Official Series Description


Lab Data Summary

Aggregate lab data for the MOOREVILLE soil series. This aggregation is based on all pedons with a current taxon name of MOOREVILLE, 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 MOOREVILLE 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
133AS95AL-023-295AL023002-pgmMooreville3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties32.0936111,-88.0630556
133BS96TX067001S96TX067001Mooreville6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties33.0872536,-94.3375931

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the MOOREVILLE 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 MOOREVILLE 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 MOOREVILLE 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 MOOREVILLE 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 MOOREVILLE 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 MOOREVILLE 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 MOOREVILLE 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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Click the image to view it full size.

Soil series sharing subgroup-level classification with MOOREVILLE, 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 MOOREVILLE 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
Urbo-Mooreville-Una complex, 0 to 3 percent slopes, frequently floodedMn269883281742svnfal00319611:20000
Urbo-Mooreville-Una complex, 0 to 3 percent slopes, frequently floodedUrB302503285702svnfal02319981:24000
Urbo-Mooreville-Una complex, 0 to 3 percent slopes, frequently floodedUuB714303286452svnfal02520041:24000
Urbo-Mooreville-Una complex, 0 to 3 percent slopes, frequently floodedUrB362003297292svnfal06520031:24000
Kinston-Mooreville complex, 0 to 1 percent slopes, frequently floodedKmA46205330467c2w7al08719971:24000
Urbo-Una-Mooreville complex, 0 to 1 percent slopes, frequently floodedUvA18288330506c2xhal08719971:24000
Mooreville, Mantachie and Kinston soils, 0 to 2 percent slopes, frequently floodedMKA288303305882svnlal09119971:24000
Urbo-Mooreville-Una complex, 0 to 3 percent slopes, frequently floodedUuB267203306052svnfal09119971:24000
Urbo-Mooreville-Una complex, 0 to 3 percent slopes, frequently floodedUuB333329950322svnfal09720181:24000
Urbo-Mooreville-Una complex, 0 to 3 percent slopes, frequently floodedUrB135003312722svnfal10719971:24000
Urbo-Mooreville-Una complex, 0 to 2 percent slopes, frequently floodedUuA4390331352c3ssal11319971:24000
Mooreville silt loam, 0 to 2 percent slopesMvA7400331397c3v7al11519831:24000
Mooreville, Mantachie and Kinston soils, 0 to 2 percent slopes, frequently floodedMMK7664131216952svnlal11919861:24000
Mooreville, frequently flooded-Spadra, occasionally flooded complex, 0 to 3 percent slopesMsA7222331549c404al12719861:24000
Mooreville silt loam, 0 to 1 percent slopes, frequently floodedMoA2165331548c403al12719861:24000
Urbo-Mooreville-Una complex, 0 to 3 percent slopes, frequently floodedUuB3607626421442svnfal12920131:24000
Mooreville, Mantachie and Kinston soils, 0 to 2 percent slopes, frequently floodedMKA308403316662svnlal13119971:24000
Urbo-Mooreville-Una complex, 0 to 3 percent slopes, frequently floodedUuB292403316802svnfal13119971:24000
Mooreville, frequently flooded-Spadra, occasionally flooded complex, 0 to 3 percent slopesMsA310825248332qdnpal13320121:24000
Mooreville silt loam, 0 to 1 percent slopes, frequently floodedMoA51625155622qfdgal13320121:24000
Mooreville, Jena and Urbo soils, 0 to 3 percent slopes, frequently floodedMJU2917231216922z3t0ms03919671:20000
Urbo-Mooreville-Una complex, 0 to 3 percent slopes, frequently floodedUuB1421731216932svnfms03919671:20000
Urbo-Mooreville-Una complex, 0 to 3 percent slopes, frequently floodedUuB1126626422512svnfms04120121:24000
Buckatunna-Mooreville complex, gently undulating, rarely floodedBuB457126421692rrxxms04120121:24000
Kirkville, Mantachie and Mooreville soilsKT9362332463c4ymms05719751:20000
Urbo-Mooreville-Una complex, 0 to 3 percent slopes, frequently flooded4472758731216912svnfms05919971:24000
Mooreville, Jena and Urbo soils, 0 to 3 percent slopes, frequently flooded4461058431216902z3t0ms05919971:24000
Mooreville, Mantachie and Kinston soils, 0 to 2 percent slopes, frequently floodedMMK2689131216942svnlms06919911:20000
Mooreville loam, 0 to 2 percent slopes, occasionally floodedMo4033332769301jkms06919911:20000
Mooreville loam, occasionally floodedMo2807333430c5ytms10319831:20000
Kinston, Mantachie, and Mooreville soils, frequently floodedKM2359214015271j1dkms15919971:24000
Mooreville-Mantachie complex, frequently floodedMm17049576453mbv8tx20319891:24000
Mooreville soils, occasionally floodedMr8291374435dkmktx61119801:20000
Mooreville-Mantachie complex, frequently floodedMm23066576482mbw6tx61620041:24000

Map of Series Extent

Approximate geographic distribution of the MOOREVILLE 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 .