Official Series Description


Lab Data Summary

Aggregate lab data for the ORO FINO soil series. This aggregation is based on all pedons with a current taxon name of ORO FINO, 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 ORO FINO were used in the calculation. Source: KSSL snapshot . Methods used to assemble the KSSL snapshot used by SoilWeb / SDE

There are insufficient data to create the lab data summary figure.


Water Balance

Monthly water balance estimated using a leaky-bucket style model for the ORO FINO 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 ORO FINO 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 ORO FINO 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 ORO FINO 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 flats position figure.

Competing Series

Soil series competing with ORO FINO 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 ORO FINO series and competing. Series are sorted according to hierarchical clustering of median values. Source: SSURGO map unit geometry and 1981-2010, 800m PRISM data .

Click the image to view it full size.

Geomorphic description summaries for the ORO FINO 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.

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

Soil series sharing subgroup-level classification with ORO FINO, 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 ORO FINO 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
Barbarela-Nieman-Oro Fino complex, 2 to 15 percent slopes27D4972609125nfv6mt60420011:24000
Libeg, very stony-Oro Fino-Poin, stony complex, 15 to 60 percent slopes4E1794608779nfh1mt60420011:24000
Oro Fino-Poin complex, 15 to 45 percent slopes94140218596464xgkmt60520071:24000
Oro Fino-Poin complex, 4 to 15 percent slopes93260185964520f3kmt60520071:24000
Oro Fino loam, 2 to 12 percent slopes92157185964420f3jmt60520071:24000
Sebud, very stony-Oro Fino, stony-Nieman, extremely bouldery complex, 15 to 35 percent slopes550E212024244062mcsnmt61220111:24000
Doolittle, stony-Rooset, very stony-Oro Fino complex, 4 to 15 percent slopes539D143824246242md0pmt61220111:24000
Oro Fino, stony-Bridger-Sebud, very stony complex, 4 to 15 percent slopes550D88524244162mcszmt61220111:24000
Sebud, very stony-Oro Fino, stony-Nieman, extremely bouldery complex, 15 to 35 percent slopes550E40625207372mcsnmt61420121:24000
Oro Fino, stony-Bridger-Sebud, very stony complex, 4 to 15 percent slopes550D5525207382mcszmt61420121:24000
Oro Fino-Poin complex, 15 to 45 percent slopes9477517079781vb92mt62319881:24000
Oro Fino-Poin complex, 15 to 45 percent slopes9443117029104xgkmt63520061:24000
Oro Fino-Highrye-Branham complex, 4 to 15 percent slopes312D5617031341v57tmt63520061:24000
Oro Fino-Poin complex, 15 to 45 percent slopes941087861465234xgkmt63619831:24000
Oro Fino-Poin complex, 4 to 15 percent slopes93215021465224xgjmt63619831:24000
Oro Fino loam, 2 to 12 percent slopes9299341465214xghmt63619831:24000
Barbarela-Nieman-Oro Fino complex, 2 to 15 percent slopes2325571466014xk2mt63619831:24000
Highrye-Beeftrail-Oro Fino complex, 1 to 8 percent slopes383C2973362087d4s7mt67020071:24000
Oro Fino-Highrye-Branham complex, 4 to 15 percent slopes312D978362084d4s4mt67020071:24000

Map of Series Extent

Approximate geographic distribution of the ORO FINO 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 .