Official Series Description


Lab Data Summary

Aggregate lab data for the OLNEST soil series. This aggregation is based on all pedons with a current taxon name of OLNEST, 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 OLNEST 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
67B97P059096CO628004Olnest6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties37.337,-103.1067778

Water Balance

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

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Competing Series

Soil series competing with OLNEST 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 OLNEST 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 OLNEST 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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Click the image to view it full size.

Soil series sharing subgroup-level classification with OLNEST, 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 OLNEST 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
Olnest sandy loam, 1 to 5 percent slopes3237684943212t519co01719851:24000
Olnest-Manzanst complex, 0 to 6 percent slopes3315631943222t51pco01719851:24000
Vona-Olnest complex, warm, 3 to 12 percent slopes52852027667092t51bco01719851:24000
Olnest loamy sand, 0 to 5 percent slopes60104829921902t51hco06119771:24000
Vona-Olnest complex, warm, 3 to 12 percent slopes5472427667082t51bco06119771:24000
Olnest-Ascalon complex, 1 to 6 percent slopes6255989685437sbco06319961:24000
Olnest sandy loam, 1 to 5 percent slopes603210968572t519co06319961:24000
Olnest sandy loam, 6 to 9 percent slopes612803968582t51lco06319961:24000
Olnest sandy loam, 0 to 3 percent slopes161184161052422t51jco07320011:24000
Haxtun-Olnest loamy sands, 0 to 3 percent slopes13863071052193jh5co07320011:24000
Olnest loamy sand, 0 to 5 percent slopes16056711052412t51hco07320011:24000
Olnest sandy loam, 6 to 9 percent slopes16356711052442t51lco07320011:24000
Olnest sandy loam, 1 to 5 percent slopes16218951052432t519co07320011:24000
Olney sandy loam, terrace, 0 to 1 percent slopesOsA18351104563py3co08719651:24000
Olnest sandy loam, 0 to 3 percent slopes124946329920622t51jco62519751:24000
Olnest sandy loam, 3 to 8 percent slopes125730129920642qnmxco62519751:24000
Olnest-Vona complex, cool, 1 to 6 percent slopes, eroded62386928376562t51gco62519751:24000
Olnest sandy loam, cool, 3 to 12 percent slopesOsC1672926088332t51kco62719801:24000
Olnest loam, 1 to 6 percent slopesFtC167821053452t51mco62820081:24000
Olnest sandy loam, 3 to 8 percent slopesOyC670525209572qnmxco62820081:24000
Olnest sandy loam, 0 to 3 percent slopesOyB44181053952t51jco62820081:24000
Olnest sandy loam, cool, 3 to 12 percent slopesOcC208829921992t51kco62820081:24000

Map of Series Extent

Approximate geographic distribution of the OLNEST 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 .