Official Series Description


Lab Data Summary

Aggregate lab data for the TEMO soil series. This aggregation is based on all pedons with a current taxon name of TEMO, 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 TEMO 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
22A00P046899CA003005Temo6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.8039703,-119.9272232
22A79P0467S1979NV031005Temo6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties39.2138901,-119.8974991
22A79P0472S1979NV031010Temo5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties39.315731,-119.8801727
22A68C0087S68CA017031Temo6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.9222,-119.9342389
22A00P0297S99CA017021Temo6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.7803861,-119.9833944

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the TEMO 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 TEMO 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 TEMO 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 TEMO 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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Click the image to view it full size.

Click the image to view it full size.

There are insufficient data to create the 3D terrace figure.

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

Competing Series

Soil series competing with TEMO 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 TEMO 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 TEMO 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.

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 TEMO, 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

Click a link below to display the diagram. Note that these diagrams may be from multiple survey areas.

  1. CA-2010-08-30-01 | Tahoe Basin Area, California and Nevada - 2007

    Representative diagram of the Meiss Meadow area (not to scale). The Sky-Callat general soil map unit is in this area (Soil Survey of the Tahoe Basin Area, California and Nevada; 2007).

  2. CA-2010-08-30-03 | Tahoe Basin Area, California and Nevada - 2007

    Representative diagram of the Freel Peak area (not to scale). The Whittell-Jobsis-Rock outcrop general soil map unit is in this area (Soil Survey of the Tahoe Basin Area, California and Nevada; 2007).

Map Units

Map units containing TEMO 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
Temo-Witefels complex, 30 to 50 percent slopes9443518216522211sg8gca69320061:24000
Temo-Witefels complex, 15 to 30 percent slopes9442338616522161sg89ca69320061:24000
Temo-Witefels complex, 50 to 70 percent slopes9444279016522171sg8bca69320061:24000
Temo-Witefels complex, 5 to 15 percent slopes944193816522151sg88ca69320061:24000
Sofgran-Klauspeak-Temo association, 15 to 50 percent slopes943120116520351sg2gca69320061:24000
Sofgran-Klauspeak-Temo association, 15 to 50 percent slopes130ty207615970071qltcca72419851:24000
Temo-Witefels complex, 5 to 15 percent slopes94414015975101qmblca72419851:24000
Temo-Witefels complex, 15 to 30 percent slopes94422515975121qmbnca72419851:24000
Sofgran-Temo-Shalgran association13115491626021p0f7ca72920061:24000
Sofgran-Klauspeak-Temo association13011209493229jk7mca72920061:24000
Sofgran-Temo-Rock outcrop association1325194779342v4z2ca72920061:24000
Temo-Dagget-Rock outcrop complex, 30 to 75 percent slopes140997493225jk7hca72920061:24000
Waterpeak-Sofgran-Temo association212951779347v4z7ca72920061:24000
Sofgran-Temo-Shalgran association131ty6361670098p0f7ca73119811:24000
Sofgran-Klauspeak-Temo association130ty3031670096jk7mca73119811:24000
Graylock-Temo-Rock outcrop complex, 30 to 70 percent slopes11006758474130hxcjnv62819801:24000
Temo-Witefels-Rock outcrop association8405792474388hxmvnv62819801:24000
Temo-Witefels-Rock outcrop association10691724628142nnrmnv62919751:24000
Graylock-Temo-Rock outcrop complex, 30 to 70 percent slopes911024628012nnr6nv62919751:24000
Temo-Witefels-Rock outcrop association9341340643992pm3ynv77319811:24000
Temo-Rock outcrop complex, 50 to 70 percent slopes932370644198pmblnv77319811:24000
Temo-Rock outcrop complex, 30 to 50 percent slopes931310644197pmbknv77319811:24000
Temo-Dagget-Rock outcrop complex, 30 to 75 percent slopes14020716977901tzpfnv77319811:24000
Witefels-Temo complex, 30 to 75 percent slopes165190644013pm4mnv77319811:24000

Map of Series Extent

Approximate geographic distribution of the TEMO 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 .