Official Series Description


Lab Data Summary

Aggregate lab data for the TINTON soil series. This aggregation is based on all pedons with a current taxon name of TINTON, 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 TINTON 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
149A92P048192NJ005008Tinton6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties40.1294441,-74.6030579
149A92P049392NJ033005Tinton6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties39.6969452,-75.3327789
149A92P049692NJ033008Tinton6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties39.7244453,-75.4052811

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the TINTON 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 TINTON 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 TINTON 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 TINTON 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 TINTON 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 TINTON 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 TINTON 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 TINTON, 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 TINTON 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
Tinton loamy sand, 2 to 5 percent slopesTsB5701378304mf4md00320031:12000
Tinton loamy sand, 5 to 10 percent slopesTsC5391378314mf5md00320031:12000
Tinton-Urban land complex, 5 to 10 percent slopesTuC2281378334mf7md00320031:12000
Tinton-Urban land complex, 0 to 5 percent slopesTuB1471378324mf6md00320031:12000
Tinton sand, thick surface, 0 to 5 percent slopesThftB3676697887rf6hnj00519671:24000
Tinton sand, 0 to 5 percent slopesThfB2127697885rf6fnj00519671:24000
Tinton sand, 5 to 10 percent slopesThfC330697886rf6gnj00519671:24000
Tinton-Urban land complex, 0 to 5 percent slopesThhB27433473632ztycnj00719641:12000
Tinton sand, 0 to 5 percent slopesThfB151710903rvrcnj00719641:12000
Tinton sand, 0 to 5 percent slopesThfB454108957215kshnj01520041:24000
Tinton loamy sand, 0 to 5 percent slopesThgB6981352194jpxnj02119691:24000
Tinton loamy sand, 0 to 5 percent slopesThgB2871354504jycnj02319851:24000
Tinton loamy sand, 0 to 5 percent slopesThgB103111348154j8wnj02519851:24000
Tinton-Urban land complex, 0 to 5 percent slopesThhB57721348184j8znj02519851:24000
Tinton loamy sand, 5 to 10 percent slopesThgC41961348164j8xnj02519851:24000
Tinton loamy sand, 10 to 25 percent slopesThgE20271348174j8ynj02519851:24000
Tinton sand, 0 to 5 percent slopesThfB608697547rdvjnj02919781:24000
Tinton loamy sand, 0to 5 percent slopesThgB527697618rdxtnj02919781:24000

Map of Series Extent

Approximate geographic distribution of the TINTON 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 .