Official Series Description


Lab Data Summary

Aggregate lab data for the TRUCKTON soil series. This aggregation is based on all pedons with a current taxon name of TRUCKTON, 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 TRUCKTON 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
4940A3927S1961CO039001Truckton6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties39.5508347,-104.4205551
67B40A3928S1959CO087007Truckton5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties40.0147209,-103.9625015
67B40A3929S1959CO087008Truckton4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties40.0755539,-103.9397202
67B06N0187S2006CO087961Truckton7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties40.1816406,-103.9132233

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the TRUCKTON 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 TRUCKTON 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 TRUCKTON 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 TRUCKTON 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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Competing Series

Soil series competing with TRUCKTON 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 TRUCKTON 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 TRUCKTON 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 mountains figure.

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Soil series sharing subgroup-level classification with TRUCKTON, 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 TRUCKTON 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
Truckton sandy loam, 0 to 3 percent slopesTuB15863940852yvrfco00119681:20000
Truckton loamy sand, 0 to 3 percent slopesTtB11508940832yvrlco00119681:20000
Blakeland-Truckton associationBt111629404834vtco00119681:20000
Truckton loamy sand, 3 to 5 percent slopesTtC9084339016331gjyco00119681:20000
Truckton sandy loam, 5 to 9 percent slopesTuD7326940872yvrhco00119681:20000
Truckton loamy sand, 5 to 9 percent slopesTtD4727339016431gjzco00119681:20000
Truckton sandy loam, 3 to 5 percent slopesTuC1604940862yvrgco00119681:20000
Bresser-Truckton sandy loams, 3 to 5 percent slopesBvC296959412134y5co00519711:20000
Bresser-Truckton sandy loams, 5 to 20 percent slopesBvE172649412234y6co00519711:20000
Bresser and Truckton soil, 3 to 9 slopes, erodedBwD278349412334y7co00519711:20000
Truckton loamy sand, 5 to 9 percent slopesTrD7186339016631gjzco00519711:20000
Truckton loamy sand, 3 to 5 percent slopesTrC5523339016531gjyco00519711:20000
Truckton loamy sand, 0 to 3 percent slopesTrB4023941672yvrlco00519711:20000
Truckton sandy loam, dry, 1 to 5 percent slopes19177691052723jjwco07320011:24000
Truckton sandy loam, dry, 5 to 9 percent slopes19234111052733jjxco07320011:24000
Truckton sandy loam, 0 to 3 percent slopes18918941052702yvrfco07320011:24000
Truckton sandy loam, 5 to 9 percent slopes1907591052712yvrhco07320011:24000
Truckton sandy loam, 3 to 5 percent slopes22475832236982yvrgco07320011:24000
Truckton loamy sand, 0 to 3 percent slopesTuB252381104762yvrlco08719651:24000
Truckton loamy sand, 3 to 5 percent slopesTuC18051339016731gjyco08719651:24000
Truckton loamy sand, 5 to 9 percent slopesTuD3939339016831gjzco08719651:24000
Bresser-Truckton sandy loams, 5 to 25 percent slopesBtE16332498706jqy9co62219681:20000
Bresser and Truckton soils, 3 to 12 percent slopes, erodedBuD21409498707jqybco62219681:20000
Truckton sandy loam, 0 to 3 percent slopesTrB6464987742yvrdco62219681:20000
Truckton sandy loam, 3 to 9 percent slopesTrD5954987752x0j2co62219681:20000
Bresser-Truckton sandy loams, 8 to 25 percent slopes968696496442jnl8co62319771:24000
Truckton sandy loam, 3 to 9 percent slopes41113704964332x0j2co62319771:24000
Truckton-Renohill complex, 8 to 25 percent slopes426185496434jnl0co62319771:24000
Bresser-Truckton-Blakeland complex, 3 to 9 percent slopesBtD44318952902xst2co62419631:20000
Yoder-Truckton-Lismas complexYt2020595353366xco62419631:20000
Truckton sandy loam, 5 to 9 percent slopesTkD6664953372yvrhco62419631:20000
Truckton sandy loam, 3 to 5 percent slopesTkC4798953362yvrgco62419631:20000
Truckton, Bresser, and Blakeland soils, 5 to 20 percent slopes, erodedTrE2405595338366fco62419631:20000
Truckton sandy loam, 0 to 3 percent slopesTkB776953352yvrfco62419631:20000
Truckton sandy loam, 3 to 9 percent slopes9772659954632x0j2co62519751:24000
Truckton sandy loam, 0 to 3 percent slopes9629401954622yvrdco62519751:24000
Truckton loamy sand, 1 to 9 percent slopes9514708954612yvrmco62519751:24000
Truckton-Bresser complex, eroded10010173953583672co62519751:24000
Truckton-Bresser sandy loams, 5 to 20 percent slopes996430954652yvrpco62519751:24000
Truckton-Blakeland complex, 9 to 20 percent slopes982249954642yvrnco62519751:24000
Truckton sandy loam, 0 to 3 percent slopes1586864974382yvrdco64119801:24000
Truckton sandy loam, 3 to 9 percent slopes1593234974392x0j2co64119801:24000

Map of Series Extent

Approximate geographic distribution of the TRUCKTON 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 .