Official Series Description


Lab Data Summary

Aggregate lab data for the TOLLHOUSE soil series. This aggregation is based on all pedons with a current taxon name of TOLLHOUSE, 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 TOLLHOUSE 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
1893P047393CA029002Tollhouse7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties35.3522222,-118.3208333
18UCD08JER013S08CASJER-013Tollhouse3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties37.0958481,-119.7444916
18UCD08JER014S08CASJER-014Tollhouse2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties37.0957413,-119.7424469
22AUCD551000755-CA-10-007TOLLHOUSE3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties37.543335,-119.4386597

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the TOLLHOUSE 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 TOLLHOUSE 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 TOLLHOUSE 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 TOLLHOUSE 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 TOLLHOUSE 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 TOLLHOUSE 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 TOLLHOUSE 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.

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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 TOLLHOUSE, 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 TOLLHOUSE 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
Tollhouse coarse sandy loam, 30 to 70 percent slopes, very stonyToG8594032959242zwsfca63819671:24000
Tollhouse coarse sandy loam, 5 to 35 percent slopes, eroded, very stonyToE23581532959252zwsgca63819671:24000
Tollhouse-Rock outcrop complex, 30 to 65 percent slopes1350303632959072zwrsca63819671:24000
Tollhouse-Rock outcrop complex, 15 to 30 percent slopes1351148432959042zwrlca63819671:24000
Tollhouse rocky coarse sandy loam, 30 to 75 percent slopesTgF3133463522hkbbca65119591:20000
Auberry-Tollhouse-Rock land complex, 30 to 70 percent slopesAzF1777464211hl1kca65419661:24000
Tollhouse extremely rocky coarse sandy loam, 30 to 70 percent slopesTmF1693464479hlb6ca65419661:24000
Ahwahnee-Tollhouse-Rock land complex, 45 to 70 percent slopesAkF624464184hl0pca65419661:24000
Sierra-Tollhouse-Rock land complex, 45 to 70 percent slopesStF293464463hl9pca65419661:24000
Tunis-Tollhouse-Sorrell association, 30 to 75 percent slopes26814394467360hpb4ca66820071:24000
Tollhouse-Tweedy-Locobill association, 30 to 60 percent slopes2868252467378hpbqca66820071:24000
Tollhouse-Sorrell-Rock outcrop complex, 30 to 60 percent slopes2698207467361hpb5ca66820071:24000
Tollhouse-Sesame-Friant association, 30 to 60 percent slopes2825945467374hpblca66820071:24000
Tollhouse-Edmundston-Sorrell association, 15 to 50 percent slopes2725880467364hpb8ca66820071:24000
Tollhouse-Martee-Edmundston association, 30 to 50 percent slopes2805312467372hpbjca66820071:24000
Tollhouse-Martee-Rock outcrop complex, 30 to 75 percent slopes2835029467375hpbmca66820071:24000
Tollhouse-Rock outcrop complex, 30 to 60 percent slopes2844209467376hpbnca66820071:24000
Tweedy-Tollhouse-Locobill complex, 9 to 30 percent slopes1881904467311hp8kca66820071:24000
Tweedy-Tollhouse-Locobill-Urban land complex, 0 to 30 percent slopes48821814212941jpz6ca66820071:24000
Godde-Tollhouse gravelly sandy loams, 30 to 75 percent slopes13819556463842hknnca67019771:24000
Edmundston-Godde-Tollhouse complex, 50 to 75 percent slopes1347850463838hknjca67019771:24000
Tunis-Tollhouse-Sorrell association, 30 to 75 percent slopes268ne31622180962dg3hca67019771:24000
Tollhouse-Tweedy-Locobill association, 30 to 60 percent slopes286ne21822181032dg3qca67019771:24000
Edmundston-Godde-Tollhouse complex, 50 to 75 percent sl opes134793739345stbvca67519681:24000
Tollhouse sandy loam, 30 to 50 percent slopesToF4460457994hcl0ca67719721:24000
Tollhouse-Rock outcrop complex, 30 to 75 percent slopes2122280458113hcpvca67819741:24000
Tollhouse rocky coarse sandy loam, 8 to 50 percent slopes, erodedTfF258996458376hczbca67919671:15840
Tollhouse sandy loam, 15 to 25 percent slopes, erodedThE21466458378hczdca67919671:15840
Tollhouse sandy loam, 5 to 15 percent slopes, erodedThD21236458377hczcca67919671:15840
Tollhouse sandy loam, 30 to 50 percent slopesToF1729133sgqfca67919671:15840
Tollhouse-Stukel-Wrentham families complex, 60 to 90 percent slopes92af2292562677hm8lca69620161:24000
Tollhouse family-Rock outcrop complex, 30 to 60 percent slopes16615587465141hm0kca75019831:24000
Auberry-Tollhouse families-Rock outcrop association, 25 to 65 percent slopes11010344465085hlyrca75019831:24000
Tollhouse family-Rock outcrop association, 60 to 85 percent slopes1677147465142hm0lca75019831:24000
Tollhouse-Rock outcrop complex, 10 to 30 percent slopes50016821465205hm2mca76019811:24000
Rock outcrop-Tollhouse complex, 15 to 30 percent slopes42115782465191hm25ca76019811:24000
Rock outcrop-Tollhouse complex, 30 to 50 percent slopes42215755465192hm26ca76019811:24000
Tollhouse-Rock outcrop complex, 50 to 75 percent slopes50211247465207hm2pca76019811:24000
Rock outcrop-Tollhouse complex, 50 to 75 percent slopes42310853465193hm27ca76019811:24000
Tollhouse-Chaix association, moderately steep5036939465208hm2qca76019811:24000
Chaix-Wind River family-Tollhouse association, sloping5095017465209hm2rca76019811:24000
Tollhouse-Rock outcrop complex, 30 to 50 percent slopes5014330465206hm2nca76019811:24000
Tollhouse variant-Shaver variant-Rock outcrop complex, 30 to 50 percent slopes1253929465162hm17ca76019811:24000
Tollhouse-Edmundston-Sorrell association, 15 to 50 percent slopes272ne239623710272kl7rca76019811:24000
Tollhouse-Martee-Edmundston association, 30 to 50 percent slopes280ne191523710302kl7vca76019811:24000
Tollhouse-Rock outcrop complex, 30 to 60 percent slopes284ne151823710352kl80ca76019811:24000
Tollhouse-Sorrell-Rock outcrop complex, 30 to 60 percent slopes269ne137723710242kl7nca76019811:24000
Tollhouse-Tweedy-Locobill association, 30 to 60 percent slopes286ne137623710362kl81ca76019811:24000
Tunis-Tollhouse-Sorrell association, 30 to 75 percent slopes268ne133223710232kl7mca76019811:24000
Tollhouse-Martee-Rock outcrop complex, 30 to 75 percent slopes283ne81023710332kl7yca76019811:24000
Tweedy-Tollhouse-Locobill complex, 9 to 30 percent slopes188ne5623710102kl76ca76019811:24000
Tollhouse extremely rocky coarse sandy loam, 30 to 70 percent slopesTmFef5223707972kl0bca76019811:24000
Oak Glen-Tollhouse families complex, 30 to 70 percent slopes6416714161471jjm5ca77219811:24000
Tollhouse-Stukel-Wrentham families complex, 60 to 90 percent slopes9211580465390hm8lca77619811:24000
Tollhouse-Knutsen-Stukel families complex, 30 to 70 percent slopes597980465359hm7lca77619811:24000
Oak Glen-Tollhouse families complex, 30 to 70 percent slopes643030465369hm7xca77619811:24000
Tollhouse-Olete-Tyee families complex, 50 to 75 percent slopesTyG2780471674htt9ca77719811:24000
Tyee-Tollhouse families complex, 30 to 50 percent slopesDeF850471629htrvca77719811:24000
Tollhouse rocky coarse sandy loam, 8 to 50 percent slopes, erodedTfF2798848236xgngca77719811:24000
Tollhouse sandy loam, 30 to 50 percent slopesToF70848223xgn1ca77719811:24000

Map of Series Extent

Approximate geographic distribution of the TOLLHOUSE 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 .