Official Series Description


Lab Data Summary

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

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

Soil series sharing subgroup-level classification with TWINADAMS, 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 TWINADAMS 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
Blackleaf, stony-Twinadams-Rock outcrop complex, 8 to 35 percent slopes190E57991482314z7nmt60420011:24000
Blackleaf, stony-Twinadams, very stony-Rock outcrop complex, 20 to 60 percent slopes9100F28671482494z87mt60420011:24000
Twinadams-Thunderhead-Blackleaf, stony complex, 8 to 25 percent slopes9101E25201482504z88mt60420011:24000
Pensore, very stony-Ferball, stony-Rock outcrop complex, 4 to 45 percent slopes229F11924508282n88zmt60420011:24000
Blackleaf, stony-Twinadams-Rock outcrop complex, 8 to 35 percent slopes190E883185949320dynmt60520071:24000
Blackleaf, stony-Twinadams, very stony-Rock outcrop complex, 20 to 60 percent slopes9100F94185950520dz1mt60520071:24000
Pensore, very stony-Ferball, stony-Rock outcrop complex, 4 to 45 percent slopes229F1024509712n8flmt60520071:24000
Twinadams-Thunderhead-Blackleaf, stony complex, 15 to 35 percent slopes134E11720797912vs93mt61220111:24000
Twinadams-Blackleaf, very stony-Thunderhead complex, 4 to 15 percent slopes134D4649797911vs92mt61220111:24000
Ferball, stony-Pensore, very stony-Rock outcrop complex, 4 to 45 percent slopes229F416216830541thc2mt61220111:24000
Blackleaf, extremely stony-Twinadams, very stony-Rock outcrop complex, 15 to 60 percent slopes134F217016724771t4bwmt61220111:24000
Twinadams, extremely stony-Blackleaf, extremely stony-Rock outcrop complex, 15 to 35 percent slopes234E132316723871t47zmt61220111:24000
Hayescreek, very stony-Thunderhead, stony-Twinadams, very stony complex, 15 to 50 percent slopes444F114723784502ktz6mt61220111:24000
Blackleaf, stony-Twinadams-Rock outcrop complex, 8 to 35 percent slopes190E58625976714z7nmt61220111:24000
Blackleaf, stony-Twinadams, very stony-Rock outcrop complex, 20 to 60 percent slopes9100F17325976734z87mt61220111:24000
Twinadams, stony-Rentsac complex, cool, 8 to 45 percent slopes75E122014876641ly15mt63720141:24000
Reedpoint-Twinadams complex, 4 to 15 percent slopes770D99714876861ly1wmt63720141:24000
Twinadams-Ruko-like complex, 15 to 50 percent slopes, very bouldery548832090502zdqgwy6291:24000
Colstrip-Bonfri-like-Twinadams complex, 30 to 75 percent slopes552829119312w7k6wy6291:24000
Seminoe-Twinadams complex, 2 to 10 percent slopes70429598472wsx7wy6301:24000
Blackleaf-Rock outcrop-Twinadams complex, 15 to 35 percent slopes71030038422x7bjwy6301:24000
Jemdilon-Rosseau-Twinadams complex, 4 to 25 percent slopes55191714222337082dzc3wy6351:24000
Twinadams-Geohrock families, complex, 10 to 30 percent slopes4045579157882598zwy65620081:24000
Twinadams-Twinadams, dry, families, complex, 10 to 20 percent slopes4034866157881598ywy65620081:24000
Twinadams-Lone Rock families, complex, 10 to 25 percent slopes4087121578865993wy65620081:24000
Twinadams-Barranco complex, 25 to 35 percent slopes272529252832wdk9wy7231:24000

Map of Series Extent

Approximate geographic distribution of the TWINADAMS 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 .