 to 60 percent slopes1157152465276hm4xca77219811:24000
Los Gatos-Kilburn-Panamint families association, 30 to 60 percent slopes2141788465287hm58ca77219811:24000
Kilburn-Wrentham-Supan families association, 10 to 30 percent slopes1033534465275hm4wca77219811:24000
Oak Glen-Wrentham-Kilburn families complex, 30 to 60 percent slopes3727787465304hm5tca77219811:24000
Los Gatos-Kilburn-Panamint families association, 10 to 30 percent slopes2019884465286hm57ca77219811:24000
Olete-Kilburn-Etsel families complex, 50 to 80 percent slopes4207580465350hm79ca77619811:24000
Olete-Kilburn-Goulding families complex, 30 to 50 percent slopesSgF4748779906v5k8ca77619811:24000
Olete-Kilburn families, moderately deep-Mollic Haploxeralfs, cool complex, 40 to 70 percent slopes6243790465365hm7sca77619811:24000
Olete-Kilburn-Goulding families complex, 30 to 50 percent slopesSgF6075471670htt5ca77719811:24000
Bairs-Kilburn family complex, 8 to 30 percent slopes1252552488018jctjca80219961:24000
Kilburn family-Watterson association, 4 to 15 percent slopes226562488149jcyrca80219961:24000
Kilburn family-Watterson-Watterson wet association, 4 to 30 percent slopes227459488151jcytca80219961:24000
Kilburn family-Watterson-Xerofluvents association, 0 to 8 percent slopes228371488153jcywca80219961:24000
Kilburn gravelly loam, 1 to 3 percent slopesKoB2916481405j4y6ut60219691:20000
Kilburn gravelly sandy loam, 3 to 6 percent slopesKnC1444481400j4y1ut60219691:20000
Kilburn gravelly sandy loam, 30 to 60 percent slopesKnG1195481404j4y5ut60219691:20000
Kilburn gravelly sandy loam, 6 to 10 percent slopesKnD585481401j4y2ut60219691:20000
Kilburn gravelly sandy loam, 10 to 20 percent slopesKnE470481402j4y3ut60219691:20000
Kilburn gravelly sandy loam, 20 to 30 percent slopesKnF406481403j4y4ut60219691:20000
Kilburn-Francis association, 30 to 50 percent slopes, erodedKFG25594481581j53wut60719651:15840
Kilburn gravelly sandy loam, deep over clean sands, 0 to 3 percent slopesKmA2329481598j54fut60719651:15840
Kilburn cobbly sandy loam, 10 to 20 percent slopes, erodedKlE22104481597j54dut60719651:15840
Kilburn gravelly sandy loam, 6 to 10 percent slopesKgD1901481594j549ut60719651:15840
Kilburn gravelly sandy loam, 10 to 20 percent slopes, erodedKgE21293481595j54but60719651:15840
Kilburn cobbly sandy loam, 3 to 10 percent slopesKlC937481596j54cut60719651:15840
Kilburn gravelly sandy loam, 3 to 6 percent slopesKgC932481593j548ut60719651:15840
Kilburn sandy loam, 0 to 1 percent slopesKbA912481588j543ut60719651:15840
Kilburn-Francis association, 10 to 20 percent slopes, erodedKFE2368481579j53tut60719651:15840
Kilburn gravelly sandy loam, deep over clean sands, 3 to 10 percent slopesKmC289481599j54gut60719651:15840
Kilburn gravelly sandy loam, 1 to 3 percent slopesKgB284481592j547ut60719651:15840
Kilburn stony sandy loam, 0 to 3 percent slopesKcA224481591j546ut60719651:15840
Kilburn-Francis association, 20 to 30 percent slopes, erodedKFF2106481580j53vut60719651:15840
Kilburn sandy loam, 3 to 6 percent slopesKbC93481590j545ut60719651:15840
Kilburn sandy loam, 1 to 3 percent slopesKbB86481589j544ut60719651:15840
Kilburn gravelly sandy loam, 2 to 10 percent slopes367949482141j5pyut61119921:24000
Kilburn very gravelly sandy loam, 30 to 50 percent slopes, erodedKNG21976483312j6xqut62119661:20000
Kilburn stony sandy loam, 3 to 15 percent slopesKOD671483313j6xrut62119661:20000
Kilburn gravelly fine sandy loam, 15 to 30 percent slopes, erodedKRE2592483314j6xsut62119661:20000

Map of Series Extent

Approximate geographic distribution of the KILBURN 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 .