Official Series Description


Lab Data Summary

Aggregate lab data for the RAGTOWN soil series. This aggregation is based on all pedons with a current taxon name of RAGTOWN, 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 RAGTOWN 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
2740A32461959NV001004Ragtown4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties39.4728611,-118.7575833
2786P048886CA035005Ragtown5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties40.2007141,-120.0129623

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the RAGTOWN 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 RAGTOWN 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 RAGTOWN 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 RAGTOWN 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 RAGTOWN 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 RAGTOWN 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 RAGTOWN 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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Click the image to view it full size.

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.

Soil series sharing subgroup-level classification with RAGTOWN, 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

No block diagrams are available.

Map Units

Map units containing RAGTOWN 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
Epot-Ragtown-Playas complex, 0 to 2 percent slopes1939692487474jc7zca60820001:24000
Nomazu-Ragtown association485585103462813qm3ca68520061:24000
Ragtown clay loam, strongly saline, 0 to 1 percent slopes1941571643842plz3nv60319711:24000
Ragtown clay loam, slightly saline, 0 to 1 percent slopes1931301643841plz2nv60319711:24000
Ragtown sandy clay loam, 0 to 1 percent slopes195617643840plz1nv60319711:24000
Isolde-Ragtown association MLRA 27432320244747432w36qnv76019941:24000
Isolde-Ragtown association MLRA 27502201344763242w36qnv76119881:24000
Mazuma-Ragtown association7081532476347hzp1nv76119881:24000
Katelana-Sheffit-Ragtown association91755173478527j1ycnv76619941:24000
Katelana-Ragtown-Timpie association84536903478491j1x6nv76619941:24000
Uvada-Ragtown association127133978478618j219nv76619941:24000
Ragtown association91011675478520j1y4nv76619941:24000
Hawsley-Ragtown association12214052475192hygsnv76919861:24000
Trocken-Ragtown association8262699475319hylwnv76919861:24000
Slaw-Ragtown association1160439475186hyglnv76919861:24000
Trocken-Ragtown association28112785476516hzvhnv77019951:24000
Isolde-Ragtown association MLRA 271749914764672w36qnv77019951:24000
Slaw-Ragtown association344414476552hzwnnv77019951:24000
Ragtown association119119039477310j0p3nv77119901:24000
Chuckles-Ragtown-Playas complex78111517477560j0y5nv77119901:24000
Gitakup-Tresed-Ragtown association75010120477555j0y0nv77119901:24000
Ragtown-Isolde complex, 0 to 15 percent slopes11909960477309j0p2nv77119901:24000
Umberland-Ragtown association14438290477368j0qznv77119901:24000
Mazuma-Ragtown association5426772477508j0whnv77119901:24000
Swingler-Ragtown association1935435477416j0sjnv77119901:24000
Typic Torriorthents-Ragtown association15905371477396j0rwnv77119901:24000
Umberland-Playas-Ragtown association14452562477370j0r1nv77119901:24000
Ragtown-Umberland association11922081477311j0p4nv77119901:24000
Ragtown-Swingler-Benin association11941736477313j0p6nv77119901:24000

Map of Series Extent

Approximate geographic distribution of the RAGTOWN 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 .