Official Series Description


Lab Data Summary

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

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

Competing Series

Soil series competing with WOODIN 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 WOODIN 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 WOODIN 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 .

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.

Soil series sharing subgroup-level classification with WOODIN, 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-2011-05-27-03 | Mendocino County, Eastern Part, and Trinity County, Southwestern Part - 1991

    Pattern of active, metastable, and stable slopes (Soil Survey of Mendocino County, Eastern Part, and Trinity County, Southwestern Part, California; 1991).

Map Units

Map units containing WOODIN 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
Yorktree-Hopland-Woodin complex, 30 to 50 percent slopes225em16076321qyw3ca09719681:20000
Woodin-Yellowhound complex, 30 to 50 percent slopes231wm16074651qypqca09719681:20000
Maymen-Woodin-Etsel complex, 50 to 75 percent slopes162em16076261qyvxca09719681:20000
Hopland-Woodin complex, 30 to 50 percent slopes152em16081881qzg1ca09719681:20000
Pardaloe-Woodin-Casabonne complex, 30 to 50 percent slopes, high ffd191wm16074622xkbnca09719681:20000
Pardaloe-Woodin complex, 50 to 75 percent slopes, low ffd41836226004452y4jjca60120111:24000
Pardaloe-Woodin-Casabonne complex, 30 to 50 percent slopes, low ffd416334701532xkbpca60120111:24000
Yorktree-Hopland-Woodin complex, 30 to 50 percent slopes22541968461110hgtjca68719851:24000
Maymen-Woodin-Etsel complex, 50 to 75 percent slopes16230552461047hgrhca68719851:24000
Pardaloe-Woodin complex, 50 to 75 percent slopes, low ffd17401563031152972y4jjca68719851:24000
Yorktree-Hopland-Woodin complex, 50 to 75 percent slopes22614008461111hgtkca68719851:24000
Maymen-Woodin-Etsel complex, 30 to 50 percent slopes16112442461046hgrgca68719851:24000
Nashmead-Woodin gravelly sandy loams, 50 to 75 percent slopes1665543461051hgrmca68719851:24000
Nashmead-Updegraff-Woodin complex, 30 to 50 percent slopes1634648461048hgrjca68719851:24000
Etsel-Woodin-Rock outcrop association, 50 to 75 percent slopes1224498461007hgq6ca68719851:24000
Hopland-Woodin complex, 50 to 75 percent slopes1534123461038hgr6ca68719851:24000
Hopland-Woodin complex, 30 to 50 percent slopes1524108461037hgr5ca68719851:24000
Nashmead-Woodin gravelly sandy loams, 30 to 50 percent slopes1653371461050hgrlca68719851:24000
Pardaloe-Woodin-Casabonne complex, 30 to 50 percent slopes, low ffd1730306731152962xkbpca68719851:24000
Nashmead-Updegraff-Woodin complex, 50 to 75 percent slopes1641500461049hgrkca68719851:24000
Pardaloe-Woodin-Casabonne complex, 30 to 50 percent slopes, high ffd17314254610582xkbnca68719851:24000
Pardaloe-Woodin complex, 50 to 75 percent slopes, high ffd17411744610592xk9wca68719851:24000
Yellowhound-Woodin-Ornbaun complex, 30 to 50 percent slopes24021336465828hmqqca69419931:24000
Woodin-Yellowhound complex, 30 to 50 percent slopes23120707465818hmqdca69419931:24000
Yellowhound-Woodin complex, 50 to 75 percent slopes23817269465825hmqmca69419931:24000
Maymen-Woodin-Etsel complex, 30 to 75 percent slopes18610391465761hmnkca69419931:24000
Woodin-Yellowhound complex, 50 to 75 percent slopes2329429465819hmqfca69419931:24000
Pardaloe-Woodin-Casabonne complex, 30 to 50 percent slopes, high ffd19164444657682xkbnca69419931:24000
Pardaloe-Woodin complex, 50 to 75 percent slopes, high ffd19060684657662xk9wca69419931:24000
Updegraff-Hopland-Woodin complex, 30 to 50 percent slopes2182612465799hmpsca69419931:24000
Pardaloe-Woodin complex, 50 to 75 percent slopes, low ffd1900239831153222y4jjca69419931:24000
Yellowhound-Woodin-Ornbaun complex, 9 to 30 percent slopes239922465826hmqnca69419931:24000
Pardaloe-Woodin-Casabonne complex, 30 to 50 percent slopes, low ffd191080831153232xkbpca69419931:24000
Maymen-Woodin-Etsel complex, 50 to 75 percent slopes162em34017011401v35hca70119841:24000
Etsel-Woodin-Rock outcrop association, 50 to 75 percent slopes122em2717011361v35cca70119841:24000
Maymen-Woodin-Etsel complex, 50 to 75 percent slopes162me2782747845hgrhca70920101:24000
Maymen-Woodin-Etsel complex, 30 to 50 percent slopes161me1612747844hgrgca70920101:24000
Nashmead-Woodin gravelly sandy loams, 30 to 50 percent slopes165me572747846hgrlca70920101:24000
Hopland-Woodin complex, 30 to 50 percent slopes152me562747841hgr5ca70920101:24000
Pardaloe-Woodin complex, 50 to 75 percent slopes, low ffd1740me3127478492y4jjca70920101:24000
Hopland-Woodin complex, 50 to 75 percent slopes153me182747842hgr6ca70920101:24000
Etsel-Woodin-Rock outcrop association, 50 to 75 percent slopes122me627478332q1zwca70920101:24000

Map of Series Extent

Approximate geographic distribution of the WOODIN 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 .