Official Series Description


Lab Data Summary

Aggregate lab data for the COPIA soil series. This aggregation is based on all pedons with a current taxon name of COPIA, 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 COPIA were used in the calculation. Source: KSSL snapshot . Methods used to assemble the KSSL snapshot used by SoilWeb / SDE

There are insufficient data to create the lab data summary figure.


Water Balance

Monthly water balance estimated using a leaky-bucket style model for the COPIA 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 COPIA 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 COPIA 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 COPIA 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 COPIA 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 COPIA 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 COPIA 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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Soil series sharing subgroup-level classification with COPIA, 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 COPIA 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
Talos-Copia-Mcnew complex, 1 to 10 percent slopes7973307190652021zwnnm68820141:24000
Copia-Wink-Tonuco complex, 0 to 18 percent slopes203814624843582rkmmnm68820141:24000
Mcnew-Copia complex, 1 to 15 percent slopes5432369190647821zv9nm68820141:24000
Copia-Patriot complex, 0 to 15 percent slopes1915800190649521zvvnm68820141:24000
Copia-Nations complex, 1 to 3 percent slopes22112294581501yhtnm71920001:24000
Mcnew-Copia-Foxtrot complex, 1 to 5 percent slopes4080296581631yj7nm71920001:24000
Copia-Patriot complex, 2 to 5 percent slopes4247361581651yj9nm71920001:24000
Elizario-Copia complex, 2 to 5 percent slopes4132173581641yj8nm71920001:24000
Foxtrot-Copia complex, 0 to 5 percent slopes3526262582051yklnm71920001:24000
Copia loamy fine sand, 5 to 15 percent slopes726154581451yhnnm71920001:24000
Mcnew-Copia complex, 2 to 5 percent slopes1720908581171ygrnm71920001:24000
Copia-Mcnew-Pendero complex, 1 to 5 percent slopes3920237581521yhwnm71920001:24000
Pendero-Copia-Nations complex, 2 to 5 percent slopes3115301581511yhvnm71920001:24000
Wessly-Copia complex, 1 to 3 percent slopes375740581461yhpnm71920001:24000
Copia loamy fine sand, 2 to 7 percent slopesCOC230324938752ppw6tx62520101:24000
Copia-Nations complex, 1 to 10 percent slopesCSD9266116022831qs9ktx62720121:24000
Copia-Azulugar complex, 3 to 10 percent slopesCRD2202616035721qtn4tx62720121:24000
Monahans-Copia complex, 1 to 8 percent slopesMNC490225072602q3d0tx62720121:24000

Map of Series Extent

Approximate geographic distribution of the COPIA 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 .