Official Series Description


Lab Data Summary

Aggregate lab data for the BREECE soil series. This aggregation is based on all pedons with a current taxon name of BREECE, 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 BREECE 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 BREECE 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 BREECE 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 BREECE 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 BREECE 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 BREECE 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 BREECE 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 BREECE 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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Soil series sharing subgroup-level classification with BREECE, 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 BREECE 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
Breece sandy loam, 2 to 18 percent slopes710897496509jnnfco62719801:24000
Breece sandy loam, 5 to 15 percent slopesCt1645472865hw1qco62820081:24000
Breece sandy loam, 9 to 25 percent slopes14180497418jplrco64119801:24000
Breece coarse sandy loam, 9 to 30 percent slopes20803210282jpvrco64319751:20000
Breece coarse sandy loam, 9 to 30 percent slopes208445497666jpvrco64419801:24000
Breece coarse sandy loam, 3 to 9 percent slopes197942497664jpvpco64419801:24000
Breece coarse sandy loam, 0 to 3 percent slopes18680497663jpvnco64419801:24000
Lone Rock-Breece gravelly sandy loams, 2 to 9 percent slopes271145512699k6hpco65320001:24000
Lininger-Breece gravelly sandy loams, 3 to 12 percent slopes241137512696k6hlco65320001:24000
Lone Rock-Breece gravelly sandy loams, 9 to 15 percent slopes28370512700k6hqco65320001:24000
Breece gravelly sandy loam, 3 to 40 percent slopes3347512675k6gxco65320001:24000
Urban land-Breece complex, 0 to 9 percent slopes6326512735k6jvco65320001:24000
Breece loam, 1 to 6 percent slopes17858496592jnr3co67919761:24000
Breece variant sandy loam, 3 to 8 percent slopesBd2491375669dlxcnm63819811:31680
Falcon, dry-Breece families complex, 3 to 20 percent slopesmt25544032026752zbv9ut6451:24000
Breece-Falcon, dry families complex, 3 to 20 percent slopesmt24287132026742zbv8ut6451:24000
Lupinto family, moist, stony-Breece family, dry association, 2 to 30 percent slopes52416235512503k69cut6461:24000
Breece family-Farnuf family association, 3 to 15 percent slopes433757512384k65jut6461:24000
Boyle, thin solum-Breece-Cathedral complex, 0 to 30 percent slopes1157961044253hnkwy03119981:24000
Ipson-Breece, dry-Evanston complex, 0 to 6 percent slopes137120191049383j63wy72119941:24000
Boyle, thin solum-Breece-Cathedral complex, 0 to 30 percent slopes11454141049153j5cwy72119941:24000
Breece fine sandy loam, 0 to 10 percent slopes11931651049203j5jwy72119941:24000

Map of Series Extent

Approximate geographic distribution of the BREECE 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 .