Official Series Description


Lab Data Summary

Aggregate lab data for the THREETOP soil series. This aggregation is based on all pedons with a current taxon name of THREETOP, 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 THREETOP 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 THREETOP 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 THREETOP 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 THREETOP 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 THREETOP 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 THREETOP 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 THREETOP 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 THREETOP 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 THREETOP, 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 THREETOP 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
Threetop-Sunup complex, 3 to 15 percent slopes2095416349720cqx9wy02719931:24000
Threetop-Deertrail-like complex, 0 to 8 percent slopes5A0133566872zb04wy04319761:24000
Threetop-Worf-like-Maysdorf complex, 0 to 15 percent slopes520733566662w7kmwy04319761:24000
Eaglenest-Threetop-Olney complex, 1 to 10 percent slopes520131708782wxmpwy6031:24000
Rencalson-Badland-Threetop complex, 30 to 60 percent slopes545731708892wxmwwy6031:24000
Sunup-Threetop-Rock outcrop complex, 10 to 40 percent slopes2371417616697372yv77wy60920061:24000
Threetop-Deertrail-like complex, 0 to 8 percent slopes5A0131970372zb04wy6171:24000
Bowbac-Worf-Threetop complex, 2 to 15 percent slopes5C0431970382zb05wy6171:24000
Strych-Kamms-Threetop complex, 10 to 35 percent slopes541931970432wxk4wy6171:24000
Chinchin-like-Threetop-Sunup-like complex, 6 to 40 percent slopes5D0733028433013wwy6171:24000
Threetop-Hiland-like-Chugcity complex, 2 to 15 percent slopes723319704653v2wy6171:24000
Olney-Threetop complex, 2 to 30 percent slopes5C06335823830zs1wy6171:24000
Terro-like-Redspear-Threetop complex, 3 to 60 percent slopes5D17335823730zs0wy6171:24000
Begay-Threetop complex, 6 to 60 percent slopes5D14335823330zrwwy6171:24000
Threetop-Worf-like-Maysdorf complex, 0 to 15 percent slopes520731708462w7kmwy6171:24000
Windwhistle-Threetop complex, 2 to 10 percent slopes521131708472w7k9wy6171:24000
Pokeman-Threetop loams, 2 to 12 percent slopes239185816888wf17wy61919711:24000
Threetop-Sunup-Frontier complex, 3 to 20 percent slopes284199125024202yb80wy62519851:24000
Pokeman-Threetop loams, 2 to 12 percent slopes2391515502365jvrbwy62519851:24000
Renohill-Threetop-Hiland complex, 1 to 4 percent slopes510632532562zyb9wy6291:24000
Rencalson-Badland-Threetop complex, 30 to 60 percent slopes545729691022wxmwwy6291:24000
Eaglenest-Threetop-Olney complex, 1 to 10 percent slopes520129690962wxmpwy6291:24000
Threetop, stony-Milldraw, very stony-Mesa-like, stony complex, 15 to 40 percent slopes542229690612wxljwy6291:24000
Strych-Kamms-Threetop complex, 10 to 35 percent slopes541929690372wxk4wy6291:24000
Threetop-Worf-like-Maysdorf complex, 0 to 15 percent slopes520729119442w7kmwy6291:24000
Windwhistle-Threetop complex, 2 to 10 percent slopes521129119342w7k9wy6291:24000
Terro-like-Redspear-Threetop complex, 3 to 60 percent slopes5D17325333030zs0wy6291:24000
Threetop-Hiland-like-Chugcity complex, 2 to 15 percent slopes72315264653v2wy6291:24000
Olney-Threetop complex, 2 to 30 percent slopes5C06325333130zs1wy6291:24000

Map of Series Extent

Approximate geographic distribution of the THREETOP 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 .