Official Series Description


Lab Data Summary

Aggregate lab data for the DRINO soil series. This aggregation is based on all pedons with a current taxon name of DRINO, 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 DRINO 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
888P044388WA037008Drino3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties46.7099991,-119.9852753

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the DRINO 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 DRINO 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 DRINO 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 DRINO 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.

There are insufficient data to create the 3D terrace figure.

There are insufficient data to create the 3D flats position figure.

Competing Series

Soil series competing with DRINO 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 DRINO 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 DRINO 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 flats position figure.

Soil series sharing subgroup-level classification with DRINO, 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 DRINO 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
Drino-Sohappy-Fortyday complex, 15 to 30 percent slopes6442813770692l63wa63720081:24000
Fortyday-Drino-Nevo complex, 15 to 30 percent slopes7172286771192l7qwa63720081:24000
Drino-Sohappy-Fortyday complex, 30 to 60 percent slopes6951943771082l7cwa63720081:24000
Drino-Fortyday complex, 3 to 15 percent slopes9221739773022lfmwa63720081:24000
Fortyday-Drino-Nevo complex, 30 to 60 percent slopes7181326771202l7rwa63720081:24000
Drino-Rubble land-Rock outcrop complex, 30 to 75 percent north slopes7741309771512l8rwa63720081:24000
Drino-Fortyday complex, 15 to 30 percent slopes742470771302l82wa63720081:24000
Drino-Sohappy-Fortyday complex, 30 to 45 percent slopes612468710482cxwwa68119941:24000
Fortyday-Drino-Nevo complex, 30 to 45 percent slopes722444711412d0wwa68119941:24000
Fortyday-Drino-Nevo complex, 15 to 30 percent slopes712371711322d0lwa68119941:24000
Fortyday-Drino-Sohappy complex, 30 to 45 percent slopes731573711512d16wa68119941:24000
Drino-Sohappy-Fortyday complex, 45 to 60 percent slopes621128710542cy2wa68119941:24000
Drino cobbly loam, 15 to 30 percent slopes56738710182cwxwa68119941:24000
Drino-Disage-Kiona complex, 30 to 45 percent slopes58712710342cxfwa68119941:24000
Drino very stony loam, 15 to 30 percent slopes57456710242cx3wa68119941:24000
Drino-Rubble land-Rock outcrop complex, 30 to 75 percent slopes59413710362cxhwa68119941:24000
Drino-Rubble land-Rock outcrop complex, 30 to 75 percent north slopes60361710432cxqwa68119941:24000

Map of Series Extent

Approximate geographic distribution of the DRINO 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 .