Soil Data Explorer - WOODHALL

Official Series Description

Lab Data Summary

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

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

Competing Series

Soil series competing with WOODHALL 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 WOODHALL 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).

Geomorphic description summaries for the WOODHALL 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 3D flats position figure.

Soil series sharing subgroup-level classification with WOODHALL, 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

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

1. CO-2012-05-09-05 | Gunnison Area; Parts of Gunnison, Hinsdale, and Saguache Counties - August 1975

   Typical pattern of soils and parent material in associations 2, 3, 4, and 6 (Soil Survey of Gunnison Area, Colorado, Parts of Gunnison, Hinsdale, and Saguache Counties; August 1975).

Map Units

Map units containing WOODHALL 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
Lambe-Woodhall complex, 5 to 65 percent slopes	LbF	18126	1151629	17ncb	co023	2009	1:24000
Rogert-Woodhall complex, 25 to 65 percent slopes	74	10725	496514	jnnl	co627	1980	1:24000
Woodhall-Rock outcrop complex, 5 to 20 percent slopes	94	638	496536	jnp9	co627	1980	1:24000
Rogert-Woodhall extremely cobbly sandy loams, 20 to 45 percent	31	20181	498396	jqm9	co635	1979	1:24000
Woodhall-Rogert extremely cobbly sandy loams, 5 to 20 percent	50	11400	498417	jqmz	co635	1979	1:24000
Woodhall family very gravelly loam, 15 to 40 percent slopes	225C	462	509311	k2zd	co647		1:24000
Woodhall loam, 15 to 50 percent slopes	92	6413	497922	jq40	co649	1977	1:24000
Woodhall loam, 6 to 15 percent slopes	91	1119	497921	jq3z	co649	1977	1:24000
Woodhall gravelly loam, 6 to 50 percent slopes, extremely stony	112	4267	497942	jq4n	co655	1984	1:24000
Woodhall-Bushvalley complex, 15 to 65 percent slopes	201	22501	509573	k37v	co660	1994	1:24000
Beachcanyon, extremely bouldery-Gothic-Woodhall, rubbly complex, 10 to 50 percent slopes	919	564	2990846	2kmmt	co660	1994	1:24000
Woodhall, dry-Bushvalley complex, 5 to 40 percent slopes	202	500	509575	k37x	co660	1994	1:24000
Gothic-Woodhall, very stony complex, 3 to 25 percent slopes	965	103	2927466	17mvw	co660	1994	1:24000
Woodhall extremely rocky loam, 5 to 50 percent slopes	WoF	16722	498235	jqg3	co662	1968	1:24000
Beachcanyon, extremely bouldery-Gothic-Woodhall, rubbly complex, 10 to 50 percent slopes	919	825	2990847	2kmmt	co662	1968	1:24000
Beachcanyon, extremely bouldery-Gothic-Woodhall, rubbly complex, 10 to 50 percent slopes	919	8405	2990848	2kmmt	co674	1998	1:24000
Gothic-Woodhall, very stony complex, 3 to 25 percent slopes	965	66	2927460	17mvw	co674	1998	1:24000
Gothic-Woodhall, very stony complex, 3 to 25 percent slopes	965	1202	2927475	17mvw	co675	1986	1:24000
Beachcanyon, extremely bouldery-Gothic-Woodhall, rubbly complex, 10 to 50 percent slopes	919	973	2927471	2kmmt	co675	1986	1:24000
Woodhall, rubbly-Gothic complex, 3 to 25 percent slopes	956	162	2927478	17sj3	co675	1986	1:24000
Woodhall, rubbly-Gothic complex, 3 to 25 percent slopes	956	321	2990894	17sj3	co676	1983	1:24000
Gothic-Woodhall, very stony complex, 3 to 25 percent slopes	965	64	2990896	17mvw	co676	1983	1:24000
Beachcanyon, extremely bouldery-Gothic-Woodhall, rubbly complex, 10 to 50 percent slopes	919	20945	2372362	2kmmt	co677	2018	1:24000
Woodhall, rubbly-Gothic complex, 3 to 25 percent slopes	956	3574	1155621	17sj3	co677	2018	1:24000
Gothic-Woodhall, very stony complex, 3 to 25 percent slopes	965	2033	1151150	17mvw	co677	2018	1:24000
Woodhall-Cheadle-Rock outcrop complex, 3 to 25 percent slopes	125	3542	496850	jp0f	co684	1984	1:24000
Philipsburg-Nieman-Woodhall complex, 4 to 15 percent slopes, very stony	550D	397	3039582	wfwc	mt602	1963	1:20000
Woodhall-Woodhurst, very stony-Bavdark complex, 8 to 15 percent slopes	38D	208	3039583	1hf4y	mt602	1963	1:20000
Woodhall-Woodhurst complex, 15 to 35 percent slopes, stony	38E	74	3039584	1hf54	mt602	1963	1:20000
Woodhall gravelly loam, 4 to 15 percent slopes	156	326	1859670	20f4c	mt605	2007	1:24000
Woodhall-Blaine-Hapgood complex, 4 to 25 percent slopes	157	133	1859671	4xcn	mt605	2007	1:24000
Woodhall-Woodhurst, very stony-Bavdark complex, 8 to 15 percent slopes	38D	95	3039704	2pg61	mt613	1975	1:24000
Libeg-Woodhall complex, 4 to 8 percent slopes	560C	642	2493430	2pqdg	mt624	2021	1:24000
Philipsburg, very bouldery-Nieman, very stony-Woodhall, very stony complex, 4 to 15 percent slopes	550D	25	2979644	2l9xv	mt624	2021	1:24000
Woodhall-Woodhurst complex, 15 to 35 percent slopes, stony	38E	10	3176848	1hf54	mt624	2021	1:24000
Woodhall-Woodhurst, very stony-Bavdark complex, 8 to 15 percent slopes	38D	3793	2486294	2pg61	mt632		1:24000
Surdal-Woodhall-Poin complex, 20 to 60 percent slopes	171F	3423	2392786	2l9wn	mt632		1:24000
Woodhall-Woodhurst complex, 15 to 35 percent slopes, stony	38E	2842	2392756	2l9vp	mt632		1:24000
Philipsburg, very bouldery-Nieman, very stony-Woodhall, very stony complex, 4 to 15 percent slopes	550D	1870	2392823	2l9xv	mt632		1:24000
Nieman, very bouldery-Woodhall, very bouldery-Sebud complex, 15 to 45 percent slopes	165E	1432	2486245	2pg4g	mt632		1:24000
Philipsburg-Woodhall, stony-Bangtail complex, 15 to 35 percent slopes	538E	1060	2486264	2pg52	mt632		1:24000
Odark-Bischoff-Woodhall, stony families, complex, 2 to 8 percent slopes	3150C	295	2724639	2sh7z	mt632		1:24000
Woodhall-Blaine-Hapgood complex, 4 to 25 percent slopes	157	11722	146433	4xcn	mt636	1983	1:24000
Woodhall gravelly loam, 4 to 15 percent slopes	156	5421	146432	4xcm	mt636	1983	1:24000
Woodhall-Woodhurst, very stony-Bavdark complex, 8 to 15 percent slopes	38D	8072	1383032	1hf4y	mt637	2014	1:24000
Woodhall-Woodhurst complex, 15 to 35 percent slopes, stony	38E	7957	1383038	1hf54	mt637	2014	1:24000
Bairspring-Woodhall-Poin complex, 20 to 60 percent slopes	171F	6019	1383373	1hfhy	mt637	2014	1:24000
Nieman, very bouldery-Woodhall, very bouldery-Sebud complex, 15 to 45 percent slopes	165E	5495	637271	pd44	mt637	2014	1:24000
Philipsburg-Woodhall, stony-Bangtail complex, 15 to 35 percent slopes	538E	2945	1389503	1hmwp	mt637	2014	1:24000
Philipsburg-Nieman-Woodhall complex, 4 to 15 percent slopes, very stony	550D	1743	817698	wfwc	mt637	2014	1:24000
Woodhall, very bouldery-Nieman, extremely stony complex, 4 to 15 percent slopes	165D	830	637260	pd3s	mt637	2014	1:24000
Odark-Bischoff-Woodhall, stony families, complex, 2 to 8 percent slopes	3150C	60	3094125	2sh7z	mt657	1990	1:24000
Wineglass-Woodhall-Spanpeak complex, 15 to 60 percent slopes	5614F	7643	156479	57tq	mt669		1:24000
Bangtail, extremely stony-Woodhal, very stony-Dalys, extremely stony, complex, 4 to 70 percent slopes	5705F	1604	699352	rgqr	mt669		1:24000
Spanpeak, very stony - Woodhall, stony - Adel complex, 15 to 60 percent slopes	8602F	1075	156766	583z	mt669		1:24000
Woodhall-Zade-like-Chittum-like complex, 2 to 12 percent slopes	7301		3133276	2ynn4	wy629		1:24000
Tepecreek-like-Woodhall complex, 2 to 8 percent slopes	7201		3133274	2ynn2	wy629		1:24000

Map of Series Extent

Approximate geographic distribution of the WOODHALL 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).