Soil Data Explorer - ELCO

Official Series Description

Lab Data Summary

Aggregate lab data for the ELCO soil series. This aggregation is based on all pedons with a current taxon name of ELCO, 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 ELCO 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
108B	77IL073018	1977IL073018	Elco	1	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	41.3177427,-90.1252136
108B	12N7651	2011IL167276	Elco	4	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	39.6016472,-89.5737556
108B	12N7652	2011IL167277	Elco	4	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	39.7185528,-89.6069861
108B	12N7653	2011IL167282	Elco	4	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	39.7804361,-89.7772944
114B	78IL119070	1978IL119070	Elco	1	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	38.8484104,-89.8589654
114B	79IL119081	1979IL119081	Elco	1	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	38.9318009,-89.8938722
115C	78IL095041	1978IL095041	Elco	1	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	41.0541369,-90.0813451
115C	93P0119	S1992IL057011	Elco	7	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	40.6850243,-90.3701096

Water Balance

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

Select annual climate data summaries for the ELCO 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 ELCO 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 ELCO share the same family level classification in Soil Taxonomy. Source: parsed OSD records (updated 2023-10-02) and snapshot of the SC database (updated 2023-10-02).

Select annual climate data summaries for the ELCO 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).

Geomorphic description summaries for the ELCO 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 3D mountains figure.

Soil series sharing subgroup-level classification with ELCO, 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

Click a link below to display the diagram. Note that these diagrams may be from multiple survey areas.

1. IL-2010-09-01-18 | Fulton County - 2003

   Typical pattern of soils and parent material in the Rozetta-Keomah-Clarksdale association (Soil Survey of Fulton County, Illinois; 2003).

2. IL-2010-09-01-26 | Hancock County - 2001

   Typical pattern of soils and parent material in the Fishhook-Elco-Atlas association (Soil Survey of Hancock County, Illinois; 2001).

3. IL-2010-09-01-54 | McDonough County - 1997

   Typical pattern of soils and parent material in the Hickory-Rozetta-Elco association (Soil Survey of McDonough County, Illinois; 1997).

4. IL-2010-09-01-75 | Stark County - 1996

   Typical pattern of soils and parent material in the Rozetta-Hickory association (Soil Survey of Stark County, Illinois; 1996).

5. IL-2010-09-24-07 | Christian County -

   Typical pattern of soils and underlying material in the Rozetta-Hickory-Keomah association (Soil Survey of Christian County, Illinois).

6. IL-2011-06-01-06 | Brown County - 1988

   Typical cross section showing the relationship of parent material to soils in Brown County (Soil Survey of Brown County, Illinois; 1988).

7. IL-2011-08-03-15 | Christian County - 1994

   Typical pattern of soils and parent material in the Rozetta-Hickory-Keomah association (Soil Survey of Christian County, Illinois; 1994).

8. IL-2011-08-04-42 | Knox County - 1986

   Typical pattern of soils and parent material in the Rozetta-Clarkdale-Elco association (Soil Survey of Knox County, Illinois; 1986).

9. IL-2011-08-04-43 | Knox County - 1986

   Typical pattern of soils and parent material in the Hickory-Marseilles association (Soil Survey of Knox County, Illinois; 1986).

10. IL-2011-08-04-81 | Peoria County - 1992

    Typical pattern of soils and parent material in the Rozetta-Keomah-Sylvan and Hickory-Strawn-Marseilles associations (Soil Survey of Peoria County, Illinois; 1992).

Map Units

Map units containing ELCO 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
Elco silt loam, 2 to 5 percent slopes	119B	160	1395229	30t7v	il007	2006	1:12000
Elco silt loam, 10 to 18 percent slopes, eroded	119D2	2178	2604154	30t7y	il009	1984	1:12000
Elco silty clay loam, 10 to 18 percent slopes, severely eroded	119D3	1133	172942	310t4	il009	1984	1:12000
Elco silt loam, 10 to 18 percent slopes	119D	720	172941	30t7x	il009	1984	1:12000
Elco silt loam, 5 to 10 percent slopes, eroded	119C2	7022	261673	310t2	il021	1999	1:12000
Elco silt loam, 10 to 18 percent slopes, eroded	119D2	214	261740	30t7y	il021	1999	1:12000
Elco silty clay loam, 10 to 15 percent slopes, severely eroded	119D3	850	174634	5vqc	il027	1992	1:15840
Elco silt loam, 5 to 10 percent slopes, eroded	119C2	3853	195699	6kmw	il033	2004	1:12000
Elco silt loam, 10 to 18 percent slopes	119D	1211	195700	6kmx	il033	2004	1:12000
Elco silt loam, 10 to 18 percent slopes, eroded	119D2	6314	615637	30t7y	il057	1997	1:12000
Elco silt loam, 18 to 25 percent slopes, eroded	119E2	4047	615638	30t80	il057	1997	1:12000
Elco silt loam, 10 to 18 percent slopes, eroded	119D2	60	211735	30t7y	il061	1968	1:15840
Elco silt loam, 5 to 10 percent slopes, eroded	119C2	59	211733	310t2	il061	1968	1:15840
Elco silty clay loam, 10 to 18 percent slopes, severely eroded	119D3	7	2542229	310t4	il061	1968	1:15840
Elco silty clay loam, 5 to 10 percent slopes, severely eroded	119C3	6	2542227	30t7w	il061	1968	1:15840
Elco-Ursa complex, 10 to 18 percent slopes, eroded	915D2	9592	175239	5wbw	il067	1993	1:15840
Elco silt loam, 5 to 10 percent slopes, eroded	119C2	3671	175155	310t2	il067	1993	1:15840
Elco-Atlas silty clay loams, 10 to 18 percent slopes, severely eroded	957D3	12	2604128	2r78d	il067	1993	1:15840
Elco-Atlas silty clay loams, 10 to 18 percent slopes, severely eroded	957D3	2461	1412396	1jdq5	il071	2005	1:12000
Elco-Atlas silt loams, 10 to 18 percent slopes, eroded	957D2	2130	1480526	1lplx	il071	2005	1:12000
Rozetta-Elco silt loams, 10 to 18 percent slopes, eroded	724D2	452	1412404	1jdqf	il071	2005	1:12000
Elco silt loam, 18 to 25 percent slopes, eroded	119E2	56	1480504	30t80	il071	2005	1:12000
Elco silt loam, 10 to 18 percent slopes, eroded	119D2	2669	244653	30t7y	il073	2001	1:12000
Elco-Atlas silty clay loams, 10 to 18 percent slopes, severely eroded	957D3	2621	244782	86q6	il073	2001	1:12000
Elco silty clay loam, 10 to 18 percent slopes, severely eroded	119D3	1406	244654	310t4	il073	2001	1:12000
Elco silty clay loam, 10 to 18 percent slopes, severely eroded	119D3	9977	728447	310t4	il083	2002	1:12000
Elco silt loam, 5 to 10 percent slopes, eroded	119C2	3274	729239	310t2	il083	2002	1:12000
Elco silt loam, 10 to 18 percent slopes, eroded	119D2	3226	728446	30t7y	il083	2002	1:12000
Elco silty clay loam, 5 to 10 percent slopes, severely eroded	119C3	1873	728454	30t7w	il083	2002	1:12000
Elco silt loam, 5 to 10 percent slopes, eroded	119C2	2176	1949538	310t2	il085	1990	1:12000
Elco silt loam, 10 to 18 percent slopes, eroded	119D2	9271	680934	30t7y	il095	2002	1:12000
Elco silt loam, 18 to 25 percent slopes, eroded	119E2	4655	680935	30t80	il095	2002	1:12000
Elco silt loam, 10 to 18 percent slopes, eroded	119D2	4430	634119	30t7y	il109	2002	1:12000
Elco silt loam, 5 to 10 percent slopes, eroded	119C2	3595	634248	310t2	il109	2002	1:12000
Elco silt loam, 18 to 25 percent slopes, eroded	119E2	977	634257	30t80	il109	2002	1:12000
Elco silt loam, 5 to 10 percent slopes, eroded	119C2	168	1913930	310t2	il115	2007	1:12000
Elco silt loam, 5 to 10 percent slopes, eroded	119C2	6631	199177	310t2	il117	1999	1:12000
Elco silt loam, 10 to 18 percent slopes, eroded	119D2	1567	199246	30t7y	il117	1999	1:12000
Elco silt loam, 2 to 5 percent slopes, eroded	119B2	1325	199176	310t1	il117	1999	1:12000
Elco silty clay loam, 10 to 18 percent slopes, severely eroded	119D3	8	641229	310t4	il117	1999	1:12000
Elco silty clay loam, 5 to 10 percent slopes, severely eroded	119C3	2	641135	30t7w	il117	1999	1:12000
Elco silty clay loam, 5 to 10 percent slopes, severely eroded	119C3	5352	198955	30t7w	il119	2001	1:12000
Elco silty clay loam, 10 to 18 percent slopes, severely eroded	119D3	4130	198954	310t4	il119	2001	1:12000
Elco silt loam, 10 to 18 percent slopes, eroded	119D2	2324	198956	6p0y	il119	2001	1:12000
Elco silty clay loam, 10 to 18 percent slopes, severely eroded	119D3	1	1407469	310t4	il129	2005	1:12000
Elco silt loam, 10 to 18 percent slopes, eroded	119D2	1	1407468	30t7y	il129	2005	1:12000
Elco-Atlas silty clay loams, 10 to 18 percent slopes, severely eroded	957D3	6602	245017	86ys	il131	2000	1:12000
Elco silt loam, 10 to 18 percent slopes	119D	2032	244958	30t7x	il131	2000	1:12000
Elco silt loam, 10 to 18 percent slopes, eroded	119D2	32	244959	30t7y	il131	2000	1:12000
Elco silt loam, 10 to 18 percent slopes, eroded	119D2	5819	1672111	30t7y	il137	1984	1:15840
Elco silt loam, 18 to 25 percent slopes, eroded	119E2	2107	1672113	30t80	il137	1984	1:15840
Elco silty clay loam, 10 to 18 percent slopes, severely eroded	119D3	868	1672112	310t4	il137	1984	1:15840
Elco-Ursa silt loams, 18 to 25 percent slopes, eroded	915E2	745	1672185	1t41g	il137	1984	1:15840
Elco-Ursa silt loams, 10 to 18 percent slopes, eroded	915D2	408	1672184	1t41f	il137	1984	1:15840
Elco silt loam, 5 to 10 percent slopes, eroded	119C2	717	208544	310t2	il141	2005	1:12000
Elco silt loam, 10 to 18 percent slopes, eroded	119D2	4287	208951	30t7y	il143	1986	1:15840
Elco silt loam, 18 to 25 percent slopes	119E	1732	208952	30t7z	il143	1986	1:15840
Elco silt loam, 10 to 18 percent slopes, eroded	119D2	2480	201127	30t7y	il149	2001	1:12000
Elco silt loam, 18 to 25 percent slopes, eroded	119E2	1446	201129	30t80	il149	2001	1:12000
Elco silty clay loam, 10 to 18 percent slopes, severely eroded	119D3	513	201128	310t4	il149	2001	1:12000
Elco silt loam, 10 to 18 percent slopes, eroded	119D2	5675	199296	30t7y	il167	1999	1:12000
Elco silty clay loam, 10 to 18 percent slopes, severely eroded	119D3	4822	199297	310t4	il167	1999	1:12000
Elco silt loam, 10 to 18 percent slopes	119D	2372	199363	30t7x	il167	1999	1:12000
Elco silt loam, 5 to 10 percent slopes, eroded	119C2	1066	199362	310t2	il167	1999	1:12000
Elco silt loam, 10 to 18 percent slopes, eroded	119D2	2185	2542065	30t7y	il171	1984	1:12000
Elco silt loam, 18 to 25 percent slopes, eroded	119E2	2061	2542067	30t80	il171	1984	1:12000
Elco silty clay loam, 10 to 18 percent slopes, severely eroded	119D3	835	2542066	310t4	il171	1984	1:12000
Elco-Ursa silt loams, 10 to 18 percent slopes, eroded	915D2	153	2542079	2qrch	il171	1984	1:12000
Elco-Ursa silt loams, 18 to 25 percent slopes, eroded	915E2	114	2542080	2qrcj	il171	1984	1:12000
Elco silt loam, 10 to 18 percent slopes, eroded	119D2	942	179051	30t7y	il175	1992	1:15840
Elco silty clay loam, 10 to 18 percent slopes, severely eroded	119D3	596	179052	310t4	il175	1992	1:15840
Elco silt loam, 18 to 25 percent slopes, eroded	119E2	407	179053	30t80	il175	1992	1:15840
Elco silt loam, 5 to 10 percent slopes, eroded	119C2	274	179050	310t2	il175	1992	1:15840
Elco silt loam, 5 to 10 percent slopes, eroded	119C2	1286	1592074	310t2	il177	2006	1:12000
Elco silt loam, 10 to 18 percent slopes, eroded	119D2	4138	244875	30t7y	il187	2002	1:12000
Elco-Atlas silty clay loams, 10 to 18 percent slopes, severely eroded	957D3	3529	244928	86vx	il187	2002	1:12000
Elco silt loam, 18 to 25 percent slopes, eroded	119E2	2752	244876	30t80	il187	2002	1:12000
Elco-Atlas silt loams, 10 to 18 percent slopes, eroded	957D2	1610	244927	86vw	il187	2002	1:12000
Elco silt loam, 2 to 5 percent slopes	119B	239	173952	30t7v	il201	1997	1:12000

Map of Series Extent

Approximate geographic distribution of the ELCO 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).