Official Series Description


Lab Data Summary

Aggregate lab data for the BOYLE soil series. This aggregation is based on all pedons with a current taxon name of BOYLE, 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 BOYLE 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
48A91P107091CO055008Boyle7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties37.9305573,-105.2002792
4901N0941S2001WY009002Boyle5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties42.6655006,-105.9383621

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the BOYLE 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 BOYLE 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 BOYLE 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 BOYLE 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 BOYLE 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 BOYLE series and competing. Series are sorted according to hierarchical clustering of median values. Source: SSURGO map unit geometry and 1981-2010, 800m PRISM data .

There are insufficient data to create the annual climate figure.

Geomorphic description summaries for the BOYLE 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.

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 BOYLE, 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 BOYLE 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
Boyle-Jodero families association, 0 to 15 percent slopes96387496569jnqcco62719801:24000
Boyle-Rock outcrop complex, warm, 25 to 55 percent slopes47440498405jqmlco63519791:24000
Boyle very gravelly sandy loam, warm, 4 to 25 percent slopes35880498394jqm7co63519791:24000
Boyle-Jodero families association, 0 to 15 percent slopes520M4679509853k3jwco63620111:24000
Boyle very gravelly sandy loam, 10 to 40 percent slopes746483498338jqkfco63719861:24000
Boyle-Rock outcrop complex, 40 to 60 percent slopes938291498360jql4co63719861:24000
Boyle-Martinsdale complex, 3 to 20 percent slopes89001498349jqksco63719861:24000
Wetmore-Boyle-Rock outcrop complex, 5 to 60 percent slopes117115866497654jpvcco64419801:24000
Farnuf-Boyle-Rock outcrop complex, 10 to 25 percent slopes3221037497679jpw5co64419801:24000
Wetmore-Boyle-Moen complex, 5 to 40 percent slopes11617293497653jpvbco64419801:24000
Boyle gravelly sandy loam, 9 to 30 percent slopes1512907497660jpvkco64419801:24000
Boyle gravelly sandy loam, 3 to 9 percent slopes1412882497659jpvjco64419801:24000
Boyle-Ratake gravelly sandy loams, 9 to 25 percent slopes178147497662jpvmco64419801:24000
Boyle-Ratake gravelly sandy loams, 1 to 9 percent slopes166803497661jpvlco64419801:24000
Boyle-Rock outcrop-Cathedral complex, 5 to 45 percent slopes122383497621jpt9co64419801:24000
Boyle-Boyle, thin solum, gravelly loams, 3 to 6 percent slopes121247497620jpt8co64419801:24000
Cathedral-Boyle complex, 10 to 30 percent slopes12319497622jptbco64419801:24000
Boyle-Rock outcrop complex, 5 to 25 percent slopes117103781044683hpywy03119981:24000
Boyle-Boyle, thin solum gravelly loams, 3 to 6 percent slopes11450591044663hpwwy03119981:24000
Boyle-Lininger association, 1 to 15 percent slopes11625711044673hpxwy03119981:24000
Boyle, thin solum-Breece-Cathedral complex, 0 to 30 percent slopes1157961044253hnkwy03119981:24000
Boyle-Rock outcrop-Cathedral complex, 5 to 45 percent slopes1186811044263hnlwy03119981:24000
Boyle-Rock outcrop complex, 5 to 25 percent slopes12467507501655jv0fwy60119911:24000
Boyle-Lininger association, 1 to 15 percent slopes12553785501657jv0hwy60119911:24000
Boyle-Alderon-Cathedral gravelly sandy loams, 5 to 25 percent slopes12212995501652jv0bwy60119911:24000
Boyle-Boyle, thin solum, gravelly sandy loams, 3 to 6 percent slopes1237163501654jv0dwy60119911:24000
Boyle-Rock outcrop complex, 5 to 25 percent slopes1144065816696621t1f2wy60920061:24000
Boyle-Lininger loams, 1 to 15 percent slopes1133079816697861t1k2wy60920061:24000
Cathedral-Boyle family, moist-Argic Cryaquolls association, 5 to 25 percent slopes702B708667rsf7wy6221:24000
Boyle family, moist- Rock outcrop complex, 0 to 20 percent slopes237BK708652rsdrwy6221:24000
Wetmore family, stony-Boyle family, moist, complex, 2 to 30 percent slopes239B708659rsdzwy6221:24000
Boyle-Boyle, thin solum, gravelly loams, 3 to 6 percent slopes113177401049143j5bwy72119941:24000
Boyle-Lininger-Boyle, thin solum, complex, 3 to 45 percent slopes116135891049173j5fwy72119941:24000
Boyle-Rock outcrop-Cathedral complex, 5 to 45 percent slopes117111601049183j5gwy72119941:24000
Boyle-Lininger association, 1 to 15 percent slopes11883951049193j5hwy72119941:24000
Cathedral-Boyle complex, 10 to 30 percent slopes12372011049243j5nwy72119941:24000
Boyle, thin solum-Breece-Cathedral complex, 0 to 30 percent slopes11454141049153j5cwy72119941:24000
Boyle-Alderon-Cathedral complex, 5 to 45 percent slopes11254081049133j59wy72119941:24000
Boyle, very stony-Boyle, thin solum-Lininger complex, 20 to 45 percent slopes11531251049163j5dwy72119941:24000

Map of Series Extent

Approximate geographic distribution of the BOYLE 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 .