Soil Data Explorer - COLLINGTON

Official Series Description

Lab Data Summary

Aggregate lab data for the COLLINGTON soil series. This aggregation is based on all pedons with a current taxon name of COLLINGTON, 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 COLLINGTON 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
149A	08N0330	07MD033003	Collington	7	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	38.8530278,-76.6978889
149A	92P0476	92NJ005003	Collington	6	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	40.1394463,-74.6272202
149A	92P0484	92NJ015002	Collington	6	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	39.7580566,-75.2483368
149A	92P0486	92NJ025001	Collington	6	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	40.2024994,-74.4986115
149A	92P0490	92NJ033002	Collington	6	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	39.7000008,-75.3655548
149A	92P0492	92NJ033004	Collington	6	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	39.7063904,-75.371109
149A	94P0200	93NJ005004	Collington	6	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	40.0708351,-74.6152802
149A	95P0264	94MD003014	Collington	7	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	39.0369453,-76.6705551
149A	92P0478	S1992NJ005005	Collington	6	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	40.1363907,-74.6444473
n/a	40A0337	61NJ025001	Collington	3	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	n/a
n/a	40A0338	61NJ025002	Collington	3	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	n/a
n/a	40A1178	S1966MD003001	Collington	5	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 COLLINGTON 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 COLLINGTON 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 COLLINGTON 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 COLLINGTON 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 COLLINGTON 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 COLLINGTON 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 COLLINGTON 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 COLLINGTON, 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. MD-2010-09-10-03 | Cecil County -

   Matapeake-Mattapex-Butlertown-Collington association (Soil Survey of Cecil County, Maryland).

2. NJ-2010-09-13-05 | Gloucester County -

   (Soil Survey of Gloucester County, New Jersey)

Map Units

Map units containing COLLINGTON 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
Collington fine sandy loam, 5 to 10 percent slopes	CnD	602	2479810	2thvp	de003	2009	1:24000
Collington fine sandy loam, 2 to 5 percent slopes	CnB	365	2479809	2sql4	de003	2009	1:24000
Collington and Annapolis soils, 10 to 15 percent slopes	CRD	5108	609565	ng9d	md003	2003	1:12000
Collington, Wist, and Westphalia soils, 15 to 25 percent slopes	CSE	4491	609566	ng9f	md003	2003	1:12000
Collington-Wist complex, 5 to 10 percent slopes	CoC	3851	137738	4mb5	md003	2003	1:12000
Collington-Wist complex, 2 to 5 percent slopes	CoB	3693	137737	4mb4	md003	2003	1:12000
Collington, Wist, and Westphalia soils, 25 to 40 percent slopes	CSF	3678	609567	ng9g	md003	2003	1:12000
Collington-Wist-Urban land complex, 0 to 5 percent slopes	CpB	1862	609569	ng9j	md003	2003	1:12000
Collington-Wist-Urban land complex, 5 to 15 percent slopes	CpD	1473	609570	ng9k	md003	2003	1:12000
Collington, Wist, and Westphalia soils, 40 to 80 percent slopes	CSG	530	609568	ng9h	md003	2003	1:12000
Collington-Wist complex, 0 to 2 percent slopes	CoA	209	137706	4m94	md003	2003	1:12000
Collington loam, 5 to 10 percent slopes	CmC	1930	2440691	2mxqz	md015	2009	1:12000
Collington loam, 10 to 15 percent slopes	CmD	1875	2440692	2mxr0	md015	2009	1:12000
Collington loam, 2 to 5 percent slopes	CmB	543	2440690	2thvn	md015	2009	1:12000
Collington-Wist complex, 5 to 10 percent slopes	CoC	336	2440696	2mxr4	md015	2009	1:12000
Collington sandy loam, 5 to 10 percent slopes	CkC	182	2440694	2thvm	md015	2009	1:12000
Collington sandy loam, 2 to 5 percent slopes	CkB	163	2440693	2thtr	md015	2009	1:12000
Collington-Wist complex, 2 to 5 percent slopes	CoB	147	2440695	2mxr3	md015	2009	1:12000
Collington fine sandy loam, 5 to 10 percent slopes	CnD	84	2440640	2thvp	md015	2009	1:12000
Collington fine sandy loam, 2 to 5 percent slopes	CnB	11	2440639	2sql4	md015	2009	1:12000
Collington and Annapolis soils, 10 to 15 percent slopes	CAD	259	1608666	1qzyg	md017	2007	1:12000
Collington and Annapolis soils, 5 to 10 percent slopes	CAC	115	1608671	1qzym	md017	2007	1:12000
Collington-Wist complex, 2 to 5 percent slopes	CnB	5271	2474874	2p29n	md033	2009	1:12000
Collington-Wist-Urban land complex, 0 to 5 percent slopes	CoB	4777	2474879	2p29t	md033	2009	1:12000
Collington-Wist complex, 5 to 10 percent slopes	CnC	4662	2474875	2p29p	md033	2009	1:12000
Collington-Wist-Urban land complex, 5 to 15 percent slopes	CoD	3937	2474880	2p29v	md033	2009	1:12000
Collington-Wist complex, 15 to 25 percent slopes	CnE	3140	2474877	2p29r	md033	2009	1:12000
Collington-Wist complex, 10 to 15 percent slopes	CnD	2331	2474876	2p29q	md033	2009	1:12000
Urban land-Collington-Wist complex, 0 to 5 percent slopes	UrdB	2149	2474882	2p29x	md033	2009	1:12000
Collington-Wist complex, 0 to 2 percent slopes	CnA	2101	2474873	2p29m	md033	2009	1:12000
Croom-Howell-Collington complex, 25 to 40 percent slopes	CsF	980	2474897	2p2bd	md033	2009	1:12000
Collington-Wist complex, 25 to 40 percent slopes	CnF	921	2474878	2p29s	md033	2009	1:12000
Croom-Howell-Collington complex, 15 to 25 percent slopes	CsE	869	2474896	2p2bc	md033	2009	1:12000
Collington-Wist-Urban land complex, 15 to 25 percent slopes	CoE	472	2474881	2p29w	md033	2009	1:12000
Croom-Howell-Collington complex, 10 to 15 percent slopes	CsD	382	2474895	2p2bb	md033	2009	1:12000
Collington fine sandy loam, 2 to 5 percent slopes	ComB	6561	697678	2sql4	nj005	1967	1:24000
Collington fine sandy loam, 0 to 2 percent slopes	ComA	3273	697677	rdzq	nj005	1967	1:24000
Collington fine sandy loam, 5 to 10 percent slopes	ComC	1102	697679	2thvp	nj005	1967	1:24000
Collington loam, 0 to 2 percent slopes	ConA	495	697680	rdzt	nj005	1967	1:24000
Urban land-Collington complex, 0 to 5 percent slopes	USCOLB	408	733661	smfh	nj005	1967	1:24000
Collington loam, 2 to 5 percent slopes	ConB	254	697681	2thvn	nj005	1967	1:24000
Collington sandy loam, 2 to 5 percent slopes	CokB	229	697675	2thtr	nj005	1967	1:24000
Collington sandy loam, 5 to 10 percent slopes, eroded	CokC2	46	697676	rdzp	nj005	1967	1:24000
Collington-Urban land complex, 0 to 10 percent slopes	CopC	2	697682	rdzw	nj005	1967	1:24000
Collington-Urban land complex, 0 to 5 percent slopes	CopB	1332	3347348	2ztxq	nj007	1964	1:12000
Collington fine sandy loam, 0 to 2 percent slopes	ComA	265	710844	rvpg	nj007	1964	1:12000
Freehold and Collington soils, 10 to 15 percent slopes	FRWD	181	710866	rvq5	nj007	1964	1:12000
Collington fine sandy loam, 2 to 5 percent slopes	ComB	175	710845	2sql4	nj007	1964	1:12000
Collington-Urban land complex, 0 to 5 percent slopes	CopB	742	1089407	15km5	nj015	2004	1:24000
Collington sandy loam, 2 to 5 percent slopes	CokB	487	1089405	2thtr	nj015	2004	1:24000
Collington sandy loam, 0 to 2 percent slopes	CokA	188	1089404	15km2	nj015	2004	1:24000
Collington loamy sand, 0 to 5 percent slopes	CogB	187	1089402	15km0	nj015	2004	1:24000
Collington sandy loam, 5 to 10 percent slopes	CokC	147	1089406	2thvm	nj015	2004	1:24000
Collington loamy sand, 5 to 10 percent slopes	CogC	39	1089403	15km1	nj015	2004	1:24000
Collington sandy loam, 2 to 5 percent slopes	CokB	8896	134745	2thtr	nj025	1985	1:24000
Collington sandy loam, 5 to 10 percent slopes, eroded	CokC2	2281	134746	4j6n	nj025	1985	1:24000
Collington loam, 0 to 2 percent slopes	ConA	1653	134748	4j6q	nj025	1985	1:24000
Collington sandy loam, 10 to 15 percent slopes, severely eroded	CokD3	1106	134747	4j6p	nj025	1985	1:24000
Collington-Urban land complex, 0 to 10 percent slopes	CopC	1068	134749	4j6r	nj025	1985	1:24000
Collington fine sandy loam, 0 to 2 percent slopes	ComA	529	697513	rdtf	nj029	1978	1:24000
Collington fine sandy loam, 2 to 5 percent slopes	ComB	306	697514	2sql4	nj029	1978	1:24000
Collington fine sandy loam, 5 to 10 percent slopes	ComC	171	697515	2thvp	nj029	1978	1:24000
Collington sandy loam, 5 to 10 percent slopes	CokC2	51	697611	2thvm	nj029	1978	1:24000
Collington sandy loam, 2 to 5 percent slopes	CokB	41	697610	2thtr	nj029	1978	1:24000
Collington loam, 0 to 2 percent slopes	ConA	13	697600	rdx7	nj029	1978	1:24000

Map of Series Extent

Approximate geographic distribution of the COLLINGTON 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).