Official Series Description


Lab Data Summary

Aggregate lab data for the TREBLOC soil series. This aggregation is based on all pedons with a current taxon name of TREBLOC, 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 TREBLOC 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 TREBLOC 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 TREBLOC 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 TREBLOC 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 TREBLOC 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 TREBLOC 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 TREBLOC 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 TREBLOC 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 TREBLOC, 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 TREBLOC 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
Trebloc silt loam, 0 to 2 percent slopes8513783179423lyppar01919831:20000
Trebloc silt loam, 0 to 2 percent slopes50970565678lzmpar05719761:20000
Trebloc silt loam, 0 to 2 percent slopes851633179313lyppar05919831:20000
Trebloc silt loam, 0 to 2 percent slopesTrB1953579211mfq7ar13919921:24000
Trebloc loamTr1498331913c4cwms01719691:20000
Myatt silt loam, (trebloc)My8618332148c4mgms03119621:15840
Latonia-Trebloc association, occasionally floodedLT10201332220c4psms03519761:20000
Trebloc silt loamTb6171332240c4qfms03519761:20000
Trebloc-Escambia complex, 0 to 2 percent slopesTeA1032332241c4qgms03519761:20000
Trebloc silt loam, frequently flooded943073567827m1w0ms03719921:20000
Trebloc silt loam, 0 to 2 percent slopes, occasionally floodedTbA329926422492rs3tms04120121:24000
Trebloc silt loam, pondedTrA215126422502rs3vms04120121:24000
Trebloc association, frequently floodedTR2992332422c4x9ms04519791:20000
Trebloc silt loamTr1510332489c4zgms05719751:20000
Trebloc silt loam, thick surface variantTb1636332701c569ms06519721:20000
Trebloc silt loam, 0 to 2 percent slopes, frequently flooded28238933327162shttms06719841:20000
Trebloc-Quitman association, occasionally flooded1713292332706c56gms06719841:20000
Trebloc silt loam2711692332715c56rms06719841:20000
Trebloc silt loam and Bibb fine sandy loam, occasionally and frequently flooded1319060332703c56cms06719841:20000
Trebloc and Osier soilsTs26398332869c5cqms07319691:20000
Trebloc silt loamTr565332868c5cpms07319691:20000
Trebloc silt loam, 0 to 1 percent slopes, frequently floodedTr14133333625c653ms11119971:20000
Bibb and Trebloc soils, frequently floodedBM10434333593c642ms11119971:20000
Harleston-Trebloc complex, 0 to 2 percent slopes, rarely floodedHt8185333606c64hms11119971:20000
Trebloc-Quitman complex, 0 to 2 percent slopes, rarely floodedTs7981333626c654ms11119971:20000
Quitman-Jena-Trebloc association, floodedQJT17506333977c6jgms12719931:20000
Trebloc silt loam, 0 to 2 percent slopes, frequently floodedTb39383339892shttms12719931:20000
Trebloc silt loam, 0 to 2 percent slopes, frequently floodedTr140453340762shttms12919971:20000
Trebloc silt loam, pondedTbA73124034422lnzdms15320081:24000

Map of Series Extent

Approximate geographic distribution of the TREBLOC 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 .