Official Series Description


Lab Data Summary

Aggregate lab data for the ROSITAS soil series. This aggregation is based on all pedons with a current taxon name of ROSITAS, 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 ROSITAS 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
3140A3413S1969CA025012ROSITAS7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties32.7086105,-115.0522232
4073C0016S1973AZ027007Rositas5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties32.9139709,-113.5418701

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the ROSITAS 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 ROSITAS 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 ROSITAS 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 ROSITAS 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 ROSITAS 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 ROSITAS 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 ROSITAS 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 ROSITAS, 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-2011-05-27-08 | Colorado River Indian Reservation - 1986

    Soil landscape profile (Soil Survey of Colorado River Indian, Reservation, Arizona; 1986)

  2. AZ-2012-05-09-01 | Colorado River Indian Reservation - November 1986

    Soil landscape profile (Soil Survey of Colorado River Indian Reservation, Arizona—California; November 1986).

Map Units

Map units containing ROSITAS 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
Rositas, superstition family and torriorthents soils, 1 to 60 percent slopes1092342415079721mm58az62720051:24000
Rositas family, superstition and torriorthents soils, 1 to 60 percent slopes108450215079711mm57az62720051:24000
Rositas sand2565423532731sfhaz64919781:24000
Tremant-Rositas complex3151124532801sfqaz64919781:24000
Rositas-Ligurta complex2612679532741sfjaz64919781:24000
Wellton-Dateland-Rositas complex347277532831sftaz64919781:24000
Rositas-Denure loamy fine sands, 1 to 10 percent slopes574539534781sn3az65319851:24000
Superstition-Rositas association, 0 to 15 percent slopes2936970547941v0kaz65619831:20000
Superstition-Coolidge-Rositas family complex, dry, 0 to 6 percent slopes3708642624402982mxb9az6571:24000
Superstition-Rositas family complex, dry, 0 to 25 percent slopes2356066524205542m7sdaz6571:24000
Rositas family-Superstition complex, 1 to 15 percent slopes6304069029338312tdtfaz6571:24000
Casa Grande-Rositas family complex, 0 to 8 percent slopes2301385724205522m7sbaz6571:24000
Rositas-Casa Grande-Slickspots complex, 1 to 15 percent slopes303010543011thnaz65819911:24000
Rositas loamy fine sand, sodic, 0 to 3 percent slopes312072543031thqaz65819911:24000
Rositas loamy fine sand406834535671sqzaz65919841:24000
Rositas sand, 4 to 30 percent slopes1311454798506vsx8az69720051:24000
Casa Grande-Rositas-Valencia complex, 0 to 5 percent slopes983178546821twyaz70319931:24000
Rositas loamy fine sand, 2 to 5 percent slopes542802546501tvxaz70319931:24000
Rositas loamy coarse sand, 2 to 9 percent slopesRsC19278456919hbgbca63819671:24000
Rositas fine sand, 0 to 2 percent slopesRoA13081456916hbg7ca63819671:24000
Rositas loamy coarse sand, 0 to 2 percent slopesRsA7529456918hbg9ca63819671:24000
Rositas loamy coarse sand, 9 to 15 percent slopesRsD1781456920hbgcca63819671:24000
Rositas fine sand, hummocky, 5 to 9 percent slopesRrC1725456917hbg8ca63819671:24000
Carsitas-Rositas-Buzzardsprings complex, 0 to 5 percent slopes70415823344153931hlyca68119681:24000
Rositas fine sand, 0 to 2 percent slopesRoA122443441533319g7ca68119681:24000
Rositas silty clay loam, 0 to 2 percent slopesRtA60963441631319g9ca68119681:24000
Rositas gravelly loamy sand, 0 to 2 percent slopesRsA2613464089hkxmca68119681:24000
Rositas fine sand, 2 to 9 percent slopesRoB25763441575319g8ca68119681:24000
Rositas fine sand, wet, 0 to 2 percent slopesRrA453464088hkxlca68119681:24000
Rositas silty clay loam, wet, 0 to 2 percent slopesRuA413464091hkxpca68119681:24000
Rositas loamy fine sand, 0 to 2 percent slopes13690253344164031hllca68319761:24000
Rositas fine sand, 0 to 2 percent slopes1327867334416262mxlnca68319761:24000
Rositas fine sand, wet1352299234415782mxlrca68319761:24000
Rositas sand, 0 to 2 percent slopes1302209234415762mxlqca68319761:24000
Rositas fine sand, 9 to 30 percent slopes13419900344163831hlkca68319761:24000
Rositas-Superstition loamy fine sands13811373455527h90fca68319761:24000
Rositas fine sand, 2 to 9 percent slopes133578734416292mxlpca68319761:24000
Rositas silt loam, 0 to 2 percent slopes137376934415942myt7ca68319761:24000
Rositas sand, 2 to 5 percent slopes131139734415732mxlmca68319761:24000
Rositas complex, 2 to 30 percent slopes2719107225355162qptfca6951:24000
Rositas-Holtville complex, 0 to 1 percent slopes272256625355142qptcca6951:24000
Rositas sandy loam, 0 to 1 percent slopes272056025355122qpt9ca6951:24000
Rositas-Cibola association, 0 to 4 percent slopes272134925355132qptbca6951:24000
Nonamewash-Rositas association880352535505hr07ca6951:24000
Carrizo-Orita-Rositas association, 0 to 8 percent slopes5516975466717hnndca69720001:24000
Rositas complex, 4 to 30 percent slopes1401172466614hnk2ca69720001:24000
Rositas-Carrizo-Bunkerhill association, 2 to 30 percent slopes141507466590hnj9ca69720001:24000
Rositas sand, 4 to 30 percent slopes15123133229666hnrdca6991:24000
Rositas sand, 0 to 2 percent slopes1304863734415772mxlqca8031:24000
Rositas fine sand, 9 to 30 percent slopes13445637344163931hlkca8031:24000
Carsitas-Rositas-Buzzardsprings complex, 0 to 5 percent slopes70422377344165231hlyca8031:24000
Rositas-Lagunita frequently ponded complex, 2 to 35 percent slopes115916034416122y0mrca8031:24000
Carsitas non gravely-Rositas-Carsitas complex, 0 to 1 percent slopes, rarely flooded and frequently flooded110613634416042qptyca8031:24000
Rositas fine sand, 2 to 9 percent slopes13357873441630319g8ca8031:24000
Rizzo-Rositas-Lagunita very rarely flooded complex, 0 to 15 percent slopes15DD508534416172ywzxca8031:24000
Rositas-Forddry-Teaque association, 0 to 35 percent slopes, frequently ponded114349634416112y0mqca8031:24000
Rositas fine sand, 0 to 2 percent slopes1325233441627319g7ca8031:24000
Rositas fine sand, wet13513434415792mxlrca8031:24000
Rositas silt loam, 0 to 2 percent slopes1371434415952myt7ca8031:24000
Rositas fine sand, 0 to 2 percent slopes13239834416282mxlnca8041:24000
Rositas fine sand, wet1351934415802mxlrca8041:24000
Sandpan-Rositas associationSAE33017124451vgy5nv60819671:24000
Azsand-Mesabase-Rositas association9653457469026hr1wnv75520061:24000
Rositas-Riverbend association5602973468909hqy3nv75520061:24000
Nonamewash-Rositas association8802709468975hr07nv75520061:24000
Sandpan-Rositas association3252415601449n5vlnv75520061:24000

Map of Series Extent

Approximate geographic distribution of the ROSITAS 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 .