Official Series Description


Lab Data Summary

Aggregate lab data for the TOLO soil series. This aggregation is based on all pedons with a current taxon name of TOLO, 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 TOLO 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
940A5472S1960OR061001TOLO6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties45.6766546,-117.8065464
940A5473S1960OR061002TOLO6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties45.6838875,-117.8816681
940A5474S1960OR061003TOLO6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties45.6775017,-117.8050003

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the TOLO 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 TOLO 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 TOLO 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 TOLO 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 TOLO 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 TOLO 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 TOLO 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 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 TOLO, 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 TOLO 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
Tolo-Dogtown complex, 12 to 35 percent north slopes165D65146215422nzor60419881:24000
Tolo-Crackler complex, 12 to 35 percent north slopes164D10806215322nyor60419881:24000
Fivebit-Klicker-Tolo complex, 30 to 60 percent slopes1707CO56625938701qzfsor60419881:24000
Tolo-Klicker-Fivebit complex, 15 to 30 percent slopes1706BO23425938681qzfror60419881:24000
Tolo-Thirstygulch-Rock outcrop complex, 0 to 15 percent slopes4125AO5125938911r0f9or60419881:24000
Klickson-Tolo-Larabee complex, 30 to 60 percent slopes5745CO456031205371r1h8or60720181:24000
Tolo-Larabee-Fivebeaver complex, 0 to 15 percent slopes5942AO403931205761r2k8or60720181:24000
Klickson-Tolo-Larabee complex, 15 to 30 percent slopes5745BO143031205361r1h7or60720181:24000
Larabee-Tolo-Fivebeaver complex, 15 to 30 percent slopes5943BO104631205771r2kbor60720181:24000
Limberjim-Tolo-Olot complex, eolian, 15 to 30 percent slopes4970BE53431207151shsror60720181:24000
Lamulita-Tolo complex, landslide, 0 to 40 percent slopes3485PL44631204711r07qor60720181:24000
Tolo ashy silt loam, 15 to 30 percent slopes5857BO39031207371sj3hor60720181:24000
Tolo-Getaway complex, 15 to 30 percent north slopes6016BN3663120224njl5or60720181:24000
Klicker-Tolo-Fivebeaver complex, 15 to 30 percent slopes5007BO29931205151r1b5or60720181:24000
Tolo-Larabee complex, eolian, 15 to 30 percent slopes4955BE14631204981r193or60720181:24000
Bandarrow-Tolo complex, 0 to 15 percent slopes0053AW14231207681t1ttor60720181:24000
Tolo ashy silt loam, 2 to 15 percent slopes5857AO1133120223njkzor60720181:24000
Tolo-Larabee complex, mass failure, 15 to 30 percent slopes4955BM10431204991r194or60720181:24000
Tolo-Klicker complex, 3 to 15 percent slopes5858AO9631207381sj3jor60720181:24000
Larabee-Tolo-Klickson complex, 0 to 15 percent slopes5013AO7531205201r1bbor60720181:24000
Peaviner-Tolo complex, 0 to 15 percent slopes0052AO5631207671t1tsor60720181:24000
Sharpridge-Tolo complex, 0 to 15 percent slopes3420AO4731204551r051or60720181:24000
Klickson-Tolo complex, mass failure, 30 to 60 percent slopes5018CM2131205241r1bjor60720181:24000
Tolo-Getaway complex, 30 to 60 percent north slopes6016CN193120225njl6or60720181:24000
Tolo-Getaway complex, dry, 15 to 30 percent north slopes5877BO431202262mt9sor60720181:24000
Tolo silt loam, 12 to 35 percent slopes59E616036400224llor62519791:20000
Tolo silt loam, 35 to 65 percent slopes59F96306400324lmor62519791:20000
Tolo-Larabee complex, eolian, 15 to 30 percent slopes4955BE151831223111r193or62620181:24000
Klickson-Tolo-Larabee complex, 30 to 60 percent slopes5745CO116931223511r1h8or62620181:24000
Klicker-Tolo-Fivebeaver complex, 15 to 30 percent slopes5007BO66531223311r1b5or62620181:24000
Sharpridge-Tolo complex, 0 to 15 percent slopes3420AO30831222551r051or62620181:24000
Larabee-Tolo-Fivebeaver complex, 15 to 30 percent slopes5943BO30633854431r2kbor62620181:24000
Tolo-Larabee-Fivebeaver complex, 0 to 15 percent slopes5942AO13131223651r2k8or62620181:24000
Limberjim-Tolo-Olot complex, eolian, 15 to 30 percent slopes4970BE8231224831shsror62620181:24000
Kahler-Klickson-Tolo complex, 1 to 8 percent slopes4228AW7133852852ksvcor62620181:24000
Tolo-Larabee complex, mass failure, 15 to 30 percent slopes4955BM5831223121r194or62620181:24000
Larabee-Tolo-Klickson complex, 0 to 15 percent slopes5013AO5731223361r1bbor62620181:24000
Klickson-Tolo complex, mass failure, 30 to 60 percent slopes5018CM3831223411r1bjor62620181:24000
Tolo-Kahler-Silvies complex, 2 to 20 percent slopes4313AO2833853951vtl6or62620181:24000
Bandarrow-Tolo complex, 0 to 15 percent slopes0053AW2431225031t1ttor62620181:24000
Tolo-Unitylake complex, 0 to 15 percent slopes3318AO531222261r01zor62620181:24000
Fivebit-Klicker-Tolo complex, 30 to 60 percent slopes1707CO310724861951qzfsor63120181:24000
Tolo-Klicker-Fivebit complex, 15 to 30 percent slopes1706BO272124861941qzfror63120181:24000
Peaviner-Tolo complex, 0 to 15 percent slopes0052AO169324845421t1tsor63120181:24000
Tolo-Thirstygulch-Rock outcrop complex, 0 to 15 percent slopes4125AO132924868181r0f9or63120181:24000
Tolo-Unitylake complex, 0 to 15 percent slopes3318AO76424867081r01zor63120181:24000
Tolo ashy silt loam, 2 to 15 percent slopes5857AO4232437373njkzor63120181:24000
Tolo-Klicker complex, 3 to 15 percent slopes5858AO22924373751sj3jor63120181:24000
Tolo ashy silt loam, 15 to 30 percent slopes5857BO20524373741sj3hor63120181:24000
Klicker-Tolo-Fivebeaver complex, 15 to 30 percent slopes5007BO9724372371r1b5or63120181:24000
Tolo-Getaway complex, dry, 15 to 30 percent north slopes5877BO8324373992mt9sor63120181:24000
Tolo-Getaway complex, 15 to 30 percent north slopes6016BN482437436njl5or63120181:24000
Tolo-Getaway complex, 30 to 60 percent north slopes6016CN352437437njl6or63120181:24000
Tolo ashy silt loam, 15 to 35 percent slopes60E60986136621vkor64819771:24000
Tolo ashy silt loam, 35 to 60 percent slopes60F9916136721vlor64819771:24000
Tolo ashy silt loam, 3 to 15 percent slopes60C5316136521vjor64819771:24000
Klickson-Tolo-Larabee complex, 15 to 30 percent slopes5745BO31831215261r1h7or64819771:24000
Tolo-Larabee-Fivebeaver complex, 0 to 15 percent slopes5942AO30631215301r2k8or64819771:24000
Klickson-Tolo-Larabee complex, 30 to 60 percent slopes5745CO19931215271r1h8or64819771:24000
Tolo silt loam, 3 to 15 percent slopes97C3137164592256mor66719841:20000
Tolo-Klicker association, 3 to 15 percent slopes100C1831564410250ror66719841:20000
Tolo silt loam, 15 to 35 percent slopes97E1194264593256nor66719841:20000
Tolo-Klicker association, 15 to 35 percent slopes100E927464411250sor66719841:20000
Tolo silt loam, granite substratum, 15 to 35 percent slopes98E194164595256qor66719841:20000
Tolo silt loam, granite substratum, 3 to 15 percent slopes98C114164594256por66719841:20000
Tolo-Kilmerque association, 3 to 15 percent slopes99C79364596256ror66719841:20000
Tolo-Kilmerque association, 15 to 35 percent slopes99E59164597256sor66719841:20000
Larabee-Tolo-Fivebeaver complex, 15 to 30 percent slopes5943BO47031214781r2kbor66719841:20000
Tolo variant silt loam, 0 to 3 percent slopes101A40864412250tor66719841:20000
Tolo-Getaway complex, 15 to 30 percent north slopes3294830847252v52or67019991:24000
Tolo-Getaway complex, 30 to 60 percent north slopes3304387847262v53or67019991:24000
Tolo-Olot complex, 2 to 15 percent slopes3334243847292v56or67019991:24000
Tolo silt loam, 2 to 15 percent slopes3263521847222v4zor67019991:24000
Tolo silt loam, 15 to 30 percent north slopes3272945847232v50or67019991:24000
Tolo-Olot complex, 15 to 30 percent south slopes3342567847302v57or67019991:24000
Tolo-Getaway complex, dry, 15 to 30 percent north slopes3311847847272v54or67019991:24000
Tolo-Getaway complex, dry, 30 to 60 percent north slopes3321139847282v55or67019991:24000
Tolo silt loam, fan, 2 to 15 percent slopes328167847242v51or67019991:24000
Tolo silt loam, 3 to 30 percent slopes1084694694012b6rwa60319841:24000
Tolo silt loam, 30 to 45 percent slopes109183694022b6swa60319841:24000
Tolo ashy silt loam, 2 to 15 percent slopes5857AO17231225522ygckwa60319841:24000
Tolo silt loam, 40 to 65 percent slopesToF8038697142bjvwa61319671:20000
Tolo silt loam, 3 to 15 percent slopesToC4688697122bjswa61319671:20000
Tolo silt loam, 15 to 40 percent slopesToE2035697132bjtwa61319671:20000
Tolo silt loam, wet subsoil variant, 3 to 15 percent slopesTsC1378697152bjwwa61319671:20000
Tolo silt loam, 40 to 60 percent slopesToF839698372bntwa62319701:20000
Tolo silt loam, 25 to 40 percent slopesToE737698362bnswa62319701:20000
Tolo silt loam, 10 to 25 percent slopesToD241698352bnrwa62319701:20000
Tolo silt loam, 40 to 65 percent slopesToF69714772dcqwa67119611:31680
Tolo silt loam, 15 to 40 percent slopesToE66714762dcpwa67119611:31680
Tolo ashy silt loam, 2 to 15 percent slopes5857AO23331144672ygckwa71420181:24000

Map of Series Extent

Approximate geographic distribution of the TOLO 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 .