Official Series Description


Lab Data Summary

Aggregate lab data for the BLIMO soil series. This aggregation is based on all pedons with a current taxon name of BLIMO, 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 BLIMO 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
28B89P056789NV007002Blimo7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties40.6236115,-115.1324997

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the BLIMO 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 BLIMO 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 BLIMO 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 BLIMO 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 BLIMO 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 BLIMO 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 BLIMO 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 BLIMO, 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 BLIMO 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
Blimo-Kunzler-Linoyer association121017087478605j20wnv76619941:24000
Blimo-Threesee association121313764478607j20ynv76619941:24000
Heist-Blimo association129012366478622j21fnv76619941:24000
Blimo-Idway-Mazuma association12168316478610j211nv76619941:24000
Kunzler-Pyrat-Blimo association8236431478478j1wsnv76619941:24000
Pyrat-Blimo association10066045478560j1zfnv76619941:24000
Okan-Eastwell-Blimo association10205486478566j1zmnv76619941:24000
Blimo-Zorravista association12154881478609j210nv76619941:24000
Mazuma-Blimo-Wintermute association8472990478493j1x8nv76619941:24000
Blimo-Kunzler-Pern association9909026340432rn2fnv77619831:63360
Sheffit-Blimo association161038341480299j3sjnv78019901:24000
Blimo-Zerk association99112675480654j44znv78019901:24000
Blimo-Kunzler-Pern association99011010480653j44ynv78019901:24000
Blimo-Pyrat association17410829480312j3synv78019901:24000
Blimo-Uwell association6039380480544j41fnv78019901:24000
Blimo-Linoyer-Tulase association9927375480655j450nv78019901:24000
Yody-Blimo-McConnel association5704763480530j40znv78019901:24000
Blimo-Heist-Tosser association6054370480546j41hnv78019901:24000
Blimo-Nyak-Raph association6023875480543j41dnv78019901:24000
Blimo-Hessing-Zerk association1703485480307j3ssnv78019901:24000
Broyles-Blimo association4722930480495j3zvnv78019901:24000
Katelana-Blimo association2462490480366j3vpnv78019901:24000
Kunzler-Blimo-Uwell association6452035480563j421nv78019901:24000
Ilton-Yody-Blimo association18101652480321j3t7nv78019901:24000

Map of Series Extent

Approximate geographic distribution of the BLIMO 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 .