Soil Data Explorer - KIPLING

Official Series Description

Lab Data Summary

Aggregate lab data for the KIPLING soil series. This aggregation is based on all pedons with a current taxon name of KIPLING, 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 KIPLING 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	S85AL-011-2	85AL011002-pgm	Kipling	3	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	32.175,-85.9286111
135A	S89AL-105-1	89AL105001-pgm	Kipling	3	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	32.3380556,-87.5086111
135A	91P1061	91MS103004	Kipling	7	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	33.1916656,-88.5941696
135A	81P0561	S1981MS101002	Kipling	7	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	32.2532349,-89.2597885
135A	06N0789	S2006AL119001	Kipling	7	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	32.6080017,-88.1974411

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the KIPLING 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 KIPLING 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 KIPLING 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 KIPLING 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 KIPLING 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 KIPLING 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 KIPLING 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 KIPLING, 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-2012-02-06-08 | Prentiss County - October 1997

   Typical pattern of soils and parent material in the Kipling-Sumter general soil map unit (Soil Survey of Prentiss County, Mississippi; October 1997).

Map Units

Map units containing KIPLING 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
Kipling fine sandy loam, 1 to 3 percent slopes, eroded	KpB2	1872	328417	c0r3	al011	1986	1:20000
Troup-Kipling association, hilly	62	43162	329102	c1g6	al047	1977	1:20000
Kipling loam, 0 to 1 percent slopes	30	24535	329067	c1f2	al047	1977	1:20000
Kipling loam, 1 to 5 percent slopes	31	13862	329068	c1f3	al047	1977	1:20000
Kipling-Urban land complex, 0 to 5 percent slopes	32	553	329069	c1f4	al047	1977	1:20000
Kipling loam, 1 to 3 percent slopes, eroded	KlB2	3229	329665	c21c	al063	2013	1:
Kipling loam, 0 to 1 percent slopes	KlA	1226	329664	c21b	al063	2013	1:
Kipling loam, 3 to 5 percent slopes, eroded	KlC2	765	329666	c21d	al063	2013	1:
Kipling loam, 5 to 8 percent slopes, eroded	KlD2	488	329667	c21f	al063	2013	1:
Kipling clay loam, 1 to 5 percent slopes	KpC	17794	329752	2s69s	al065	2003	1:24000
Kipling fine sandy loam, 1 to 5 percent slopes	KpC	2539	2514932	2qdhn	al085	2011	1:24000
Kipling fine sandy loam, 5 to 12 percent slopes	KpD	236	2514933	2qdhp	al085	2011	1:24000
Kipling clay loam, 1 to 5 percent slopes	KpC	7560	330582	2s69s	al091	1997	1:24000
Kipling-Urban land complex, 0 to 5 percent slopes	KuC	410	330583	c2zz	al091	1997	1:24000
Kipling clay loam, 0 to 1 percent slopes	KcA	7559	330922	c3bx	al101	1958	1:20000
Kipling silty clay	Kb	2439	330921	c3bw	al101	1958	1:20000
Kipling very fine sandy loam, eroded, nearly level phase	KcB2	1456	330923	c3by	al101	1958	1:20000
Kipling clay loam, 1 to 5 percent slopes	KpB	17070	331236	2s69s	al105	1996	1:24000
Demopolis-Kipling complex, 3 to 20 percent slopes, moderately eroded	DkE2	73164	331473	2tjlh	al119	1986	1:24000
Kipling silty clay loam, 1 to 5 percent slopes, eroded	KpB2	34899	331479	c3xw	al119	1986	1:24000
Kipling loam, 0 to 1 percent slopes	KpA	15645	331478	c3xv	al119	1986	1:24000
Kipling-Urban land complex, 1 to 8 percent slopes	KuC	435	331480	c3xx	al119	1986	1:24000
Kipling fine sandy loam, 1 to 5 percent slopes	KpB	613	2642030	2rjpl	al129	2013	1:24000
Kipling silty clay loam, 5 to 12 percent slopes, eroded	KpD2	1170	331657	c43m	al131	1997	1:24000
Kipling silt loam, 0 to 2 percent slopes	31	8239	3179364	lyms	ar019	1983	1:20000
Kipling silty clay loam, 2 to 5 percent slopes	32	7528	3179365	lymt	ar019	1983	1:20000
Kipling loam, 1 to 3 percent slopes	14	10050	565638	lzld	ar057	1976	1:20000
Kipling silty clay loam, 3 to 8 percent slopes, eroded	15	9197	565639	lzlf	ar057	1976	1:20000
Kipling silt loam, 2 to 5 percent slopes	37	7069	564911	lyty	ar670	1981	1:20000
Kipling silt loam, 2 to 5 percent slopes, moderately eroded	KlB2	19012	331887	30wbj	ms017	1969	1:20000
Kipling silt loam, 0 to 2 percent slopes	KlA	8703	331886	30wbg	ms017	1969	1:20000
Kipling silty clay, 5 to 12 percent slopes, severely eroded	KsD3	6251	331890	c4c4	ms017	1969	1:20000
Demopolis-Kipling complex, 8 to 25 percent slopes, severely eroded	DkE3	4552	331882	c4bw	ms017	1969	1:20000
Kipling silt loam, 5 to 8 percent slopes, eroded	KlC2	3125	331888	c4c2	ms017	1969	1:20000
Kipling silt loam, 2 to 5 percent slopes, moderately eroded	KpB2	18790	332087	30wbj	ms025	1974	1:20000
Kipling silt loam, 5 to 8 percent slopes, moderately eroded	KpC2	10221	332088	2shsx	ms025	1974	1:20000
Kipling silt loam, 0 to 2 percent slopes	KpA	4964	332086	30wbg	ms025	1974	1:20000
Kipling silty clay loam, 8 to 12 percent slopes, eroded	KpD2	1479	332466	c4yq	ms057	1975	1:20000
Kipling silty clay loam, 2 to 5 percent slopes, eroded	KpB2	1262	332464	c4yn	ms057	1975	1:20000
Kipling silty clay loam, 5 to 8 percent slopes, eroded	KpC2	1151	332465	c4yp	ms057	1975	1:20000
Kipling silty clay loam, 2 to 5 percent slopes, moderately eroded	KpB2	4683	332761	2shsz	ms069	1991	1:20000
Kipling silty clay loam, 0 to 2 percent slopes	KpA	4638	332760	2shsy	ms069	1991	1:20000
Kipling silt loam, 5 to 8 percent slopes, moderately eroded	KpC2	2395	2109254	2shsx	ms079	2008	1:24000
Kipling silt loam, 2 to 5 percent slopes	KpB	387	2109253	2shsv	ms079	2008	1:24000
Kipling silt loam, 0 to 2 percent slopes	KpA	492	333012	30wbg	ms081	1968	1:20000
Kipling silty clay loam, 2 to 5 percent slopes, eroded	KpB2	3662	333073	c5l9	ms087	1977	1:20000
Kipling silty clay loam, 0 to 2 percent slopes	KpA	2537	333072	c5l8	ms087	1977	1:20000
Kipling silty clay loam, 5 to 8 percent slopes, eroded	KpC2	1596	333074	c5lb	ms087	1977	1:20000
Kipling silt loam, 0 to 2 percent slopes	VaA	14974	333222	30wbg	ms095	1963	1:15840
Kipling silt loam, 2 to 5 percent slopes, moderately eroded	VaB	14843	333223	30wbj	ms095	1963	1:15840
Kipling silt loam, moderately well drained variant, 0 to 2 percent slopes	KpA	2089	333179	c5pq	ms095	1963	1:15840
Kipling silt loam, moderately well drained variant, 2 to 5 percent slopes	KpB	156	333180	c5pr	ms095	1963	1:15840
Kipling silt loam, 0 to 2 percent slopes	KpA	15938	333417	2shst	ms103	1983	1:20000
Kipling silt loam, 2 to 5 percent slopes, moderately eroded	KpB2	7207	333418	2shsw	ms103	1983	1:20000
Kipling silt loam, 5 to 8 percent slopes, moderately eroded	KpC2	5046	333419	2shsx	ms103	1983	1:20000
Kipling silt loam, 8 to 12 percent slopes, eroded	KpD2	721	333420	c5yh	ms103	1983	1:20000
Kipling silty clay loam, 2 to 5 percent slopes, moderately eroded	KlB2	7316	333486	2shsz	ms105	1968	1:20000
Kipling silty clay loam, 5 to 8 percent slopes, eroded	KlC2	6721	333487	c60n	ms105	1968	1:20000
Kipling silty clay loam, 0 to 2 percent slopes	KlA	6356	333485	2shsy	ms105	1968	1:20000
Kipling and Sumter soils, 17 to 40 percent slopes, severely eroded	KsF3	4929	333488	c60p	ms105	1968	1:20000
Kipling silt loam, 8 to 12 percent slopes, eroded	KiD2	2142	333702	c67l	ms115	1969	1:20000
Kipling soils, 8 to 12 percent slopes, severely eroded	KnD3	1254	333703	c67m	ms115	1969	1:20000
Kipling silt loam, 5 to 8 percent slopes	KiC	971	333701	c67k	ms115	1969	1:20000
Kipling silt loam, 2 to 5 percent slopes	KiB	837	333700	c67j	ms115	1969	1:20000
Kipling silty clay loam, 5 to 8 percent slopes, severely eroded	KrC3	6909	333807	c6bz	ms117	1995	1:24000
Kipling silty clay loam, 8 to 12 percent slopes, severely eroded	KrD3	4209	333808	c6c0	ms117	1995	1:24000
Kipling silt loam, 2 to 5 percent slopes, eroded	KpB2	3329	333806	c6by	ms117	1995	1:24000
Kipling silty clay loam, 12 to 40 percent slopes, severely eroded	KrF3	2318	333809	c6c1	ms117	1995	1:24000
Kipling-Falkner association, undulating	67B	36240	333877	c6f7	ms121	1984	1:20000
Kipling silt loam, 2 to 5 percent slopes	55B	19394	333868	2shsv	ms121	1984	1:20000
Kipling silt loam, 5 to 8 percent slopes, moderately eroded	55C2	8759	333869	2shsx	ms121	1984	1:20000
Kipling-Urban land complex, 2 to 8 percent slopes	36B	5693	333855	c6dj	ms121	1984	1:20000
Kipling silt loam, 0 to 2 percent slopes	55A	954	333867	2shst	ms121	1984	1:20000
Kipling silty clay loam, 2 to 5 percent slopes	KpB	32658	2431379	2mm1l	ms123	2009	1:24000
Kipling silty clay loam, 5 to 8 percent slopes, eroded	KpC2	17815	2431380	2mm1m	ms123	2009	1:24000
Kipling silty clay loam, 8 to 12 percent slopes, eroded	KpD2	5136	2431381	2mm1n	ms123	2009	1:24000

Map of Series Extent

Approximate geographic distribution of the KIPLING 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).