Official Series Description


Lab Data Summary

Aggregate lab data for the TOIYABE soil series. This aggregation is based on all pedons with a current taxon name of TOIYABE, 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 TOIYABE 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
22A68C0088S1968NV005001TOIYABE5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.9615669,-119.8540573
22A40A3417S1975NV031003TOIYABE6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties39.2315636,-119.8743362
2678P058178NV005142Toiyabe6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.9625015,-119.8416672
n/a69C0111S1969NV005001Toiyabe5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Propertiesn/a

Water Balance

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

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

Competing Series

Soil series competing with TOIYABE 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 TOIYABE 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 TOIYABE 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 TOIYABE, 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 TOIYABE 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
Toiyabe-Lasco-Quartzburg complex, 30 to 50 percent slopes3827916487743jcjnca60820001:24000
Toiyabe-Lasco complex, 2 to 30 percent slopes3834499487745jcjqca60820001:24000
Toiyabe-Bonta loamy coarse sands, 30 to 75 percent slopes complexTbG2482486560jb9hca61419671:24000
Toiyabe-Bonta loamy coarse sands, 2 to 30 percent slopes complexTbE1485486559jb9gca61419671:24000
Haypress-Toiyabe loamy coarse sands, 2 to 30 percent slopesHtE85132330762zmr8ca61419671:24000
Haypress-Toiyabe complex, 30 to 75 percent slopesHAG44132330732zmr6ca61419671:24000
Haypress-Toiyabe loamy coarse sands, 30 to 75 percent slopesHtG9032330782zmr9ca61419671:24000
Toiyabe-Haypress-Rock outcrop complex, 30 to 75 percent slopes, erodedHAG24632330752zmr7ca61419671:24000
Haypress-Toiyabe complex, 2 to 30 percent slopesHAE432330712zmr5ca61419671:24000
Rock outcrop-Toiyabe complex, 50 to 75 percent slopesRTG132331072zmrrca61419671:24000
Toiyabe-Corbett-Rock outcrop complex, 30 to 50 percent slopes71167324247842md5vca68620101:24000
Toiyabe-Lasco-Quartzburg complex, 30 to 50 percent slopes382su24015283801n9dlca70819841:24000
Toiyabe-Lasco complex, 2 to 30 percent slopes383su12215283821n9dnca70819841:24000
Haypress-Toiyabe families complex, 30 to 50 percent slopes.1948400471203htb3ca71319841:24000
Haypress-Toiyabe families complex, 2 to 30 percent slopes.1935378471202htb2ca71319841:24000
Bonta-Toiyabe families complex, 2 to 30 percent slopes.1053693471114ht77ca71319841:24000
Switchback-Delleker-Toiyabe families complex, 15 to 50 percent slopes.2673498471276htdgca71319841:24000
Toiyabe-Haypress families complex, 30 to 70 percent slopes.2743489471283htdpca71319841:24000
Switchback-Delleker-Toiyabe families complex, 50 to 70 percent slopes.2682590471277htdhca71319841:24000
Haypress-Toiyabe families-Rock outcrop complex, 2 to 50 percent slopes.1951979471204htb4ca71319841:24000
Toiyabe-Haypress families complex, 0 to 30 percent slopes.2731850471282htdnca71319841:24000
Bonta-Toiyabe families complex, 30 to 50 percent slopes.1061745471115ht78ca71319841:24000
Toiyabe family-Rubble land complex, 30 to 70 percent slopes.2761553471285htdrca71319841:24000
Toiyabe-Bonta families complex, 30 to 50 percent slopes.2721408471281htdmca71319841:24000
Toiyabe-Bonta families complex, 0 to 30 percent slopes.2711352471280htdlca71319841:24000
Toiyabe-Bonta loamy coarse sands, 30 to 75 percent slopesTbGsv86315461171nwvrca71319841:24000
Toiyabe family-Rubble land complex, 0 to 30 percent slopes.275391471284htdqca71319841:24000
Toiyabe-Bonta loamy coarse sands, 2 to 30 percent slopesTbEsv20615461151nwvpca71319841:24000
Toiyabe-Haypress-Rock outcrop complex, 30 to 75 percent slopes, erodedHAG2332632330742zmr7ca71919821:24000
Haypress-Toiyabe complex, 2 to 30 percent slopesHAE200932330702zmr5ca71919821:24000
Haypress-Toiyabe complex, 30 to 75 percent slopesHAG196632330722zmr6ca71919821:24000
Rock outcrop-Toiyabe complex, 50 to 75 percent slopesRTG151132331062zmrrca71919821:24000
Toiyabe-Rock outcrop-Haypress complex, 30 to 75 percent slopes, severely erodedTPG31012464812hlnyca71919821:24000
Haypress-Toiyabe-Cryumbrepts, wet complex, 30 to 75 percent slopesHBG736464678hljmca71919821:24000
Haypress-Toiyabe-Cryumbrepts, wet complex, 2 to 30 percent slopesHBE419464677hljlca71919821:24000
Haypress-Toiyabe loamy coarse sands, 30 to 75 percent slopesHtG9632330792zmr9ca71919821:24000
Haypress-Toiyabe loamy coarse sands, 2 to 30 percent slopesHtE7432330772zmr8ca71919821:24000
Toiyabe-Corbett-Rock outcrop complex, 30 to 50 percent slopes12035290493224jk7gca72920061:24000
Corbett-Toiyabe-Rock outcrop complex, 15 to 50 percent slopes810435813860121hj82ca72920061:24000
Toiyabe-Corbett-Rock outcrop complex, 50 to 75 percent slopes1222286822431wlt1ca72920061:24000
Toiyabe-Corbett-Rock outcrop complex, 8 to 30 percent slopes1211800626020p0f6ca72920061:24000
Koppes-Toiyabe complex, 40 to 60 percent slopes30345715416555f2id65219771:24000
Koppes-Toiyabe gravelly loamy coarse sands, 40 to 60 percent slopesKtF2015615423155h6id66219691:31680
Toiyabe-Rock outcrop complex, 60 to 80 percent slopesBa27915420255g8id66219691:31680
Toiyabe-Corbett-Rock outcrop association, steep7534995474370hxm8nv62819801:24000
Toiyabe-Corbett-Haypress association7564830474372hxmbnv62819801:24000
Toiyabe-Corbett-Rock outcrop association, moderately steep7522057474369hxm7nv62819801:24000
Toiyabe-Rock outcrop complex, 50 to 70 percent slopes754753474371hxm9nv62819801:24000
Toiyabe-Corbett complex, 30 to 50 percent slopes67247624627772nnqfnv62919751:24000
Toiyabe-Rock outcrop complex, 30 to 50 percent slopes68205424627782nnqgnv62919751:24000
Toiyabe-Rock outcrop complex, 50 to 75 percent slopes6952424627792nnqhnv62919751:24000
Toiyabe, bouldery-Rock outcrop complex, 50 to 70 percent slopes10740324628152nnrnnv62919751:24000
Corbett-Toiyabe association1037524627202nnnlnv62919751:24000
Toiyabe-Rock outcrop complex, 50 to 75 percent slopes9424215644200pmbnnv77319811:24000
Toiyabe-Rock outcrop complex, 30 to 50 percent slopes9413336644199pmbmnv77319811:24000
Corbett-Toiyabe complex, 30 to 50 percent slopes1072876644232pmcpnv77319811:24000
Corbett-Toiyabe association1073710644233pmcqnv77319811:24000
Toiyabe-Corbett-Rock outcrop complex, 30 to 50 percent slopes12061516977891tzpdnv77319811:24000
Toiyabe-Corbett-Rock outcrop complex, 8 to 30 percent slopes9984216977321tzmknv77319811:24000

Map of Series Extent

Approximate geographic distribution of the TOIYABE 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 .