Official Series Description


Lab Data Summary

Aggregate lab data for the ORLIE soil series. This aggregation is based on all pedons with a current taxon name of ORLIE, 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 ORLIE 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 ORLIE 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 ORLIE 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 ORLIE 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 ORLIE 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 ORLIE 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 ORLIE 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 ORLIE 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.

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

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Soil series sharing subgroup-level classification with ORLIE, 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. NM-2010-09-13-05 | McKinley County -

    Generalized cross section illustrating soil-geomorphic-geologic relationships of soils on the Chaco slope of the San Juan Basin (Soil Survey of McKinley County, New Mexico).

  2. NM-2012-02-14-07 | Jicarilla Apache Nation, Parts of Rio Arriba and Sandoval Counties - 2004

    Conceptual diagram of the major soil and landscape positions of the Tapicito Plateau (Soil Survey of Jicarilla Apache Nation, New Mexico, Parts of Rio Arriba and Sandoval Counties; 2004).

Map Units

Map units containing ORLIE 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
Vessilla-Menefee-Orlie complex, 1 to 30 percent slopes110168998561632vd1rnm65019891:24000
Orlie fine sandy loam, 1 to 8 percent slopes10398863561572vd1tnm65019891:24000
Orlie-Nalivag loams, 2 to 8 percent slopes8023496562812wljhnm65019891:24000
Gobernador-Orlie association, 0 to 8 percent slopes3116444562491wjhnm65019891:24000
Vessilla-Menefee-Orlie association, 0 to 30 percent slopes42226540564261wq6nm65619871:24000
Orlie-Sparham association, 0 to 5 percent slopes2422785563711wnfnm65619871:24000
Orlie loam, 0 to 8 percent slopes264577563752vd1vnm65619871:24000
Orlie loam, 0 to 8 percent slopesOiC720729006302vd1vnm6721:24000
Vessilla-Menefee-Orlie complex, 1 to 30 percent slopesVoE207527701702vd1rnm6721:24000
Orlie fine sandy loam, 1 to 8 percent slopesOrC62929006332vd1tnm6721:24000
Gobernador-Orlie association, 0 to 8 percent slopesGoC23627701942tlb4nm6721:24000
Orlie-Cementlake complex, 1 to 6 percent slopesOzC2327702082v5q0nm6721:24000
Orlie-Nalivag loams, 2 to 8 percent slopesOnC2327702042wljhnm6721:24000
Orlie fine sandy loam, 1 to 8 percent slopesOrC582029346012vd1tnm6781:24000
Orlie loam, 0 to 8 percent slopesOiC228929346022vd1vnm6781:24000
Orlie-Lindrith complex, 1 to 15 percent slopesOLC127229425672wllcnm6781:24000
Orlie-Nalivag loams, 2 to 8 percent slopesOnC58829425292wljhnm6781:24000
Orlie-Cementlake complex, 1 to 6 percent slopesOzC12029425762v5q0nm6781:24000
Orlie-Tinian complex, 1 to 6 percent slopes3028445572441xklnm69220011:24000
Orlie-Cementlake complex, 1 to 6 percent slopes57122343574991xttnm69820001:24000
Vessilla-Menefee-Orlie complex, 1 to 30 percent slopes15520618574892vd1rnm69820001:24000
Orlie-Nalivag loams, 2 to 8 percent slopes30419644574942wljhnm69820001:24000
Orlie loam, 0 to 8 percent slopes30319444574932vd1vnm69820001:24000
Orlie fine sandy loam, 1 to 8 percent slopes37018754574962vd1tnm69820001:24000
Orlie-Sparham association, 0 to 5 percent slopes2410237575051xv0nm69820001:24000

Map of Series Extent

Approximate geographic distribution of the ORLIE 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 .