Official Series Description


Lab Data Summary

Aggregate lab data for the MCCAREY soil series. This aggregation is based on all pedons with a current taxon name of MCCAREY, 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 MCCAREY 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
1040A1099S1958ID013016McCarey6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties43.3240662,-113.6406021

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the MCCAREY 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 MCCAREY 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 MCCAREY 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 MCCAREY 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 MCCAREY 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 MCCAREY 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 MCCAREY 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 terrace figure.

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

Soil series sharing subgroup-level classification with MCCAREY, 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. ID-2010-08-31-12 | Wood River Area, Gooding County and Parts of Blaine, Lincoln, and Minidoka Counties - 2005

    Typical pattern of soils and underlying material in general soil map unit 7 (Soil Survey of Wood River Area, Idaho; 2005).

Map Units

Map units containing MCCAREY 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
McCarey-Justesen-Rock outcrop complex, 2 to 15 percent slopes7516464793642nl4id68019851:24000
McCarey-Justesen loams, 2 to 8 percent slopes743123793632nl3id68019851:24000
McCarey-Beartrap complex, 1 to 6 percent slopes11341505818412r51id68119931:24000
McCarey-Molyneux-Rock outcrop complex, 2 to 15 percent slopes11628820818442r54id68119931:24000
McCarey-Beartrap-Rock outcrop complex, 2 to 15 percent slopes11523900818432r53id68119931:24000
McCarey-Beartrap complex, 6 to 20 percent slopes1144500818422r52id68119931:24000
McCarey-Pedleford complex, 8 to 20 percent slopes117820818452r55id68119931:24000
McCarey-Rock outcrop complex, undulating3540786826102ryvid70919761:24000
McCarey-Molyneux-Rock outcrop complex, 2 to 15 percent slopes1163510692128r76qid70919761:24000
McCarey-Beartrap complex, 1 to 6 percent slopes114838692124r76lid70919761:24000
McCarey-Beartrap-Rock outcrop complex, 2 to 15 percent slopes1152692127r76pid70919761:24000
Lava flows-McCarey-McCarey variant complex, 1 to 8 percent slopes747114829492s9sid71119831:24000
Arbone-McCarey-Lava flows complex, 4 to 12 percent slopes41076829112s8kid71119831:24000
Hutchley-Araveton-McCarey complex, 4 to 40 percent slopes44926199062v06xid7131:24000
Hutchley-Araveton-McCarey complex, 4 to 40 percent slopes441413731635932v06xid71519941:24000
McCarey-Vickton-Lava flows complex, 0 to 15 percent slopes6944248790892n98id76319981:24000
McCarey-Beartrap complex, 1 to 6 percent slopes6434988790842n93id76319981:24000
McCarey-Beartrap-Rock outcrop complex, 2 to 15 percent slopes6613252790862n95id76319981:24000
McCarey-Splittop-Lava flows complex, 4 to 8 percent slopes6810364790882n97id76319981:24000
McCarey-Molyneux-Lava flows complex, 2 to 15 percent slopes673092790872n96id76319981:24000
McCarey-Beartrap complex, 6 to 20 percent slopes651243790852n94id76319981:24000
Tenno-Splittop-McCarey complex, 1 to 4 percent slopes129160789552n4yid76319981:24000
McCarey-Beartrap-Rock outcrop complex, 2 to 15 percent slopes392173515314271ndkwid78019981:24000
McCarey-Beartrap complex, 1 to 6 percent slopes372125515314191ndkmid78019981:24000
McCarey-Pedleford complex, 2 to 30 percent slopes431516615316071ndrpid78019981:24000
McCarey-Molyneux complex, 2 to 8 percent slopes411036115316031ndrkid78019981:24000
McCarey-Molyneux-Rock outcrop complex, 2 to 15 percent slopes42897515316051ndrmid78019981:24000
McCarey-Beartrap complex, 6 to 20 percent slopes38429915314251ndktid78019981:24000
McCarey-Rock outcrop complex, 0 to 12 percent slopes4592715316111ndrtid78019981:24000
McCarey-Pedleford complex, 8 to 20 percent slopes4446815316091ndrrid78019981:24000
McCarey-Splittop-Lava flows complex, 4 to 8 percent slopes4637515316131ndrwid78019981:24000
McCarey-Justesen complex, 2 to 8 percent slopes403715316001ndrgid78019981:24000
Cloud Rim, dry-McCarey loams, 4 to 15 percent slopesCBD1730503817jx85ut60419801:24000
Preussrange family-McCarey family-Pernty family, extremely stony complex, 10 to 40 percent slopes27C3997796586vqxbut6511:24000
McCarey-Everry-Watkins Ridge families complex, 8 to 25 percent slopes30C2474791111vk6qut6511:24000

Map of Series Extent

Approximate geographic distribution of the MCCAREY 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 .