Soil Data Explorer - KENDALLVILLE

Official Series Description

Lab Data Summary

Aggregate lab data for the KENDALLVILLE soil series. This aggregation is based on all pedons with a current taxon name of KENDALLVILLE, 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 KENDALLVILLE were used in the calculation. Source: KSSL snapshot (updated 2020-03-18). Methods used to assemble the KSSL snapshot used by SoilWeb / SDE

There are insufficient data to create the lab data summary figure.

Pedons used in the lab summary:

MLRA	Lab ID	Pedon ID	Taxonname	CI	NSSL / NASIS Reports	Link To SoilWeb GMap
n/a	DL-003	1955-OH041-003	Kendallville	2	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	n/a
n/a	PB-028	1959-OH135-028	Kendallville	2	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	n/a
n/a	PB-031	1959-OH135-031	Kendallville	2	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	n/a
n/a	RO-079	1959-OH141-079	Kendallville	2	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	n/a
n/a	CH-041	1960-OH021-041	Kendallville	2	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	n/a
n/a	WA-044	1961-OH165-044	Kendallville	3	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	n/a
n/a	BR-011	1971-OH017-011	Kendallville	4	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	n/a
n/a	PY-024	1971-OH129-024	Kendallville	3	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	n/a
n/a	PY-026	1972-OH129-026	Kendallville	3	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	n/a
n/a	FR-051	1974-OH049-051	Kendallville	3	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	n/a

Water Balance

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

Soil series sharing subgroup-level classification with KENDALLVILLE, 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

No block diagrams are available.

Map Units

Map units containing KENDALLVILLE 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
Miami-Kendallville loams, 12 to 18 percent slopes, eroded	XrkD2	89	639201	pg4d	in005	2002	1:12000
Miami-Kendallville loams, 12 to 18 percent slopes, eroded	XrkD2	11	1651396	1sfdv	in013	1985	1:15840
Ockley, till substratum-Kendallville clay loams, 6 to 12 percent slopes, severely eroded	OhC3	697	165215	5jxj	in015	1987	1:15840
Kendallville silt loam, 12 to 18 percent slopes, eroded	KnqD2	371	242399	847b	in045	1999	1:12000
Miami-Kendallville loams, 12 to 18 percent slopes, eroded	XrkD2	166	1652791	1sgvv	in081	1975	1:15840
Kendallville loam, 2 to 6 percent slopes, moderately eroded	KeB2	515	187996	69md	mi067	1965	1:15840
Kendallville sandy loam, 6 to 12 percent slopes, moderately eroded	KhC2	416	188001	69mk	mi067	1965	1:15840
Kendallville sandy loam, 2 to 6 percent slopes, moderately eroded	KhB2	255	188000	69mj	mi067	1965	1:15840
Kendallville sandy loam, 2 to 6 percent slopes	KhB	241	187999	69mh	mi067	1965	1:15840
Kendallville loam, 2 to 6 percent slopes	KeB	220	187995	69mc	mi067	1965	1:15840
Kendallville loam, 6 to 12 percent slopes, moderately eroded	KeC2	186	187997	69mf	mi067	1965	1:15840
Kendallville loam, 0 to 2 percent slopes	KeA	141	187994	69mb	mi067	1965	1:15840
Kendallville sandy loam, 12 to 18 percent slopes, moderately eroded	KhD2	96	188002	69ml	mi067	1965	1:15840
Kendallville sandy clay loam, 6 to 12 percent slopes, severely eroded	KgC3	79	187998	69mg	mi067	1965	1:15840
Kendallville sandy loam, 7 to 15 percent slopes	KbC	402	188500	6b4n	mi091	1957	1:20000
Kendallville loam, 7 to 15 percent slopes, moderately eroded	KaC2	398	188499	6b4m	mi091	1957	1:20000
Kendallville loam, 7 to 15 percent slopes	KaC	311	188498	6b4l	mi091	1957	1:20000
Kendallville soils, 7 to 15 percent slopes, moderately or severely eroded	KcC2	71	188501	6b4p	mi091	1957	1:20000
Kendallville sandy loam, 2 to 6 percent slopes	KhB	3193	187806	69f8	mi155	1967	1:12000
Kendallville sandy loam, 6 to 12 percent slopes, moderately eroded	KhC2	715	187809	69fc	mi155	1967	1:12000
Kendallville sandy loam, 6 to 12 percent slopes	KhC	708	187808	69fb	mi155	1967	1:12000
Kendallville sandy loam, 2 to 6 percent slopes, moderately eroded	KhB2	345	187807	69f9	mi155	1967	1:12000
Kendallville loam, 2 to 6 percent slopes	KeB	3237	191634	6fdr	mi161	1974	1:20000
Kendallville loam, 6 to 12 percent slopes	KeC	747	191635	6fds	mi161	1974	1:20000
Kendallville-Eldean silt loams, 12 to 18 percent slopes, eroded	KeD2	7	1589969	1qchb	oh017	1977	1:15840
Kendallville-Eldean silt loams, 6 to 12 percent slopes, eroded	KeC2	5	1589968	1qch9	oh017	1977	1:15840
Kendallville silt loam, 2 to 6 percent slopes	KeB	1276	171452	2w0vr	oh021	1966	1:15840
Kendallville silt loam, 6 to 12 percent slopes, moderately eroded	KeC2	411	171453	5rdr	oh021	1966	1:15840
Kendallville silt loam, 0 to 2 percent slopes	KeA	87	171451	5rdp	oh021	1966	1:15840
Kendallville silt loam, 12 to 18 percent slopes, moderately eroded	KeD2	70	171454	5rds	oh021	1966	1:15840
Miami-Kendallville silt loams, 18 to 25 percent slopes, eroded	MfE2	16	1392127	1hqmb	oh037	1984	1:15840
Kendallville-Eldean silt loams, 12 to 18 percent slopes, eroded	KeD2	6	1392123	1hqm6	oh037	1984	1:15840
Kendallville silt loam, 2 to 6 percent slopes, moderately eroded	KeB2	562	169242	5p3f	oh047	1968	1:15840
Kendallville silt loam, 2 to 6 percent slopes	KeB	431	169241	2w0vr	oh047	1968	1:15840
Kendallville clay loam, 12 to 18 percent slopes, severely eroded	KlD3	286	169245	5p3j	oh047	1968	1:15840
Kendallville silt loam, 6 to 12 percent slopes, moderately eroded	KeC2	267	169243	5p3g	oh047	1968	1:15840
Kendallville clay loam, 6 to 12 percent slopes, severely eroded	KlC3	267	169244	5p3h	oh047	1968	1:15840
Miamian-Kendallville silt loams, 6 to 12 percent slopes, eroded	MnC2	15	1907597	2210d	oh047	1968	1:15840
Kendallville silt loam, 2 to 6 percent slopes	KeB	2965	167907	2w0vr	oh049	1977	1:15840
Kendallville silt loam, 0 to 2 percent slopes	KeA	363	167906	5mqb	oh049	1977	1:15840
Kendallville silt loam, 6 to 12 percent slopes, eroded	KeC2	357	167908	5mqd	oh049	1977	1:15840
Kendallville silt loam, 2 to 6 percent slopes	KaB	1108	168940	5nsp	oh065	1987	1:15840
Kendallville-Urban land complex, 2 to 6 percent slopes	KuB	4	3216907	2zkfr	oh065	1987	1:15840
Kendallville silt loam, 2 to 6 percent slopes	KeB	781	1420447	2w0vr	oh071	1973	1:15840
Kendallville silt loam, 6 to 12 percent slopes, moderately eroded	KeC2	647	1420448	1jp2x	oh071	1973	1:15840
Kendallville silt loam, 12 to 18 percent slopes, moderately eroded	KeD2	194	1420449	1jp2y	oh071	1973	1:15840
Kendallville clay loam, 12 to 18 percent slopes, severely eroded	KfD3	154	1420450	1jp2z	oh071	1973	1:15840
Kendallville silt loam, 2 to 6 percent slopes	KeB	1	1593187	1qgv4	oh091	1977	1:15840
Kendallville silt loam, 2 to 6 percent slopes	KeB	948	169897	2w0vr	oh097	1978	1:15840
Kendallville silt loam, 6 to 12 percent slopes, eroded	KeC2	188	169898	5psl	oh097	1978	1:15840
Miamian-Kendallville silt loams, 2 to 6 percent slopes	MrB	2	1402813	1j2r1	oh097	1978	1:15840
Miamian-Kendallville silt loams, 6 to 12 percent slopes, eroded	MrC2	1	1402814	1j2r2	oh097	1978	1:15840
Kendallville loam, 2 to 6 percent slopes	KeB	1702	171199	5r4k	oh101	1984	1:15840
Kendallville loam, 12 to 18 percent slopes, eroded	KeD2	200	171200	5r4l	oh101	1984	1:15840
Kendallville silt loam, 2 to 6 percent slopes	KeB	180	170263	2w0vr	oh113	1969	1:15840
Kendallville silt loam, 0 to 2 percent slopes	KeA	142	170262	5q5b	oh113	1969	1:15840
Kendallville silt loam, 6 to 12 percent slopes, moderately eroded	KeC2	96	170264	5q5d	oh113	1969	1:15840
Miamian-Kendallville silt loams, 25 to 50 percent slopes, eroded	MgF2	11	1590114	1qcn0	oh113	1969	1:15840
Kendallville-Eldean silt loams, 12 to 18 percent slopes, eroded	KfD2	2	1590111	1qcmx	oh113	1969	1:15840
Miamian-Kendallville silt loams, 2 to 6 percent slopes	MkB	12589	171280	5r75	oh129	1977	1:15840
Eldean-Kendallville loams, 2 to 6 percent slopes	EpB	2720	171261	5r6k	oh129	1977	1:15840
Miamian-Kendallville silt loams, 6 to 12 percent slopes, eroded	MkC2	2325	171281	5r76	oh129	1977	1:15840
Eldean-Kendallville loams, 6 to 12 percent slopes, eroded	EpC2	1505	171262	5r6l	oh129	1977	1:15840
Miamian-Kendallville silt loams, 0 to 2 percent slopes	MkA	1117	171279	5r74	oh129	1977	1:15840
Eldean-Kendallville loams, 0 to 2 percent slopes	EpA	621	171260	5r6j	oh129	1977	1:15840
Casco-Kendallville complex, 12 to 18 percent slopes	ChD	603	171242	5r5y	oh129	1977	1:15840
Miamian-Kendallville silt loams, 12 to 18 percent slopes, eroded	MkD2	387	171282	5r77	oh129	1977	1:15840
Casco-Kendallville complex, 18 to 35 percent slopes	ChE	230	171243	5r5z	oh129	1977	1:15840
Kendallville silt loam, 2 to 6 percent slopes	KeB	88	1402980	2w0vr	oh129	1977	1:15840
Kendallville-Eldean complex, 20 to 35 percent slopes, eroded	KeE2	13	1403053	1j2zs	oh129	1977	1:15840
Kendallville-Eldean complex, 12 to 20 percent slopes, eroded	KeD2	4	1403052	1j2zr	oh129	1977	1:15840
Kendallville silt loam, 6 to 12 percent slopes, eroded	KaC2	3	1403162	1j339	oh129	1977	1:15840
Kendallville-Eldean complex, 6 to 12 percent slopes, eroded	KeC2	0	1403051	1j2zq	oh129	1977	1:15840
Kendallville-Eldean silt loams, 6 to 12 percent slopes, eroded	KeC2	1574	622386	nwmz	oh135	2005	1:12000
Miamian-Kendallville silt loams, 25 to 50 percent slopes, eroded	MgF2	1138	623347	nxmz	oh135	2005	1:12000
Kendallville-Eldean silt loams, 12 to 18 percent slopes, eroded	KeD2	736	622555	nwtf	oh135	2005	1:12000
Miamian-Kendallville silt loams, 18 to 25 percent slopes, eroded	MgE2	446	623346	nxmy	oh135	2005	1:12000
Rodman-Kendallville complex, 25 to 50 percent slopes, eroded	RoF2	365	624785	nz4c	oh135	2005	1:12000
Miami-Kendallville silt loams, 18 to 25 percent slopes, eroded	McE2	279	623837	ny4s	oh135	2005	1:12000
Rodman-Kendallville complex, 18 to 25 percent slopes, eroded	RoE2	198	624779	nz45	oh135	2005	1:12000
Miami-Kendallville silt loams, 25 to 50 percent slopes, eroded	McF2	113	623838	ny4t	oh135	2005	1:12000
Kendallville-Eldean complex, 6 to 12 percent slopes, eroded	KeC2	4139	170890	5qtl	oh141	1997	1:15840
Kendallville silt loam, 2 to 6 percent slopes	KeB	3317	170889	2w0vr	oh141	1997	1:15840
Kendallville-Eldean complex, 12 to 20 percent slopes, eroded	KeD2	3131	170891	5qtm	oh141	1997	1:15840
Kendallville-Eldean complex, 20 to 35 percent slopes, eroded	KeE2	2232	170892	5qtn	oh141	1997	1:15840
Kendallville silt loam, 0 to 2 percent slopes	KaA	395	170888	5qtj	oh141	1997	1:15840
Kendallville silt loam, 2 to 6 percent slopes	KeB	283	1406077	1j64b	oh159	1970	1:15840
Kendallville silt loam, 0 to 2 percent slopes	KeA	100	1406076	1j649	oh159	1970	1:15840
Kendallville loam, 6 to 12 percent slopes, moderately eroded	KeC2	221	171366	5r9y	oh165	1967	1:20000
Kendallville loam, 2 to 6 percent slopes	KeB	105	171365	5r9x	oh165	1967	1:20000
Kendallville-Urban land complex, 2 to 6 percent slopes	KeUB	47	3422279	31gjf	oh165	1967	1:20000
Kendallville-Urban land complex, 6 to 12 percent slopes, moderately eroded	KeUC2	23	3422280	31gjg	oh165	1967	1:20000
Kendallville loam, 2 to 6 percent slopes	KeB	5	1542647	1ns7t	oh175	1980	1:15840

Map of Series Extent

Approximate geographic distribution of the KENDALLVILLE 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).