Official Series Description


Lab Data Summary

Aggregate lab data for the SONDOA soil series. This aggregation is based on all pedons with a current taxon name of SONDOA, 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 SONDOA 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
2708N04922008NV027252Sondoa8Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties40.0895278,-118.5800833

Water Balance

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

Click the image to view it full size.

Click the image to view it full size.

Soil series sharing subgroup-level classification with SONDOA, 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. NV-2012-05-09-21 | Pershing County, East Part - May 1994

    General soil map units representative of those on a semibolson that is an externally drained intermontane basin. These units are 4—Humboldt-Sonoma-Sondoa; 6—Jerval-Dun Glen-Tenabo; 7—Chiara-Cortez-Orovada; 8—Jerval-Misad-Knoss; 9—Theon-Singatse; 10—Trunk-Burrita-Hoot; and 11—Reluctan-Roca-Iver (Soil Survey of Pershing County, Nevada, East Part; May 1994).

Map Units

Map units containing SONDOA 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
Sondoa-Swingler-Isolde association563715524391642mw4qnv60219851:24000
Sondoa silt loam, strongly saline-sodic, 0 to 2 percent slopes142295214089141j92vnv60219851:24000
Isolde-Appian-Sondoa association730177124408252mxw9nv60219851:24000
Parran-Sondoa association240728223986352lhzbnv60319711:24000
Parran-Sondoa association7103177024255752mf0cnv62519811:24000
Sondoa-Isolde association56375396474758hy0snv76019941:24000
Sondoa-Swingler-Isolde association56320432476333hznlnv76119881:24000
Sondoa silt loam, strongly saline-sodic, 0 to 2 percent slopes5623430476332hznknv76119881:24000
Sondoa-Ixian-Ixian, strongly saline-Sodic association1869850474925hy65nv76519861:24000
Toano-Enko-Sondoa association2090885474944hy6snv76519861:24000
Sondoa-Swingler-Isolde association5634425475281hyknnv76919861:24000
Isolde-Appian-Sondoa association7301213724529362nbgznv76919861:24000
Sondoa silt loam, strongly saline-sodic, 0 to 2 percent slopes562198924529342nbgxnv76919861:24000
Parran-Sondoa association710815124524942nb0qnv77019951:24000
Yelbrick-Izamatch-Sondoa association405215778480120j3lrnv77920041:24000
Izamatch-Sondoa-Yelbrick association405014672480118j3lpnv77920041:24000
Sondoa-Timpie association31308929480009j3h5nv77920041:24000
Yelbrick-Sondoa associatiion31808345480015j3hcnv77920041:24000
Sondoa-Yelbrick-Izamatch association40513368480119j3lqnv77920041:24000
Piltdown-Benin-Sondoa association32313124480035j3j0nv77920041:24000
Sondoa-Yelbrick association33412713480055j3jnnv77920041:24000
Benin-Sondoa-Playas association32702565480046j3jcnv77920041:24000
Toano-Sondoa association30001914479980j3g7nv77920041:24000
Sondoa-Timpie association8265313897151hn3jut61119921:24000

Map of Series Extent

Approximate geographic distribution of the SONDOA 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 .