Official Series Description


Lab Data Summary

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

Click the image to view it full size.

Pedons used in the lab summary:

MLRALab IDPedon IDTaxonnameCINSSL / NASIS ReportsLink To SoilWeb GMap
133AS86AL-087-386AL087003-pgmAnnemaine2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties32.4455556,-85.8972222
133AS86AL-105-486AL105004-pgmAnnemaine3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties32.5569444,-87.22
133AS88AL-091-288AL091002-pgmAnnemaine3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties32.4308333,-88.0047222
133AS89AL-023-289AL023002-pgmAnnemaine3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties32.2052778,-88.0255556

Water Balance

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

Click the image to view it full size.



Click the image to view it full size.

Sibling Summary

Siblings are those soil series that occur together in map units, in this case with the ANNEMAINE series. Sketches are arranged according to their subgroup-level taxonomic structure. Source: SSURGO snapshot , parsed OSD records and snapshot of SC database .

Click the image to view it full size.

Select annual climate data summaries for the ANNEMAINE series and siblings. 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 ANNEMAINE 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 .

Click the image to view it full size.

Click the image to view it full size.

There are insufficient data to create the 3D mountains figure.

Click the image to view it full size.

Click the image to view it full size.

Competing Series

Soil series competing with ANNEMAINE share the same family level classification in Soil Taxonomy. Source: parsed OSD records and snapshot of the SC database .

Click the image to view it full size.

Select annual climate data summaries for the ANNEMAINE 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 ANNEMAINE 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 .

Click the image to view it full size.

Click the image to view it full size.

There are insufficient data to create the 3D mountains figure.

Click the image to view it full size.

Click the image to view it full size.

Soil series sharing subgroup-level classification with ANNEMAINE, 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

Click a link below to display the diagram. Note that these diagrams may be from multiple survey areas.

  1. AL-2010-02-25-02 | Wilcox County - March 1999

    Generalized patterns of soils, geomorphology, and landscape relationships in the Urbo-Mooreville-Una, Annemaine-Izagora-Lenoir, Luverne-Halso, Arundel-Cantuche, and Bama-Malbis-Luverne general soil map units along the Alabama River in the central part of Wilcox County (Soil Survey of Wilcox County, Alabama; 1999).

Map Units

Map units containing ANNEMAINE 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
Annemaine-Wahee complex, 0 to 2 percent slopes, rarely floodedAwA8450328251c0kral00520011:24000
Annemaine silt loam, 0 to 2 percent slopes, rarely floodedAnA126022302472dvrgal00720071:24000
Annemaine silt loam, 2 to 5 percent slopes, rarely floodedAnB2022302482dvrhal00720071:24000
Annemaine silt loam, 0 to 2 percent slopes, rarely floodedAnA3420328572c0x3al02319981:24000
Annemaine-Wahee complex, 0 to 2 percent slopes, rarely floodedAnA3826608132ndt5al06920021:24000
Annemaine fine sandy loam, 0 to 2 percent slopes, rarely floodedAnA953525146012svnqal08520111:24000
Annemaine fine sandy loam, 2 to 5 percent slopes, rarely floodedAnB284825146022qcv1al08520111:24000
Annemaine-Cahaba complex, 5 to 12 percent slopes, occasionally floodedAcD173129950712x5rgal09720181:24000
Annemaine fine sandy loam, 0 to 3 percent slopes, rarely floodedAnB288533100930wk2al10119581:20000
Anthroportic Udorthents-Urban land-Annemaine complex, 0 to 2 percent slopesAuA61531162762z478al10119581:20000
Annemaine-Anthroportic Udorthents complex, 0 to 3 percent slopes, rarely floodedAnB52131162752z477al10119581:20000
Annemaine silt loam, 0 to 2 percent slopes, rarely floodedAnA10820331224c3nnal10519961:24000
Annemaine loam, 0 to 2 percent slopes, occasionally floodedAnA4490331274c3q8al10719971:24000
Annemaine fine sandy loam, 0 to 2 percent slopes, rarely floodedAnA26003313602svnqal11319971:24000
Annemaine sandy loam, 0 to 2 percent slopes, occasionally floodedAnA25985331470c3xlal11919861:24000
Annemaine-Cahaba complex, 5 to 12 percent slopes, occasionally floodedAcD198426420462x5rgal12920131:24000
Annemaine fine sandy loam, 0 to 2 percent slopes, rarely floodedAaA114126420452rjqfal12920131:24000
Annemaine fine sandy loam, 0 to 2 percent slopes, occasionally floodedAnA8200331634c42wal13119971:24000
Annemaine fine sandy loam, 2 to 5 percent slopes, occasionally floodedAnB6920331635c42xal13119971:24000
Flint fine sandy loam, loamy substratum, 0 to 2 percent slopes (annemaine)FfA521331992c4gfms02319631:15840
Flint fine sandy loam, loamy substratum, 2 to 5 percent slopes (annemaine)FfB407331993c4ggms02319631:15840
Annemaine fine sandy loam, 2 to 5 percent slopes, rarely floodedAnB241226421542rrxcms04120121:24000
Annemaine fine sandy loam, 0 to 2 percent slopes, rarely floodedAnA179026421532rrxbms04120121:24000
Annemaine silt loam, occasionally flooded223270332711c56mms06719841:20000
Annemaine fine sandy loam, 0 to 2 percent slopes, rarely floodedAa1650332873301jzms07519801:20000
Annemaine loamAn678333051c5klms08719771:20000
Cahaba-Annemaine complex, 0 to 2 percent slopes, rarely floodedCa15239333601c64bms11119971:20000
Annemaine fine sandy loam, 0 to 2 percent slopes, rarely floodedAn582334039c6lgms12919971:20000
Annemaine loam, occasionally flooded1615334080c6msms13119971:24000
Annemaine fine sandy loam, 0 to 2 percent slopes, rarely floodedAnA588124034292lnyzms15320081:24000

Map of Series Extent

Approximate geographic distribution of the ANNEMAINE 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 .