Soil Data Explorer - ROBINSONVILLE

Official Series Description

Lab Data Summary

Aggregate lab data for the ROBINSONVILLE soil series. This aggregation is based on all pedons with a current taxon name of ROBINSONVILLE, 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 ROBINSONVILLE 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
131A	M0514304	2005MO14304	ROBINSONVILLE	4	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	36.5333333,-89.4

Water Balance

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

Competing Series

Soil series competing with ROBINSONVILLE 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 ROBINSONVILLE 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).

There are insufficient data to create the annual climate figure.

Geomorphic description summaries for the ROBINSONVILLE 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 2D hillslope position figure.

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

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.

Soil series sharing subgroup-level classification with ROBINSONVILLE, 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. KY-2012-01-27-18 | Carlisle and Hickman Counties - July 1997

   Relationship of soils to topography and underlying material in the Openlake-Commerce-Bardwell general soil map unit in Carlisle County (Soil Survey of Carlisle and Hickman Counties, Kentucky; July 1997).

2. MS-2012-04-26-09 | De Soto County - September 1959

   Soil associations in De Soto County (Soil Survey of De Soto County, Mississippi; September 1959).

3. MS-2012-04-27-09 | Tunica County - May 1956

   Soil association map of Tunica County, Miss (Soil Survey of Tunica County, Mississippi; May 1956).

4. MS-2012-04-27-10 | Bolivar County - December 1958

   Soil associations in Bolivar County: 1. Alluvial soils; 2. Commerce-Robinsonville-Crevasse; 3. Forestdale-Dundee-Bosket; 4. Brittain-Pearson-Dexter; 5. Dowling-Alligator-Sharkey (Soil Survey of Bolivar County, Mississippi; December 1958).

5. OK-2012-02-17-47 | Sequoyah County - June 1970

   Typical pattern of soils in associations 2 and 4 (Soil Survey of Sequoyah County, Oklahoma; June 1970).

6. TN-2012-03-19-10 | Lauderdale County - June 1990

   Typical pattern of soils and underlying material in the Commerce-Robinsonville and Sharkey-Keyespoint-Openlake general soil map units on the Mississippi River flood plain (Soil Survey of Lauderdale County, TN; 1990).

Map Units

Map units containing ROBINSONVILLE 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
Robinsonville loam, gently undulating	RoU	2505	565281	lz6w	ar017	1964	1:20000
Robinsonville very fine sandy loam	Rn	9040	564176	ly27	ar035	1970	1:20000
Robinsonville very fine sandy loam, frequently flooded	Ro	2980	564177	ly28	ar035	1970	1:20000
Bowdre, Desha, and Robinsonville soils, gently undulating	BdU	1440	564186	ly2k	ar041	1968	1:20000
Robinsonville fine sandy loam	Ro	5310	564106	lxzz	ar077	1974	1:20000
Robinsonville soils, frequently flooded	Rs	1960	564107	ly00	ar077	1974	1:20000
Robinsonville fine sandy loam	Ro	4480	564250	ly4m	ar107	1971	1:20000
Robinsonville soils, frequently flooded	Rs	2850	564251	ly4n	ar107	1971	1:20000
Robinsonville fine sandy loam, frequently flooded	28	1150	566655	m0n6	ar145	1980	1:20000
Robinsonville fine sandy loam, frequently flooded	Ro	1040	549145	lffc	ky055	1985	1:20000
Robinsonville-Huntington complex, frequently flooded	Ru	468	549146	lffd	ky055	1985	1:20000
Robinsonville fine sandy loam, 0 to 3 percent slopes, occasionally flooded	Rc	993	655048	pzml	ky075	2002	1:12000
Robinsonville fine sandy loam, 0 to 3 percent slopes, frequently flooded	Rf	903	655027	pzlx	ky075	2002	1:12000
Robinsonville fine sandy loam, 0 to 3 percent slopes, protected	Rb	339	655028	pzly	ky075	2002	1:12000
Robinsonville fine sandy loam, natural levee, 8 to 25 percent slopes, occasionally flooded	RmD	133	655029	pzlz	ky075	2002	1:12000
Robinsonville fine sandy loam	Rf	1239	549782	lg2x	ky169	1965	1:15840
Robinsonville-Crevasse complex, frequently flooded	Rc	3542	570540	m4pj	ky611	1991	1:20000
Bowdre-Robinsonville complex, frequently flooded	Br	1660	570517	m4ns	ky611	1991	1:20000
Robinsonville fine sandy loam	Ro	1615	549530	lfts	ky635	1978	1:20000
Huntington-Robinsonville complex	Hu	1483	549509	lft3	ky635	1978	1:20000
Convent and Robinsonville soils, frequently flooded	CRC	4521	577013	mcfb	la033	2007	1:24000
Convent and Robinsonville soils, frequently flooded	CX	2355	1451375	1kq8k	la047	1975	1:24000
Cancienne and Carville soils, undulating, frequently flooded	Cg	1259	1451366	1kq88	la047	1975	1:24000
Robinsonville and Commerce soils, occasionally flooded	RE	31034	1678432	1tbjz	la077	1980	1:24000
Robinsonville and Commerce soils, occasionally flooded	RE	10492	1397384	1hx2x	la121	2004	1:24000
Robinsonville and Convent soils, occasionally flooded	RC	9934	1725612	1vxmx	la125	2002	1:24000
Robinsonville very fine sandy loam	Ro	2301	567426	m1g2	ms001	1966	1:15840
Robinsonville fine sandy loam	Ra	1287	567508	m1jq	ms011	1956	1:20000
Commerce-Robinsonville-Crevasse soils	Cg	1123	567479	m1hs	ms011	1956	1:20000
Robinsonville and Marietta soils	Rm	3557	331903	c4ck	ms017	1969	1:20000
Crevasse, Commerce, and Robinsonville soils, (bruno, commerce and robinsonville)	Cr	6255	567578	m1lz	ms021	1961	1:20000
Robinsonville very fine sandy loam, 0 to 3 percent slopes	Ra	2231	567655	m1pg	ms027	1956	1:24000
Robinsonville-crevasse soils, 0 to 3 percent slopes (robinsonville, bruno)	Rc	1813	567657	m1pj	ms027	1956	1:24000
Robinsonville-crevasse soils, 3 to 7 percent slopes (robinsonville, bruno)	Rd	386	567658	m1pk	ms027	1956	1:24000
Robinsonville very fine sandy loam, 3 to 7 percent slopes	Rb	175	567656	m1ph	ms027	1956	1:24000
Robinsonville very fine sandy loam, nearly level phase	Rf	190	567790	m1tt	ms033	1955	1:24000
Robinsonville very fine sandy loam, 0 to 2 percent slopes	Ro	1450	568055	m23c	ms055	1960	1:20000
Robinsonville very fine sandy loam, 2 to 5 percent slopes	Rs	230	568056	m23d	ms055	1960	1:20000
Bruin-Robinsonville association	BR	3639	568068	m23s	ms063	1976	1:20000
Robinsonville very fine sandy loam	Rb	752	568095	m24n	ms063	1976	1:20000
Robinsonville soils	Ro	2201	333040	c5k7	ms081	1968	1:20000
Robinsonville sandy loam	Ro	4254	333729	c68g	ms115	1969	1:20000
Robinsonville very fine sandy loam, 0 to 2 percent slopes	Ro	330	568433	m2hk	ms125	1960	1:20000
Robinsonville very fine sandy loam, 0 to 2 percent slopes	261	3427	1715969	1vllv	ms143	2006	1:24000
Commerce and Robinsonville very fine sandy loams, land leveled	380	1813	1716075	1vlq8	ms143	2006	1:24000
Robinsonville very fine sandy loam, 0 to 2 percent slopes, frequently flooded	262	740	1715970	1vllw	ms143	2006	1:24000
Commerce, Robinsonville, and Crevasse soils, frequently flooded (commerce, robinsonville, bruno)	CrC	37531	2693457	2rp1y	ms149	1962	1:15840
Robinsonville loam	Ro	352	568710	m2sh	ms149	1962	1:15840
Robinsonville very fine sandy loam, 0 to 2 percent slopes	Ro	1510	568765	m2v8	ms151	1959	1:20000
Robinsonville silt loam, frequently flooded	23	4202	571086	m584	ms157	2006	1:24000
Robinsonville loam	Rs	4028	566813	m0t9	tn045	1963	1:15840
Robinsonville fine sandy loam	Ro	2547	566812	m0t8	tn045	1963	1:15840
Robinsonville fine sandy loam, frequently flooded	Rm	4708	567132	m14l	tn095	1966	1:20000
Robinsonville silt loam, occasionally flooded	Rc	7409	567181	m165	tn097	1985	1:24000
Robinsonville fine sandy loam, occasionally flooded	Rb	5765	567180	m164	tn097	1985	1:24000
Robinsonville silty clay loam, overwash, occasionally flooded	Rd	2082	567182	m166	tn097	1985	1:24000
Robinsonville silt loam	Rn	5181	567320	m1bn	tn157	1966	1:15840
Robinsonville fine sandy loam	Rb	1681	567319	m1bm	tn157	1966	1:15840
Robinsonville fine sandy loam, rarely flooded	Ro	5313	567356	m1ct	tn167	1989	1:24000
Robinsonville silt loam, occasionally flooded	Rb	3888	567355	m1cs	tn167	1989	1:24000

Map of Series Extent

Approximate geographic distribution of the ROBINSONVILLE 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).