Official Series Description


Lab Data Summary

Aggregate lab data for the TOLBY soil series. This aggregation is based on all pedons with a current taxon name of TOLBY, 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 TOLBY 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
48A88P008887CO107004Tolby6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties40.7688904,-106.7638855
48A92P028991CO117006Tolby6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties39.5866661,-105.9424973
n/a92P028591CO097002Tolby6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Propertiesn/a
n/a92P029391CO117010Tolby6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Propertiesn/a

Water Balance

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

Competing Series

Soil series competing with TOLBY 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 TOLBY 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 TOLBY 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.

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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.

Soil series sharing subgroup-level classification with TOLBY, 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 TOLBY 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
Tolby-Legault families complex, moist, 40 to 75 percent slopes7745C20800762999tlywco6451:24000
Tolby-Legault families complex, moist, 5 to 40 percent slopes7745B20543762998tlyvco6451:24000
Tolby family-Rubble land-Legault family complex, moist, 40 to 150 percent slopes7746D12596763000tlyxco6451:24000
Tolby family cobbly sandy loam, 30 to 60 percent slopes, extremely bouldery569856509356k30vco6471:24000
Tolby family-Rock outcrop-Hiwan family, moist complex, 40 to 75 percent slopes654D1399314150461jhgnco6541:24000
Leighcan-Tolby families complex, 40 to 65 percent slopes670C1059714150511jhgtco6541:24000
Legault-Tolby families complex, 5 to 40 percent slopes661B957514150481jhgqco6541:24000
Tolby family, till substratum, 15 to 25 percent slopes293B227132086412zd61co6541:24000
Tolby family, till substratum, 0 to 15 percent slopes293A61514148991jh9xco6541:24000
Tolby family-Rock outcrop-Hiwan family, moist complex, 40 to 75 percent slopes654D69231769461jhgnco66119681:31680
Scout-Mulgon-Tolby complex, 5 to 65 percent slopes1166884496840jp03co68419841:24000
Tolby-Lolopeak families complex, moderately steep mountain slopes32H4125224227312mb1mmt63819851:24000
Leighcan-Tolby-Crawfish families complex, breaklands, moist61D152524227422mb1zmt63819851:24000
Tolby-Agneston-Shermount families, complex, dissected mountain slopes, moist31D15912242380651c7mt64520131:12000
Leighcan-Tolby-Shermount families, complex, breaklands, moist61D15467242381551g2mt64520131:12000
Tolby-Leighcan families, complex, steep mountain slopes, moist30D1627224238022mc55mt64520131:12000
Tolby-Agneston families, complex, steep mountain slopes30D3025924238032mc56mt64520131:12000
Leighcan-Tolby-Shermount families, complex, breaklands, moist61D151620615035251g2mt64720071:24000
Tolby-Agneston-Shermount families, complex, dissected mountain slopes, moist31D151561315026451c7mt64720071:24000
Tolby-Mohaggin-Shermount families, complex, moderately steep mountain slopes32G411308215029051d2mt64720071:24000
Tolby-Agneston-Shermount families, complex, dissected mountain slopes31G151247515026851ccmt64720071:24000
Tolby-Lolopeak families, complex, moderately steep mountain slopes, moist32D41781015028251ctmt64720071:24000
Mohaggin-Tolby families, complex, moderately steep mountain slopes32D43700415028351cvmt64720071:24000
Tolby-Agneston families, complex, steep mountain slopes30D30692515023651bbmt64720071:24000
Mohaggin-Tolby-Shermount families, complex, mountain ridges33G41681815030251dgmt64720071:24000
Mohaggin-Tolby families, complex, steep mountain slopes30G43619515024751bpmt64720071:24000
Tolby-Shermount-Lolopeak families, association, dissected mountain slopes31Y15597415027651cmmt64720071:24000
Tolby-Lolopeak families, complex, moderately steep mountain slopes32H41556815029451d6mt64720071:24000
Tolby-Leighcan families, complex, steep mountain slopes, moist30D16508915023251b6mt64720071:24000
Mohaggin-Tolby families, complex, steep mountain slopes, cold30H41323715024851bqmt64720071:24000
Leighcan-Tolby-Shermount families, complex, breaklands61G15293615035651g6mt64720071:24000
Tolby-Lolopeak families, complex, steep mountain slopes30D41251415023951bfmt64720071:24000
Tolby-Leighcan families, complex, steep mountain slopes30G16247015024251bjmt64720071:24000
Tolby-Lolopeak-Shermount families, association, moderately steep mountain slopes and ridges34Y15127615030651dlmt64720071:24000
Leighcan-Tolby families-Rock outcrop complex, landslides61G18116615035751g7mt64720071:24000
Tolby-Agneston families, complex, moderately steep mountain slopes32G3081115028651cymt64720071:24000
Tolby-Shermount families-Rubble land association, breaklands61Y157915036851glmt64720071:24000
Angostura-Tolby association, steepAN57242507709k19qnm00719741:24000
Tolby-Hiwan familie,s association, 30 to 60 percent slopes209625273nzn3ut6491:24000
Tolby-Bottle families-Rock outcrop, complex88536177330565622xttgwy66519961:62500
Tolby-Sig families-Rock outcrop, complex83575029330565552xttcwy66519961:62500
Matcher, stony-Moran-Tolby families, complex, 2 to 8 percent slopes2487229804412wqqrwy6671:24000

Map of Series Extent

Approximate geographic distribution of the TOLBY 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 .