Official Series Description


Lab Data Summary

Aggregate lab data for the THUNDERBIRD soil series. This aggregation is based on all pedons with a current taxon name of THUNDERBIRD, 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 THUNDERBIRD 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
3840A3596S1965AZ025013Thunderbird7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties34.6603203,-112.6296387
3840A3597S1965AZ025017Thunderbird4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties34.6597214,-112.6516647

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the THUNDERBIRD 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 THUNDERBIRD 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 THUNDERBIRD 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 THUNDERBIRD 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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Competing Series

Soil series competing with THUNDERBIRD 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 THUNDERBIRD 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 THUNDERBIRD 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 THUNDERBIRD, 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. AZ-2011-05-27-07 | Coconino County Area, Central Part - 1983

    Soil-landscape profile in an area north of Seligman (Soil Survey of Coconino County Area, Arizona, Central Part; 1983).

Map Units

Map units containing THUNDERBIRD 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
Showlow-Thunderbird complex, 2 to 25 percent slopes6933175524211rk0az62319941:24000
Thunderbird-Springerville association, strongly sloping49105850526831rtgaz63119801:24000
Thunderbird-Rock outcrop complex, 30 to 60 percent slopes4841390526821rtfaz63119801:24000
Thunderbird-Cabezon complex, 2 to 30 percent slopes4726293526811rtdaz63119801:24000
Cross-Thunderbird-Lava flows complex, 2 to 12 percent slopes3574518133812402yw9jaz63119801:24000
Thunderbird cobbly silty clay loam, 1 to 12 percent slopes6541425542411tfqaz63319941:24000
Thunderbird cobbly clay loam, 0 to 15 percent slopesTDB12240017185401vp8saz63519681:31680
Thunderbird gravelly clay loam, 1 to 5 percent slopesTbC187017185451vp8yaz63519681:31680
Thunderbird cobbly clay loam, 0 to 15 percent slopesTdC46591529311s2gaz63719681:31680
Venezia-Thunderbird complex, 15 to 40 percent slopesVtE39180529441s2waz63719681:31680
Thunderbird-Cabezon complex, 0 to 15 percent slopesThC38812529331s2jaz63719681:31680
Thunderbird cobbly clay loam, 15 to 40 percent slopesTdE24281529321s2haz63719681:31680
Springerville-Thunderbird complex, 0 to 8 percent slopesStB16811529271s2baz63719681:31680
Cabezon-Thunderbird complex, 5 to 15 percent slopesCdC11111528331rz9az63719681:31680
Venezia-Thunderbird complex, 5 to 15 percent slopesVtC525529431s2vaz63719681:31680
Thunderbird cobbly clay loam, 0 to 8 percent slopes98B59939540221t6naz68319741:24000
Thunderbird cobbly clay loam, 8 to 30 percent slopes99D53741540231t6paz68319741:24000
Thunderbird-Rock outcrop complex, 0 to 8 percent slopes101B17172539121t33az68319741:24000
Thunderbird cobbly clay loam, 30 to 50 percent slopes100E16650539111t32az68319741:24000
Thunderbird-Rock outcrop complex, 15 to 30 percent slopes102D13347539131t34az68319741:24000
Thunderbird gravelly clay loam, 0 to 8 percent slopes97B8166540211t6maz68319741:24000
Thunderbird-Chevelon-Rock outcrop complex, 30 to 50 percent slopes103E3330539141t35az68319741:24000
Thunderbird-Showlow complex, 15 to 30 percent slopes105D2893539161t37az68319741:24000
Thunderbird-Roundtop-Rock outcrop complex, 30 to 50 percent slopes, eroded104E1592539151t36az68319741:24000
Thunderbird-Ferno complex, 2 to 23 percent slopes300578081344149730sgsaz6951:24000
Hosta-Thunderbird complex, 1 to 11 percent slopes300154956344149530sfsaz6951:24000
Goldust-Thunderbird complex, 4 to 35 percent slopes300728297344149830sgyaz6951:24000
Cross-Thunderbird-Lava flows complex, 2 to 12 percent slopes3574369344151631kgwaz6951:24000
Luzena-Thunderbird complex, 3 to 20 percent slopes7838538798411vst6az69720051:24000
Luzena-Thunderbird complex, 3 to 20 percent slopes2016880545031tq5az69919931:24000
Thunderbird-Torreon association, undulatingTH8117507787k1d7nm00719741:24000
Torreon-Thunderbird association, gently slopingTT20880375727dlz7nm63819811:31680
Cabezon-Thunderbird-Celsosprings complex, 3 to 25 percent slopes36575233567891x2xnm64819821:48000
Thunderbird-Cabezon association, moderately rolling7914777565581wvgnm66019811:48000
Thunderbird gravelly loam, 1 to 10 percent slopes4051663571011xdznm66419841:24000
Motoqua-Thunderbird association192145261478168j1ksnv75419921:24000

Map of Series Extent

Approximate geographic distribution of the THUNDERBIRD 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 .