Official Series Description


Lab Data Summary

Aggregate lab data for the RENO soil series. This aggregation is based on all pedons with a current taxon name of RENO, 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 RENO 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
2640A3153S1959NV005003Reno4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.9269447,-119.6980591
2640A3154S1959NV005004RENO5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.9436111,-119.6980591

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the RENO 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 RENO 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 RENO 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 RENO 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 RENO 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 RENO 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 RENO 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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There are insufficient data to create the 3D flats position figure.

Soil series sharing subgroup-level classification with RENO, 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 RENO 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
Fulstone-Reno complex, 2 to 30 percent slopes31402549331101762ttw3nv62519811:24000
Old Camp-Reno variant-Hyloc association11434329473887hx3pnv62519811:24000
Fulstone-Stucky-Reno association31527534739472w4cxnv62519811:24000
Indian Creek-Reno-Washoe association1768108474236hxgynv62819801:24000
Fulstone-Reno complex, 2 to 30 percent slopes3140529031101832ttw3nv62819801:24000
Reno stony sandy loam, 2 to 8 percent slopes6832586474365hxm3nv62819801:24000
Reno very stony fine sandy loam, 8 to 15 percent slopes681354474364hxm2nv62819801:24000
Fulstone-Reno complex, 2 to 30 percent slopes314033731101872ttw3nv62919751:24000
Fulstone-Reno complex, 2 to 30 percent slopes3140637831101772ttw3nv77219851:24000
Springmeyer-Reno association120530479336j2sgnv77219851:24000
Reno-Saralegui association7873280644162pm9fnv77319811:24000
Reno-Stucky association7883070644163pm9gnv77319811:24000
Reno extremely cobbly sandy loam, 2 to 8 percent slopes66022910644520pmnznv77319811:24000
Saralegui-Haybourne-Reno association66491543644173pm9snv77319811:24000
Reno-Phing-Springmeyer association66071130644523pmp2nv77319811:24000
Reno very cobbly loam, 2 to 8 percent slpoes66051040644522pmp1nv77319811:24000
Holbrook-Greenbrae-Reno association445840644080pm6snv77319811:24000
Indian Creek-Reno-Cassiro association486682644091pm74nv77319811:24000
Phing variant-Reno association785294644160pm9cnv77319811:24000
Washoe-Reno association6817205644230pmcmnv77319811:24000
Fulstone-Reno complex, 2 to 30 percent slopes314210829452312ttw3nv77419851:24000

Map of Series Extent

Approximate geographic distribution of the RENO 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 .