Soil Data Explorer - NEVIN

Official Series Description

Lab Data Summary

Aggregate lab data for the NEVIN soil series. This aggregation is based on all pedons with a current taxon name of NEVIN, 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 NEVIN 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
115B	M9005352	1990MO053052	Nevin	4	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	38.9672203,-92.3450012
n/a	X49-88-1	S1988IA097900	Nevin	2	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 NEVIN 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 NEVIN 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 NEVIN 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 NEVIN 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 NEVIN 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 NEVIN 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 NEVIN 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 NEVIN, 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. IA-2010-09-09-04 | Adams County - 2008

   Typical pattern of soils and parent material in the Zook-Nodaway association (Soil Survey of Adams County, Iowa; 2008).

2. IA-2010-09-09-18 | Iowa County - 2007

   Typical pattern of soils and parent material in the Colo-Nevin-Nodaway association (Soil Survey of Iowa County, Iowa; 2007).

3. IA-2011-06-01-21 | Montgomery County - 1989

   Typical pattern of soils and parent material in the Nodaway-Colo-Zook association (Soil Survey of Montgomery County, Iowa; 1989).

4. IA-2011-06-01-39 | Ringgold County - 1992

   Typical pattern of soils and parent material in the Nodaway-Humeston-Wabash association (Soil Survey of Ringgold County, Iowa; 1992).

5. IA-2011-06-01-46 | Tama County - 1995

   Typical pattern of soils and parent material in the Colo-Bremer-Nodaway association (Soil Survey of Tama County, Iowa; 1995).

Map Units

Map units containing NEVIN 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
Nevin silty clay loam, 0 to 2 percent slopes, rarely flooded	88	1078	1404887	2xbmm	ia003	2008	1:12000
Nevin silty clay loam, sandy substratum, 0 to 2 percent slopes	1088	3726	402807	fj4s	ia011	1977	1:15840
Nevin silty clay loam, 0 to 2 percent slopes	88	3970	413201	fvz2	ia013	2001	1:12000
Nevin-Urban land complex, 0 to 2 percent slopes	4088	304	449419	h2nd	ia013	2001	1:12000
Nevin silty clay loam, 0 to 2 percent slopes	88	1092	403447	fjtf	ia023	1978	1:15840
Nevin silty clay loam, 0 to 2 percent slopes, rarely flooded	88	2788	1868003	2xbmm	ia029	2010	1:12000
Nevin silty clay loam, 0 to 2 percent slopes, rarely flooded	88	546	1397141	1hwv2	ia031	2008	1:12000
Nevin silty clay loam, 0 to 2 percent slopes	88	2668	404467	fkwb	ia045	1978	1:15840
Nevin silty clay loam, 0 to 2 percent slopes, rarely flooded	88	1209	404633	2xbmm	ia049	1980	1:15840
Nevin silty clay loam, heavy till, 0 to 2 percent slopes, rarely flooded	88	533	404851	2wbdl	ia053	1986	1:15840
Nevin slilt clay loam, 0 to 2 percent slopes	88	52	2479284	2p6wx	ia067	1989	1:15840
Nevin silty clay loam, 0 to 2 percent slopes, rarely flooded	88	2557	406169	2xbmm	ia071	1968	1:20000
Nevin silty clay loam, 0 to 2 percent slopes	88	1941	406325	fmt8	ia075	1973	1:15840
Nevin silty clay loam, 0 to 2 percent slopes, rarely flooded	88	1629	406432	2xbmm	ia077	1968	1:15840
Nevin silty clay loam, 0 to 2 percent slopes	88	277	406910	fnf4	ia087	1982	1:15840
Nevin silty clay loam, heavy till, 0 to 2 percent slopes, rarely flooded	S88	121	3004654	2wbdl	ia087	1982	1:15840
Nevin silty clay loam, 0 to 2 percent slopes, rarely flooded	88	4976	452982	h6cb	ia095	2005	1:12000
Nevin silty clay loam, 0 to 2 percent slopes	88	6046	407700	fp7m	ia099	1975	1:15840
Nevin silty clay loam, 0 to 2 percent slopes	88	1647	408065	fpmd	ia103	1979	1:15840
Nevin silty clay loam	88	795	408689	fq8j	ia113	1970	1:15840
Nevin silty clay loam, 0 to 2 percent slopes, rarely flooded	88	1337	409231	2xbmm	ia121	1968	1:15840
Nevin silty clay loam, 2 to 5 percent slopes, rarely flooded	88B	373	409232	2xbmn	ia121	1968	1:15840
Nevin silty clay loam, 0 to 2 percent slopes	88	568	409384	fqzy	ia123	1971	1:15840
Nevin silty clay loam, 0 to 2 percent slopes	88	1647	412810	fvkg	ia125	1976	1:15840
Nevin silty clay loam, 0 to 2 percent slopes, rarely flooded	Y88	806	3046430	2xbmm	ia125	1976	1:15840
Nevin silty clay loam, heavy till, 0 to 2 percent slopes, rarely flooded	S88	244	3004655	2wbdl	ia125	1976	1:15840
Nevin silty clay loam, 1 to 3 percent slopes	88	1460	409510	fr40	ia127	1978	1:15840
Nevin silty clay loam, 0 to 2 percent slopes, rarely flooded	88	1740	409595	2xbmm	ia129	1979	1:15840
Nevin silty clay loam, 0 to 2 percent slopes, rarely flooded	88	695	409890	2xbmm	ia137	1987	1:15840
Nevin silty clay loam, 0 to 2 percent slopes, rarely flooded	88	2734	410232	2xbmm	ia145	1975	1:20000
Nevin silty clay loam, 0 to 2 percent slopes, rarely flooded	Y88	772	3046432	2xbmm	ia153	1993	1:12000
Nevin silty clay loam, 0 to 2 percent slopes	88	607	412985	fvr3	ia153	1993	1:12000
Nevin silty clay loam, 0 to 2 percent slopes, rarely flooded	88	1196	410516	2xbmm	ia155	1986	1:15840
Nevin silty clay loam, 0 to 2 percent slopes	88	1206	410636	fs9b	ia157	1978	1:15840
Nevin silty clay loam, heavy till, 0 to 2 percent slopes, rarely flooded	S88	226	3004656	2wbdl	ia159	1987	1:15840
Nevin silty clay loam, 0 to 2 percent slopes, rarely flooded	88	220	410746	2xbmm	ia159	1987	1:15840
Nevin silty clay loam, 0 to 2 percent slopes	88	13058	411565	ft89	ia171	1989	1:15840
Nevin silty clay loam, 0 to 2 percent slopes, rarely flooded	88	569	411660	2xbmm	ia173	1989	1:15840
Nevin silty clay loam, heavy till, 0 to 2 percent slopes, rarely flooded	S88	1617	3004657	2wbdl	ia179	1978	1:15840
Nevin silty clay loam, 0 to 2 percent slopes	88	471	411862	ftkw	ia179	1978	1:15840
Nevin silty clay loam, 0 to 2 percent slopes, rarely flooded	88	3057	411975	2xbmm	ia181	1975	1:15840
Nevin silty clay loam, 2 to 5 percent slopes, rarely flooded	88B	467	411976	2xbmn	ia181	1975	1:15840
Nevin silty clay loam, 0 to 2 percent slopes	88	2038	412115	ftv1	ia183	1983	1:15840
Nevin silt loam, 0 to 2 percent slopes, rarely flooded	36028	656	2532146	2qnvv	mo025	1967	1:24000
Nevin silt loam, 1 to 3 percent slopes, rarely flooded	36086	125	2544565	2qs29	mo025	1967	1:24000
Nevin silt loam, 0 to 2 percent slopes, rarely flooded	36028	2685	2532147	2qnvv	mo049	1981	1:24000
Nevin silt loam, 1 to 3 percent slopes, rarely flooded	36086	13	2544566	2qs29	mo049	1981	1:24000
Nevin silt loam, 0 to 2 percent slopes, rarely flooded	36028	4644	2532145	2qnvv	mo075	1982	1:24000
Nevin silt loam, 1 to 3 percent slopes, rarely flooded	36086	66	2544567	2qs29	mo075	1982	1:24000
Nevin silty clay loam, 0 to 2 percent slopes	12504	5944	887662	ysp8	mo147	1983	1:24000
Nevin-Urban land complex, 0 to 2 percent slopes	66047	6870	991523	128rm	mo189	1979	1:24000
Nevin silt loam, 0 to 2 percent slopes	66046	344	991501	128qx	mo189	1979	1:24000
Nevin silty clay loam, 0 to 2 percent slopes, rarely flooded	36027	186	984569	2xbmm	mo227	1965	1:24000

Map of Series Extent

Approximate geographic distribution of the NEVIN 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).