Soil Data Explorer - TARRUS

Official Series Description

Lab Data Summary

Aggregate lab data for the TARRUS soil series. This aggregation is based on all pedons with a current taxon name of TARRUS, 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 TARRUS 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
136	13N4953	S2012NC135008	Tarrus	7	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	36.1622306,-79.1122222

Water Balance

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

There are insufficient data to create the 3D mountains figure.

There are insufficient data to create the 3D terrace figure.

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

Competing Series

Soil series competing with TARRUS 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 TARRUS 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 TARRUS 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 mountains figure.

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

Soil series sharing subgroup-level classification with TARRUS, 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 TARRUS 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
Tarrus gravelly silt loam, 2 to 8 percent slopes	TaB	4366	114562	3v6k	nc007	1999	1:24000
Tarrus-Georgeville complex, 8 to 15 percent slopes	TgC	2395	114563	3v6l	nc007	1999	1:24000
Tarrus silt loam, 2 to 8 percent slopes	TaB	5900	2422523	2m9tx	nc025	1983	1:24000
Tarrus silt loam, 8 to 15 percent slopes	TaD	3535	2422524	2m9ty	nc025	1983	1:24000
Tarrus silty clay loam, 2 to 8 percent slopes, moderately eroded	TbB2	1430	2422525	2m9tz	nc025	1983	1:24000
Tarrus silty clay loam, 8 to 15 percent slopes, moderately eroded	TbD2	765	2422526	2m9v0	nc025	1983	1:24000
Badin-Tarrus complex, 2 to 8 percent slopes	BdB	982	1485485	1lvrw	nc037	2005	1:24000
Badin-Tarrus complex, 8 to 15 percent slopes, moderately eroded	BeC2	663	1485491	1lvs2	nc037	2005	1:24000
Badin-Tarrus complex, 8 to 15 percent slopes	BdC	326	1485489	1lvs0	nc037	2005	1:24000
Badin-Tarrus complex, 2 to 8 percent slopes, moderately eroded	BeB2	310	1485487	1lvry	nc037	2005	1:24000
Tarrus silt loam, 2 to 8 percent slopes	TaB	2389	2442022	2mz3x	nc105	1982	1:24000
Tarrus silt loam, 15 to 30 percent slopes	TaE	2072	2442024	2mz3z	nc105	1982	1:24000
Tarrus silt loam, 8 to 15 percent slopes	TaD	1794	2442023	2mz3y	nc105	1982	1:24000
Badin-Tarrus complex, 8 to 15 percent slopes	BdC	22374	2233552	2dz62	nc123	2007	1:24000
Badin-Tarrus complex, 15 to 25 percent slopes	BdD	18682	2233553	2dz63	nc123	2007	1:24000
Badin-Tarrus complex, 2 to 8 percent slopes, moderately eroded	BeB2	12015	2233555	2dz65	nc123	2007	1:24000
Badin-Tarrus complex, 2 to 8 percent slopes	BdB	10457	2233551	2dz61	nc123	2007	1:24000
Badin-Tarrus complex, 8 to 15 percent slopes, moderately eroded	BeC2	4878	2233556	2dz66	nc123	2007	1:24000
Badin-Tarrus complex, 25 to 45 percent slopes	BdE	3931	2233554	2dz64	nc123	2007	1:24000
Tarrus and Nanford soils, 15 to 25 percent slopes	TnE	9206	2450401	2n7v6	nc125	1987	1:24000
Tarrus silt loam, 8 to 15 percent slopes	TaD	15200	2450744	2n868	nc135	1975	1:20000
Tarrus silt loam, 15 to 25 percent slopes	TaE	7486	2450745	2n869	nc135	1975	1:20000
Tarrus loam, 10 to 15 percent slopes	TaD	5084	2439325	2mw9x	nc145	1987	1:24000
Tarrus loam, 15 to 35 percent slopes	TaE	4539	2439326	2mw9y	nc145	1987	1:24000
Badin-Tarrus complex, 15 to 25 percent slopes	BaD	40691	117426	3y5y	nc151	1998	1:24000
Badin-Tarrus complex, 2 to 8 percent slopes, moderately eroded	BtB2	30502	117428	3y60	nc151	1998	1:24000
Badin-Tarrus complex, 8 to 15 percent slopes, moderately eroded	BtC2	27066	117429	3y61	nc151	1998	1:24000
Badin-Tarrus complex, 8 to 15 percent slopes	BaC	22812	117425	3y5x	nc151	1998	1:24000
Badin-Tarrus complex, 2 to 8 percent slopes	BaB	12486	117424	3y5w	nc151	1998	1:24000
Badin-Tarrus complex, 25 to 45 percent slopes	BaE	7530	117427	3y5z	nc151	1998	1:24000
Tarrus-Badin complex, 2 to 8 percent slopes	TaB	1279	2422566	2m9w9	nc159	1996	1:24000
Tarrus-Badin complex, 2 to 8 percent slopes, moderately eroded	TbB2	1134	2422568	2m9wc	nc159	1996	1:24000
Tarrus-Badin complex, 8 to 15 percent slopes	TaC	446	2422567	2m9wb	nc159	1996	1:24000
Tarrus channery silt loam, 2 to 8 percent slopes	TbB	23660	2440263	2mx95	nc167	1984	1:24000
Tarrus channery silty clay loam, 2 to 8 percent slopes, moderately eroded	TcB2	5349	2440265	2mx97	nc167	1984	1:24000
Tarrus channery silt loam, 8 to 15 percent slopes	TbD	4538	2440264	2mx96	nc167	1984	1:24000
Tarrus-Urban land complex, 2 to 8 percent slopes	TdB	2396	2440267	2mx99	nc167	1984	1:24000
Tarrus gravelly loam, 15 to 35 percent slopes	TaF	2183	2440262	2mx94	nc167	1984	1:24000
Tarrus channery silty clay loam, 8 to 15 percent slopes, moderately eroded	TcD2	1382	2440266	2mx98	nc167	1984	1:24000
Tarrus gravelly silty clay loam, 2 to 8 percent slopes, moderately eroded	TbB2	49164	2440249	2mx8q	nc179	1991	1:24000
Tarrus gravelly silt loam, 2 to 8 percent slopes	TaB	19582	2440243	2mx8j	nc179	1991	1:24000
Tarrus gravelly silty clay loam, 8 to 15 percent slopes, moderately eroded	TbC2	7014	2440250	2mx8r	nc179	1991	1:24000
Tarrus gravelly silt loam, 8 to 15 percent slopes	TaC	3149	2440244	2mx8k	nc179	1991	1:24000
Tarrus-Urban land complex, 2 to 8 percent slopes	TuB	2486	2440251	2mx8s	nc179	1991	1:24000
Tarrus gravelly silt loam, 15 to 35 percent slopes	TaD	595	2440245	2mx8l	nc179	1991	1:24000
Tarrus silt loam, 10 to 15 percent slopes	TaD	4494	130073	2wb9y	sc047	1973	1:20000
Tarrus silt loam, 15 to 25 percent slopes	TaE	547	130074	2wb9z	sc047	1973	1:20000
Tarrus loam, 10 to 15 percent slopes, moderately eroded	TaD2	7418	130332	2wb9w	sc057	1967	1:20000
Tarrus silty clay loam, 10 to 25 percent slopes, severely eroded	TcE3	6092	130334	2wbb0	sc057	1967	1:20000
Tarrus loam, 15 to 25 percent slopes, moderately eroded	TaE2	3872	130333	2wb9x	sc057	1967	1:20000
Tarrus silt loam, 15 to 25 percent slopes	TaE	3016	130541	2wb9z	sc063	1972	1:20000
Tarrus silt loam, 10 to 15 percent slopes	TaD	3742	130723	2wb9y	sc065	1973	1:20000
Tarrus silt loam, 15 to 25 percent slopes	TaE	898	130724	2wb9z	sc065	1973	1:20000
Tarrus silt loam, 15 to 30 percent slopes	GoE	1046	131195	2yclv	sc081	1960	1:20000
Tarrus-Badin complex, 2 to 8 percent slopes	47B	7493	1472856	1lfmh	va083	2004	1:24000
Tarrus-Badin complex, 8 to 15 percent slopes	47C	6114	1472857	1lfmj	va083	2004	1:24000
Tarrus-Badin complex, 15 to 25 percent slopes	47D	2610	1472858	1lfmk	va083	2004	1:24000

Map of Series Extent

Approximate geographic distribution of the TARRUS 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).