Official Series Description


Lab Data Summary

Aggregate lab data for the TOWERVILLE soil series. This aggregation is based on all pedons with a current taxon name of TOWERVILLE, 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 TOWERVILLE 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 TOWERVILLE 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 TOWERVILLE 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 TOWERVILLE 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 TOWERVILLE 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 terrace figure.

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

Competing Series

Soil series competing with TOWERVILLE 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 TOWERVILLE 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 TOWERVILLE 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.

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 TOWERVILLE, 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 TOWERVILLE 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
Towerville silt loam, 25 to 35 percent slopes72E3289299969b24fny00320131:24000
Towerville silt loam, 15 to 25 percent slopes72D3064299968b24dny00320131:24000
Lordstown and Towerville soils, 35 to 60 percent slopes, extremely stony171F24862997972zffjny00320131:24000
Towerville silt loam, 35 to 50 percent slopes72F1450299970b24gny00320131:24000
Towerville silt loam, 8 to 15 percent slopes72C1101299967b24cny00320131:24000
Lordstown and Towerville soils, 15 to 25 percent slopes, extremely stony171D3362997952zffgny00320131:24000
Towerville silt loam, 3 to 8 percent slopes72B298299966b24bny00320131:24000
Lordstown and Towerville soils, 25 to 35 percent slopes, extremely stony171E2662997962zffhny00320131:24000
Towerville silt loam, 25 to 35 percent slopes72E55822896929qfxny00920021:24000
Towerville silt loam, 15 to 25 percent slopes72D32962896919qfwny00920021:24000
Towerville silt loam, 35 to 50 percent slopes72F32422896939qfyny00920021:24000
Towerville silt loam, 8 to 15 percent slopes72C26322896909qfvny00920021:24000
Towerville silt loam, 3 to 8 percent slopes72B17462896899qftny00920021:24000
Towerville silt loam, 35 to 50 percent slopesToF29112898879qn6ny01319881:15840
Towerville silt loam, 25 to 35 percent slopesToE17882898869qn5ny01319881:15840
Towerville silt loam, 8 to 15 percent slopesToC15562898849qn3ny01319881:15840
Towerville silt loam, 15 to 25 percent slopesToD9782898859qn4ny01319881:15840
Towerville silt loam, 3 to 8 percent slopesToB5212898839qn2ny01319881:15840
Lordstown-Manlius-Towerville complex, 35 to 80 percent slopes, extremely stony81F245031057082wzmbny05120191:24000
Lordstown-Manlius-Towerville complex, 25 to 35 percent slopes, extremely stony81E165831057072ywlwny05120191:24000
Towerville silt loam, 8 to 15 percent slopes87C32031057162y9wmny05120191:24000
Towerville silt loam, 15 to 25 percent slopes87D30831057172y9wnny05120191:24000
Towerville silt loam, 25 to 35 percent slopes87E16831057182y9wpny05120191:24000
Lordstown-Manlius-Towerville complex, 35 to 80 percent slopes, extremely stony171F912525042542wzmbny06920121:12000
Lordstown-Manlius-Towerville complex, 25 to 35 percent slopes, extremely stony171E397525042532ywlwny06920121:12000
Lordstown-Manlius-Towerville complex, 15 to 25 percent slopes, very stony171D184625042522ywlxny06920121:12000
Lordstown-Manlius-Towerville complex, 8 to 15 percent slopes, very stony171C26325124242zfflny06920121:12000
Towerville silt loam, 15 to 25 percent slopesTkD4242942909w77ny07719931:24000
Towerville silt loam, 3 to 8 percent slopesTkB3492942889w75ny07719931:24000
Towerville silt loam, 8 to 15 percent slopesTkC3122942899w76ny07719931:24000
Lordstown-Manlius-Towerville complex, 35 to 80 percent slopes, extremely stony171F358214078302wzmbny12319481:12000
Lordstown-Manlius-Towerville complex, 25 to 35 percent slopes, extremely stony171E242414078262ywlwny12319481:12000
Lordstown-Manlius-Towerville complex, 15 to 25 percent slopes, very stony171D102832504022ywlxny12319481:12000
Lordstown-Manlius-Towerville complex, 8 to 15 percent slopes, very stony171C44532504042zfflny12319481:12000
Towerville silt loam, 6 to 12 percent slopesToC91298920b11loh00720011:12000
Towerville silt loam, 12 to 18 percent slopesToD80298921b11moh00720011:12000
Towerville silt loam, 12 to 18 percent slopesToD12868609mhkoh08519761:15840
Towerville and Valois soils, 40 to 70 percent slopesTvF522626330812rg7tpa04920121:12000

Map of Series Extent

Approximate geographic distribution of the TOWERVILLE 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 .