Official Series Description


Lab Data Summary

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

Soil series sharing subgroup-level classification with MCFADDEN, 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 MCFADDEN 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
McFadden gravelly fine sandy loam, 1 to 6 percent slopes1884181045443hsdwy03119981:24000
McFadden-Elk Mountain complex, 2 to 9 percent slopes -- draft12813369186264020j75wy0411:24000
McFadden gravelly fine sandy loam, 1 to 6 percent slopes1889198501731jv2wwy60119911:24000
McFadden-Edlin-Blackhall complex, 5 to 40 percent slopes21933613502329jvq5wy62519851:24000
Rock River-Ryan Park-McFadden complex, 5 to 30 percent slopes26118407502397jvscwy62519851:24000
Rawlins-McFadden-Blackhall complex, 2 to 20 percent slopes2414963502367jvrdwy62519851:24000
Worfstone-McFadden-Lupinto complex, 6 to 50 percent slopes3084723502453jvv5wy62519851:24000
McFadden-Blackhall-Edlin sandy loams, 5 to 50 percent slopes -- draft3175681123764642krx4wy6301:24000
McFadden-Brownsto-Rawlins complex 6 to 20 percent slopes -- draft3213982323781072ktm4wy6301:24000
McFadden-Blackhall sandy loams, 2 to 15 percent slopes -- draft3163469723781002ktlxwy6301:24000
McFadden-Rock River complex, 0 to 6 percent slopes -- draft3232193223780782ktl6wy6301:24000
McFadden-Edlin association, 2 to 20 percent slopes -- draft3221415123767762ks76wy6301:24000
McFadden-Carmody complex, 0 to 15 percent slopes -- draft3431096423785522kv2hwy6301:24000
McFadden-Brownsto complex, 0 to 6 percent slopes -- draft318AB967823849822l1rxwy6301:24000
McFadden-Brownsto complex, 0 to 2 percent slopes -- draft318A833223782682ktsbwy6301:24000
McFadden-Brownsto-Blackhall complex, 6 to 20 percent slopes -- draft320819223778722ktckwy6301:24000
Tisworth-McFadden sandy loams, 0 to 6 percent slopes -- draft340635623784522ktz8wy6301:24000
McFadden-Brownsto complex, 0 to 8 percent slopes -- draft319631223775272kt0fwy6301:24000
McFadden-Brownsto complex, 2 to 6 percent slopes -- draft318B620123782692ktscwy6301:24000
McFadden variant-Browntso variant complex, wet, 0 to 3 percent slopes -- draft318W147623782702ktsdwy6301:24000
Brownsto-Luhon-McFadden complex, 3 to 15 percent slopes1117814503951jxdhwy63819901:24000
McFadden fine sandy loam, 0 to 6 percent slopes1523424504006jxg8wy63819901:24000
McFadden-Brownsto-Rock outcrop complex, 20 to 60 percent slopes1552573504009jxgcwy63819901:24000
Kappes-McFadden fine sandy loams, 2 to 6 percent slopes1411152503991jxfswy63819901:24000
McFadden fine sandy loam, 6 to 10 percent slopes153724504007jxg9wy63819901:24000
McFadden gravelly sandy loam, 2 to 6 percent slopes154329504008jxgbwy63819901:24000
Brownsto-McFadden-Rock outcrop complex, 5 to 60 percent slopes0402926015754758y5wy6471:24000
McFadden-Elk Mountain complex, 2 to 9 percent slopes -- draft412890251874320j75wy7231:24000
Mcfadden fine sandy loam, 2 to 5 percent slopes -- draft22428925546392rbzfwy7231:24000
McFadden-Elk Mountain complex, 2 to 9 percent slopes -- draft71288257257243820j75wy7371:24000
McFadden-Castello complex, 4 to 12 percent slopes -- draft5273312572286jx1xwy7371:24000

Map of Series Extent

Approximate geographic distribution of the MCFADDEN 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 .