Official Series Description


Lab Data Summary

Aggregate lab data for the PANTERA soil series. This aggregation is based on all pedons with a current taxon name of PANTERA, 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 PANTERA 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
42S04TX377003S2004-TX377-003Pantera6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties29.7070885,-104.4514847

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the PANTERA 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 PANTERA 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 PANTERA 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 PANTERA 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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There are insufficient data to create the 3D flats position figure.

Competing Series

Soil series competing with PANTERA 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 PANTERA 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 PANTERA 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 PANTERA, 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-2010-11-02-01 | Big Bend National Park -

    Altuda, Bissett, Blackgap, Pantera, Riverwash, Stillwell, Strawhouse,

  2. TX-2010-11-02-05 | Big Bend National Park -

    Corazones, Geefour, Ninepoint, Pantera, Riverwash, Solis, Studybutte, Tornillo

  3. TX-2012-05-09-02 | Big Bend National Park - 2011

    Relationship of soil mapping units to elevation, geology, and landscape positions. Altuda soils are at elevations around 5,000 feet, and formed from the Santa Elena limestone. Blackgap and Bissett soils formed in residuum and colluvium (Soil Survey of Big Bend National Park, Texas; 2011).

  4. TX-2012-05-09-03 | Big Bend National Park - 2011

    Relationship of soil mapping units, geologic formations, and landscape positions of the Pen Clay, Aguja sandstone, loamy alluvium, and Javelina Formations (Soil Survey of Big Bend National Park, Texas; 2011).

Map Units

Map units containing PANTERA 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
Riverwash and Pantera soils, 0 to 2 percent slopes, frequently floodedRIA5708659627201gtx37720121:31680
Melado-Pantera complex, 1 to 5 percent slopesMPB24464190633321zpmtx37720121:31680
Baviza-Pantera complex, 1 to 8 percent slopes, floodedBAC6940115009517lrvtx37720121:31680
Riverwash and Pantera soils, 0 to 2 percent slopes, frequently floodedRIA1060624068532lsjftx62119821:31680
Riverwash-Pantera complex, 0 to 2 percent slopes, frequently floodedRIA18433588731z84tx62219981:31680
Pantera-Riverwash complex, 0 to 2 percent slopes, frequently floodedPRA385250417828sr0tx62620121:24000
Pantera-Riverwash complex, 0 to 2 percent slopes, frequently floodedPRA18695210914728sr0tx62720121:24000

Map of Series Extent

Approximate geographic distribution of the PANTERA 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 .