Official Series Description


Lab Data Summary

Aggregate lab data for the PAJARITO soil series. This aggregation is based on all pedons with a current taxon name of PAJARITO, 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 PAJARITO 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
4240A0769S1961NM013009PAJARITO3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties32.4873505,-106.9155731
n/a40A5523S1959NM013012Pajarito3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Propertiesn/a
n/a40A0192S1967NM013003Pajarito4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Propertiesn/a

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the PAJARITO 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 PAJARITO 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 PAJARITO 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 PAJARITO 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 PAJARITO 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 PAJARITO 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 PAJARITO 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 mountains figure.

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Click the image to view it full size.

Soil series sharing subgroup-level classification with PAJARITO, 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 PAJARITO 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
Pajarito-Sonoita complex355339535611sqsaz65919841:24000
Pajarito-Sahuarita complex, 1 to 3 percent slopes4779126546321tvbaz70319931:24000
Glendale-Pajarito complex, 1 to 3 percent slopes308888545891tsyaz70319931:24000
Turney-Pajarito complex, 0 to 2 percent slopes102132940612xhsknm02319671:31680
Largo-Pajarito complex, rarely floodedLP10234376440dmq7nm02519671:20000
Pajarito loamy fine sand, 1 to 9 percent slopesPAC13090556721vxwnm60019731:24000
Pajarito fine sandy loam, 1 to 5 percent slopesPbB9120556771vy1nm60019731:24000
Pajarito fine sandy loamPH4148558191w2mnm61219701:24000
Pajarito loamy fine sandPa2601558211w2pnm61219701:24000
Pajarito loamy fine sand, hummockyPf326558221w2qnm61219701:24000
Berino complex, 0 to 3 percent slopes, erodedBB137875558651w43nm61419661:20000
Pajarito-Dune land complex, 0 to 3 percent slopesPD44483558981w55nm61419661:20000
Pajarito loamy fine sand, 0 to 3 percent slopes, erodedPA33971558971w54nm61419661:20000
Berino-Pajarito complex, 0 to 3 percent slopes, erodedBP5387558671w45nm61419661:20000
Pajarito-Bluepoint complex, hummockyPBB16499375787dm15nm64419811:24000
Alama, dry-Pajarito complex, hummockyASB11106375737dlzknm64419811:24000
Pajarito loamy fine sand, 0 to 3 percent slopesPaA6881375790dm18nm64419811:24000
Canutio-Pajarito association, moderately rolling264536565021wsnnm66019811:48000
Pajarito fine sandy loam662645565501wv6nm66019811:48000
Pajarito loamy sand, 1 to 5 percent slopes65480565491wv5nm66019811:48000
Whitlock-Pajarito-Nations complex, 1 to 8 percent slopes88114914571552tm5hnm66419841:24000
Pajarito-Pintura complexPb21784559791w7snm66619741:24000
Pajarito loamy fine sandPa2358559781w7rnm66619741:24000
Whitlock-Pajarito-Nations complex, 1 to 8 percent slopes889880524042962tm5hnm68820141:24000
Pajarito sandy loam, 0 to 9 percent slopes592103125021302q20fnm68820141:24000
Pajarito-Mcnew complex, 1 to 8 percent slopes618260190647321zv4nm68820141:24000
Pajarito-Adelino-Riverwash complex, 0 to 10 percent slopes60148625021342rh7pnm68820141:24000
Onite-Pajarito associationOP92244634579p9b9nm6901:24000
Pajarito-Pintura complexPb13052634582p9bdnm6901:24000
Pajarito fine sandy loamPa9010634581p9bcnm6901:24000
Monahans-Pajarito association, nearly level1735499585061yw9tx37119771:31680
Monahoans-Pajarito complex, nearly levelMPA11931586081yzltx61519941:31680
Pajarito association, levelPAA8074696635rcx3tx62419671:31680
Monahans-Pajarito complex, 0 to 5 percent slopesMPB798224938762ppw7tx62520101:24000

Map of Series Extent

Approximate geographic distribution of the PAJARITO 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 .