Official Series Description


Lab Data Summary

Aggregate lab data for the SUNBURST soil series. This aggregation is based on all pedons with a current taxon name of SUNBURST, 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 SUNBURST were used in the calculation. Source: KSSL snapshot . Methods used to assemble the KSSL snapshot used by SoilWeb / SDE

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Pedons used in the lab summary:

MLRALab IDPedon IDTaxonnameCINSSL / NASIS ReportsLink To SoilWeb GMap
5290P054390MT041001Sunburst6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties48.4968643,-109.8094482

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the SUNBURST 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 SUNBURST 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 SUNBURST 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 SUNBURST 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 SUNBURST 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 SUNBURST 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 SUNBURST 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.

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

Soil series sharing subgroup-level classification with SUNBURST, 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 SUNBURST 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
Sunburst-Neldore complex, 15 to 60 percent slopes974F43403441202t076mt04119941:24000
Sunburst clay loam, 15 to 60 percent slopes92F73513442802vytfmt05119921:24000
Sunburst-Kevin clay loams, 4 to 15 percent slopes92D40313442792sy80mt05119921:24000
Sunburst clay loam, 15 to 60 percent slopes13069323443282vytfmt05519811:24000
Sunburst-Neldore complex, 15 to 60 percent slopes1153023443052t076mt05519811:24000
Sunburst-Kevin clay loams, 4 to 15 percent slopes12922083443262sy80mt05519811:24000
Kevin-Sunburst clay loams, 2 to 8 percent slopes1288353443252vyt8mt05519811:24000
Sunburst-Neldore complex, 15 to 60 percent slopes222F207853451002t076mt10119921:24000
Sunburst-Bascovy-Neldore complex, 8 to 25 percent slopes222E87083450992vytcmt10119921:24000
Sunburst-Kevin clay loams, 4 to 15 percent slopes53D36693452122sy80mt10119921:24000
Sunburst clay loam, 15 to 60 percent slopes53F33033452142vytfmt10119921:24000
Sunburst-Neldore complex, 15 to 60 percent slopes611466963455802t076mt10519761:24000
Sunburst clay loam, 15 to 60 percent slopes60942743455792vytfmt10519761:24000
Sunburst-Kevin clay loams, 4 to 15 percent slopes59807423455772sy80mt10519761:24000
Elloam-Sunburst clay loam, 9 to 35 percent slopes918628345599clmcmt10519761:24000
Sunburst clay loam, 15 to 60 percent slopesSU131951469232vytfmt60019691:24000
Sunburst-Neldore complex, 15 to 60 percent slopes81473353465432t076mt60819761:24000
Sunburst-Neldore complex, 15 to 60 percent slopes974F334653470082t076mt61519921:24000
Sunburst-Lambeth complex, 25 to 70 percent slopes925F18173346980cn1xmt61519921:24000
Sunburst-Bascovy-Neldore complex, 8 to 25 percent slopes92E10993469822vytcmt61519921:24000
Sunburst-Neldore complex, 15 to 60 percent slopes1920F753963476202t076mt64119941:24000
Sunburst-Bascovy-Neldore complex, 8 to 25 percent slopes924E429543478082vytcmt64119941:24000
Sunburst clay loam, 15 to 60 percent slopes923F295673478072vytfmt64119941:24000
Sunburst-Kevin clay loams, 4 to 15 percent slopes921D291983478022sy80mt64119941:24000
Kevin-Sunburst clay loams, 2 to 8 percent slopes444C265543477242vyt8mt64119941:24000
Sunburst-Bascovy-Weingart complex, 2 to 8 percent slopes925C15532347810cnxpmt64119941:24000
Kevin-Sunburst very gravelly clay loams, 8 to 15 percent slopes446D5548347728cnv1mt64119941:24000
Sunburst-Kevin gravelly clay loams, 2 to 8 percent slopes923C4820347805cnxjmt64119941:24000
Sunburst-Neldore complex, 15 to 60 percent slopes161F78893483742t076mt65719901:24000

Map of Series Extent

Approximate geographic distribution of the SUNBURST 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 .