Soil Data Explorer - INVILLE

Official Series Description

Lab Data Summary

Aggregate lab data for the INVILLE soil series. This aggregation is based on all pedons with a current taxon name of INVILLE, 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 INVILLE 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
22A	68C0092	S1968CA017017	Inville	6	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	38.896389,-119.9205551

Water Balance

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

Competing Series

Soil series competing with INVILLE 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 INVILLE 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 INVILLE 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 INVILLE, 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 INVILLE 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
Almanor-Whorled-Inville, lacustrine complex, 3 to 15 percent slopes	2000	9112	3172032	2y0fs	ca608	2000	1:24000
Inville very gravelly sandy loam, 0 to 5 percent slopes	257	3892	487556	jcbm	ca608	2000	1:24000
Almanor-Whorled-Inville complex, 0 to 15 percent slopes	101	3576	487319	jc2z	ca608	2000	1:24000
Inville gravelly medial sandy loam, 0 to 8 percent slopes	2004	1269	3172037	2z40g	ca608	2000	1:24000
Inville-Pit complex, 0 to 3 percent slopes	2017	692	3225044	2z40v	ca608	2000	1:24000
Inville gravelly coarse sandy loam, 2 to 9 percent slopes, stony	7141	1479	1652076	1sg3s	ca693	2006	1:24000
Inville gravelly coarse sandy loam, 9 to 15 percent slopes, stony	7142	619	1652077	1sg3t	ca693	2006	1:24000
Inville gravelly coarse sandy loam, 15 to 30 percent slopes, stony	7143	429	1652083	1sg40	ca693	2006	1:24000
Inville-Wintoner families complex, 2 to 15 percent slopes.	146	22735	470367	hsg4	ca702	1984	1:24000
Inville family, 15 to 50 percent slopes.	145	9522	470366	hsg3	ca702	1984	1:24000
Inville-Wintoner families association, 30 to 50 percent slopes.	147	8323	470368	hsg5	ca702	1984	1:24000
Yallani-Inville families complex, 8 to 20 inch pumice overburden, 5 to 30 percent slopes.	278mf	131	1906214	21zks	ca702	1984	1:24000
Inville-Yallani families complex, 10 to 20 inch pumice overburden, 2 to 20 percent slopes.	186	4920	470501	hslg	ca703	1983	1:24000
Yallani-Inville families complex, 8 to 20 inch pumice overburden, 5 to 30 percent slopes.	278	3900	470591	hspc	ca703	1983	1:24000
Inville-Jayar families association, 20 to 50 percent slopes.	146	2953	470744	hsv9	ca707	1983	1:24000
Inville-Jayar, deep, families complex, 15 to 40 percent slopes.	147	1784	470745	hsvb	ca707	1983	1:24000
Inville family-Sheld family, moderately deep-Rubble Land association, 15 to 50 percent slopes.	35	81964	471008	ht3t	ca708	1984	1:24000
Trojan-Inville-Patio families association, 0 to 35 percent slopes.	105	72231	471078	ht62	ca708	1984	1:24000
Inville-Wintoner families complex, 0 to 35 percent slopes.	36	39399	471009	ht3v	ca708	1984	1:24000
Inville-Patio-Trojan families association, 0 to 35 percent slopes.	33	19927	471006	ht3r	ca708	1984	1:24000
Trojan-Inville-Boomtowm families association, 0 to 35 percent slopes.	104	17762	471077	ht61	ca708	1984	1:24000
Sheld-Inville families-Sheld family, moderately deep complex, 0 to 35 percent slopes.	81	10931	471054	ht59	ca708	1984	1:24000
Inville-Yallani families complex, 0 to 35 percent slopes.	38	9306	471011	ht3x	ca708	1984	1:24000
Inville-Patio families association, 15 to35 percent slopes.	32	7775	471005	ht3q	ca708	1984	1:24000
Klicker family, sedimentary-Lithic Ultic Argixerolls-Inville family association, 0 to 50 percent slopes.	47	7761	471020	ht46	ca708	1984	1:24000
Inville-Klicker-Wintoner families association, 0 to 35 percent slopes.	30	5987	471003	ht3n	ca708	1984	1:24000
Almanor-Whorled-Inville, lacustrine complex, 3 to 15 percent slopes	2000	5375	3110147	2y0fs	ca708	1984	1:24000
Inville-Yallani families, cobbly complex, 15 to 50 percent slopes	40	4260	471013	ht3z	ca708	1984	1:24000
Inville-Klicker-Wintoner families association, 35 to 50 percent slopes.	31	4207	471004	ht3p	ca708	1984	1:24000
Inville-Yallani families, rhyolitic association, 0 to 35 percent slopes.	41	4086	471014	ht40	ca708	1984	1:24000
Inville-Wintoner families complex, 35 to 50 percent slopes.	37	4008	471010	ht3w	ca708	1984	1:24000
Inville-Patio-Trojan families association, 35 to 50 percent slopes.	34	3334	471007	ht3s	ca708	1984	1:24000
Inville-Yallani families, rhyolitic association,35 to 50 percent slopes.	42	3013	471015	ht41	ca708	1984	1:24000
Inville-Yallani families complex, 35 to 50 percent slopes.	39	1603	471012	ht3y	ca708	1984	1:24000
Inville gravelly medial sandy loam, 0 to 8 percent slopes	2004	791	3172038	2z40g	ca708	1984	1:24000
Inville-Pit complex, 0 to 3 percent slopes	2017	575	3225030	2z40v	ca708	1984	1:24000
Inville very gravelly sandy loam, 0 to 5 percent slopes	257su	395	1528339	1n9c8	ca708	1984	1:24000
Inville-Woodseye families complex, 10 to 50 percent slopes.	216p	163	1528780	1n9th	ca708	1984	1:24000
Almanor-Whorled-Inville complex, 0 to 15 percent slopes	101su	9	1528306	1n9b6	ca708	1984	1:24000
Ultic Haploxeralfs-Inville family complex, 10 to 50 percent slopes.	281	31417	471290	htdx	ca713	1984	1:24000
Inville-Woodseye families complex, 10 to 50 percent slopes.	216	22001	471225	htbt	ca713	1984	1:24000
Inville-Woodseye-Goodlow families complex, 10 to 25 percent slopes.	217	3727	471226	htbv	ca713	1984	1:24000
Haploxeralfs- Inville family complex, 50 to 70 percent slopes.	282	2807	471291	htdy	ca713	1984	1:24000
Tallac-Inville-Goodlow families complex, 15 to 65 percent slopes.	269	2311	471278	htdj	ca713	1984	1:24000
Inville very gravelly sandy loam, 0 to 5 percent slopes	257su	62	1546058	1nwsv	ca713	1984	1:24000
Inville-Wintoner families complex, 35 to 50 percent slopes.	L37	52	1546123	1nwvy	ca713	1984	1:24000
Klicker family, sedimentary-Lithic Ultic Argixerolls-Inville family association, 0 to 50 percent slopes.	L47	51	1546213	1nwyv	ca713	1984	1:24000
Almanor-Whorled-Inville, lacustrine complex, 3 to 15 percent slopes	2000	48	3295636	2y0fs	ca713	1984	1:24000
Inville-Riverwash-Aquolls complex, 2 to 5 percent slopes	EWB	2385	464646	hlhl	ca719	1982	1:24000
Inville-Martis variant complex, 2 to 5 percent slopes	EVB	1266	464645	hlhk	ca719	1982	1:24000
Inville-Woodseye families complex, 10 to 50 percent slopes.	216pf	5	1586548	1q7xz	ca719	1982	1:24000
Lithic Cryumbrepts-Inville family, moderately deep-Rock complex, 10 to 50 percent slopes	164	19395	465039	hlx8	ca731	1981	1:24000
Inville family, moderately deep-Deep complex, 15 to 35 percent slopes	148	9517	465024	hlws	ca731	1981	1:24000
Inville family, deep-Moderately deep complex, 15 to 35 percent slopes	147	4299	465023	hlwr	ca731	1981	1:24000
Inville family, moderately deep-Lithic Cryumbrepts comp lex, 20 to 50 percent slopes	150	2810	465026	hlwv	ca731	1981	1:24000
Wintoner-Inville families complex, 15 to 40 percent slo pes	198	1406	465072	hlyb	ca731	1981	1:24000
Inville family, moderately deep-Deep complex, 35 to 60 percent slopes	149	1296	465025	hlwt	ca731	1981	1:24000
Inville variant gravelly sandy loam, 2 to 8 percent slopes	1080	698	474126	hxcd	nv628	1980	1:24000

Map of Series Extent

Approximate geographic distribution of the INVILLE 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).