Official Series Description


Lab Data Summary

Aggregate lab data for the AUTOMAL soil series. This aggregation is based on all pedons with a current taxon name of AUTOMAL, 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 AUTOMAL 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
28B89P057089NV007005Automal7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties40.143055,-114.7877808

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the AUTOMAL 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 AUTOMAL 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 AUTOMAL 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 AUTOMAL 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 AUTOMAL 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 AUTOMAL 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 AUTOMAL 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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Soil series sharing subgroup-level classification with AUTOMAL, 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 AUTOMAL 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
Palinor-Automal association4299125114352q8zpnv76420211:24000
Wintermute-Automal association49059705478354j1rsnv76619941:24000
Palinor-Automal association42124074478328j1qynv76619941:24000
Palinor-Automal-Palinor, eroded association429169414783362wbj0nv76619941:24000
Automal-Okan-Wintermute association50315609478364j1s3nv76619941:24000
Palinor-Automal-Shabliss association85412374478500j1xhnv76619941:24000
Automal-Wintermute association504114944783652wbjbnv76619941:24000
Palinor-Automal-Wintermute association42610553478333j1r3nv76619941:24000
Pyrat-Automal-Gravier association11719754478592j20gnv76619941:24000
Zafod-Automal-Okan association10708975478578j200nv76619941:24000
Okan-Automal association11208018478584j206nv76619941:24000
Palinor-Automal-Izar association1887999478251j1ngnv76619941:24000
Zerk-Automal-Linoyer association9006042478518j1y2nv76619941:24000
Gravier-Automal-Zerk association1185465478220j1mgnv76619941:24000
Wintermute-Pyrat-Automal association4945014478358j1rxnv76619941:24000
Pyrat-Parisa-Automal association10074589478561j1zgnv76619941:24000
Palinor-Automal-Linoyer association8583762478504j1xmnv76619941:24000
Okan-Automal-Hundraw association4603595478345j1rhnv76619941:24000
Pyrat-Automal association11731620478594j20jnv76619941:24000
Pyrat-Automal, very stony-Automal association11721596478593j20hnv76619941:24000
Automal-Izar-Palinor association31436572480011j3h7nv77920041:24000
Automal-Shabliss association31422260480010j3h6nv77920041:24000
Palinor-Automal-Palinor, eroded association42901930114449617dy7nv77920041:24000
Automal-Wintermute association113093479936j3dtnv77920041:24000
Automal-Wintermute association373428594804532wbjbnv78019901:24000
Automal gravelly silt loam, 2 to 4 percent slopes3728355480452j3ygnv78019901:24000

Map of Series Extent

Approximate geographic distribution of the AUTOMAL 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 .