Soil Data Explorer - YOUGA

Official Series Description

Lab Data Summary

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

There are insufficient data to create the lab data summary figure.

Pedons used in the lab summary:

MLRA	Lab ID	Pedon ID	Taxonname	CI	NSSL / NASIS Reports	Link To SoilWeb GMap
48A	07N0571	S2007CO007005	Youga	6	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	37,-106.4583359

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the YOUGA 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 YOUGA series. Sketches are arranged according to their subgroup-level taxonomic structure. Source: SSURGO snapshot (updated 2024-02-21), parsed OSD records (updated 2023-10-02) and snapshot of SC database (updated 2023-10-02).

Select annual climate data summaries for the YOUGA 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 YOUGA 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 YOUGA share the same family level classification in Soil Taxonomy. Source: parsed OSD records (updated 2023-10-02) and snapshot of the SC database (updated 2023-10-02).

Select annual climate data summaries for the YOUGA 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 YOUGA 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 YOUGA, 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 YOUGA 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
Bushvalley-Youga complex, 3 to 25 percent slopes	8	14800	498631	jqvw	co630	1975	1:24000
Youga sandy loam, 3 to 10 percent slopes	130	3205	498276	jqhf	co637	1986	1:24000
Libeg-Youga-Bywell families, association, 0 to 20 percent slopes	155A	7746	509302	k2z3	co647		1:24000
Gebson, moist-Youga complex, 5 to 25 percent slopes, extremely stony	84	88	3106842	jpfs	co648		1:24000
Youga-Gelkie-Clayburn, warm complex, 25 to 45 percent slopes, extremely bouldery	221	67	3106836	jpch	co648		1:24000
Youga loam, 15 to 45 percent slopes	95	12517	497925	2tz4x	co649	1977	1:24000
Youga loam, 6 to 15 percent slopes	94	9867	497924	2tz4q	co649	1977	1:24000
Youga loam, 1 to 6 percent slopes	93	5651	497923	2tz4z	co649	1977	1:24000
Libeg-Youga-Bywell families, association, 0 to 20 percent slopes	155A	7241	3176974	k2z3	co650		1:24000
Quander-Youga complex, 15 to 55 percent slopes	S17F	34	1414846	1jh86	co654		1:24000
Youga loam, 12 to 30 percent slopes	118	741	497948	jq4v	co655	1984	1:24000
Youga loam, 3 to 30 percent slopes	YgE	1996	498237	jqg5	co662	1968	1:24000
Youga-Gateview complex, 3 to 25 percent slopes	174	9088	2453704	2nc8r	co664	1987	1:24000
Mulgon-Youga complex, 12 to 30 percent slopes	H1-E	2585	780800	v6h3	co668	2018	1:24000
Conejos-Youga-Cryaquolls complex, 0 to 30 percent slopes	H3-D	1373	780326	v5zt	co668	2018	1:24000
Youga-Quazar, cool complex, 5 to 20 percent slopes	D1-D	950	737747	srp9	co668	2018	1:24000
Quazar family-Youga complex, 20 to 45 percent slopes, very bouldery	D3-E	610	796393	vqq3	co668	2018	1:24000
Youga-Tine loams, 5 to 50 percent slopes	126	5455	496851	jp0g	co684	1984	1:24000
Youga-Gelkie-Clayburn, warm complex, 25 to 45 percent slopes, extremely bouldery	221	6538	497193	jpch	co686	1992	1:31680
Clayburn-Youga, moist complex, 15 to 45 percent slopes	35	4086	497210	jpd1	co686	1992	1:31680
Gebson, moist-Youga complex, 5 to 25 percent slopes, extremely stony	84	2520	497264	jpfs	co686	1992	1:31680
Youga-Dinnen complex, 3 to 12 percent slopes	220	1973	497192	jpcg	co686	1992	1:31680
Morset-Youga complex, 3 to 12 percent slopes	137	1927	497099	jp8g	co686	1992	1:31680
Youga loam, 3 to 15 percent slopes	219	1073	497190	jpcd	co686	1992	1:31680
Youga loam, 15 to 45 percent slopes	19F	2190	497299	2tz4x	co690	1974	1:24000
Youga loam, 6 to 15 percent slopes	19D	1770	497298	2tz4q	co690	1974	1:24000
Quander-Youga complex, 15 to 55 percent slopes	17F	1290	497295	jpgs	co690	1974	1:24000
Youga loam, 1 to 6 percent slopes	19C	1140	497297	2tz4z	co690	1974	1:24000
Youga loam, thick surface, 6 to 15 percent slopes	20D	830	497302	jph0	co690	1974	1:24000
Youga loam, thick surface, 15 to 50 percent slopes	20F	650	497303	jph1	co690	1974	1:24000
Decross-Auzqui, very stony-Youga complex, 8 to 35 percent slopes	217	6691	2376195	2krmg	wy041		1:24000
Briston-Buffmeyer-Youga complex, 7 to 25 percent slopes	521	6157	2516195	2qftj	wy630		1:24000
Youga-Warrow, rubbly complex, 4 to 25 percent slopes	3603	16042	1676013	1t80y	wy635		1:24000
Warrow-Youga-Bigrant, very bouldery complex, 1 to 25 percent slopes	3502	5493	1675880	1t7wn	wy635		1:24000
Sledrunner-Youga-Groomer complex, 5 to 30 percent slopes	5525	4721	2485297	2pf4w	wy635		1:24000
Norriston, rubbly-Ellena, extremely stony-Rock outcrop complex, 15 to 50 percent slopes	7601	4338	1475591	1ljgq	wy635		1:24000
Inchau-Youga complex, 10 to 30 percent slopes	165D	127	157926	59bd	wy656	2008	1:24000
Warrow-Youga-Bigrant, very bouldery complex, 1 to 25 percent slopes	3502	283	2514398	1t7wn	wy662	1998	1:24000
Norriston, rubbly-Ellena, extremely stony-Rock outcrop complex, 15 to 50 percent slopes	7601	251	2515461	1ljgq	wy662	1998	1:24000
Youga-Warrow, rubbly complex, 4 to 25 percent slopes	3603	88	2514400	1t80y	wy662	1998	1:24000
Sledrunner-Youga-Groomer complex, 5 to 30 percent slopes	5525	20	2514405	2pf4w	wy662	1998	1:24000
Sledrunner-Youga-Groomer complex, 5 to 30 percent slopes	5525	89	2633690	2pf4w	wy663	2012	1:24000
Leavitt-Youga complex, 0 to 3 percent slopes	23	2977	153271	54h7	wy666	1978	1:24000
Youga-Tineman complex	71	1203	153324	54jy	wy666	1978	1:24000
Leavitt-Youga complex, 3 to 6 percent slopes	24	741	153272	54h8	wy666	1978	1:24000
Quander-Youga-Onason complex, steep	188	18203	503053	jwgj	wy713	1986	1:24000
Youga-Quander complex, 2 to 25 percent slopes	223	12190	503103	jwj4	wy713	1986	1:24000
Inchau-Youga loams, 10 to 30 percent slopes	165	856	503030	jwfs	wy713	1986	1:24000

Map of Series Extent

Approximate geographic distribution of the YOUGA 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).