Official Series Description


Lab Data Summary

Aggregate lab data for the CORVUS soil series. This aggregation is based on all pedons with a current taxon name of CORVUS, 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 CORVUS 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
4206N1099S2006NM688016Corvus8Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties32.7389717,-106.1705246
4212N7979S2012NM035006Corvus8Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties32.7241111,-106.3346944

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the CORVUS 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 CORVUS 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 CORVUS 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 CORVUS 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 CORVUS 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 CORVUS 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 CORVUS 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 CORVUS, 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. TX-2012-05-09-05 | Guadalupe Mountains National Park - 2010

    Patterns of soils and underlying material from the high country down the western escarpment into the salt basin. General Soil Map Units 1, 2, 3, 4, 5, and 6 appear on this diagram. The "High Country" includes General Soil Map Units 3—Victorio-Lozen-Rock outcrop; 5—Biduya-Desario-Lazarus; and 6—Lostpeak-Rock outcrop. The Salt Basin includes General Soil Map Unit 2—Monahans-Corvus-Peligro. At the upper end of the basin, General Soil Map Unit 1—Chilicotal-Bissett-Chispa-Tenneco occurs, and is on the fan remnants of the escarpment (Soil Survey of Guadalupe Mountains National Park, Texas; 2010).

Map Units

Map units containing CORVUS 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
Corvus-Peligro complex, 0 to 10 percent slopes214798190652721zwwnm68820141:24000
Typic Torriorthents-Corvus complex, 0 to 6 percent slopes86190726468342rkmwnm68820141:24000
Corvus-Peligro-Nasa complex, 0 to 5 percent slopes931003426468622rkn4nm78120151:24000
Typic Torriorthents-Corvus complex, 0 to 6 percent slopes86320926468522rkmwnm78120151:24000
Corvus-Astrobee-Lark complex, 0 to 25 percent slopes92157826468642rkn6nm78120151:24000
Corvus-Peligro complex, 0 to 10 percent slopes21776264687321zwwnm78120151:24000
Corvus-Peligro complex, 1 to 5 percent slopesCPB515624938712ppw2tx62520101:24000
Corvus-Peligro-Yesum complex, 1 to 8 percent slopesCTC3121825103212q8c8tx62620121:24000
Yesum-Loki-Corvus complex, 0 to 1 percent slopesYLA1074525103222q8c9tx62620121:24000
Corvus-Peligro-Yesum complex, 1 to 8 percent slopesCTC5229224080862ltt6tx62720121:24000
Yesum-Loki-Corvus complex, 0 to 1 percent slopesYLA52212589971zd4tx62720121:24000

Map of Series Extent

Approximate geographic distribution of the CORVUS 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 .