Official Series Description


Lab Data Summary

Aggregate lab data for the MOLLVILLE soil series. This aggregation is based on all pedons with a current taxon name of MOLLVILLE, 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 MOLLVILLE 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
133B93P077893TX616011SMollville6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties33.0786095,-94.2444153
133BS81TX225001S81TX225001Mollville6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties31.5356941,-95.1677704
133BS96TX315002S96TX315002Mollville5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties32.8256683,-94.4022522

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the MOLLVILLE 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 MOLLVILLE 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 MOLLVILLE 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 MOLLVILLE 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 MOLLVILLE 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 MOLLVILLE 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 MOLLVILLE 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 hills figure.

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

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

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Soil series sharing subgroup-level classification with MOLLVILLE, 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. TX-2012-03-19-06 | Angelina County - February 1988

    Typical pattern of soils and underlying material in the Besner-Mollville-Bienville map unit (Soil Survey of Angelina County, TX; 1988).

Map Units

Map units containing MOLLVILLE 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
Mollville-Besner complex, 0 to 1 percent slopes, frequently pondedMp94545752282tcprtx00519841:24000
Mollville loam, 0 to 1 percent slopesMoA195575227m9kqtx00519841:24000
Latch-Mollville, frequently ponded complex, 0 to 1 percent slopesLaA50555764442sb4xtx20319891:24000
Mollville-Besner complex, 0 to 1 percent slopes, frequently pondedMpA37265755372tcprtx22519941:24000
Mollville loam, 0 to 1 percent slopesMoA800575536m9wptx22519941:24000
Mollville-Besner complex, 0 to 1 percent slopes, frequently ponded4061925756512tcprtx34719761:24000
Mollville loam391344575649mb0btx34719761:24000
Latch-Mollville, frequently ponded complex, 0 to 1 percent slopesBm99585756892sb4xtx36519711:20000
Mollville-Besner complex, 0 to 1 percent slopes, frequently pondedMvA5725782342tcprtx40119931:24000
Mollville-Besner complex, 0 to 1 percent slopes, frequently pondedMpA50945757702tcprtx41920021:24000
Mollville-Besner complex, 0 to 1 percent slopes, frequently pondedMpA14845770892tcprtx45519991:24000
Mollville-Besner complex, 0 to 1 percent slopes, frequently pondedMpA378114793642tcprtx45720071:24000
Latch-Mollville, frequently ponded complex, 0 to 1 percent slopesLaA27685760592sb4xtx49919931:24000
Mollville loam, 0 to 1 percent slopesMoA863576063mbfptx49919931:24000
Latch-Mollville, frequently ponded complex, 0 to 1 percent slopesLaA71815761552sb4xtx60819811:24000
Mollville very fine sandy loam, 0 to 1 percent slopesMoA1621576159mbjstx60819811:24000
Besner-Mollville complex, gently undulatingBeB28824374413dklvtx61119801:20000
Latch-Mollville, frequently ponded complex, 0 to 1 percent slopesLmB137945765152sb4xtx61620041:24000
Mollville loam, 0 to 1 percent slopesMlA7050576522mbxhtx61620041:24000
Mollville-Kildare complex, 0 to 1 percent slopesMkA561576550mbydtx61620041:24000
Mollville-Besner complex, 0 to 1 percent slopes, frequently pondedMpA258018947982tcprtx61920071:24000

Map of Series Extent

Approximate geographic distribution of the MOLLVILLE 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 .