Official Series Description


Lab Data Summary

Aggregate lab data for the EVARO soil series. This aggregation is based on all pedons with a current taxon name of EVARO, 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 EVARO 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
43B89P054988MT0771235Evaro6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties46.8191681,-113.289444
43B91P054290MT0391272Evaro6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties46.6333351,-113.3416672

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the EVARO 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 EVARO 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 EVARO 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 EVARO 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 EVARO 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 EVARO 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 EVARO 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 hills figure.

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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 EVARO, 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 EVARO 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
Holloway-Evaro-Bata families, complex, steep ridges and mountain slopes51ND32593300507750hxmt60319891:24000
Evaro-Holloway-Tigeron families, complex, steep ridges and mountain slopes51NC2269300507450hwmt60319891:24000
Evaro-Holloway-Elvick families, complex, nivational mountain slopes and ridges71NDB14300507350kfmt60319891:24000
Evaro, stony-Tigeron complex, 20 to 50 percent slopes939F668185973820f6kmt60520071:24000
Evaro gravelly ashy loam, cold, 35 to 60 percent slopes597F245185958220f1jmt60520071:24000
Worock-Evaro-Elvick families, complex, nivational mountain slopes and ridges71UDB11185961120f2gmt60520071:24000
Evaro-Holloway-Elvick families, complex, high relief mountain slopes and ridges71ND33185960920f2dmt60520071:24000
Evaro gravelly ashy loam, cold, 15 to 35 percent slopes597E2344154952567gmt61620031:24000
Evaro gravelly ashy loam, moist, 8 to 25 percent slopes897E178315513856fgmt61620031:24000
Evaro stony ashy loam, 35 to 60 percent slopes782F131015506256c0mt61620031:24000
Evaro gravelly ashy loam, cold, 35 to 60 percent slopes597F1228609585ngb1mt61620031:24000
Evaro stony ashy loam, 15 to 35 percent slopes782E109515506156bzmt61620031:24000
Evaro gravelly ashy loam, 15 to 35 percent slopes97E106315519056h4mt61620031:24000
Evaro gravelly ashy loam, 8 to 15 percent slopes97D52915518956h3mt61620031:24000
Evaro gravelly ashy loam, cold, 8 to 15 percent slopes597D307154951567fmt61620031:24000
Evaro gravelly ashy loam, 35 to 60 percent slopes97F27615519156h5mt61620031:24000
Evaro stony ashy loam, 4 to 15 percent slopes782D13215506056bymt61620031:24000
Evaro gravelly ashy loam, 15 to 35 percent slopes97E38031446614vjhmt62119971:24000
Evaro gravelly loam, 35 to 60 percent slopes97F9651446624vjjmt62119971:24000
Evaro gravelly ashy loam, 8 to 15 percent slopes97D6491446604vjgmt62119971:24000
Evaro gravelly loam, moist, 35 to 60 percent slopes197F5661442644v3pmt62119971:24000
Evaro gravelly loam, moist, 15 to 35 percent slopes197E1741442634v3nmt62119971:24000
Evaro gravelly loam, moist, 8 to 15 percent slopes197D1281442624v3mmt62119971:24000
Evaro-Holloway-Elvick families, complex, high relief mountain slopes and ridges71ND33239414949450kdmt63520061:24000
Holloway-Evaro-Bata families, complex, steep ridges and mountain slopes51ND33085714944850hxmt63520061:24000
Evaro family-Rubble land complex, high relief mountain slopes and ridges71NC32058114949250kbmt63520061:24000
Evaro-Holloway-Tigeron families, complex, steep ridges and mountain slopes51NC2850814944750hwmt63520061:24000
Evaro-Holloway-Elvick families, complex, nivational mountain slopes and ridges71NDB790814949550kfmt63520061:24000
Elve-Evaro-Elvick families, complex, high relief mountain slopes and ridges71NB3458914949150k9mt63520061:24000
Tigeron-Garlet-Evaro families, complex, steep ridges and mountain slopes51UC2351314945150j0mt63520061:24000
Worock-Evaro-Elvick families, complex, nivational mountain slopes and ridges71UDB291314950450kqmt63520061:24000
Evaro-Holloway-Tigeron families, complex, nivational mountain slopes and ridges71NCB227514949350kcmt63520061:24000
Cowood family-Rock outcrop-Evaro family, complex, very steep cirques31UD4178514941650gwmt63520061:24000
Evaro-Waldbillig-Littlesalmon families, complex, moderately steep young moraines21ND2110514956050mjmt63520061:24000
Evaro gravelly ashy loam, 15 to 35 percent slopes97E89017029991v53gmt63520061:24000
Evaro gravelly ashy loam, cold, 15 to 35 percent slopes597E63017029011v509mt63520061:24000
Evaro gravelly ashy loam, 35 to 60 percent slopes97F58117030001v53hmt63520061:24000
Evaro-Eastridge-Vitroff complex, 20 to 50 percent slopes548F41717031881v59kmt63520061:24000
Evaro-Vitroff complex, 8 to 30 percent slopes550E38417031891v59lmt63520061:24000
Evaro-Vitroff-Germangulch, very stony, complex, 20 to 50 percent slopes543F32517031861v59hmt63520061:24000
Evaro gravelly ashy loam, 8 to 15 percent slopes97D31917029981v53fmt63520061:24000
Evaro-Germangulch complex, 4 to 25 percent slopes, extremely stony540D13417031831v59dmt63520061:24000
Evaro stony ashy loam, 15 to 35 percent slopes782E12817029021v50bmt63520061:24000
Evaro-Eastridge complex, 20 to 50 percent slopes567F11717031931v59qmt63520061:24000
Evaro, stony-Tigeron complex, 20 to 50 percent slopes939F1917032231v5bpmt63520061:24000
Evaro-Holloway-Elvick families, complex, high relief mountain slopes and ridges27095817034501v5l0mt63619831:24000
Elve-Evaro-Elvick families, complex, high relief mountain slopes and ridges26794217034471v5kxmt63619831:24000
Evaro family-Rubble land complex, high relief mountain slopes and ridges268635170344850kbmt63619831:24000
Evaro-Holloway-Tigeron families, complex, steep ridges and mountain slopes25834817034381v5kmmt63619831:24000
Evaro-Holloway-Tigeron families, complex, nivational mountain slopes and ridges26914417034491v5kzmt63619831:24000
Cowood family-Rock outcrop-Evaro family, complex, very steep cirques3188317034341v5khmt63619831:24000
Evaro gravelly loam, 30 to 60 percent slopes37142251454544wc2mt63819851:24000
Evaro gravelly loam, 8 to 30 percent slopes3662441454534wc1mt63819851:24000
Evaro gravelly loam, dry, 15 to 35 percent slopes97E36171459724wwsmt64419951:24000
Evaro gravelly loam, dry, 35 to 60 percent slopes97F32811459734wwtmt64419951:24000
Evaro gravelly loam, 35 to 60 percent slopes197F31131455924whjmt64419951:24000
Evaro gravelly loam, 15 to 35 percent slopes197E26121455914whhmt64419951:24000
Evaro gravelly loam, dry, 4 to 15 percent slopes97D10951459714wwrmt64419951:24000
Evaro gravelly loam, 4 to 15 percent slopes197D5361455904whgmt64419951:24000
Evaro-Eastridge-Vitroff complex, 20 to 50 percent slopes548F2761361830d4hymt67020071:24000
Evaro-Vitroff complex, 8 to 30 percent slopes550E2452361826d4htmt67020071:24000
Evaro-Vitroff-Germangulch, very stony complex, 20 to 50 percent slopes543F1192361835d4j3mt67020071:24000
Evaro-Germangulch complex, 4 to 25 percent slopes, extremely stony540D58214247391jtkbmt67020071:24000
Evaro-Coslaw-Hungryhill complex, 15 to 50 percent slopes568F524361846d4jgmt67020071:24000
Evaro, stony-Tigeron complex, 20 to 50 percent slopes939F47214248341jtndmt67020071:24000
Evaro-Savenac complex, 15 to 30 percent slopes569E399361831d4hzmt67020071:24000
Evaro-Eastridge complex, 20 to 50 percent slopes567F377361825d4hsmt67020071:24000
Evaro-Savenac complex, 4 to 15 percent slopes594D20314247591jtkzmt67020071:24000

Map of Series Extent

Approximate geographic distribution of the EVARO 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 .