Official Series Description


Lab Data Summary

Aggregate lab data for the BURNETTE soil series. This aggregation is based on all pedons with a current taxon name of BURNETTE, 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 BURNETTE 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
48A40A3266S1975CO081014BURNETTE6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties40.2335815,-107.8326111

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the BURNETTE 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 BURNETTE 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 BURNETTE 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 BURNETTE 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 BURNETTE 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 BURNETTE 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 BURNETTE 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 BURNETTE, 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 BURNETTE 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
Owen Creek-Jerry-Burnette complex, 5 to 35 percent slopes834253496929jp2zco68419841:24000
Burnette clay loam, 3 to 40 percent slopes111337496833jnzwco68419841:24000
Owen Creek-Jerry-Burnette loams, 5 to 35 percent slopes5726846497009jp5kco68519791:24000
Bachus-Burnette family-Ticanot, very stony surface, complex, 15 to 50 percent slopes8381069127334482slrkid7131:24000
Bachus-Burnette family-Ticanot, very stony surface, complex, 15 to 50 percent slopes83818731634372slrkid7161:24000
Bachus-Burnette family-Ticanot, very stony surface, complex, 15 to 50 percent slopes83851228586452slrkid75819981:24000
Burnette-Burnette variant silty clay loams, 8 to 15 percent slopes362870342535chfjmt02719791:24000
Burnette-Burnette variant silty clay loams, 2 to 8 percent slopes351982342534chfhmt02719791:24000
Burnette silty clay loam, 2 to 8 percent slopes34581342533chfgmt02719791:24000
Burnette stony loam, hillyBP201101467704xqjmt60019691:24000
Doby-Burnette complex, hillyDH55381467944xr9mt60019691:24000
Burnette-Adel association, rollingBW45541467714xqkmt60019691:24000
Nettleton-Burnette association, undulatingNB29611468954xvkmt60019691:24000
Burnette loam, undulatingBu6511467834xqymt60019691:24000
Elispring-Skaggs-Burnette families, complex, 2 to 15 percent slopes1155D82930396712qbzgmt60219631:20000
Burnette-Doolittle complex, 4 to 15 percent slopes956D84025980082pgb6mt60520071:24000
Burnette-Doolittle complex, 15 to 35 percent slopes956E26825980092pgb7mt60520071:24000
Tiban, extremely bouldery-Rooset, very stony-Burnette complex, 8 to 45 percent slopes, landslides815F8924962902pdjqmt60520071:24000
Burnette-Adel complex, 15 to 50 percent slopes, landslides738F274925153842ppjfmt61220111:24000
Knep, stony-Philipsburg-Burnette complex, 8 to 35 percent slopes, landslides749E264724850142pdvrmt61220111:24000
Burnette-Rooset-Maciver, very stony complex, 4 to 35 percent slopes, landslides814E139724847482pdl5mt61220111:24000
Tiban, extremely bouldery-Rooset, very stony-Burnette complex, 8 to 45 percent slopes, landslides815F92124847032pdjqmt61220111:24000
Cowcoulee-Burnette family-Herakle family, stony, complex, 8 to 35 percent slopes1156E92830397222qbzhmt61319751:24000
Elispring-Skaggs-Burnette families, complex, 2 to 15 percent slopes1155D28630397212qbzgmt61319751:24000
Burnette-Rooset-Maciver, very stony complex, 4 to 35 percent slopes, landslides814E319524929632pdl5mt61420121:24000
Burnette-Doolittle complex, 15 to 35 percent slopes956E154724864242pgb7mt61420121:24000
Tiban, extremely bouldery-Rooset, very stony-Burnette complex, 8 to 45 percent slopes, landslides815F85525207472pdjqmt61420121:24000
Burnette-Doolittle complex, 4 to 15 percent slopes956D85524864232pgb6mt61420121:24000
Knep, stony-Philipsburg-Burnette complex, 8 to 35 percent slopes, landslides749E1725416362pdvrmt61420121:24000
Burnette-Adel complex, 15 to 50 percent slopes, landslides738F625416492ppjfmt61420121:24000
Cowcoulee-Burnette family-Herakle family, stony, complex, 8 to 35 percent slopes1156E697326322372qbzhmt6321:24000
Elispring-Skaggs-Burnette families, complex, 2 to 15 percent slopes1155D517526322362qbzgmt6321:24000
Gaylord-Burnette complex, 4 to 15 percent slopes4831821464724xdxmt63619831:24000
Cowcoulee-Burnette family-Herakle family, stony, complex, 8 to 35 percent slopes1156E14929796572qbzhmt63720141:24000
Adel-Burnette-Bynum complex, 4 to 35 percent slopes294E3943348547cppgmt65719901:24000
Adel-Burnette-Sebud complex, 4 to 35 percent slopes394E855348618cprrmt65719901:24000
Burnette-Lucky Star association1015311152053536ywy04319761:24000
Clayburn-Wallrock association1358341520565371wy04319761:24000
Burnette-Lucky Star association101223816471wdlswy61919711:24000
Clayburn-Wallrock association1381816474wdlwwy61919711:24000
Bachus-Burnette family-Ticanot, very stony surface, complex, 15 to 50 percent slopes83874328586642slrkwy62319711:20000
Burnette loam, 3 to 10 percent slopes126D14615792359b9wy65620081:24000
Groomer-Foxton-Burnette families, complex, 0 to 15 percent slopes171198151951533nwy66320121:24000
Burnette loam, 3 to 10 percent slopes1262374502991jwdjwy71319861:24000

Map of Series Extent

Approximate geographic distribution of the BURNETTE 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 .