Soil Data Explorer - WODOMONT

Official Series Description

Lab Data Summary

Aggregate lab data for the WODOMONT soil series. This aggregation is based on all pedons with a current taxon name of WODOMONT, 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 WODOMONT were used in the calculation. Source: KSSL snapshot (updated 2020-03-18). 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 WODOMONT 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.

Sibling Summary

Siblings are those soil series that occur together in map units, in this case with the WODOMONT series. Sketches are arranged according to their subgroup-level taxonomic structure. Source: SSURGO snapshot (updated 2024-02-21), parsed OSD records (updated 2023-10-06) and snapshot of SC database (updated 2023-10-02).

Select annual climate data summaries for the WODOMONT series and siblings. Series are sorted according to hierarchical clustering of median values. Source: SSURGO map unit geometry and 1981-2010, 800m PRISM data (updated 2023-10-09).

Geomorphic description summaries for the WODOMONT 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 (updated 2023-10-04).

Competing Series

Soil series competing with WODOMONT share the same family level classification in Soil Taxonomy. Source: parsed OSD records (updated 2023-10-06) and snapshot of the SC database (updated 2023-10-02).

Select annual climate data summaries for the WODOMONT series and competing. Series are sorted according to hierarchical clustering of median values. Source: SSURGO map unit geometry and 1981-2010, 800m PRISM data (updated 2023-10-09).

There are insufficient data to create the annual climate figure.

Geomorphic description summaries for the WODOMONT 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 (updated 2023-10-04).

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 WODOMONT, 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 (updated 2023-10-02).

Block Diagrams

No block diagrams are available.

Map Units

Map units containing WODOMONT 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
Wodomont-Atlatl-Rock outcrop complex, 1 to 10 percent slopes	3557	11305	3381263	2zmzf	az631	1980	1:24000
Wodomont taxadjunct-Atlatl complex,1 to 7 percent slopes	3556	7952	3381262	2zmzd	az631	1980	1:24000
Chunkmonk taxadjunct-Wodomont-Rock outcrop complex, 1 to 10 percent slopes	3528	4682	3381266	30sf4	az631	1980	1:24000
Wodomont-Metuck-Rock outcrop complex, 25 to 45 percent slopes	169	21014	798479	vswd	az697	2005	1:24000
Wodomont-Rock outcrop complex, 5 to 40 percent slopes	170	20923	798478	vswc	az697	2005	1:24000
Wodomont-Kydestea complex, 5 to 40 percent slopes	168	4989	798480	vswf	az697	2005	1:24000
Wodomont-Rock outcrop complex, 5 to 40 percent slopes	57	45758	54477	1tpb	az699	1993	1:24000
Topocoba-Wodomont complex, 2 to 15 percent slopes	46	33760	54512	2v1bw	az699	1993	1:24000
Wodomont-Coconino complex, 2 to 15 percent slopes	56	18425	54523	1tqt	az699	1993	1:24000
Chunkmonk-Wodomont-Toqui families complex, 2 to 15 percent slopes	23	24576	615823	nnt8	az701	2001	1:24000
Wodomont-Topocoba-Plumasano families complex, 2 to 15 percent slopes	167	15963	616059	np1w	az701	2001	1:24000
Chunkmonk-Wodomont-Houserock families complex, 15 to 40 percent slopes	22	541	615815	nnt0	az701	2001	1:24000
Topocoba-Wodomont complex, 2 to 15 percent slopes	123	460	616015	2v1bw	az701	2001	1:24000
Wodomont-Quintana, moderately deep families complex, dry, 0 to 15 percent slopes	283	1091	2934311	2wgl3	nm678		1:24000
Barranca, moderately deep-Wodomont, very stony families complex, very dry, 0 to 15 percent slopes	508	970	2934366	2whf3	nm678		1:24000

Map of Series Extent

Approximate geographic distribution of the WODOMONT 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 (updated 2023-10-04).