Soil Data Explorer - EVERLY

Official Series Description

Lab Data Summary

Aggregate lab data for the EVERLY soil series. This aggregation is based on all pedons with a current taxon name of EVERLY, 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 EVERLY 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
102A	UMN2324	S1976MN1272324	Everly	2	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	44.1976128,-95.4281693
107A	84P0396	83IA041201	Everly	5	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	43.1324997,-95.3494415
107A	84P0397	83IA041202	Everly	5	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	43.1297226,-95.3497238
107A	84P0398	83IA041203	Everly	5	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	43.1297226,-95.3502808
107A	85P0382	84IA0410041	Everly	5	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	43.2408333,-95.309166
107A	85P0383	84IA0410042	Everly	5	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	43.2405548,-95.309166
107A	85P0384	84IA0410043	Everly	5	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	43.2408333,-95.3094406
107A	40A1402	S1959IA041007	EVERLY	6	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	43.1263885,-95.2455521
107A	40A1403	S1959IA041008	EVERLY	6	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	43.2180557,-95.1686096
107A	UMN2726	S1978MN133003 (2726)	Everly	3	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	43.7442017,-96.1224518
107A	UMN3199	S1979MN1013199	Everly	3	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	43.8547211,-96.0047455

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the EVERLY 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 EVERLY 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 EVERLY 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 EVERLY 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 EVERLY 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 EVERLY 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 EVERLY 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 terrace figure.

Soil series sharing subgroup-level classification with EVERLY, 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-2011-06-01-28 | Osceola County - 1988

   Typical pattern of soils and parent material in the Everly-Wilmonton-Letri association (Soil Survey of Osceola County, Iowa; 1988).

Map Units

Map units containing EVERLY 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
Everly clay loam, 5 to 9 percent slopes, moderately eroded	577C2	670	403315	fjp5	ia021	1973	1:15840
Everly clay loam, 2 to 5 percent slopes	577B	561	403313	fjp3	ia021	1973	1:15840
Everly clay loam, 5 to 9 percent slopes	577C	187	403314	fjp4	ia021	1973	1:15840
Everly clay loam, 9 to 14 percent slopes, moderately eroded	577D2	1123	403946	fkbj	ia035	1987	1:15840
Everly clay loam, 5 to 9 percent slopes, moderately eroded	577C2	951	403945	fkbh	ia035	1987	1:15840
Everly clay loam, 2 to 5 percent slopes, moderately eroded	577B2	547	403943	fkbf	ia035	1987	1:15840
Everly clay loam, 5 to 9 percent slopes	577C	283	403944	fkbg	ia035	1987	1:15840
Everly clay loam, 2 to 5 percent slopes	577B	17366	399387	fdlg	ia041	2002	1:12000
Everly clay loam, 5 to 9 percent slopes, moderately eroded	577C2	2914	399389	fdlj	ia041	2002	1:12000
Everly-Moneta complex, 9 to 14 percent slopes, moderately eroded	637D2	1514	399403	fdlz	ia041	2002	1:12000
Everly clay loam, 2 to 5 percent slopes	577B	4235	1869070	20qxl	ia059	2011	1:12000
Everly clay loam, 5 to 9 percent slopes, moderately eroded	577C2	376	1869071	20qxm	ia059	2011	1:12000
Everly clay loam, 2 to 5 percent slopes	577B	1621	409127	fqqn	ia119	1973	1:15840
Everly clay loam, 9 to 14 percent slopes	577D	349	410085	frqk	ia141	1977	1:15840
Everly clay loam, 5 to 9 percent slopes, moderately eroded	577C2	232	410084	frqj	ia141	1977	1:15840
Everly clay loam, 2 to 5 percent slopes	577B	17218	410157	frsw	ia143	1985	1:15840
Everly clay loam, 0 to 2 percent slopes	577	5588	410156	frsv	ia143	1985	1:15840
Everly clay loam, 2 to 5 percent slopes, moderately eroded	577B2	1170	410158	frsx	ia143	1985	1:15840
Everly clay loam, 5 to 9 percent slopes, moderately eroded	577C2	995	410160	frsz	ia143	1985	1:15840
Everly clay loam, 5 to 9 percent slopes	577C	375	410159	frsy	ia143	1985	1:15840
Everly clay loam, 9 to 14 percent slopes, moderately eroded	577D2	296	410161	frt0	ia143	1985	1:15840
Everly clay loam, 4 to 9 percent slopes, moderately eroded	577C2	706	410817	fsh5	ia161	1975	1:15840
Everly clay loam, 9 to 14 percent slopes, moderately eroded	577D2	316	410818	fsh6	ia161	1975	1:15840
Everly clay loam, 3 to 6 percent slopes, eroded	149B2	45	1859023	20dgh	mn083	2008	1:12000
Everly clay loam, 6 to 12 percent slopes, eroded	149C2	11	1859024	20dgj	mn083	2008	1:12000
Everly clay loam, 2 to 4 percent slopes	149B	4	1859022	20dgg	mn083	2008	1:12000
Storden-Everly complex, 12 to 18 percent slopes, eroded	894D2	3	1859050	20dhc	mn083	2008	1:12000
Everly silty clay loam, 2 to 6 percent slopes	P12B	7930	725696	sc4k	mn101	2008	1:12000
Everly-Moneta complex, 6 to 12 percent slopes, moderately eroded	P53C2	417	725683	sc44	mn101	2008	1:12000
Moneta-Everly complex, 12 to 18 percent slopes, moderately eroded	P54D2	212	725682	sc43	mn101	2008	1:12000
Moneta-Everly-Talmo complex, 12 to 18 percent slopes, moderately eroded	P52D2	63	725684	sc45	mn101	2008	1:12000
Everly-Moneta-Talmo complex, 6 to 12 percent slopes, moderately eroded	P51C2	1	1946880	23bwl	mn101	2008	1:12000
Everly silty clay loam, 6 to 12 percent slopes, moderately eroded	P12C2	1	1532648	1nfv8	mn101	2008	1:12000
Everly silty clay loam, 2 to 6 percent slopes	P12B	31865	630072	p4mx	mn105	2004	1:12000
Everly silty clay loam, 6 to 12 percent slopes, moderately eroded	P12C2	2231	630071	p4mw	mn105	2004	1:12000
Everly-Moneta-Talmo complex, 6 to 12 percent slopes, moderately eroded	P51C2	630	630069	p4mt	mn105	2004	1:12000
Everly-Moneta complex, 6 to 12 percent slopes, moderately eroded	P53C2	329	630070	p4mv	mn105	2004	1:12000
Everly-Kanaranzi complex, 2 to 6 percent slopes	P50B	242	630073	p4my	mn105	2004	1:12000
Moneta-Everly complex, 12 to 18 percent slopes, moderately eroded	P54D2	223	630062	p4ml	mn105	2004	1:12000
Moneta-Everly-Talmo complex, 12 to 18 percent slopes, moderately eroded	P52D2	144	630061	p4mk	mn105	2004	1:12000
Everly silty clay loam, 2 to 6 percent slopes	P12B	504	725531	sbz7	mn117	2005	1:12000
Everly silty clay loam, 6 to 12 percent slopes, moderately eroded	P12C2	83	725530	sbz6	mn117	2005	1:12000
Everly silty clay loam, 2 to 6 percent slopes	P12B	3911	432687	gj7n	mn133	2002	1:12000
Everly silty clay loam, 6 to 12 percent slopes, eroded	P12C2	622	432688	gj7p	mn133	2002	1:12000

Map of Series Extent

Approximate geographic distribution of the EVERLY 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).