Official Series Description


Lab Data Summary

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

Click the image to view it full size.

Click the image to view it full size.

Click the image to view it full size.

There are insufficient data to create the 3D terrace figure.

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

Competing Series

Soil series competing with WITHERELL 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 WITHERELL 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 WITHERELL 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 .

There are insufficient data to create the 2D hillslope position figure.

There are insufficient data to create the 3D hills figure.

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 WITHERELL, 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

Click a link below to display the diagram. Note that these diagrams may be from multiple survey areas.

  1. CA-2011-05-27-04 | Mendocino County, Eastern Part, and Trinity County, Southwestern Part - 1991

    Pattern of terraces in Ukiah Valley and adjacent mountains (Soil Survey of Mendocino County, Eastern Part, and Trinity County, Southwestern Part, California; 1991).

Map Units

Map units containing WITHERELL 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
Hopland-Witherell-Ashokawna complex, 30 to 50 percent slopes, MLRA 5149em16077192w91tca09719681:20000
Ashokawna-Garcia-Witherell complex, 15 to 50 percent slopes205wm16074641qyppca09719681:20000
Bearwallow-Hellman-Witherell complex, 30 to 50 percent slopes105em16076181qyvnca09719681:20000
Ashokawna-Witherell complex, 15 to 50 percent slopes, MLRA 5201em16076272w91rca09719681:20000
Ashokawna-Witherell complex, 50 to 75 percent slopes, MLRA 5202em16076292w91qca09719681:20000
Witherell-Hopland-Ashokawna complex, 50 to 75 percent slopes, high ffd211em16076302xkbsca09719681:20000
Yorkville-Ashokawna Witherell complex, 30 to 50 percent slopes, MLRA 5233em16076362w916ca09719681:20000
Dryfield-Yorknorth-Witherell complex, 5 to 30 percent slopes66729942747684v6lhca60020171:24000
Yorknorth-Witherell complex, 15 to 30 percent slopes65518692747679hs85ca60020171:24000
Yorknorth-Witherell complex, 30 to 50 percent slopes66218202747682v6lgca60020171:24000
Dryfield-Yorknorth-Witherell complex, 30 to 50 percent slopes66872827476852lgsjca60020171:24000
Yorknorth-Witherell complex, 2 to 15 percent slopes657482747680hs87ca60020171:24000
Yorknorth-Witherell complex, 15 to 30 percent slopes65522002470182hs85ca60120111:24000
Yorknorth-Witherell complex, 30 to 50 percent slopes66213344780904v6lgca60120111:24000
Dryfield-Yorknorth-Witherell complex, 5 to 30 percent slopes6675817780905v6lhca60120111:24000
Dryfield-Yorknorth-Witherell complex, 30 to 50 percent slopes668282723974942lgsjca60120111:24000
Yorknorth-Witherell complex, 2 to 15 percent slopes657683470184hs87ca60120111:24000
Yorknorth-Witherell complex, 30 to 50 percent slopes66214661451950v6lgca60520131:24000
Yorknorth-Witherell complex, 15 to 30 percent slopes6557472670255hs85ca60520131:24000
Yorkville-Ashokawna Witherell complex, 30 to 50 percent slopes, MLRA 5233592034611182w916ca68719851:24000
Shortyork-Yorkville-Witherell complex, 30 to 50 percent slopes, MLRA 5200357704610852w914ca68719851:24000
Hopland-Witherell-Ashokawna complex, 30 to 50 percent slopes, MLRA 5149299204610342w91tca68719851:24000
Bearwallow-Hellman-Witherell complex, 30 to 50 percent slopes10514263460990hgpnca68719851:24000
Shortyork-Yorkville-Witherell complex, 15 to 30 percent slopes, MLRA 5199130214610842w91sca68719851:24000
Yorkville-Ashokawna Witherell complex, 15 to 30 percent slopes, MLRA 5232110364611172w915ca68719851:24000
Ashokawna-Witherell complex, 50 to 75 percent slopes, MLRA 520271954610872w91qca68719851:24000
Witherell-Hopland-Ashokawna complex, 50 to 75 percent slopes, high ffd21151894610962xkbsca68719851:24000
Witherell-Hopland-Ashokawna complex, 50 to 75 percent slopes, low ffd2110455731153042xkbrca68719851:24000
Shortyork-Witherell-Updegraff complex, 50 to 75 percent slopes1974274461082hgsmca68719851:24000
Shortyork-Yorkville-Witherell complex, 9 to 15 percent slopes, MLRA 519834884610832w913ca68719851:24000
Ashokawna-Witherell complex, 15 to 50 percent slopes, MLRA 520130354610862w91rca68719851:24000
Shortyork-Tyson-Witherell complex, 30 to 50 percent slopes, MLRA 519621854610812wgq3ca68719851:24000
Yorknorth-Witherell complex, 15 to 30 percent slopes655sh21762600436hs85ca68719851:24000
Hopland-Witherell-Ashokawnacomplex, 15 to 30 percent slopes1481994461033hgr1ca68719851:24000
Yorknorth-Witherell complex, 30 to 50 percent slopes662sh14972600438v6lgca68719851:24000
Yorknorth-Witherell complex, 2 to 15 percent slopes657sh312600437hs87ca68719851:24000
Shortyork-Yorkville-Witherell complex, 15 to 30 percent slopes, MLRA 520298604657812w91sca69419931:24000
Ashokawna-Garcia-Witherell complex, 50 to 75 percent slopes2069037465785hmpbca69419931:24000
Yorkville-Ashokawna Witherell complex, 30 to 50 percent slopes, MLRA 524389474658312w916ca69419931:24000
Ashokawna-Garcia-Witherell complex, 15 to 50 percent slopes2058928465784hmp9ca69419931:24000
Hopland-Witherell-Ashokawna complex, 30 to 50 percent slopes, MLRA 516977384657382w91tca69419931:24000
Ashokawna-Witherell complex, 15 to 50 percent slopes, MLRA 520771764657862w91rca69419931:24000
Shortyork-Yorkville-Witherell complex, 30 to 50 percent slopes, MLRA 520340934657822w914ca69419931:24000
Yorkville-Ashokawna Witherell complex, 15 to 30 percent slopes, MLRA 524232214658302w915ca69419931:24000
Shortyork-Yorkville-Witherell complex, 9 to 15 percent slopes, MLRA 520121824657802w913ca69419931:24000
Witherell-Hopland-Ashokawna complex, 50 to 75 percent slopes, high ffd2289784658132xkbsca69419931:24000
Shortyork-Tyson-Witherell complex, 30 to 50 percent slopes, MLRA 52005394657792wgq3ca69419931:24000
Ashokawna-Witherell complex, 50 to 75 percent slopes, MLRA 52084694657872w91qca69419931:24000
Yorknorth-Witherell complex, 15 to 30 percent slopes655sh632495501hs85ca69419931:24000
Shortyork-Yorkville-Witherell complex, 15 to 30 percent slopes, MLRA 5199em24517011462w91sca70119841:24000
Shortyork-Yorkville-Witherell complex, 30 to 50 percent slopes, MLRA 5200em22817011472w914ca70119841:24000
Hopland-Witherell-Ashokawna complex, 30 to 50 percent slopes, MLRA 5149em5817011392w91tca70119841:24000
Yorkville-Ashokawna Witherell complex, 15 to 30 percent slopes, MLRA 5232em3417011512w915ca70119841:24000
Yorknorth-Witherell complex, 30 to 50 percent slopes662sh232514186v6lgca70119841:24000
Ashokawna-Witherell complex, 50 to 75 percent slopes, MLRA 5202em217011482w91qca70119841:24000
Shortyork-Yorkville-Witherell complex, 30 to 50 percent slopes, MLRA 5200me279827478562w914ca70920101:24000
Yorkville-Ashokawna Witherell complex, 30 to 50 percent slopes, MLRA 5233me57027478642w916ca70920101:24000
Shortyork-Yorkville-Witherell complex, 15 to 30 percent slopes, MLRA 5199me17527478552w91sca70920101:24000
Shortyork-Tyson-Witherell complex, 30 to 50 percent slopes, MLRA 5196me4427478542wgq3ca70920101:24000
Ashokawna-Witherell complex, 50 to 75 percent slopes, MLRA 5202me827478572w91qca70920101:24000

Map of Series Extent

Approximate geographic distribution of the WITHERELL 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 .