Soil Data Explorer - FUGHES

Official Series Description

Lab Data Summary

Aggregate lab data for the FUGHES soil series. This aggregation is based on all pedons with a current taxon name of FUGHES, 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 FUGHES were used in the calculation. Source: KSSL snapshot (updated 2020-03-13). Methods used to assemble the KSSL snapshot used by SoilWeb / SDE

Pedons used in the lab summary:

MLRA	Lab ID	Pedon ID	Taxonname	CI	NSSL / NASIS Reports	Link To SoilWeb GMap
n/a	40A1142	S1977UT021009	Fughes	6	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	n/a

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the FUGHES 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 FUGHES series. Sketches are arranged according to their subgroup-level taxonomic structure. Source: SSURGO snapshot (updated 2024-10-24), parsed OSD records (updated 2024-10-23) and snapshot of SC database (updated 2024-10-23).

Select annual climate data summaries for the FUGHES 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 2024-10-23).

Geomorphic description summaries for the FUGHES 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 2024-10-23).

Competing Series

Soil series competing with FUGHES share the same family level classification in Soil Taxonomy. Source: parsed OSD records (updated 2024-10-23) and snapshot of the SC database (updated 2024-10-23).

Select annual climate data summaries for the FUGHES 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 2024-10-23).

Geomorphic description summaries for the FUGHES 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 2024-10-23).

Soil series sharing subgroup-level classification with FUGHES, 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 2024-10-23).

Block Diagrams

No block diagrams are available.

Map Units

Map units containing FUGHES 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
Fughes sandy clay loam, 3 to 15 percent slopes	19	3162	496453	jnlm	co627	1980	1:24000
Fughes family, 5 to 25 percent slopes	505M	491	509837	k3jc	co636	2011	1:24000
Herm-Fughes complex, 10 to 20 percent slopes, extremely bouldery	98	12	3106843	jpg8	co648		1:24000
Fughes-Godding families complex, 5 to 40 percent slopes	333B	29532	1414937	1jhc4	co654		1:24000
Herm-Fughes families complex, 5 to 40 percent slopes, eroded	430B	3442	1415024	1jhfy	co654		1:24000
Curecanti-Fughes complex, 12 to 25 percent slopes	22	3163	497961	jq58	co655	1984	1:24000
Curecanti-Fughes complex, 6 to 12 percent slopes	21	1058	497960	jq57	co655	1984	1:24000
Fughes stony loam, 3 to 12 percent slopes	48	766	497989	jq65	co655	1984	1:24000
Herm-Fughes-Kolob family complex, 25 to 40 percent slopes	158	34861	509517	k361	co660	1994	1:24000
Fughes-Fughes, cool-Fughes, very stony, cool complex, 5 to 25 percent slopes	GR6	17171	3084832	2ypr6	co660	1994	1:24000
Kolob family, dry-Fughes complex, 5 to 45 percent slopes, extremely stony	165	12214	509527	k36c	co660	1994	1:24000
Fughes-Fughes, very stony complex, cool, 5 to 25 percent slopes	GR5	9006	3084831	2ypr5	co660	1994	1:24000
Fughes-Fughes, very stony complex, cool, 25 to 65 percent slopes	GR7	4759	3084833	2ypr8	co660	1994	1:24000
Fughes-Kolob family, warm complex, 5 to 45 percent slopes	146	3590	509503	k35l	co660	1994	1:24000
Fughes clay loam, 3 to 9 percent slopes, stony	144	71	509500	k35h	co660	1994	1:24000
Fughes clay loam, 2 to 6 percent slopes	143	13	509498	k35f	co660	1994	1:24000
Fughes-Hesperus complex, 3 to 12 percent slopes	145	9	509502	k35k	co660	1994	1:24000
Fughes-Herm complex, 1 to 35 percent slopes	40	1110	57643	2wqy8	co671	1997	1:24000
Fughes loam, 1 to 12 percent slopes	39	995	57638	2wqy7	co671	1997	1:24000
Fughes-Sheek complex, 15 to 30 percent slopes	41	400	57644	2wr82	co671	1997	1:24000
Granath-Fughes complex, 0 to 15 percent slopes	46	334	57650	1xzp	co671	1997	1:24000
Granath-Fughes complex, 0 to 15 percent slopes	511	20710	507191	k0s0	co672	2003	1:24000
Fughes-Sheek complex, 15 to 30 percent slopes	801	13494	507257	2wr82	co672	2003	1:24000
Fughes loam, 1 to 12 percent slopes	13	5854	737680	2wqy7	co672	2003	1:24000
Fughes-Herm complex, 1 to 35 percent slopes	58	3034	737693	2wqy8	co672	2003	1:24000
Shawa-Fughes complex, 30 to 60 percent slopes	806	2969	507261	k0v8	co672	2003	1:24000
Shawa-Fughes complex, 15 to 30 percent slopes	805	1210	507260	k0v7	co672	2003	1:24000
Fughes-Herm complex, 25 to 45 percent slopes	59	588	737694	srml	co672	2003	1:24000
Fughes silty clay loam, 5 to 30 percent slopes	813	497	507265	k0vd	co672	2003	1:24000
Herm-Fughes-Godding complex, 5 to 45 percent slopes	122	600	505174	jyny	co674	1998	1:24000
Fughes-Fughes, cool-Fughes, very stony, cool complex, 5 to 25 percent slopes	GR6	12056	3084838	2ypr6	co679	1976	1:24000
Fughes-Curecanti stony loams, 10 to 40 percent slopes	41	10039	496619	jnrz	co679	1976	1:24000
Fughes loam, 25 to 65 percent slopes	39	8190	496616	jnrw	co679	1976	1:24000
Fughes loam, 5 to 15 percent slopes	37	3864	496614	jnrt	co679	1976	1:24000
Fughes-Fughes, very stony complex, cool, 5 to 25 percent slopes	GR5	3350	3084837	2ypr5	co679	1976	1:24000
Fughes-Fughes, very stony complex, cool, 25 to 65 percent slopes	GR7	1456	3170533	2ypr8	co679	1976	1:24000
Fughes clay loam, 2 to 6 percent slopes	37	4724	496698	jnvj	co682	1986	1:24000
Fughes-Hesperus complex, 3 to 12 percent slopes	39	2957	496700	jnvl	co682	1986	1:24000
Fughes clay loam, 3 to 9 percent slopes, stony	38	1582	496699	jnvk	co682	1986	1:24000
Herm-Fughes complex, 10 to 20 percent slopes, extremely bouldery	98	7027	497279	jpg8	co686	1992	1:31680
Fughes-Crooked Creek-Fentonlake families association, 0 to 15 percent slopes	5	2220	2934358	2whdv	nm678		1:24000
Fughes loam, 4 to 10 percent slopes	31	3158	55351	1vlj	ut633	1983	1:24000
Fughes-Sheckle loams, 4 to 25 percent slopes	380	14918	483908	j7jy	ut634	1997	1:24000
Fughes silty clay loam, 0 to 4 percent slopes	52	2059	504447	jxxh	ut636	1984	1:24000
Sirref-Fughes-Harpole families complex, 3 to 25 percent slopes	mt45	6630	3314838	30hl1	ut645		1:24000
Fughes-Detra families complex, 3 to 20 percent slopes	mt22	3431	3202673	2zbv7	ut645		1:24000
Fughes family, 3 to 15 percent slopes	24	3699	512382	k65g	ut646		1:24000
Fughes family, extremely stony-Blaincreek family, very stony complex, 25 to 60 percent slopes	145	3447	791185	vk93	ut651		1:24000
Blackleaf-like-Modo-like-Fughes complex, 8 to 60 percent slopes	5D44		3358330	30zv8	wy617		1:24000

Map of Series Extent

Approximate geographic distribution of the FUGHES 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 2024-10-30).