Soil Data Explorer - KINSTON

Official Series Description

Lab Data Summary

Aggregate lab data for the KINSTON soil series. This aggregation is based on all pedons with a current taxon name of KINSTON, 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 KINSTON were used in the calculation. Source: KSSL snapshot (updated 2020-03-18). 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
133A	S66_016	1979-FL131-S66_016	Kinston	3	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	30.6826725,-85.8723602

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the KINSTON 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 KINSTON series. Sketches are arranged according to their subgroup-level taxonomic structure. Source: SSURGO snapshot (updated 2024-02-21), parsed OSD records (updated 2023-10-06) and snapshot of SC database (updated 2023-10-02).

Select annual climate data summaries for the KINSTON 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 KINSTON 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.

Competing Series

Soil series competing with KINSTON share the same family level classification in Soil Taxonomy. Source: parsed OSD records (updated 2023-10-06) and snapshot of the SC database (updated 2023-10-02).

Select annual climate data summaries for the KINSTON 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).

There are insufficient data to create the annual climate figure.

Geomorphic description summaries for the KINSTON 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 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 KINSTON, 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 KINSTON 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
Mantachie, Kinston and Iuka soils, 0 to 1 percent slopes, frequently flooded	MAA	31540	328260	2s69d	al005	2001	1:24000
Mantachie, Kinston and Iuka soils, 0 to 1 percent slopes, frequently flooded	MIA	20625	2232533	2s69d	al007	2007	1:24000
Ochlockonee, Kinston, and Iuka soils, 0 to 1 percent slopes, frequently flooded	OKA	26540	328569	c0x0	al023	1998	1:24000
Mantachie, Kinston and Iuka soils, 0 to 1 percent slopes, frequently flooded	MKA	29350	328874	2s69d	al041	2005	1:24000
Mantachie, Kinston and Iuka soils, 0 to 1 percent slopes, frequently flooded	MKA		2965322	2s69d	al051	1948	1:20000
Mantachie, Kinston and Iuka soils, 0 to 1 percent slopes, frequently flooded	MIA	21825	329771	2s69d	al065	2003	1:24000
Bibb, Osier, and Kinston soils, 0 to 1 percent slopes, frequently flooded	BOA	31335	608102	nds6	al069	2002	1:24000
Mantachie, Iuka, and Kinston soils, 0 to 1 percent slopes, frequently flooded	MIA	4580	640568	phkh	al069	2002	1:24000
Urban land-Bibb-Kinston complex, 0 to 2 percent slopes, frequently flooded	UbA	773	656572	q16r	al069	2002	1:24000
Kinston-Mantachie complex, 0 to 1 percent slopes, frequently flooded	KnA	54462	2494541	2sh4v	al075	2010	1:24000
Kinston silt loam, 0 to 1 percent slopes	21	11395	330203	c2lq	al081	1979	1:20000
Mantachie, Kinston and Iuka soils, 0 to 1 percent slopes, frequently flooded	MKI	7207	2514613	2s69d	al085	2011	1:24000
Kinston-Mooreville complex, 0 to 1 percent slopes, frequently flooded	KmA	46205	330467	c2w7	al087	1997	1:24000
Mooreville, Mantachie and Kinston soils, 0 to 2 percent slopes, frequently flooded	MKA	28830	330588	2svnl	al091	1997	1:24000
Bibb, Johnston and Kinston soils, 0 to 1 percent slopes, frequently flooded	BJK	3250	2994966	2x5rk	al097	2018	1:24000
Mantachie, Kinston and Iuka soils, 0 to 1 percent slopes, frequently flooded	MKA	21571	330954	2s69d	al101	1958	1:20000
Mantachie, Kinston and Iuka soils, 0 to 1 percent slopes, frequently flooded	MIA	29790	331240	2s69d	al105	1996	1:24000
Kinston-Mantachie complex, 0 to 1 percent slopes, frequently flooded	KmA	73260	331287	2sh4v	al107	1997	1:24000
Ochlockonee-Kinston-Iuka complex, 0 to 2 percent slopes, frequently flooded	OcA	5480	331269	c3q3	al107	1997	1:24000
Mantachie, Kinston and Iuka soils, 0 to 1 percent slopes, frequently flooded	MAA	65430	331318	2s69d	al109	1996	1:20000
Kinston, Mantachie, and Iuka soils, 0 to 1 percent slopes, frequently flooded	KMA	40230	331344	c3sj	al113	1997	1:24000
Mooreville, Mantachie and Kinston soils, 0 to 2 percent slopes, frequently flooded	MMK	76641	3121695	2svnl	al119	1986	1:24000
Kinston-Iuka complex, 0 to 1 percent slopes, frequently flooded	KnA	1300	1476420	1lkbg	al123	2005	1:24000
Bibb, Johnston and Kinston soils, 0 to 1 percent slopes, frequently flooded	BJK	74887	2642057	2x5rk	al129	2013	1:24000
Mooreville, Mantachie and Kinston soils, 0 to 2 percent slopes, frequently flooded	MKA	30840	331666	2svnl	al131	1997	1:24000
Croatan, Kinston, and Surrency soils, frequently flooded	68	16031	1481053	1lq4x	fl013	1997	1:20000
Kinston, Johnston, and Bibb soils, frequently flooded	43	44700	1444725	1khc1	fl091	1989	1:20000
Bibb-Kinston association	3	51450	823750	wn5l	fl113	1978	1:24000
Kinston-Johnston-Bibb complex, frequently flooded	15	38970	323984	bw43	fl131	1985	1:20000
Kinston-Bibb association, frequently flooded	43	9510	324014	bw52	fl131	1985	1:20000
Kinston and Bibb soils, 0 to 2 percent slopes, frequently flooded	KFA	63910	324768	2tl1s	ga107	1993	1:20000
Kinston and Bibb soils, 0 to 2 percent slopes, frequently flooded	KBA	23455	334753	2tl1s	ga243	2002	1:24000
Kinston and Bibb soils, 0 to 2 percent slopes, frequently flooded	KBA	15010	2580386	2qdyj	ga251	2011	1:24000
Kinston and Bibb soils, 0 to 2 percent slopes, frequently flooded	KBA	19835	2425367	2tl1s	ga259	2009	1:12000
Kinston and Osier fine sandy loams	KO	14683	324937	bx3v	ga277	1979	1:20000
Kinston and Johnston soils, 0 to 2 percent slopes, frequently flooded	KJA	23115	2408357	2wwt9	ga299	2008	1:24000
Kinston and Osier soils, 0 to 2 percent slopes, frequently flooded	KOA	6435	2408358	2lv2z	ga299	2008	1:24000
Kinston and Bibb soils, 0 to 2 percent slopes, frequently flooded	KBA	18540	2455419	2tl1s	ga307	2009	1:12000
Kinston fine sandy loam, frequently flooded	Ko	9465	325117	bx9n	ga321	1985	1:20000
Kinston and Johnston soils, 0 to 2 percent slopes, frequently flooded	KJ	99290	125174	2wwt9	ga602	1983	1:20000
Kinston-Bibb association, 0 to 2 percent slopes, frequently flooded	KB	113062	325386	2wz35	ga610	1992	1:20000
Kinston and Johnston soils, 0 to 2 percent slopes, frequently flooded	KJA	60245	2686767	2wwt9	ga611	2012	1:24000
Kinston and Osier soils, 0 to 2 percent slopes, frequently flooded	KOA	17570	2686772	2rz8s	ga611	2012	1:24000
Kinston and Johnston soils, 0 to 2 percent slopes, frequently flooded	KJA	49615	2686805	2wwt9	ga626	2013	1:24000
Kinston silt loam, occasionally flooded	Ki	18635	126547	47p5	ga630	1995	1:20000
Kinston and Osier soils	KO	9457	325596	bxt3	ga631	1978	1:20000
Kinston and Bibb soils, 0 to 2 percent slopes, frequently flooded	BK	45985	325758	2tl1s	ga634	1980	1:20000
Kinston and Bibb soils, 0 to 2 percent slopes, frequently flooded	Kb	15635	326002	2tl1s	ga643	1974	1:20000
Kinston and Bibb soils, 0 to 2 percent slopes, frequently flooded	Kib	35025	326260	2tl1s	ga652	1969	1:20000
Kinston and Bibb soils, 0 to 2 percent slopes, frequently flooded	Bk	77515	326338	2tl1s	ga654	1979	1:20000
Kinston and Bibb soils, 0 to 2 percent slopes, frequently flooded	KBA	17220	1605086	2tl1s	ga658	2005	1:24000
Kinston loam, 0 to 2 percent slopes, frequently flooded	11	17655	331763	2tjlq	ms007	1997	1:24000
Mantachie, Bibb, and Iuka soils (kirkville, kinston, iuka)	Mn	31002	332011	c4h1	ms023	1963	1:15840
Bibb, Johnston and Kinston soils, 0 to 1 percent slopes, frequently flooded	BJK	13957	2642164	2x5rk	ms041	2012	1:24000
Mooreville, Mantachie and Kinston soils, 0 to 2 percent slopes, frequently flooded	MMK	26891	3121694	2svnl	ms069	1991	1:20000
Kinston loam, 0 to 2 percent slopes, occasionally flooded	Kn	7967	332759	301jh	ms069	1991	1:20000
Jena-Kirkville-Kinston complex, 0 to 5 percent slopes, frequently flooded	JkB	20244	1603551	2tjlp	ms079	2008	1:24000
Kinston loam, 0 to 2 percent slopes, frequently flooded	Kn	4503	332947	2tjlq	ms079	2008	1:24000
Kinston fine sandy loam	Kn	7109	333011	c5j9	ms081	1968	1:20000
Kinston loam	Kn	2565	333071	c5l7	ms087	1977	1:20000
Kinston loam, frequently flooded	Kn	1274	333805	c6bx	ms117	1995	1:24000
Jena-Kirkville-Kinston complex, 0 to 5 percent slopes, frequently flooded	JkB	8367	2426470	2tjlp	ms123	2009	1:24000
Kinston loam, 0 to 1 percent slopes, frequently flooded	Kn	720	2426471	2mfy8	ms123	2009	1:24000
Kinston, Mantachie, and Mooreville soils, frequently flooded	KM	23592	1401527	1j1dk	ms159	1997	1:24000
Kinston loam, 0 to 2 percent slopes, frequently flooded	Ke	20427	334600	2tjlq	ms159	1997	1:24000
Kinston loam, frequently flooded	KN	4019	112805	3scw	nc079	1978	1:24000
Kinston loam, frequently flooded	Kn	4347	116005	3wq3	nc107	1973	1:20000
Kinston loam	Kn	5243	116244	3wyt	nc191	1968	1:20000
Kinston loam, frequently flooded	Kn	10543	130639	4cy5	sc069	1995	1:24000
Kinston loam, frequently flooded	Kn	648	131347	4dp0	sc696	1988	1:15840
Kinston silt loam and frequently flooded soils	KN	8131	327219	bzhg	tn023	1989	1:24000
Kinston and Mantachie soils	Kn	3967	119251	402t	va087	1973	1:15840
Kinston silt loam	Km	2141	119250	402s	va087	1973	1:15840
Kinston loam	7	11555	119331	405d	va093	1982	1:15840
Kinston and Bibb soils, 0 to 2 percent slopes, occasionally flooded	7A	8804	118657	3zgn	va097	1995	1:24000
Bibb and Kinston soils, 0 to 2 percent slopes, frequently flooded	3A	8805	694772	r9z0	va101	1995	1:15840
Kinston-Bibb complex	11	4356	119630	40h1	va119	1982	1:15840
Kinston complex	14	15434	120312	4161	va149	1980	1:15840
Kinston loam, 0 to 2 percent slopes, frequently flooded	20A	3403	122521	43h9	va181	1997	1:24000

Map of Series Extent

Approximate geographic distribution of the KINSTON 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).