Official Series Description


Lab Data Summary

Aggregate lab data for the SLAVEN soil series. This aggregation is based on all pedons with a current taxon name of SLAVEN, 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 SLAVEN 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
2482P071782NV027010Slaven7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties40.3497238,-117.5169449

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the SLAVEN 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 SLAVEN 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 SLAVEN 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 SLAVEN 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 SLAVEN 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 SLAVEN 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 SLAVEN 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 SLAVEN, 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-2012-05-09-22 | Pershing County, East Part - May 1994

    The physiographic position of various detailed soil map units. These units are 233—Dun Glen very fine sandy loam, 0 to 2 percent slopes; 322—Humboldt silty clay loam, strongly saline-sodic; 652—Burrita-Hoot-Rock outcrop association; 663—Oxcorel-Weso-Beoska association; 901—Roca-Reluctan association; and 1291—Slaven-Iver-Cleavage association (Soil Survey of Pershing County, Nevada, East Part; May 1994).

  2. NV-2012-05-09-23 | Pershing County, East Part - May 1994

    The physiographic position of various detailed soil map units. These units are 233—Dun Glen very fine sandy loam, 0 to 2 percent slopes; 322—Humboldt silty clay loam, strongly saline-sodic; 652—Burrita-Hoot-Rock outcrop association; 663—Oxcorel-Weso-Beoska association; 901—Roca-Reluctan association; and 1291—Slaven-Iver-Cleavage association (Soil Survey of Pershing County, Nevada, East Part; May 1994).

Map Units

Map units containing SLAVEN 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
Slaven-Mascamp associationSD14485476156hzgwnv61219681:24000
Slaven-Torro associationSH7066476160hzh0nv61219681:24000
Slaven-Primeaux associationSE5332476157hzgxnv61219681:24000
Slaven-Ramires associationSF3657476158hzgynv61219681:24000
Slaven-Toeja associationSG2686476159hzgznv61219681:24000
Slaven-Linrose-Cleavage association1201171625193722qj94nv61219681:24000
Chen-Slaven-Chen association262169125193842qj9jnv61219681:24000
Slaven-Iver-Cleavage association129137484475201hyh2nv76919861:24000
Slaven-Linrose-Iver association129028096475200hyh1nv76919861:24000
Alyan-Slaven association13217324475206hyh7nv76919861:24000
Slaven-Iver-Rock outcrop association12923369475202hyh3nv76919861:24000
Slaven-Glean-Cleavage association120311377479436j2wpnv77519851:24000
Chen-Slaven-Chen, cobbly, association2629125479568j30ynv77519851:24000
Slaven-Linrose-Cleavage association12017865479434j2wmnv77519851:24000
Slaven-Wiskan-Graley variant association12026940479435j2wnnv77519851:24000
Quarz-Linrose-Slaven association8144655479722j35xnv77519851:24000
Floer-Slaven-Roca association16622670479489j2ydnv77519851:24000

Map of Series Extent

Approximate geographic distribution of the SLAVEN 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 .