Soil Data Explorer - FALKNER

Official Series Description

Lab Data Summary

Aggregate lab data for the FALKNER soil series. This aggregation is based on all pedons with a current taxon name of FALKNER, 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 FALKNER 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
135A	40A4312	S1961MS139001	FALKNER	5	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	34.6403999,-89.0195007
135A	40A4316	S1961MS139002	FALKNER	5	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	34.6576233,-88.9789429

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the FALKNER 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 FALKNER 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 FALKNER 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 FALKNER 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 FALKNER 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 FALKNER 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 FALKNER 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 flats position figure.

Soil series sharing subgroup-level classification with FALKNER, 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. MS-2012-04-27-04 | Tippah County - February 1966

   Distribution and pattern of major soils in Wilcox-Dulac-Falkner association (Soil Survey of Tippah County, Mississippi; February 1966).

Map Units

Map units containing FALKNER 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
Falkner silt loam, 0 to 2 percent slopes	18	7276	331510	2w9wt	al125	1980	1:20000
Falkner silt loam, 1 to 3 percent slopes, moderately eroded	FkB2	731	565301	2xz29	ar025	1965	1:15840
Falkner silt loam, 0 to 1 percent slopes	FkA	285	565300	2xz28	ar025	1965	1:15840
Falkner silt loam, 1 to 3 percent slopes	FlB	10425	565547	lzhg	ar047	1967	1:20000
Falkner complex, mounded	Fc	4478	565545	lzhd	ar047	1967	1:20000
Falkner silt loam, 0 to 1 percent slopes	FlA	2783	565546	lzhf	ar047	1967	1:20000
Falkner silt loam, 0 to 2 percent slopes	Fa	15293	1725643	30g3s	la021	1985	1:24000
Falkner silt loam, 0 to 2 percent slopes	Fa	31853	1600164	30g3s	la059	1986	1:24000
Falkner-Boswell association, gently sloping	FBB	7895	1720665	1vrhb	la081	1973	1:24000
Boswell-Falkner association, sloping	BFC	4394	1720658	1vrh3	la081	1973	1:24000
Falkner silt loam, 2 to 5 percent slopes, eroded	FkB2	1454	331842	c49l	ms013	1963	1:15840
Falkner silt loam, 2 to 5 percent slopes	FkB	1019	331841	2w9ww	ms013	1963	1:15840
Falkner silt loam, 5 to 8 percent slopes, eroded	FkC2	935	331843	c49m	ms013	1963	1:15840
Falkner silt loam, 0 to 2 percent slopes	Fa	23631	331883	2w9wt	ms017	1969	1:20000
Falkner silt loam, 2 to 5 percent slopes, lower coastal plain	FaB	1346	332139	2w8yn	ms031	1962	1:15840
Falkner silt loam, 0 to 2 percent slopes	FaA	389	332138	2w9wt	ms031	1962	1:15840
Falkner-Susquehanna-Urban land complex, 2 to 5 percent slopes	FsB	2846	332214	c4pl	ms035	1976	1:20000
Falkner silt loam, 2 to 5 percent slopes, lower coastal plain	FaB	1225	332213	2w8yn	ms035	1976	1:20000
Falkner and Cadeville soils, 5 to 12 percent slopes	FcD	9899	332673	c55d	ms065	1972	1:20000
Falkner and Cadeville soils, 2 to 5 percent slopes	FcB	5834	332672	c55c	ms065	1972	1:20000
Falkner silt loam, 2 to 5 percent slopes, lower coastal plain	FaB	2677	332852	2w8yn	ms073	1969	1:20000
Cadeville and Falkner soils, 8 to 12 percent slopes	CgD	7166	332923	c5fg	ms077	1972	1:20000
Cadeville and Falkner soils, 4 to 8 percent slopes	CgC	5651	332922	c5ff	ms077	1972	1:20000
Falkner silt loam, 0 to 3 percent slopes	FaB	3335	332926	c5fk	ms077	1972	1:20000
Falkner silt loam, 0 to 2 percent slopes	FaA	1068	333008	2w9wt	ms081	1968	1:20000
Falkner-Benndale association, undulating	FB	7165	333118	c5mr	ms091	1983	1:20000
Falkner silt loam, 2 to 5 percent slopes, lower coastal plain	FaB	4162	333119	2w8yn	ms091	1983	1:20000
Falkner silt loam, 5 to 8 percent slopes	FaC	3667	333120	c5mt	ms091	1983	1:20000
Falkner silt loam, level	Fk	23592	333412	c5y7	ms103	1983	1:20000
Wilcox-Falkner association, undulating	WF	11340	333467	c600	ms103	1983	1:20000
Longview-Falkner association, undulating	LR	8940	333423	c5yl	ms103	1983	1:20000
Falkner silt loam, 0 to 2 percent slopes	FaA	4804	333410	2w9wt	ms103	1983	1:20000
Falkner silt loam, 2 to 5 percent slopes	FaB	761	333411	2w9ww	ms103	1983	1:20000
Falkner silt loam, 0 to 2 percent slopes	FaA	8496	333479	2w9wt	ms105	1968	1:20000
Falkner silt loam, 2 to 5 percent slopes	FaB	2622	333480	2w9ww	ms105	1968	1:20000
Falkner silt loam, 2 to 5 percent slopes, lower coastal plain	FaB	1046	333540	2w8yn	ms109	1980	1:20000
Falkner silt loam, 0 to 2 percent slopes	FaA	353	333539	c62b	ms109	1980	1:20000
Falkner silt loam, 2 to 5 percent slopes	FkB	12894	333692	2w9ww	ms115	1969	1:20000
Falkner silt loam, 0 to 2 percent slopes	FkA	3904	333691	2w9wt	ms115	1969	1:20000
Falkner silt loam, 5 to 8 percent slopes	FkC	3101	333693	c679	ms115	1969	1:20000
Falkner silt loam, 5 to 8 percent slopes, eroded	FkC2	1845	333694	c67b	ms115	1969	1:20000
Kipling-Falkner association, undulating	67B	36240	333877	c6f7	ms121	1984	1:20000
Falkner silt loam, 2 to 5 percent slopes	51B	8370	333866	2w9ww	ms121	1984	1:20000
Falkner silt loam, 0 to 2 percent slopes	FaA	19660	2431371	2w9wt	ms123	2009	1:24000
Falkner silt loam, 2 to 5 percent slopes	FaB	6754	2431372	2w9ww	ms123	2009	1:24000
Falkner silt loam, 2 to 5 percent slopes, eroded	FkB2	4663	334189	c6r9	ms139	1963	1:15840
Falkner silt loam, 5 to 8 percent slopes, severely eroded	FkC3	1782	334192	c6rd	ms139	1963	1:15840
Falkner silt loam, 2 to 5 percent slopes, severely eroded	FkB3	1531	334190	c6rb	ms139	1963	1:15840
Falkner silt loam, 0 to 2 percent slopes	FkA	415	334188	2w9wt	ms139	1963	1:15840
Falkner silt loam, 5 to 8 percent slopes, eroded	FkC2	394	334191	c6rc	ms139	1963	1:15840
Falkner silt loam, 2 to 5 percent slopes	FaB	3878	334258	2w9ww	ms145	1975	1:20000
Falkner silt loam, 0 to 2 percent slopes	FaA	3147	334257	2w9wt	ms145	1975	1:20000
Falkner silt loam, 2 to 5 percent slopes	FaB	1298	334451	2w9ww	ms155	1974	1:20000
Falkner silt loam, 0 to 2 percent slopes	FaA	967	334450	2w9wt	ms155	1974	1:20000
Falkner silt loam, 0 to 2 percent slopes	FaA	3369	334595	2w9wt	ms159	1997	1:24000
Falkner silt loam, 1 to 5 percent slopes, eroded	FaB2	66	2545341	2qsg0	tn005	2011	1:12000
Falkner silty clay loam, 2 to 5 percent slopes, severely eroded	FaB3	299	327212	bzh7	tn023	1989	1:24000
Falkner silt loam	Fk	554	327466	bzrf	tn069	1996	1:24000
Falkner silt loam, 1 to 5 percent slopes, eroded	FaB2	261	2545255	2qs7z	tn079	2012	1:12000

Map of Series Extent

Approximate geographic distribution of the FALKNER 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).