Official Series Description


Lab Data Summary

Aggregate lab data for the PALINOR soil series. This aggregation is based on all pedons with a current taxon name of PALINOR, 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 PALINOR 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
28B81P0663S1981NV033025PALINOR6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.9893875,-114.7303009
28B06N0242S2005NV007001Palinor8Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties40.9032516,-114.8570023

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the PALINOR 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 PALINOR 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 PALINOR 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 PALINOR 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 PALINOR 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 PALINOR 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 PALINOR 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 hills figure.

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 PALINOR, 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

Click a link below to display the diagram. Note that these diagrams may be from multiple survey areas.

  1. NV-2012-05-09-27 | Western White Pine County Area, Parts of White Pine and Eureka Counties - 1998

    The location of individual map unit components on a bolson landscape (Soil Survey of Western White Pine County Area, Nevada, Parts of White Pine and Eureka Counties; 1998).

Map Units

Map units containing PALINOR 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
Palinor-Parisa association38056326340102wbhfnv62119711:24000
Palinor-Urmafot association28375725898632r374nv76420211:24000
Palinor-Automal association4299125114352q8zpnv76420211:24000
Shabliss-Palinor association48037939478348j1rlnv76619941:24000
Palinor-Automal association42124074478328j1qynv76619941:24000
Palinor very gravelly loam, 2 to 15 percent slopes3212395626339622t6gwnv76619941:24000
Palinor-Urmafot association53205364781842t6h6nv76619941:24000
Palinor-Automal-Palinor, eroded association429169414783362wbj0nv76619941:24000
Palinor-Pharo-Hundraw association18614398478249j1ndnv76619941:24000
Palinor-Automal-Shabliss association85412374478500j1xhnv76619941:24000
Palinor-Parisa association856118384785022wbhfnv76619941:24000
Palinor-Shabliss-Linoyer association85710554478503j1xlnv76619941:24000
Palinor-Automal-Wintermute association42610553478333j1r3nv76619941:24000
Palinor-Automal-Izar association1887999478251j1ngnv76619941:24000
Zafod-Pyrat-Palinor association2307743478265j1nxnv76619941:24000
Palinor-Zimbob-Tecomar association8517558478497j1xdnv76619941:24000
Izar-Palinor-Shabliss association2515531478274j1p6nv76619941:24000
Palinor-Pyrat-Shabliss association8525404478498j1xfnv76619941:24000
Palinor-Hundraw-Okan association4245247478331j1r1nv76619941:24000
Hundraw-Shabliss-Palinor association2444649478272j1p4nv76619941:24000
Sodhouse-Palinor association4974453478360j1rznv76619941:24000
Palinor-Wintermute-Okan association8504332478496j1xcnv76619941:24000
Palinor-Automal-Linoyer association8583762478504j1xmnv76619941:24000
Palinor-Zimbob-Okan association4222972478329j1qznv76619941:24000
Palinor very gravelly loam, 2 to 15 percent slopes28457226340472rn2knv77619831:63360
Palinor-Yody-Broland association62881069722157832dcpwnv77820131:24000
Palinor-Urmafot-Palinor association6296809022157852dcpynv77820131:24000
Palinor-Palinor, moderately steep association4516785625842322r1gbnv77820131:24000
Urmafot-Palinor association1282765722156232dcjqnv77820131:24000
Palinor, moist-Urmafot association4608696526326412rfwwnv77820131:24000
Palinor very gravelly loam, 2 to 15 percent slopes6321524422157872t6gwnv77820131:24000
Palinor-Urmafot-Urmafot, very shallow association6292300522157842dcpxnv77820131:24000
Palinor-Urmafot association6283194122156712dcl8nv77820131:24000
Palinor-Parisa association3302185722156902dclwnv77820131:24000
Palinor-Shabliss association6286106922157812dcptnv77820131:24000
Urmafot-Bobs-Palinor association632381322157882dcq1nv77820131:24000
Palinor-Wintermute association628759722157822dcpvnv77820131:24000
Zimbob-Palinor association611936522157702dcpgnv77820131:24000
Yody-Palinor-Shabliss association657320322158032dcqjnv77820131:24000
Parisa-Palinor-Shabliss association63346922157902dcq3nv77820131:24000
Palinor-Izar-Biken association12873922156242dcjrnv77820131:24000
Shabliss-Palinor association106010301479928j3dknv77920041:24000
Palinor-Tulase-Izar association30257253479989j3gjnv77920041:24000
Automal-Izar-Palinor association31436572480011j3h7nv77920041:24000
Palinor-Urmafot association30246109479988j3ghnv77920041:24000
Urmafot-Palinor-Shree association34104710480068j3k2nv77920041:24000
Palinor-Urmafot-Urmafot, very shallow association10511940479927j3djnv77920041:24000
Palinor-Automal-Palinor, eroded association42901930114449617dy7nv77920041:24000
Palinor-Shabliss association10521306636698pcjnnv77920041:24000
Palinor-Urmafot-Palinor association629632528172542tzhznv77920041:24000
Palinor very gravelly loam, 2 to 15 percent slopes2821684034803962t6gwnv78019901:24000
Palinor-Urmafot association538381726339352t6h6nv78019901:24000
Palinor-Shabliss association28679203480400j3wsnv78019901:24000
Palinor-Shabliss-Tulase association29029348480404j3wxnv78019901:24000
Urmafot-Bobs-Palinor association32328780480419j3xdnv78019901:24000
Palinor-Urmafot-Urmafot, very shallow association29225148480406j3wznv78019901:24000
Palinor-Yody-Broland association28821586480402j3wvnv78019901:24000
Parisa-Palinor-Shabliss association33417890480430j3xrnv78019901:24000
Urmafot-Palinor association128214439480222j3q1nv78019901:24000
Palinor-Roden association29514001480409j3x2nv78019901:24000
Palinor-Parisa association380133074804552wbhfnv78019901:24000
Shabliss-Pyrat-Palinor association45810659480490j3zpnv78019901:24000
Palinor-Molion-Broland association12809015480220j3pznv78019901:24000
Palinor-Wintermute association2878897480401j3wtnv78019901:24000
Sodhouse-Palinor association18218149480325j3tcnv78019901:24000
Zimbob-Palinor association1196094480191j3p1nv78019901:24000
Palinor-Urmafot-Roden association3266072480422j3xhnv78019901:24000
Parisa-Palinor-Tulase association3386025480434j3xwnv78019901:24000
Yody-Palinor-Shabliss association5735244480533j412nv78019901:24000
Palinor-Izar-Biken association12874545480226j3q5nv78019901:24000
Palinor-Roden-Urmafot association3223625480418j3xcnv78019901:24000
Biken-Palinor-Barfan association12422115480207j3pknv78019901:24000
Pyrat-Palinor-Tulase association14911449480277j3rtnv78019901:24000
Palinor-Parisa association330240276480950j4gjnv78319911:24000
Handpah-Palinor-Parisa association333434243480955j4gpnv78319911:24000
Palinor very gravelly loam, 2 to 15 percent slopes3300324724809482t6gwnv78319911:24000
Palinor-Nuc association330111596480949j4ghnv78319911:24000
Palinor-Urmafot association460860028172782tzjznv78319911:24000
Palinor-Urmafot-Urmafot, very shallow association121130591481145j4ntnv78420061:24000
Palinor very gravelly loam, 2 to 15 percent slopes1210109684811442t6gwnv78420061:24000
Urmafot-Bobs-Palinor association12004410481143j4nrnv78420061:24000
Palinor-Yody-Broland association1212158481146j4nvnv78420061:24000

Map of Series Extent

Approximate geographic distribution of the PALINOR 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 .