Soil Data Explorer - BADIN

Official Series Description

Lab Data Summary

Aggregate lab data for the BADIN soil series. This aggregation is based on all pedons with a current taxon name of BADIN, 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 BADIN 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	90P0839	90NC153008	Badin	6	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	35.065834,-79.8477783
136	90P0840	90NC153009	Badin	6	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	35.0275002,-79.8644409
136	S86SC025-45	S1986SC025001	Badin	3	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	34.7980285,-80.23375
136	S86SC025-46	S1986SC025703	Badin	3	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	34.7882751,-80.2781963
136	S87SC025-24	S1987SC025703	Badin	3	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	34.752594,-80.4537582
136	S87SC025-23	S1987SC025704	Badin	3	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	34.812336,-80.4581299
136	S87SC025-7	S1987SC025705	Badin	3	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	34.769558,-80.4403534
136	S95AL-123-3	S1995AL123003	Badin	3	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	33.0941667,-85.7766667
137	90P0841	90NC153010	Badin	6	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	35.0819435,-79.6183319
137	S87SC025-11	S1987SC025706	Badin	3	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	34.731739,-80.0740204

Water Balance

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

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 BADIN 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 BADIN 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 BADIN 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 BADIN, 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 BADIN 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
Tallapoosa-Badin-Fruithurst complex, 6 to 15 percent slopes, moderately eroded	TaD2	35695	1895739	2rrtj	al037	2006	1:24000
Badin-Tallapoosa-Fruithurst complex, 3 to 10 percent slopes	BfC	9620	1895711	21mmz	al037	2006	1:24000
Badin-Tatum-Tallapoosa complex, 2 to 6 percent slopes, moderately eroded	BdB2	1604	1895710	21mmy	al037	2006	1:24000
Tallapoosa-Badin-Fruithurst complex, 6 to 15 percent slopes, moderately eroded	TbD2	17788	1476445	2rrtj	al123	2005	1:24000
Badin-Tallapoosa-Fruithurst complex, 3 to 10 percent slopes	BfC	5780	1476447	1lkcb	al123	2005	1:24000
Badin-Tatum-Tallapoosa complex, 2 to 6 percent slopes, moderately eroded	BdB2	2905	1476396	1lk9p	al123	2005	1:24000
Badin silt loam, 10 to 25 percent slopes	BaE	5780	127066	486x	ga645	1995	1:12000
Badin silt loam, 2 to 10 percent slopes	BaC	4005	127065	486w	ga645	1995	1:12000
Badin channery silt loam, 2 to 8 percent slopes	BaB	16135	114497	2t80y	nc007	1999	1:24000
Badin channery silt loam, 8 to 15 percent slopes	BaC	13775	114498	3v4h	nc007	1999	1:24000
Badin-Goldston complex, 2 to 8 percent slopes	BgB	6781	114499	3v4j	nc007	1999	1:24000
Badin-Goldston complex, 15 to 25 percent slopes	BgD	6293	114501	3v4l	nc007	1999	1:24000
Badin silty clay loam, 2 to 8 percent slopes, moderately eroded	BdB2	4579	114495	3v4d	nc007	1999	1:24000
Badin-Goldston complex, 8 to 15 percent slopes	BgC	4333	114500	3v4k	nc007	1999	1:24000
Badin silty clay loam, 8 to 15 percent slopes, moderately eroded	BdC2	3569	114496	3v4f	nc007	1999	1:24000
Badin channery silt loam, 2 to 8 percent slopes	BaB	11495	111630	2t80y	nc025	1983	1:24000
Badin channery silt loam, 8 to 15 percent slopes	BaD	6860	111631	3r50	nc025	1983	1:24000
Badin channery silt loam, 15 to 45 percent slopes	BaF	2550	111632	3r51	nc025	1983	1:24000
Nanford-Badin complex, 6 to 10 percent slopes	NaC	29853	1485633	1lvxn	nc037	2005	1:24000
Nanford-Badin complex, 2 to 6 percent slopes	NaB	25426	1485631	1lvxl	nc037	2005	1:24000
Georgeville-Badin complex, 10 to 15 percent slopes	GkD	17512	1485563	1lvvd	nc037	2005	1:24000
Nanford-Badin complex, 10 to 15 percent slopes	NaD	17001	1485629	1lvxj	nc037	2005	1:24000
Georgeville-Badin complex, 15 to 30 percent slopes	GkE	11222	1485565	1lvvg	nc037	2005	1:24000
Badin-Nanford complex, 15 to 30 percent slopes	BaE	8047	1485483	1lvrt	nc037	2005	1:24000
Goldston-Badin complex, 2 to 15 percent slopes	GoC	3662	1485574	1lvvr	nc037	2005	1:24000
Goldston-Badin complex, 15 to 35 percent slopes	GoE	2133	1485572	1lvvp	nc037	2005	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
Badin channery silt loam, 2 to 8 percent slopes	BaB	22975	112141	2t80y	nc057	1985	1:24000
Badin channery silt loam, 8 to 15 percent slopes	BaD	13383	112142	3rph	nc057	1985	1:24000
Badin channery silt loam, 15 to 30 percent slopes	BaE	5840	112143	3rpj	nc057	1985	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
Goldston-Badin complex, 15 to 45 percent slopes	GoE	9086	2233578	2dz6x	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
Badin-Goldston complex, 8 to 15 percent slopes, moderately eroded	BaC2	2508	2233550	2dz60	nc123	2007	1:24000
Badin-Goldston complex, 2 to 8 percent slopes, moderately eroded	BaB2	1122	2233549	2dz5z	nc123	2007	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
Georgeville-Badin complex, 8 to 15 percent slopes, moderately eroded	UxC2	9333	2450731	2n85v	nc153	1996	1:24000
Goldston-Badin complex, 15 to 55 percent slopes	GdD	7614	114709	3vc9	nc153	1996	1:24000
Georgeville-Badin complex, 15 to 25 percent slopes	UxD	4938	2450732	2n85w	nc153	1996	1:24000
Georgeville-Badin complex, 2 to 8 percent slopes, moderately eroded	UxB2	2674	2450730	2n85t	nc153	1996	1:24000
Badin-Goldston complex, 8 to 15 percent slopes	BgC	1921	114697	3vbx	nc153	1996	1:24000
Badin channery silt loam, 2 to 8 percent slopes	BcB	574	114696	2t80y	nc153	1996	1:24000
Badin channery silt loam, 2 to 8 percent slopes	BaB	3960	114966	2t80y	nc159	1996	1:24000
Badin-Goldston complex, 2 to 8 percent slopes	BgB	1914	114969	3vmp	nc159	1996	1:24000
Badin channery silt loam, 8 to 15 percent slopes	BaC	1374	114967	3vmm	nc159	1996	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
Badin-Goldston complex, 8 to 15 percent slopes	BgC	783	114970	3vmq	nc159	1996	1:24000
Tarrus-Badin complex, 8 to 15 percent slopes	TaC	446	2422567	2m9wb	nc159	1996	1:24000
Badin channery silt loam, 15 to 30 percent slopes	BaD	210	114968	3vmn	nc159	1996	1:24000
Badin channery silt loam, 2 to 8 percent slopes	BaB	36068	115151	2t80y	nc167	1984	1:24000
Badin channery silt loam, 8 to 15 percent slopes	BaD	28158	115152	3vtl	nc167	1984	1:24000
Badin channery silt loam, 15 to 45 percent slopes	BaF	8569	115153	3vtm	nc167	1984	1:24000
Badin-Urban land complex, 2 to 8 percent slopes	BbB	4240	115154	3vtn	nc167	1984	1:24000
Badin-Urban land complex, 8 to 25 percent slopes	BbD	1361	115155	3vtp	nc167	1984	1:24000
Badin channery silt loam, 2 to 8 percent slopes	BaB	53723	115333	2t80y	nc179	1991	1:24000
Goldston-Badin complex, 2 to 8 percent slopes	GsB	30866	115352	3w11	nc179	1991	1:24000
Badin channery silty clay loam, 2 to 8 percent slopes, moderately eroded	BdB2	30043	2440232	2mx85	nc179	1991	1:24000
Goldston-Badin complex, 8 to 15 percent slopes	GsC	13320	115353	3w12	nc179	1991	1:24000
Badin channery silt loam, 8 to 15 percent slopes	BaC	9497	115334	3w0g	nc179	1991	1:24000
Badin-Urban land complex, 2 to 8 percent slopes	BuB	7950	115337	3w0k	nc179	1991	1:24000
Badin channery silty clay loam, 8 to 15 percent slopes, moderately eroded	BdC2	6417	2440233	2mx86	nc179	1991	1:24000
Goldston-Badin complex, 15 to 45 percent slopes	GsE	3538	115354	3w13	nc179	1991	1:24000
Badin-Urban land complex, 8 to 15 percent slopes	BuC	307	115338	3w0l	nc179	1991	1:24000
Badin silt loam, 15 to 25 percent slopes	BaE	15644	131990	4fbr	sc025	1989	1:20000
Badin silt loam, 10 to 15 percent slopes	BaD	8624	131989	4fbq	sc025	1989	1:20000
Badin silt loam, 6 to 10 percent slopes	BaC	8184	131988	4fbp	sc025	1989	1:20000
Badin silty clay loam, 2 to 6 percent slopes, eroded	BdB2	7706	131991	4fbs	sc025	1989	1:20000
Badin silt loam, 2 to 6 percent slopes	BaB	5336	131987	4fbn	sc025	1989	1:20000
Badin silty clay loam, 6 to 10 percent slopes, eroded	BdC2	5235	131992	4fbt	sc025	1989	1:20000
Badin silt loam, 15 to 40 percent slopes	BaF	289	130605	4cx2	sc069	1995	1:24000
Badin silt loam, 2 to 15 percent slopes	BaD	95	130604	4cx1	sc069	1995	1:24000
Georgeville-Badin complex, 15 to 25 percent slopes, moderately eroded	GrE2	14317	2513844	2lq17	sc091	2013	1:15840
Georgeville-Badin complex, 10 to 15 percent slopes, moderately eroded	GrD2	3790	2513843	2lq14	sc091	2013	1:15840
Tatum-Badin complex, 8 to 15 percent slopes	27C	1569	2420760	2m801	va025	2007	1:24000
Badin-Goldston complex, 8 to 15 percent slopes	4C	803	2420718	2m7yp	va025	2007	1:24000
Tatum-Badin complex, 2 to 8 percent slopes	27B	520	2420759	2m800	va025	2007	1:24000
Goldston-Badin complex, 15 to 35 percent slopes	15D	481	2420741	2m7zf	va025	2007	1:24000
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
Nanford-Badin complex, 8 to 15 percent slopes	35C	4099	1472835	1lflt	va083	2004	1:24000
Nanford-Badin complex, 2 to 8 percent slopes	35B	2763	1472834	1lfls	va083	2004	1:24000
Tarrus-Badin complex, 15 to 25 percent slopes	47D	2610	1472858	1lfmk	va083	2004	1:24000
Nanford-Badin complex, 15 to 25 percent slopes	35D	2406	1472836	1lflv	va083	2004	1:24000

Map of Series Extent

Approximate geographic distribution of the BADIN 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).