Soil Data Explorer - MILLINGTON

Official Series Description

Lab Data Summary

Aggregate lab data for the MILLINGTON soil series. This aggregation is based on all pedons with a current taxon name of MILLINGTON, 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 MILLINGTON 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
103	UMN2819	S1979MN091017(2819)	Millington	3	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	43.7788734,-94.7432556
103	UMN2820	S1979MN091018(2820)	Millington	2	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	43.6797104,-94.615097
108B	80IL103014	1980IL103014	Millington	1	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	41.8999799,-89.4255521

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the MILLINGTON 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 MILLINGTON 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 MILLINGTON 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 MILLINGTON 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 MILLINGTON 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 MILLINGTON 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 MILLINGTON 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 hills figure.

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 MILLINGTON, 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-2010-09-02-10 | Emmet County - 1997

   Typical pattern of soils and parent material in the Millington-Spillville-Colo association (Soil Survey of Emmet County, Iowa; 1997).

Map Units

Map units containing MILLINGTON 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
Millington loam, 0 to 2 percent slopes, occasionally flooded	458	677	403335	2y6b7	ia021	1973	1:15840
Millington loam, channeled, 0 to 2 percent slopes	1458	1237	403463	fjty	ia025	1979	1:15840
Millington silt loam, channeled, 0 to 2 percent slopes	1458	1536	405513	flz2	ia063	1989	1:15840
Millington loam, 0 to 2 percent slopes	458	348	406231	fmq7	ia073	1983	1:15840
Millington loam, somewhat poorly drained, 0 to 2 percent slopes	458	1313	409120	fqqf	ia119	1973	1:15840
Millington silt loam, 0 to 2 percent slopes, frequently flooded	3082A	1258	1407157	1j785	il007	2006	1:12000
Millington silt loam, 0 to 2 percent slopes, occasionally flooded	8082A	62	1482683	1lrvh	il007	2006	1:12000
Millington silt loam, undrained, 0 to 2 percent slopes, occasionally flooded	1082A	10	1483400	1lslm	il007	2006	1:12000
Millington silt loam, 0 to 2 percent slopes, frequently flooded	3082A	233	796068	vqcm	il015	2005	1:12000
Millington silt loam, undrained, 0 to 2 percent slopes, frequently flooded	1082A	157	796070	vqcp	il015	2005	1:12000
Millington clay loam, 0 to 2 percent slopes, rarely flooded	7082A	118	1542853	1nsgg	il015	2005	1:12000
Millington silt loam, 0 to 2 percent slopes, frequently flooded	3082A	1541	271321	93b9	il089	2000	1:12000
Millington silt loam, 0 to 2 percent slopes, occasionally flooded	8082A	1320	271319	93b7	il089	2000	1:12000
Millington silt loam, 0 to 2 percent slopes, frequently flooded	3082A	182	991323	128k5	il091	2003	1:12000
Millington silt loam, 0 to 2 percent slopes, frequently flooded	3082A	1473	1710637	1vf1v	il093	2007	1:12000
Millington silt loam, 0 to 2 percent slopes, occasionally flooded	8082A	505	1715643	1vl8b	il093	2007	1:12000
Millington silt loam, undrained, 0 to 2 percent slopes, occasionally flooded	1082A	66	778482	v42b	il097	2003	1:12000
Millington silt loam, 0 to 2 percent slopes, occasionally flooded	8082A	9	778485	v42f	il097	2003	1:12000
Millington silt loam, 0 to 2 percent slopes, frequently flooded	3082A	2755	1427835	1jxs6	il099	2006	1:12000
Millington silt loam, undrained, 0 to 2 percent slopes, frequently flooded	1082A	656	923931	100f7	il103	2004	1:12000
Millington silt loam, 0 to 2 percent slopes, occasionally flooded	8082A	2460	182787	646c	il111	1997	1:12000
Millington silt loam, 0 to 2 percent slopes, undrained, occasionally flooded	1082A	1936	182358	63rj	il111	1997	1:12000
Millington silt loam, 0 to 2 percent slopes, frequently flooded	3082A	504	1144338	17ds4	il141	2005	1:12000
Millington silt loam, 0 to 2 percent slopes, frequently flooded	3082A	1477	198693	6nrg	il161	2002	1:12000
Millington silt loam, undrained, 0 to 2 percent slopes, frequently flooded	1082A	542	198687	6nr8	il161	2002	1:12000
Millington silt loam, 0 to 2 percent slopes, occasionally flooded	8082A	152	1595977	1qkr4	il177	2006	1:12000
Millington clay loam, 0 to 2 percent slopes, rarely flooded	7082A	1375	793126	vm9q	il195	2003	1:12000
Millington silt loam, undrained, 0 to 2 percent slopes, frequently flooded	1082A	389	793103	vm8z	il195	2003	1:12000
Millington silt loam, 0 to 2 percent slopes, frequently flooded	3082A	482	616131	np46	il197	2002	1:12000
Millington silt loam, undrained, 0 to 2 percent slopes, frequently flooded	1082A	261	616130	np45	il197	2002	1:12000
Millington silt loam, 0 to 2 percent slopes, occasionally flooded	8082A	192	616132	np47	il197	2002	1:12000
Millington silt loam, 0 to 2 percent slopes, frequently flooded	3082A	2397	174213	5v8s	il201	1997	1:12000
Millington clay loam	269	3139	396275	f9c2	mn015	1984	1:20000
Millington clay loam, sandy substratum	1887	1572	396263	f9bp	mn015	1984	1:20000
Millington clay loam	269	302	397100	fb6p	mn043	1989	1:20000
Millington clay loam, frequently flooded	362	656	398509	fcp4	mn063	1984	1:20000
Millington loam, frequently flooded	362	840	399166	fdcb	mn085	1993	1:20000
Millington clay loam, occasionally flooded	269	206	399160	fdc4	mn085	1993	1:20000
Millington clay loam, occasionally flooded	269	509	400041	ff8k	mn091	1985	1:20000
Millington clay loam	269	2663	400585	ffv3	mn103	1990	1:20000
Millington clay loam, occasionally flooded	269	3460	428936	gdbn	mn165	1987	1:20000
Millington clay loam, frequently flooded	362	617	428946	gdbz	mn165	1987	1:20000
Millington silt loam	Mf	1523	426342	g9mz	wi105	1970	1:20000

Map of Series Extent

Approximate geographic distribution of the MILLINGTON 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).