Soil Data Explorer - QUARZ

Official Series Description

Lab Data Summary

Aggregate lab data for the QUARZ soil series. This aggregation is based on all pedons with a current taxon name of QUARZ, 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 QUARZ 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
25	06N0251	S2005NV007010	Quarz	7	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	41.3054848,-115.3726578

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the QUARZ 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 QUARZ 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 QUARZ 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 QUARZ 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 QUARZ 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 QUARZ 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 QUARZ 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 terrace figure.

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

Soil series sharing subgroup-level classification with QUARZ, 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. NV-2012-05-09-06 | Elko County, Central Part - November 1997

   General soil map units representative of those on a semibolson that is an externally drained intermontane basin. The units are as follows: 1—Devilsgait-Woofus-Moranch; 4—Orovadal-Bioya-Puett; 5—Hunnton-Wieland-Bilbo; 6—McIvey-Stampede-Betra; 7—Donna-Stampede-Bilbo; 17—Cleavage-Quarz-Loncan; 18—Cotant-McIvey-Lerrow; and 10—Sumine-Cleavage-Hapgood (Soil Survey of Elko County, Nevada, Central Part; November 1997).

2. NV-2012-05-09-10 | Lander County, North Part - May 1992

   Typical relationship of general soil map units and landscapes: Sonoma-Rixie-Paranat (3); Orovada-Broyles-Shabliss (7); Buffaran-Allor-Chiara (11); Bioya-Chiara-Cortez (12); Robson-Akerue-Buffaran (16); Sumine-Chen-Rock outcrop (19); and Quarz-Walti-Glean (21) (Soil Survey of Lander County, Nevada, North Part; May 1992).

Map Units

Map units containing QUARZ 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
Eboda-Quarz-Loncan association	993	3547	2518891	2qj83	nv612	1968	1:24000
Quarz-Cleavage-Loncan association	1725	1338	2518903	2qj8j	nv612	1968	1:24000
Linkup-Quarz association	1676	965	2517918	2qhm0	nv612	1968	1:24000
Devoy association	DE	2080	477925	j19y	nv621	1971	1:24000
Quarz-McIvey-Cleavage association	1724	59	2633987	2rhhc	nv621	1971	1:24000
Leevan-Quarz-McIvey association	702	14	2633988	2rhhd	nv621	1971	1:24000
Chen-Quarz-Arcia association	1874	15990	477140	j0hm	nv763	1986	1:24000
Graley-Quarz-Ninemile association	1732	14955	477114	j0gs	nv763	1986	1:24000
Chen-Graley-Quarz association	1870	13510	477137	2t6wh	nv763	1986	1:24000
Alyan, moderately steep-Alyan-Quarz association	2002	11912	477162	j0jb	nv763	1986	1:24000
Cavanaugh-Quarz-Alyan association	221	9050	477173	j0jp	nv763	1986	1:24000
Ratsow-Quarz-Susie Creek association	3100	6040	477244	j0lz	nv763	1986	1:24000
Linkup-Quarz-Alyan association	1673	3520	477096	j0g6	nv763	1986	1:24000
Quarz-Cleavage-Hackwood association	1740	3372	477116	2qhlq	nv763	1986	1:24000
Quarz-Alyan-Ninemile association	1720	3320	477110	j0gn	nv763	1986	1:24000
Quarz-Cleavage-Loncan association	1725	3185	477111	j0gp	nv763	1986	1:24000
Lerrow-Quarz-Rugar association	1921	2780	477153	j0j1	nv763	1986	1:24000
Cotant-Quarz-Ninemile association	1700	2775	477104	j0gg	nv763	1986	1:24000
Deseed-Quarz association	2173	2360	477169	j0jk	nv763	1986	1:24000
Linkup-Quarz association	1676	1530	477098	j0g8	nv763	1986	1:24000
Quarz-Ninemile-Pequop association	1726	1465	477112	j0gq	nv763	1986	1:24000
Quarz-Cleavage-Hackwood association	1740	14096	2517909	2qhlq	nv764	2021	1:24000
Chen-McIvey-Tweener association	219	11459	2517702	2q90m	nv764	2021	1:24000
Cotant-McIvey-Quarz association	1821	6596	474603	hxvs	nv764	2021	1:24000
Quarz-Quarz, very steep-Arcia association	1723	1116	2517700	2q90k	nv764	2021	1:24000
Shalcleav-Quarz association	232	38583	474957	hy76	nv765	1986	1:24000
Quarz-Shalper-Shalcleav association	280	4375	474970	hy7m	nv765	1986	1:24000
McIvey-Quarz association	040	3700	474851	hy3s	nv765	1986	1:24000
Quarz-Cotant association	281	2450	474971	hy7n	nv765	1986	1:24000
Rodie-Quarz-Shalcleav association	422	1675	475032	hy9m	nv765	1986	1:24000
Quarz, steep-Quarz-Arcia association	282	1150	474972	hy7p	nv765	1986	1:24000
Quarz-Cleavage-Loncan association	1725	48601	478772	j268	nv767	1986	1:24000
Cotant-McIvey-Quarz association	1821	36651	478782	j26l	nv767	1986	1:24000
McIvey-Quarz-Rock outcrop association	213	13497	478830	j284	nv767	1986	1:24000
Ninemile-Quarz-Rock outcrop association	840	10351	479012	j2g0	nv767	1986	1:24000
Susie Creek-Kleckner-Quarz association	1662	9195	478763	j25z	nv767	1986	1:24000
Chen-Cleavage-Quarz association	1886	7067	478805	j27b	nv767	1986	1:24000
Quarz-Tusel-Cleavage association	1729	6937	478775	j26c	nv767	1986	1:24000
Donna-Stampede-Quarz association	448	5583	478913	j2bt	nv767	1986	1:24000
Chen-Quarz-Linkup association	1885	4793	478804	j279	nv767	1986	1:24000
Quarz-Susie Creek-Loncan association	1727	4759	478773	j269	nv767	1986	1:24000
Bullump-Quarz-Gando association	925	4743	479021	j2g9	nv767	1986	1:24000
Quarz-Cleavage-Tusel association	1728	4478	478774	j26b	nv767	1986	1:24000
Leevan-Quarz-McIvey association	702	4333	478985	j2f4	nv767	1986	1:24000
Quarz-McIvey-Cleavage association	1724	4093	478771	j267	nv767	1986	1:24000
Akler-Quarz-Soughe association	306	3664	478878	j29p	nv767	1986	1:24000
Eboda-Quarz-Loncan association	993	3462	479029	j2gk	nv767	1986	1:24000
Quarz-Quarz, sloping-Arcia association	1721	3019	478769	j265	nv767	1986	1:24000
Quarz-Pernty, moderately steep-Pernty association	1722	2732	478770	j266	nv767	1986	1:24000
Yuko-Tuffo-Quarz association	760	2453	478994	j2ff	nv767	1986	1:24000
Quarz-Quarz, very steep-Arcia association	1723	1909	3270900	2q90k	nv767	1986	1:24000
Chen-Graley-Quarz association	1888	1730	478807	2t6wh	nv767	1986	1:24000
Linkup-Quarz association	1676	611	2633969	2rhgr	nv767	1986	1:24000
Bregar-Roca-Quarz association	3432	5065	479630	j32y	nv775	1985	1:24000
Quarz-Linrose-Slaven association	814	4655	479722	j35x	nv775	1985	1:24000
Quarz-Linrose-Cleavage association	816	2080	479723	j35y	nv775	1985	1:24000
Quarz-Chen-Duff association	813	10895	479891	j3cc	nv776	1983	1:63360
Quarz-Bregar-Duff association	812	7045	479890	j3cb	nv776	1983	1:63360
Quarz-Highams-Atrypa variant association	811	7025	479889	j3c9	nv776	1983	1:63360
Whitepeak-Quarz-Softscrabble association	891	6070	479905	j3ct	nv776	1983	1:63360
Freznik-Quarz-Jivas association	801	4540	479887	j3c7	nv776	1983	1:63360
Quarz-Duff association	814	2070	479892	j3cd	nv776	1983	1:63360
Bregar variant-Hymas-Quarz association	975	1115	479915	j3d4	nv776	1983	1:63360

Map of Series Extent

Approximate geographic distribution of the QUARZ 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).