Official Series Description


Lab Data Summary

Aggregate lab data for the MAUBILA soil series. This aggregation is based on all pedons with a current taxon name of MAUBILA, 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 MAUBILA 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
133AS89AL-105-489AL105004-pgmMaubila3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties32.8283333,-87.13
133AS89AL-105-589AL105005-pgmMaubila3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties32.8186111,-87.0694444

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the MAUBILA 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 MAUBILA 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 MAUBILA 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 MAUBILA 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 MAUBILA 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 MAUBILA 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 MAUBILA 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 MAUBILA, 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 MAUBILA 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
Smithdale-Maubila-Boykin complex, 15 to 35 percent slopesSmE2321331162132z471al00119721:20000
Smithdale-Maubila-Boykin complex, 8 to 15 percent slopesSmD892131162142z472al00119721:20000
Cowarts-Maubila complex, 15 to 25 percent slopes, flaggyCmE42830328228c0k0al00520011:24000
Cowarts-Maubila Complex, 8 to 15 percent slopes, flaggyCmD18130328225c0jxal00520011:24000
Maubila-Smithdale complex, 15 to 35 percent slopesMsF4854022325492s69wal00720071:24000
Maubila-Smithdale-Boykin complex, 5 to 20 percent slopesMsD1527522329852dylsal00720071:24000
Maubila flaggy loam, 2 to 8 percent slopes, erodedMkC2749022325452svnwal00720071:24000
Maubila-Smithdale complex, 35 to 45 percent slopesMsG525522326752dy8sal00720071:24000
Maubila-Smithdale complex, 15 to 35 percent slopesMsE12231161982s69wal02119671:20000
Maubila-Wadley-Smithdale complex, 8 to 30 percent slopesMbF49630600074n4f7al02520041:24000
Olla-Maubila complex, 2 to 8 percent slopesOmC12530600075n4f8al02520041:24000
Smithdale-Luverne-Maubila complex, 15 to 35 percent slopesCuE494833295532sh52al05919621:15840
Maubila-Smithdale complex, 15 to 35 percent slopesMsF95213297682s69wal06520031:24000
Maubila-Smithdale-Boykin complex, 5 to 20 percent slopesMsD5513329767c24nal06520031:24000
Maubila flaggy loam, 2 to 8 percent slopes, erodedMkC233343297662svnwal06520031:24000
Maubila-Smithdale complex, 35 to 45 percent slopesMsG1162725099sbj9al06520031:24000
Smithdale-Luverne-Maubila complex, 15 to 35 percent slopesSmE13460024948342psg3al07520101:24000
Maubila flaggy fine sandy loam, 2 to 8 percent slopesMbC298624945532psfral07520101:24000
Smithdale-Luverne-Maubila complex, 15 to 35 percent slopesSsE281624948372sh52al07520101:24000
Maubila-Olla-Rattlesnake Forks complex, 8 to 35 percent slopes, moderately erodedMbF24709029950592x5s7al09720181:24000
Maubila-Smithdale complex, 15 to 35 percent slopesMsE358903312422s69wal10519961:24000
Maubila flaggy loam, 2 to 8 percent slopes, erodedMkC244703312412svnwal10519961:24000
Saffell-Maubila complex, 2 to 5 percent slopesSbB1580331251c3pjal10519961:24000
Smithdale-Luverne-Maubila complex, 15 to 35 percent slopesSnF1945903312862sh52al10719971:24000
Maubila-Olla-Rattlesnake Forks complex, 8 to 35 percent slopes, moderately erodedMbF22832326421092x5s7al12920131:24000
Maubila-Olla-Rattlesnake Forks complex, 2 to 8 percent slopesMbC984626421082rjsjal12920131:24000
Notcher-Maubila complex, 8 to 12 percent slopes69596014253741jv6tfl03319981:24000
Notcher-Maubila complex, 2 to 5 percent slopes67116014253721jv6rfl03319981:24000
Notcher-Maubila complex, 5 to 8 percent slopes6890014253731jv6sfl03319981:24000
Nankin-Cowarts-Maubila complex, 15 to 45 percent slopesNmF2221524253872svnhga25920091:12000
Cowarts-Maubila-Ailey complex, 5 to 15 percent slopesCyD88524253432mdrwga25920091:12000
Nankin-Cowarts-Maubila complex, 15 to 45 percent slopesNmF2738516050992svnhga65820051:24000
Maubila-Olla-Rattlesnake forks complex, 35 to 60 percent slopesMbG676726422162rs2rms04120121:24000
Maubila-Olla-Rattlesnake Forks complex, 8 to 35 percent slopes, moderately erodedMbF2213826422152x5s7ms04120121:24000
Maubila-Olla-Rattlesnake forks complex, 2 to 8 percent slopesMbC33326422142rs2pms04120121:24000
Smithdale-Luverne-Maubila complex, 15 to 35 percent slopesRsF686173332032sh52ms09519631:15840
Maubila-Olla-Rattlesnake Forks complex, 8 to 35 percent slopesMbE216124034902lp0yms15320081:24000
Olla-Maubila complex, 2 to 8 percent slopesOmC48424034892lp0xms15320081:24000

Map of Series Extent

Approximate geographic distribution of the MAUBILA 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 .