Soil Data Explorer - BARX

Official Series Description

Lab Data Summary

Aggregate lab data for the BARX soil series. This aggregation is based on all pedons with a current taxon name of BARX, 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 BARX were used in the calculation. Source: KSSL snapshot (updated 2020-03-18). 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
35	86P0494	86AZ017008	Barx	7	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	34.5024986,-110.2358322
35	40A0706	S1956AZ017026	Barx	5	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	34.4652786,-110.0833359
36	80P0375	80CO113001	Barx	7	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	38.1197205,-108.7244415
36	92P0912	92UT037164A	Barx	7	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	37.5999985,-109.913887
36	93P0645	93CO083003	Barx	7	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	37.4644432,-108.9850006
n/a	82P0781	82UT037001	Barx	7	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 BARX 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 BARX 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 BARX 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 BARX 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 BARX 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 BARX 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 BARX 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 BARX, 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 BARX 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
Barx fine sandy loam, 1 to 5 percent slopes	8	17366	52433	1rkd	az623	1994	1:24000
Barx-Strych complex, 1 to 10 percent slopes	9	2696	52261	1rcv	az623	1994	1:24000
Barx fine sandy loam, 1 to 5 percent slopes	2	40160	52476	1rls	az625	1992	1:24000
Mellenthin-Barx complex, 1 to 15 percent slopes	31	14636	52508	1rmt	az625	1992	1:24000
Barx loam, 1 to 4 percent slopes	3	2459	52504	1rmp	az625	1992	1:24000
Barx gravelly loam, 1 to 6 percent slopes	4	13080	54125	1t9z	az629	1985	1:24000
Barx-Pensom complex, 1 to 6 percent slopes	5	1300	54144	1tbl	az629	1985	1:24000
Barx fine sandy loam, 3 to 10 percent slopes	6	28605	54235	1tfj	az633	1994	1:24000
Barx fine sandy loam, 0 to 3 percent slopes	5	2375	54224	1tf5	az633	1994	1:24000
Plaintank-Barx complex, 1 to 5 percent slopes	32	8500	54528	1tqz	az699	1993	1:24000
Barx fine sandy loam, 1 to 6 percent slopes	4	2595	54508	1tqb	az699	1993	1:24000
Barx-Strych-Doakum families complex, 5 to 65 percent slopes	9	31995	58097	2sfl5	az715	2007	1:24000
Barx loam, 3 to 12 percent slopes	103	13	509443	2wr7n	co660	1994	1:24000
Barx-Gapmesa complex, 2 to 6 percent slopes	4	1863	59437	2wr7p	co670	2005	1:24000
Barx very fine sandy loam, 1 to 4 percent slopes	6	784	59436	1zv9	co670	2005	1:24000
Barx loam, 6 to 12 percent slopes	5	1	725709	2tky0	co670	2005	1:24000
Barx-Gapmesa complex, 2 to 6 percent slopes	11	5877	57555	2wr7p	co671	1997	1:24000
Barx loam, 3 to 6 percent slopes	8	4085	57707	1y1j	co671	1997	1:24000
Barx very fine sandy loam, 1 to 4 percent slopes	10	842	57544	1xw8	co671	1997	1:24000
Barx loam, 6 to 12 percent slopes	9	826	57725	2tky0	co671	1997	1:24000
Barx-Progresso complex, 3 to 12 percent slopes	17	26815	502007	jvcs	co675	1986	1:24000
Barx fine sandy loam, 1 to 3 percent slopes	14	17453	501999	jvcj	co675	1986	1:24000
Barx fine sandy loam, 3 to 6 percent slopes	15	16647	502003	jvcn	co675	1986	1:24000
Barx fine sandy loam, 6 to 12 percent slopes	16	1055	502005	jvcq	co675	1986	1:24000
Barx-Progresso complex, 3 to 12 percent slopes	MC64	263	3170454	k09z	co675	1986	1:24000
Barx-Lazear, very flaggy-Rock outcrop complex, 3 to 35 percent slopes	B31	5852	2990906	k296	co676	1983	1:24000
Barx-Progresso complex, 3 to 12 percent slopes	MC64	3676	3170467	k09z	co676	1983	1:24000
Barx-Panitchen complex, 3 to 12 percent slopes	MC38	1780	3170465	k096	co676	1983	1:24000
Barx-Lazear, very flaggy-Rock outcrop complex, 3 to 35 percent slopes	B31	41451	508654	k296	co677	2018	1:24000
Barx loam, 3 to 15 percent slopes	34D	2486	508576	k26p	co677	2018	1:24000
Barx-Samala complex, 3 to 15 percent slopes	32D	1231	508575	k26n	co677	2018	1:24000
Barx-Lazear, very flaggy-Rock outcrop complex, 3 to 35 percent slopes	B31	3987	2990948	k296	co679	1976	1:24000
Barx-Progresso complex, 3 to 12 percent slopes	64	10817	506756	k09z	co680	1970	1:31680
Barx-Panitchen complex, 3 to 12 percent slopes	38	3659	506732	k096	co680	1970	1:31680
Barx-Lazear, very flaggy-Rock outcrop complex, 3 to 35 percent slopes	B31	2929	3084830	k296	co680	1970	1:31680
Abra-Barx complex, 3 to 12 percent slopes	71U	2810	506665	k071	co680	1970	1:31680
Barx-Clapper complex, 3 to 12 percent slopes	200	219	506707	k08d	co680	1970	1:31680
Barx loam, 3 to 12 percent slopes	3	14014	2990830	2wr7n	co682	1986	1:24000
Barx-Clapper complex, 3 to 12 percent slopes	4	3934	496701	jnvm	co682	1986	1:24000
Barx-Clapper complex, 3 to 12 percent slopes	MC200	131	3170509	k08d	co682	1986	1:24000
Abra-Barx complex, 3 to 12 percent slopes	MC71U	8	3170529	k071	co682	1986	1:24000
Barx fine sandy loam, 1 to 5 percent slopes	McB	4541	2408397	2lv47	ut013		1:24000
Leebench-Smithpond-Barx complex, 2 to 8 percent slopes	085	3495	504985	jygv	ut623	2011	1:24000
Barx fine sandy loam	2	20439	504512	jxzl	ut624	1985	1:24000
Hostage-Barx complex	20	9559	504513	jxzm	ut624	1985	1:24000
Abra-Barx complex	1	2399	504501	jxz7	ut624	1985	1:24000
Abra-Barx complex, 3 to 12 percent slopes	671U	1229	2990964	k071	ut624	1985	1:24000
Barx-Progresso complex, 3 to 12 percent slopes	664	28	2990973	k09z	ut624	1985	1:24000
Barx fine sandy loam, 3 to 8 percent slopes	6	4630	55382	1vmj	ut633	1983	1:24000
Barx fine sandy loam, 2 to 10 percent slopes	12	4800	504348	jxt9	ut636	1984	1:24000
Rizno-Barx-Yarts complex	45	126069	55470	1vqc	ut638	1985	1:24000
Barx very fine sandy loam, 1 to 4 percent slopes	5	22803	55475	1vqj	ut638	1985	1:24000
Barx-Strych-Skos complex	6	8795	55482	1vqr	ut638	1985	1:24000
Mivida-Barx, dry complex, 1 to 8 percent slopes	54	361	2433235	2mnzg	ut642		1:63360
Barx very fine sandy loam, 0 to 8 percent slopes	200	16183	2883912	2sp8g	ut643	1976	1:63000
Milok-Barx-Rizno complex, 0 to 8 percent slopes	201	9422	2883913	2sp8h	ut643	1976	1:63000
Barx family, 3 to 8 percent slopes	mt5	460	3202662	2zbtx	ut645		1:24000
Barx-Remorris complex, 5 to 45 percent slopes	5	1567	2608453	1ifso	ut685	1990	1:24000
Barx-Radnik, moist-Progresso, dry complex, 2 to 8 percent slopes	5112	11663	59804	2075	ut686	2004	1:24000
Ruinpoint-Barx complex, 2 to 8 percent slopes	5172	11173	608467	nf4z	ut686	2004	1:24000
Strych-Horsemountain-Barx complex, 2 to 15 percent slopes	5132	11151	59861	2090	ut686	2004	1:24000
Barx fine sandy loam, 2 to 10 percent slopes	5037	10177	59782	206g	ut686	2004	1:24000
Barx-Remorris complex, 5 to 45 percent slopes	5103	6927	59736	204z	ut686	2004	1:24000
Mivida-Barx, dry complex, 1 to 8 percent slopes	5055	5864	59817	207l	ut686	2004	1:24000
Milok, cool-Barx, dry complex, 1 to 5 percent slopes	5003	3718	59748	205c	ut686	2004	1:24000

Map of Series Extent

Approximate geographic distribution of the BARX 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).