Official Series Description


Lab Data Summary

Aggregate lab data for the TUB soil series. This aggregation is based on all pedons with a current taxon name of TUB, 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 TUB 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
1040A0891S1957OR065015TUBn/aPrimary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties44.83712,-120.798532
1011N0364S2010OR069004Tubn/aPrimary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties45.0314178,-120.1272888
1020N0049S2019OR013503Tubn/aPrimary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties44.1577072143555,-120.355613708496
n/a40A0892S1957OR065016Tubn/aPrimary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties44.8236122,-120.7555542
n/a98P0245S1997OR023035TUBn/aPrimary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties44.3719444,-119.101944

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the TUB 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 TUB 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 TUB 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 TUB 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 TUB 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 TUB 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 TUB 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 terrace figure.

There are insufficient data to create the 3D flats position figure.

Soil series sharing subgroup-level classification with TUB, 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 TUB 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
Tub stony silty clay loam, 12 to 40 percent slopes46E26326109921kyor02119781:24000
Tub gravelly clay loam, 1 to 12 percent slopes46C15316109821kxor02119781:24000
Tub-Wylie-Badland association, 20 to 50 percent slopes169D3334725512fg3wor02119781:24000
Tub gravelly clay loam, 20 to 40 percent north slopes153E4347247326c0or02119781:24000
Tub-Wylie complex, 20 to 50 percent north slopes4004BO16312017321zrbor60720181:24000
Tub-Wylie complex, 2 to 20 percent slopes4004AO12312015421zl1or60720181:24000
Tub-Prill-Elderflat complex, 12 to 30 percent north slopes113294434349652mrnor6181:24000
Tub loam, 1 to 12 percent slopes112197734376262msdor6181:24000
Prill-Tub-Elderflat complex, 35 to 60 percent north slopes114150334375182mrcor6181:24000
Schrier-Tub complex, 30 to 60 percent north slopes110Em32734348022mnkor6181:24000
Schrier-Tub complex, 12 to 30 percent north slopes11830134347982ms7or6181:24000
Schrier-Tub complex, 30 to 60 percent north slopes110E28796339723z2or62019921:24000
Schrier-Tub complex, 15 to 30 percent north slopes110D21056339623z1or62019921:24000
Tub-Wylie complex, 2 to 20 percent slopes160C9454342510321zl1or6271:24000
Tub-Wylie complex, 20 to 50 percent north slopes160E5373342504521zrbor6271:24000
Tub-Wylie-Badland association, 20 to 50 percent slopes169D508334251042fg3wor6271:24000
Tub-Starkey complex, 2 to 20 percent slopes172C495934262521vdnror6271:24000
Tub-Prill-Rockly complex, 2 to 50 percent slopes172E13633425108nk6por6271:24000
Tub-Prill-Rockly association, 2 to 50 percent slopes172D133934294891nv9hor6271:24000
Tub-Ritter-Ninetysix complex, 2 to 20 percent slopes173C12863429497rcqjor6271:24000
Tub-Prill-Badland complex, 20 to 50 percent north slopes165E11893429517nk6hor6271:24000
Tub-Sweek-Badland complex, 20 to 50 percent north slopes175E8053429579rcqlor6271:24000
Prill-Tub complex, MLRA 9, 2 to 20 percent slopes626C76334319512ss4mor6271:24000
Tub-Wylie-Badland complex, 20 to 50 percent slopes169E4313432071zhxmor6271:24000
Tub loam, 1 to 12 percent slopes11229634376042msdor6271:24000
Tub clay loam, 3 to 20 percent slopes150D15342509226bzor6271:24000
Curant and Tub silt loams, 8 to 40 percent slopesCtE486336288623flor66619701:31680
Tub cobbly clay loam, 12 to 40 percent slopesThE484136292323gsor66619701:31680
Curant and Tub silt loams, 40 to 70 percent slopesCtF415446288723fmor66619701:31680
Tub gravelly clay loam, 1 to 12 percent slopesTgC295676292223gror66619701:31680
Tub very stony soils, 1 to 20 percent slopesTvD256706292523gvor66619701:31680
Tub very stony clay loam, 40 to 70 percent slopesTuF147296292423gtor66619701:31680
Tub loam, 1 to 12 percent slopes11268734724642msdor66619701:31680
Tub-Prill-Elderflat complex, 12 to 30 percent north slopes11346734724462mrnor66619701:31680
Schrier-Tub complex, 30 to 60 percent north slopes110Em35634725172mnkor66619701:31680
Schrier-Tub complex, 15 to 30 percent north slopes14256287823fbor66619701:31680
Schrier-Tub complex, 12 to 30 percent north slopes1181734724402ms7or66619701:31680
Prill-Tub-Elderflat complex, 35 to 60 percent north slopes1141434724542mrcor66619701:31680
Tub-Venator-Oldsferry complex, 0 to 15 percent slopes208B291334218052lf05or6771:24000
Tub-Wylie complex, 20 to 50 percent north slopes160E1504342191421zrbor6771:24000
Tub-Wylie complex, 2 to 20 percent slopes160C1241339168921zl1or6771:24000
Tub gravelly clay loam, 1 to 12 percent slopes46Cmg107433916342krkyor6771:24000
Tub clay loam, 3 to 7 percent slopes150B981342197526byor6771:24000
Tub-Wylie-Badland association, 20 to 50 percent slopes169D65033916932fg3wor6771:24000
Tub clay loam, 3 to 20 percent slopes150D492339165626bzor6771:24000
Tub-Prill-Rockly complex, 2 to 50 percent slopes172E4843424538nk6por6771:24000
Tub clay loam, 20 to 40 percent north slopes308E372342461328sp6or6771:24000
Tub gravelly clay loam, 20 to 40 percent north slopes153E370339167026c0or6771:24000
Tub clay loam, 0 to 3 percent slopes150A355339166326bxor6771:24000
Tub gravelly clay loam, 12 to 40 percent north slopes46Emg14433916682krkzor6771:24000
Prill-Tub-Elderflat complex, 35 to 60 percent north slopes1142934725482mrcor6771:24000

Map of Series Extent

Approximate geographic distribution of the TUB 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 .