Soil Data Explorer - SENACHWINE

Official Series Description

Lab Data Summary

Aggregate lab data for the SENACHWINE soil series. This aggregation is based on all pedons with a current taxon name of SENACHWINE, 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 SENACHWINE 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
108A	83P0552	1982IL011187	Senachwine	6	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	41.27375,-89.57175
108A	84IL147012	1984IL147012	Senachwine	2	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	39.9806861,-88.6935556
108A	90P1083	1990IL045001	Senachwine	7	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	39.5499992,-87.6833344
110	52IL075001	1952IL075001	Senachwine	5	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	40.8065072,-87.6124157

Water Balance

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

Soil series sharing subgroup-level classification with SENACHWINE, 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. IL-2010-09-01-04 | Edgar County - 2002

   Typical pattern of soils and parent material in the Senachwine-Russell association (Soil Survey of Edgar County, Illinois; 2002).

2. IL-2010-09-01-43 | Marshall County - 2002

   Typical pattern of soils and parent material in the Hennepin-Birkbeck-Senachwine association (Soil Survey of Marshall County, Illinois; 2002).

3. IL-2010-09-01-63 | Moultrie County - 2004

   Typical association of soils along major drainageways in the county (Soil Survey of Moultrie County, Illinois; 2004).

Map Units

Map units containing SENACHWINE 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
Senachwine silt loam, 2 to 5 percent slopes	618B	52	1482677	2ww95	il007	2006	1:12000
Senachwine silt loam, 18 to 35 percent slopes	618F	4309	1862767	2ww99	il011	2007	1:12000
Senachwine silt loam, 10 to 18 percent slopes, eroded	618D2	2164	1862766	2ww98	il011	2007	1:12000
Senachwine silt loam, 5 to 10 percent slopes, eroded	618C2	1343	1862765	2ww97	il011	2007	1:12000
Senachwine silt loam, 15 to 25 percent slopes	618E	31	1867636	2ww9c	il011	2007	1:12000
Senachwine silt loam, 5 to 10 percent slopes, eroded	618C2	850	242984	2ww97	il019	1999	1:12000
Senachwine silt loam, 10 to 18 percent slopes, eroded	618D2	632	242986	2ww98	il019	1999	1:12000
Senachwine silt loam, 18 to 25 percent slopes, eroded	618E2	510	243026	2ww9d	il019	1999	1:12000
Senachwine silt loam, 18 to 35 percent slopes	618F	398	242991	2ww99	il019	1999	1:12000
Senachwine silt loam, 2 to 5 percent slopes	618B	270	243018	2ww95	il019	1999	1:12000
Senachwine silt loam, 35 to 60 percent slopes	618G	402	261744	2ww9b	il021	1999	1:12000
Senachwine silt loam, 5 to 10 percent slopes, eroded	618C2	850	1595995	2ww97	il023	2006	1:12000
Senachwine clay loam, 10 to 18 percent slopes, severely eroded	618D3	524	1596002	1qkry	il023	2006	1:12000
Senachwine silt loam, 10 to 18 percent slopes, eroded	618D2	518	1595999	2ww98	il023	2006	1:12000
Senachwine clay loam, 5 to 10 percent slopes, severely eroded	618C3	263	1595997	1qkrs	il023	2006	1:12000
Senachwine silt loam, 5 to 10 percent slopes, eroded	618C2	13222	1547460	2ww97	il029	2005	1:12000
Senachwine silt loam, 35 to 60 percent slopes	618G	10222	1547462	2ww9b	il029	2005	1:12000
Senachwine silt loam, 18 to 35 percent slopes	618F	5912	1547456	2ww99	il029	2005	1:12000
Senachwine silt loam, 10 to 18 percent slopes, eroded	618D2	2558	1547458	2ww98	il029	2005	1:12000
Senachwine clay loam, 5 to 10 percent slopes, severely eroded	618C3	703	1547459	1ny81	il029	2005	1:12000
Senachwine clay loam, 10 to 18 percent slopes, severely eroded	618D3	526	1547457	1ny7z	il029	2005	1:12000
Senachwine silt loam, 2 to 5 percent slopes, eroded	618B2	1244	174805	2ww96	il035	1992	1:15840
Senachwine silt loam, 5 to 10 percent slopes, eroded	618C2	520	174806	2ww97	il035	1992	1:15840
Senachwine silt loam, 35 to 60 percent slopes	618G	395	174810	2ww9b	il035	1992	1:15840
Senachwine silt loam, 18 to 35 percent slopes	618F	190	174809	2ww99	il035	1992	1:15840
Senachwine silt loam, 10 to 18 percent slopes, eroded	618D2	144	174808	2ww98	il035	1992	1:15840
Senachwine silt loam, 18 to 35 percent slopes	618F	5371	1585652	2ww99	il039	2005	1:12000
Senachwine silt loam, 35 to 60 percent slopes	618G	2717	1602674	2ww9b	il039	2005	1:12000
Senachwine silt loam, 5 to 10 percent slopes, eroded	618C2	1616	166416	2ww97	il041	2004	1:12000
Senachwine silt loam, 10 to 18 percent slopes, eroded	618D2	1196	262933	2ww98	il041	2004	1:12000
Senachwine silt loam, 18 to 35 percent slopes	618F	766	200200	2ww99	il041	2004	1:12000
Senachwine silt loam, 5 to 10 percent slopes, eroded	618C2	11245	843573	2ww97	il045	1997	1:12000
Senachwine silt loam, 35 to 60 percent slopes	618G	6085	843578	2ww9b	il045	1997	1:12000
Senachwine silt loam, 18 to 35 percent slopes	618F	4785	843577	2ww99	il045	1997	1:12000
Senachwine silt loam, 10 to 18 percent slopes, eroded	618D2	3505	843575	2ww98	il045	1997	1:12000
Senachwine clay loam, 5 to 10 percent slopes, severely eroded	618C3	1680	843574	x9t2	il045	1997	1:12000
Senachwine clay loam, 10 to 18 percent slopes, severely eroded	618D3	900	843576	x9t4	il045	1997	1:12000
Senachwine silt loam, 5 to 10 percent slopes, eroded	618C2	705	244805	2ww97	il073	2001	1:12000
Senachwine silt loam, 10 to 18 percent slopes, eroded	618D2	481	244806	2ww98	il073	2001	1:12000
Senachwine silt loam, 2 to 5 percent slopes	618B	918	175569	2ww95	il075	1980	1:15840
Senachwine silt loam, 10 to 18 percent slopes	618D2	898	1949628	23fr7	il085	1990	1:12000
Senachwine silt loam, 12 to 20 percent slopes	618E	3845	271564	93l4	il089	2000	1:12000
Senachwine silt loam, 20 to 30 percent slopes	618F	518	271561	93l1	il089	2000	1:12000
Senachwine silt loam, 5 to 10 percent slopes, eroded	618C2	2061	921461	2ww97	il103	2004	1:12000
Senachwine clay loam, 10 to 18 percent slopes, severely eroded	618D3	733	921509	zxx3	il103	2004	1:12000
Senachwine fine sandy loam, 2 to 5 percent slopes, eroded	757B2	598	942136	10mch	il103	2004	1:12000
Senachwine silt loam, 18 to 35 percent slopes	618F	470	921536	2ww99	il103	2004	1:12000
Senachwine fine sandy loam, 5 to 10 percent slopes, eroded	757C2	464	942137	10mcj	il103	2004	1:12000
Senachwine silt loam, 2 to 5 percent slopes	618B	263	921460	2ww95	il103	2004	1:12000
Senachwine-Russell silt loams, 10 to 18 percent slopes, eroded	736D2	1865	1596079	1qkvf	il107	2006	1:12000
Birkbeck-Senachwine complex, 5 to 10 percent slopes, severely eroded	733C3	810	1596081	1qkvh	il107	2006	1:12000
Senachwine silt loam, 18 to 35 percent slopes	618F	772	1600630	2ww99	il107	2006	1:12000
Birkbeck-Senachwine silt loams, 5 to 10 percent slopes, eroded	733C2	428	1596080	1qkvg	il107	2006	1:12000
Senachwine silt loam, 12 to 20 percent slopes	618E	511	182753	6458	il111	1997	1:12000
Senachwine silt loam, 20 to 30 percent slopes	618F	281	182754	6459	il111	1997	1:12000
Senachwine-Hennepin loams, 35 to 60 percent slopes	883G	127	2648894	2rlv8	il113	2000	1:12000
Senachwine-Hennepin loams, 18 to 35 percent slopes	883F	118	2648893	2rlv7	il113	2000	1:12000
Senachwine silt loam, 18 to 35 percent slopes	618F	3871	1913961	2ww99	il115	2007	1:12000
Senachwine silt loam, 5 to 10 percent slopes, eroded	618C2	3765	1913958	2ww97	il115	2007	1:12000
Senachwine silt loam, 10 to 18 percent slopes, eroded	618D2	2723	1913959	2ww98	il115	2007	1:12000
Senachwine clay loam, 10 to 18 percent slopes, severely eroded	618D3	1128	1913960	227mn	il115	2007	1:12000
Senachwine silt loam, 35 to 60 percent slopes	618G	466	1913962	2ww9b	il115	2007	1:12000
Senachwine silt loam, 15 to 25 percent slopes	618E	2971	182144	2ww9c	il123	1997	1:15840
Senachwine silt loam, 10 to 18 percent slopes, eroded	618D2	2071	182142	2ww98	il123	1997	1:15840
Senachwine-Hennepin loams, 18 to 35 percent slopes	883F	1996	182259	63nb	il123	1997	1:15840
Senachwine-Hennepin loams, 35 to 60 percent slopes	883G	17	2650870	2rmmn	il123	1997	1:15840
Senachwine silt loam, 18 to 35 percent slopes	618F	3923	246529	2ww99	il139	1999	1:12000
Senachwine silt loam, 5 to 10 percent slopes, eroded	618C2	3436	246524	2ww97	il139	1999	1:12000
Senachwine silt loam, 10 to 18 percent slopes, eroded	618D2	3429	246527	2ww98	il139	1999	1:12000
Senachwine silt loam, 35 to 60 percent slopes	618G	1379	246530	2ww9b	il139	1999	1:12000
Senachwine clay loam, 10 to 18 percent slopes, severely eroded	618D3	482	246528	88jj	il139	1999	1:12000
Senachwine silt loam, 2 to 5 percent slopes, eroded	618B2	286	246523	2ww96	il139	1999	1:12000
Senachwine clay loam, 5 to 10 percent slopes, severely eroded	618C3	261	246525	88jf	il139	1999	1:12000
Senachwine silt loam, 5 to 10 percent slopes, eroded	618C2	6214	1478550	2ww97	il141	2005	1:12000
Senachwine silt loam, 10 to 18 percent slopes, eroded	618D2	2780	1478604	2ww98	il141	2005	1:12000
Senachwine silt loam, 2 to 5 percent slopes	618B	894	1478549	2ww95	il141	2005	1:12000
Senachwine-Hennepin loams, 18 to 35 percent slopes	883F	63	2604039	2qj6r	il143	1986	1:15840
Senachwine-Hennepin loams, 35 to 60 percent slopes	883G	15	2604040	2qj6s	il143	1986	1:15840
Senachwine silt loam, 10 to 18 percent slopes, eroded	618D2	1173	1910855	2ww98	il147	2009	1:12000
Senachwine silt loam, 5 to 10 percent slopes, eroded	618C2	964	1722804	2ww97	il147	2009	1:12000
Senachwine silt loam, 18 to 35 percent slopes	618F	583	1910854	2ww99	il147	2009	1:12000
Senachwine silt loam, 35 to 60 percent slopes	618G	403	1722807	2ww9b	il147	2009	1:12000
Senachwine silt loam, 18 to 35 percent slopes	618F	1731	172748	2ww99	il155	1987	1:15840
Senachwine silt loam, 5 to 10 percent slopes, eroded	618C2	1023	172740	2ww97	il155	1987	1:15840
Senachwine silt loam, 10 to 18 percent slopes, eroded	618D2	1003	172743	2ww98	il155	1987	1:15840
Senachwine-Hennepin loams, 18 to 35 percent slopes	883F	88	2650839	2r21k	il155	1987	1:15840
Senachwine silt loam, 18 to 35 percent slopes	618F	4915	179014	2ww99	il173	1990	1:15840
Senachwine silt loam, 5 to 10 percent slopes, eroded	618C2	4702	179012	2ww97	il173	1990	1:15840
Senachwine silt loam, 35 to 60 percent slopes	618G	3857	179015	2ww9b	il173	1990	1:15840
Senachwine silt loam, 10 to 18 percent slopes, eroded	618D2	3079	179013	2ww98	il173	1990	1:15840
Senachwine silt loam, 2 to 5 percent slopes, eroded	618B2	1425	179011	2ww96	il173	1990	1:15840
Senachwine silt loam, 18 to 35 percent slopes	618F	343	179087	2ww99	il175	1992	1:15840
Senachwine clay loam, 10 to 18 percent slopes, severely eroded	618D3	313	179086	60bz	il175	1992	1:15840
Senachwine silt loam, 5 to 10 percent slopes, eroded	618C2	2205	1591943	2ww97	il177	2006	1:12000
Senachwine clay loam, 5 to 10 percent slopes, severely eroded	618C3	214	1591944	1qfk1	il177	2006	1:12000
Senachwine silt loam, 10 to 18 percent slopes, eroded	618D2	194	1591948	2ww98	il177	2006	1:12000
Senachwine-Hennepin loams, 35 to 60 percent slopes	883G	12847	179434	60q6	il179	1991	1:15840
Senachwine-Hennepin loams, 18 to 35 percent slopes	883F	7283	179433	60q5	il179	1991	1:15840
Senachwine silt loam, 10 to 18 percent slopes, eroded	618D2	3489	179390	2ww98	il179	1991	1:15840
Senachwine silt loam, 18 to 35 percent slopes	618F	5	2507901	2ww99	il179	1991	1:15840
Senachwine silt loam, 5 to 10 percent slopes, eroded	618C2	1561	1686348	2ww97	il183	2006	1:12000
Senachwine silt loam, 18 to 35 percent slopes	618F	1054	1651409	2ww99	il183	2006	1:12000
Senachwine clay loam, 5 to 10 percent slopes, severely eroded	618C3	755	1651407	1sff6	il183	2006	1:12000
Senachwine silt loam, 10 to 18 percent slopes, eroded	618D2	588	1613342	2ww98	il183	2006	1:12000
Senachwine silt loam, 18 to 25 percent slopes, eroded	618E2	272	1613343	2ww9d	il183	2006	1:12000
Senachwine silt loam, 5 to 10 percent slopes, eroded	618C2	835	174141	2ww97	il201	1997	1:12000
Senachwine silt loam, 2 to 5 percent slopes	618B	615	174140	2ww95	il201	1997	1:12000
Senachwine-Hennepin loams, 35 to 60 percent slopes	883G	12199	1913534	2275x	il203	2008	1:12000
Senachwine-Hennepin loams, 18 to 35 percent slopes	883F	7526	869259	y5jm	il203	2008	1:12000
Senachwine silt loam, 10 to 18 percent slopes, eroded	618D2	3707	2215575	2ww98	il203	2008	1:12000
Senachwine silt loam, 5 to 10 percent slopes, eroded	618C2	1725	2215574	2ww97	il203	2008	1:12000
Senachwine loam, 25 to 70 percent slopes	SifG	1169	207316	6yqm	in005	2002	1:12000
Senachwine loam, 18 to 25 percent slopes	SifE	610	207317	6yqn	in005	2002	1:12000
Senachwine silt loam, 18 to 25 percent slopes, eroded	SigE2	241	696002	rc7p	in011	2003	1:12000
Senachwine loam, 25 to 70 percent slopes	SifG	54	1651384	1sfdg	in013	1985	1:15840
Senachwine loam, 25 to 70 percent slopes	SifG	23	723259	s8ly	in079	2010	1:12000
Senachwine loam, 18 to 25 percent slopes	SifE	15	723258	s8lx	in079	2010	1:12000
Senachwine loam, 25 to 70 percent slopes	SifG	68	1652778	1sgvf	in081	1975	1:15840
Senachwine silt loam, 10 to 18 percent slopes, eroded	MeD2	1040	160444	2ww98	in165	1977	1:20000

Map of Series Extent

Approximate geographic distribution of the SENACHWINE 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).