Official Series Description


Lab Data Summary

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

There are insufficient data to create the lab data summary figure.


Water Balance

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

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

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Click the image to view it full size.

Competing Series

Soil series competing with MARIETTA 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 MARIETTA series and competing. Series are sorted according to hierarchical clustering of median values. Source: SSURGO map unit geometry and 1981-2010, 800m PRISM data .

There are insufficient data to create the annual climate figure.

Geomorphic description summaries for the MARIETTA 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 .

There are insufficient data to create the 2D hillslope position figure.

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.

There are insufficient data to create the 3D flats position figure.

Soil series sharing subgroup-level classification with MARIETTA, 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. MS-2012-02-06-10 | Prentiss County - October 1997

    Typical pattern of soils and parent material in the Leeper-Marietta-Catalpa general soil map unit (Soil Survey of Prentiss County, Mississippi; October 1997).

Map Units

Map units containing MARIETTA 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
Leeper-Marietta complex, 0 to 2 percent slopes, occasionally floodedLaA218015328721ng2hal04120051:24000
Iuka-Marietta complex, 0 to 2 percent slopes, frequently floodedImA86015329981ng6kal04120051:24000
Marietta and Leeper soilsMr13267329681c21wal06320131:
Leeper-Marietta complex, 0 to 2 percent slopes, occasionally floodedLmA2214225149262qdhgal08520111:24000
Iuka-Marietta complex, 0 to 2 percent slopes, frequently floodedImA276825146502qcwkal08520111:24000
Mixed local alluvial landMc6923330933c3c8al10119581:20000
Mixed alluvial landMb4191330932c3c7al10119581:20000
Marietta fine sandy loam, occasionally flooded40125023179374lyn3ar01919831:20000
Marietta loam, occasionally flooded206482565645lzlmar05719761:20000
Marietta loam, 0 to 2 percent slopes, occasionally flooded4012915429191nsjlar10920051:20000
Marietta fine sandy loamMa13013331892c4c6ms01719691:20000
Robinsonville and Marietta soilsRm3557331903c4ckms01719691:20000
Marietta loam, 0 to 2 percent slopes, occasionally floodedMr32063324742w6fjms05719751:20000
Marietta silt loamMr6055332635c545ms06119741:20000
Marietta loam, 0 to 2 percent slopes, occasionally floodedMr203233330202w6fjms08119681:20000
Marietta loam, occasionally floodedMe3985333429c5ysms10319831:20000
Marietta fine sandy loamMt8421333497c60zms10519681:20000
Marietta loam, 0 to 2 percent slopes, occasionally floodedMe66663337062w6fjms11519691:20000
Marietta fine sandy loam, occasionally floodedMr5738333816c6c8ms11719951:24000
Marietta loam, 0 to 2 percent slopes, occasionally floodedMr24043342612w6fjms14519751:20000
Marietta fine sandy loam, frequently floodedMf2645575225m9kntx00519841:24000
Marietta fine sandy loam, occasionally floodedMe2555575224m9kmtx00519841:24000
Marietta clay loamId13037575340m9pctx07319491:20000
Marietta soils, frequently flooded3818597575648mb09tx34719761:24000
Marietta fine sandy loamMr11454575700mb1ztx36519711:20000

Map of Series Extent

Approximate geographic distribution of the MARIETTA 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 .