Official Series Description


Lab Data Summary

Aggregate lab data for the TYSON soil series. This aggregation is based on all pedons with a current taxon name of TYSON, 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 TYSON 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
15UCD585202758-CA-52-027TYSON2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties39.8195839,-122.6833572
5UCD581201058-CA-12-010xTYSON2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties40.9913292,-123.7764969
5UCD621202762-CA-12-027xTYSON3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties40.9279518,-123.7775116

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the TYSON 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 TYSON 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 TYSON 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 TYSON 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 TYSON 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 TYSON 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 TYSON 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 flats position figure.

Soil series sharing subgroup-level classification with TYSON, 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 TYSON 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
Tyson gravelly loam, 30 to 50 percent slopesTtE861458888hdhvca02119611:20000
Tyson gravelly laom, shallow, 30 to 50 percent slopesTvE2741458891hdhyca02119611:20000
Tyson gravelly loam, deep, 10 to 30 percent slopesTuD253458889hdhwca02119611:20000
Tyson gravelly loam, deep, 30 to 50 percent slopesTuE73458890hdhxca02119611:20000
Tyson gravelly loam, shallow, 50 to 65 percent slopes, erodedTvF250458892hdhzca02119611:20000
Tyson-Neuns gravelly loams, 30 to 75 percent slopes240la1125048712q429ca02119611:20000
Tyson gravelly sandy loam, 30 to 50 percent slopesTyEte525069812q42lca02119611:20000
Tyson-Neuns gravelly loams, 30 to 75 percent slopes2401021459643hf96ca03319851:24000
Tyson very gravelly loam, 30 to 50 percent slopes, rocky371mnf1625048642q422ca03319851:24000
Tyson-Rock outcrop complex, 10 to 50 percent slopes372mnf825048622q420ca03319851:24000
Tyson-Rock outcrop, sedimentary complex, 40 to 75 percent slopes373mnf525048652q423ca03319851:24000
Tyson gravelly sandy loam, 30 to 50 percent slopesTyE5005460959hgnnca64519611:20000
Tyson gravelly sandy loam, 50 to 65 percent slopesTyF1763460960hgnpca64519611:20000
Tyson gravelly sandy loam, 10 to 30 percent slopesTyD184460958hgnmca64519611:20000
Neuns-Bluenose-Tyson complex, 50 to 75 percent slopes16811586461053hgrpca68719851:24000
Neuns-Bluenose-Tyson complex, 30 to 50 percent slopes16710929461052hgrnca68719851:24000
Tyson-Updegraff complex, 30 to 50 percent slopes, low ffd20557184610902xkb0ca68719851:24000
Tyson-Updegraff complex, 50 to 75 percent slopes2063424461091hgsxca68719851:24000
Shortyork-Tyson-Witherell complex, 30 to 50 percent slopes, MLRA 519621854610812wgq3ca68719851:24000
Tyson-Updegraff complex, 30 to 50 percent slopes, low ffd2166884657972xkb0ca69419931:24000
Shortyork-Tyson-Witherell complex, 30 to 50 percent slopes, MLRA 52005394657792wgq3ca69419931:24000
Tyson-Updegraff complex, 9 to 30 percent slopes215414465796hmppca69419931:24000
Neuns-Bluenose-Tyson complex, 30 to 50 percent slopes167em51317011411v35jca70119841:24000
Neuns-Bluenose-Tyson complex, 50 to 75 percent slopes168em3917011421v35kca70119841:24000
Tyson-Updegraff complex, 30 to 50 percent slopes, low ffd205em3917011492xkb0ca70119841:24000
Tyson very gravelly loam, 30 to 50 percent slopes, rocky371837027478152q1z8ca70920101:24000
Tyson-Rock outcrop complex, 10 to 50 percent slopes372619927478162q1z9ca70920101:24000
Tyson-Rock outcrop, sedimentary complex, 40 to 75 percent slopes373127527478172q1zbca70920101:24000
Neuns-Bluenose-Tyson complex, 50 to 75 percent slopes168me12622747848hgrpca70920101:24000
Tyson gravelly sandy loam, 30 to 50 percent slopesTyEte48227478932q415ca70920101:24000
Tyson very gravelly loam, deep, 10 to 40 percent slopes10343627477942q1ylca70920101:24000
Tyson-Neuns gravelly loams, 30 to 75 percent slopes240la26627478752q3rhca70920101:24000
Neuns-Bluenose-Tyson complex, 30 to 50 percent slopes167me2382747847hgrnca70920101:24000
Tyson-Updegraff complex, 30 to 50 percent slopes, low ffd205me6927478592xkb0ca70920101:24000
Shortyork-Tyson-Witherell complex, 30 to 50 percent slopes, MLRA 5196me4427478542wgq3ca70920101:24000
Tyson gravelly loam, 30 to 50 percent slopesTtEgl3127479092q41pca70920101:24000
Tyson gravelly sandy loam, 50 to 65 percent slopesTyFte1627478942q416ca70920101:24000
Tyson-Updegraff complex, 50 to 75 percent slopes206me22747860hgsxca70920101:24000

Map of Series Extent

Approximate geographic distribution of the TYSON 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 .