Soil Data Explorer - QUANDER

Official Series Description

Lab Data Summary

Aggregate lab data for the QUANDER soil series. This aggregation is based on all pedons with a current taxon name of QUANDER, 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 QUANDER 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
48A	87P0712	87CO065001	Quander	7	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	39.2772217,-106.327774
48A	88P0123	88CO119001	Quander	5	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	38.7236099,-105.1452789

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the QUANDER 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 QUANDER 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 QUANDER 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 QUANDER 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 QUANDER 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 QUANDER 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 QUANDER 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).

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

Soil series sharing subgroup-level classification with QUANDER, 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

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

1. WY-2012-03-23-01 | Fremont County, East Part and Dubois Area - July 1993

   Soils and their landscape positions as they relate to parent material, precipitation zones, and temperature regimes (Soil Survey of Fremont County, East Part and Dubois Area, WY; 1993).

Map Units

Map units containing QUANDER 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
Quander-Bushpark very gravelly loams, 5 to 40 percent slopes complex	151	1341	2497289	k0xv	co637	1986	1:24000
Quander-Bushpark very gravelly loams, 5 to 40 percent slopes complex	82	23375	507341	k0xv	co638	2010	1:24000
Quander stony loam, 15 to 55 percent slopes	66	12	3106906	jq32	co648		1:24000
Quander stony loam, 15 to 55 percent slopes	66	28136	497893	jq32	co649	1977	1:24000
Quander cobbly loam, 2 to 15 percent slopes	65	6372	497892	jq31	co649	1977	1:24000
Quander family, till substratum, 5 to 40 percent slopes	281B	2689	1414890	1jh9m	co654		1:24000
Quander family, till substratum, 40 to 60 percent slopes	281C	529	1414891	1jh9n	co654		1:24000
Quander-Youga complex, 15 to 55 percent slopes	S17F	34	1414846	1jh86	co654		1:24000
Clayburn-Quander-Guero complex, 5 to 30 percent slopes	122	15788	509470	k34j	co660	1994	1:24000
Clayburn-Quander-Guero complex, 30 to 65 percent slopes	123	2126	509471	k34k	co660	1994	1:24000
Quander family, till substratum, 5 to 40 percent slopes	281B	332	3176950	1jh9m	co661	1968	1:31680
Clayburn-Quander-Guero complex, 5 to 30 percent slopes	122	1	2927467	k34j	co662	1968	1:24000
Tellura, moist-Quander complex, 5 to 25 percent slopes	142	29714	505048	jyjw	co663	2000	1:24000
Quander, cool-Bushpark-Rock outcrop complex, 15 to 45 percent slopes	133	15570	505037	jyjj	co663	2000	1:24000
Quander very gravelly loam, dry, 5 to 25 percent slopes	132	7813	505039	jyjl	co663	2000	1:24000
Cochedome-Quander, dry-Snowdon, warm complex, 25 to 65 percent slopes	104	5692	505009	jyhm	co663	2000	1:24000
Lagarita-Quander, dry complex, 5 to 40 percent slopes	122	5100	505023	jyj2	co663	2000	1:24000
Cochedome-Quander, dry-Snowdon, warm complex, 5 to 25 percent slopes	103	2814	505008	jyhl	co663	2000	1:24000
Goldpark-Quander, dry complex, 5 to 25 percent slopes	111	2254	505016	jyhv	co663	2000	1:24000
Quander-Seitz-Rock outcrop complex, 25 to 65 percent slopes	134	1462	505040	jyjm	co663	2000	1:24000
Quander loam, 5 to 25 percent slopes	131	1389	505038	jyjk	co663	2000	1:24000
Quander-Bushvalley association, 15 to 60 percent slopes	160	30435	2453697	2nc8j	co664	1987	1:24000
Quander-Bowen association, 15 to 60 percent slopes	159	25285	2453694	2nc8f	co664	1987	1:24000
Quander stony loam, 5 to 60 percent slopes	157	18621	2453692	2nc8c	co664	1987	1:24000
Quander stony loam, cool, 15 to 50 percent slopes	158	10877	2453693	2nc8d	co664	1987	1:24000
Quander-Cryaquolls-Cryohemists association, 1 to 30 percent slopes	161	9197	2453698	2nc8k	co664	1987	1:24000
Quander-Angostura-Mulgon complex, 20 to 65 percent slopes	97	9708	496944	jp3g	co684	1984	1:24000
Cowdrey-Cochetopa-Quander loams, 5 to 25 percent slopes	32	7452	496873	jp15	co684	1984	1:24000
Cochetopa-Gothic-Quander loams, 5 to 25 percent slopes	25	7017	496865	jp0x	co684	1984	1:24000
Quander-Clayburn-Adel loams, 3 to 25 percent slopes	99	4233	496946	jp3j	co684	1984	1:24000
Hapgood-Rhone-Quander loams, 20 to 65 percent slopes	57	2364	496900	jp21	co684	1984	1:24000
Cochetopa-Gothic-Quander loams, 25 to 65 percent slopes	26	2116	496866	jp0y	co684	1984	1:24000
Quander-Blackwell-Emerald loams, 3 to 15 percent slopes	98	2043	496945	jp3h	co684	1984	1:24000
Cochetopa-Gourley-Quander complex, 5 to 25 percent slopes	27	1870	496867	jp0z	co684	1984	1:24000
Quander cobbly loam, 15 to 55 percent slopes	16E	3922	497294	jpgr	co690	1974	1:24000
Quander cobbly loam, 6 to 15 percent slopes	16D	1430	497293	jpgq	co690	1974	1:24000
Quander-Youga complex, 15 to 55 percent slopes	17F	1290	497295	jpgs	co690	1974	1:24000
Quander cobbly loam, 0 to 6 percent slopes	16C	270	497292	jpgp	co690	1974	1:24000
Quander-Bowen, cool association, 15 to 60 percent slopes, stony	QbF	62	2770161	2tl91	nm672		1:24000
Quander-Cryaquolls, occasionally flooded-Cryohemists, frequently flooded, association, 1 to 30 percent slopes, stony	QcE	42	2770162	2tl92	nm672		1:24000
Hanson-Quander complex, 3 to 15 percent slopes	171	8043	501712	jv28	wy601	1991	1:24000
Leavitt-Quander complex, 15 to 45 percent slopes	183	7973	501726	jv2q	wy601	1991	1:24000
Surdal-Irson-Quander complex, 25 to 60 percent slopes, extremely stony -- Draft	940		2551470	2qts7	wy629		1:24000
Irson-Rock outcrop-Quander complex, 25 to 90 percent slopes, extremely stony -- Draft	960		2551471	2qts8	wy629		1:24000
Bavdark-Quander, stony-Dailybasin complex, 12 to 40 percent slopes	7402		3136900	2ypq4	wy629		1:24000
Dailybasin-Odark-Quander, stony complex, 4 to 40 percent slopes	7403		3136902	2ypq6	wy629		1:24000
Beavmid-like-Quander-Foolhen complex, 15 to 60 percent slopes -- Draft	7502		2551509	2qttk	wy629		1:24000
Hanson-Quander complex, 3 to 15 percent slopes	1171	3093	2573052	2x8pc	wy630		1:24000
Leavitt-Quander complex, 15 to 45 percent slopes	1183	3035	2573053	2x8pd	wy630		1:24000
Foothill Sideslopes, Aspen-Big Sagebrush Complex	6631	166	2554706	532t	wy635		1:24000
Bavdark-Quander, stony-Dailybasin complex, 12 to 40 percent slopes	7402		3253340	2ypq4	wy656	2008	1:24000
Foothill Sideslopes, Aspen-Big Sagebrush Complex	6631	2739	151925	532t	wy662	1998	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

Map of Series Extent

Approximate geographic distribution of the QUANDER 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).