Official Series Description


Lab Data Summary

Aggregate lab data for the TIMPANOGOS soil series. This aggregation is based on all pedons with a current taxon name of TIMPANOGOS, 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 TIMPANOGOS 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 TIMPANOGOS 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 TIMPANOGOS 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 TIMPANOGOS 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 TIMPANOGOS 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 TIMPANOGOS 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 TIMPANOGOS 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 TIMPANOGOS 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 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 TIMPANOGOS, 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 TIMPANOGOS 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
Timpanogos silt loam, 1 to 6 percent slopesToB8021481510j51lut60219691:20000
Timpanogos loam, 0 to 3 percent slopesTmA1607481507j51hut60219691:20000
Timpanogos silt loam, 6 to 10 percent slopesToC1603481511j51mut60219691:20000
Timpanogos loam, cool, 0 to 3 percent slopesTnA449481509j51kut60219691:20000
Timpanogos loam, 3 to 6 percent slopesTmB384481508j51jut60219691:20000
TIMPANOGOS SILT LOAM, 0 TO 3 PERCENT SLOPESTmA1928482845j6fnut60319681:20000
TIMPANOGOS SILT LOAM, DEEP WATER TABLE, 0 TO 3 PERCENT SLOPESTnA1850482849j6fsut60319681:20000
HILLFIELD-TIMPANOGOS SILT LOAMS, 10 TO 30 PERCENT SLOPES, ERODEDHhE21250482744j6bdut60319681:20000
TIMPANOGOS SILT LOAM, 3 TO 6 PERCENT SLOPESTmB1033482846j6fput60319681:20000
TIMPANOGOS SILT LOAM, 6 TO 10 PERCENT SLOPESTmC814482847j6fqut60319681:20000
TIMPANOGOS SILT LOAM, 10 TO 20 PERCENT SLOPES, ERODEDTmD2328482848j6frut60319681:20000
Timpanogos loam, 0 to 1 percent slopesTbA2360481663j56jut60719651:15840
Timpanogos loam, 1 to 3 percent slopesTbB2055481664j56kut60719651:15840
Hillfield-Timpanogos-Parleys complex, 30 to 60 percent slopes, erodedHTG21706481568j53gut60719651:15840
Timpanogos loam, 3 to 6 percent slopesTbC978481665j56lut60719651:15840
Hillfield-Timpanogos-Parleys complex, 20 to 30 percent slopes, erodedHTF2658481567j53fut60719651:15840
Timpanogos loam, 10 to 20 percent slopes, erodedTbE2511481667j56nut60719651:15840
Timpanogos loam, 6 to 10 percent slopes, erodedTbD2435481666j56mut60719651:15840
Timpanogos variant-Draper complex, 3 to 10 percent slopesTDD160481661j56gut60719651:15840
Timpanogos very fine sandy loam, noncalcareous variant, 6 to 10 percent slopesTcD79481668j56put60719651:15840
Timpanogos very fine sandy loam, noncalcareous variant, 10 to 20 percent slopesTcE63481669j56qut60719651:15840
Timpanogos loam, 3 to 6 percent slopesTuB1675482983j6l3ut61219671:20000
Timpanogos sandy loam, 6 to 10 percent slopesTtC579482982j6l2ut61219671:20000
Timpanogos sandy loam, 1 to 3 percent slopesTtA564482981j6l1ut61219671:20000
Timpanogos loam, 0 to 3 percent slopesTmB4324483391j708ut62119661:20000
Timpanogos loam, 3 to 6 percent slopesTmC644483392j709ut62119661:20000
Timpanogos loam, water table, 0 to 3 percent slopesToB605483393j70but62119661:20000

Map of Series Extent

Approximate geographic distribution of the TIMPANOGOS 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 .