Soil Data Explorer - COLLAMER

Official Series Description

Lab Data Summary

Aggregate lab data for the COLLAMER soil series. This aggregation is based on all pedons with a current taxon name of COLLAMER, 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 COLLAMER 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
140	02N0752	S01NY003010	Collamer	6	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	42.4452744,-78.1069183
n/a	88P0713	88NY109001	Collamer	6	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	n/a
n/a	40A1187	S1976NY045003	COLLAMER	6	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 COLLAMER 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 COLLAMER series. Sketches are arranged according to their subgroup-level taxonomic structure. Source: SSURGO snapshot (updated 2024-02-21), parsed OSD records (updated 2023-10-06) and snapshot of SC database (updated 2023-10-02).

Select annual climate data summaries for the COLLAMER 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 COLLAMER 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 COLLAMER share the same family level classification in Soil Taxonomy. Source: parsed OSD records (updated 2023-10-06) and snapshot of the SC database (updated 2023-10-02).

Select annual climate data summaries for the COLLAMER 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).

There are insufficient data to create the annual climate figure.

Geomorphic description summaries for the COLLAMER 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 2D hillslope position figure.

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.

There are insufficient data to create the 3D flats position figure.

Soil series sharing subgroup-level classification with COLLAMER, 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. NY-2012-02-15-05 | Cayuga County - 1971

   Typical cross section of Ontario association in the north-central part of the county (Soil Survey of Cayuga County, New York; 1971).

2. NY-2012-02-15-07 | Chautauqua County - August 1994

   Soils and parent material on a bedrock escarpment and on a lake plain that includes the Beach Ridge (Soil Survey of Chautauqua County, New York; August 1994).

3. NY-2012-02-15-17 | Genesee County - March 1969

   Cross section showing typical soil patterns in the Ontario-Hilton association, the Collamer-Galen-Canandaigua-Lamson association, and the Muck association in northern Genesee County (Soil Survey of Genesee County, New York; March 1969).

4. NY-2012-02-16-08 | Wyoming County - April 1974

   Typical pattern of soils in association 18 (Soil Survey of Wyoming County, New York; April 1974).

Map Units

Map units containing COLLAMER 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
Collamer silt loam, 8 to 15 percent slopes	31C	498	299858	b20v	ny003	2013	1:24000
Collamer silt loam, 15 to 25 percent slopes	31D	386	318643	bpkt	ny003	2013	1:24000
Collamer silt loam, 3 to 8 percent slopes	31B	330	849300	xhrs	ny003	2013	1:24000
Collamer silt loam, 0 to 3 percent slopes	31A	64	822859	wm7v	ny003	2013	1:24000
Collamer silt loam, 8 to 15 percent slopes	31C	1327	289582	9qbc	ny009	2002	1:24000
Collamer silt loam, 3 to 8 percent slopes	31B	679	289581	9qbb	ny009	2002	1:24000
Collamer silt loam, 2 to 6 percent slopes	ClB	3219	289382	9q3x	ny011	1968	1:15840
Collamer silt loam, 0 to 2 percent slopes	ClA	2204	289381	9q3w	ny011	1968	1:15840
Collamer silt loam, 3 to 8 percent slopes	CsB	614	289811	9qkr	ny013	1988	1:15840
Collamer silt loam, 8 to 15 percent slopes	CsC	376	289812	9qks	ny013	1988	1:15840
Collamer silt loam, 0 to 3 percent slopes	CoA	357	289915	9qp3	ny015	1969	1:20000
Collamer silt loam, 3 to 8 percent slopes	CoB	314	289916	9qp4	ny015	1969	1:20000
Collamer silt loam, 3 to 8 percent slopes	CoB	2322	290323	9r38	ny021	1985	1:15840
Collamer silt loam, 8 to 15 percent slopes	CoC	770	290324	9r39	ny021	1985	1:15840
Collamer silt loam, 0 to 3 percent slopes	CoA	653	290322	9r37	ny021	1985	1:15840
Collamer silt loam, 8 to 15 percent slopes	CoC	332	290473	9r83	ny025	1999	1:24000
Collamer silt loam, 3 to 8 percent slopes	CoB	157	290472	9r82	ny025	1999	1:24000
Collamer silt loam, 3 to 8 percent slopes	CsB	2693	290783	9rl3	ny029	1979	1:15840
Collamer silt loam, till substratum, 3 to 8 percent slo pes	CtB	2259	290785	9rl5	ny029	1979	1:15840
Urban land-Collamer complex, 1 to 6 percent slopes	UmA	2218	290914	9rqb	ny029	1979	1:15840
Collamer silt loam, 8 to 15 percent slopes	CsC	961	290784	9rl4	ny029	1979	1:15840
Collamer silt loam, 0 to 3 percent slopes	CsA	511	290782	9rl2	ny029	1979	1:15840
Collamer silt loam, 2 to 8 percent slopes	CrB	791	316458	bm9b	ny031	2007	1:24000
Collamer silt loam, 2 to 6 percent slopes	ClB	4557	301688	b3xw	ny037	2004	1:24000
Collamer silt loam, 3 to 8 percent slopes	CnB	20124	291800	9smx	ny045	1981	1:15840
Collamer silt loam, 8 to 15 percent slopes	CnC	4246	291801	9smy	ny045	1981	1:15840
Collamer silt loam, bedrock substratum, 3 to 8 percent slopes	CoB	3560	291803	9sn0	ny045	1981	1:15840
Collamer silt loam, 8 to 15 percent slopes, severely eroded	CnC3	419	291802	9smz	ny045	1981	1:15840
Collamer silt loam, 8 to 15 percent slopes	31C	2046	3105667	2y9vy	ny051	2019	1:24000
Hudson and Collamer soils, 8 to 15 percent slopes	132C	1155	3105730	2y9x2	ny051	2019	1:24000
Hudson and Collamer soils, 15 to 25 percent slopes	132D	914	3105731	2y9x3	ny051	2019	1:24000
Collamer silt loam, 3 to 8 percent slopes	31B	904	3105666	2y9vx	ny051	2019	1:24000
Hudson and Collamer soils, 3 to 8 percent slopes	132B	846	3105729	2y9x1	ny051	2019	1:24000
Collamer silt loam, 15 to 25 percent slopes	31D	772	3105668	2y9vz	ny051	2019	1:24000
Hudson and Collamer soils, 25 to 35 percent slopes	132E	646	3105732	2y9x5	ny051	2019	1:24000
Hudson and Collamer soils, 0 to 3 percent slopes	132A	3	3105728	2y9x0	ny051	2019	1:24000
Collamer silt loam, 3 to 8 percent slopes	CkB	700	292541	9tdt	ny053	1975	1:15840
Collamer silt loam, rolling	CkC	611	292542	9tdv	ny053	1975	1:15840
Collamer silt loam, 0 to 3 percent slopes	CkA	396	292540	9tds	ny053	1975	1:15840
Collamer silt loam, hilly	CkD	310	292543	9tdw	ny053	1975	1:15840
Collamer silt loam, 2 to 6 percent slopes	ClB	14288	292682	9tkc	ny055	1967	1:15840
Collamer silt loam, 0 to 2 percent slopes	ClA	9962	292681	9tkb	ny055	1967	1:15840
Collamer silt loam, loamy subsoil variant, 2 to 6 percent slopes	CmB	1515	292685	9tkg	ny055	1967	1:15840
Collamer silt loam, loamy subsoil variant, 0 to 2 percent slopes	CmA	1097	292684	9tkf	ny055	1967	1:15840
Collamer silt loam, 6 to 12 percent slopes	ClC	732	292683	9tkd	ny055	1967	1:15840
Collamer silt loam, 3 to 8 percent slopes	77B	434	293486	9vd9	ny065	1993	1:24000
Collamer silt loam, 15 to 25 percent slopes	77D	395	293488	9vdc	ny065	1993	1:24000
Collamer silt loam, 8 to 15 percent slopes	77C	394	293487	9vdb	ny065	1993	1:24000
Collamer silt loam, 0 to 3 percent slopes	77A	203	293485	9vd8	ny065	1993	1:24000
Collamer silt loam, 2 to 6 percent slopes	ChB	13303	293549	9vgb	ny067	1973	1:20000
Collamer silt loam, 0 to 2 percent slopes	ChA	4494	293548	9vg9	ny067	1973	1:20000
Collamer silt loam, 0 to 3 percent slopes	31A	1825	2378286	2ktsx	ny069	2012	1:12000
Collamer silt loam, 15 to 25 percent slopes	31D	1109	2378285	2ktsw	ny069	2012	1:12000
Collamer silt loam, 3 to 8 percent slopes	31B	849	2378288	2ktsz	ny069	2012	1:12000
Collamer silt loam, 8 to 15 percent slopes	31C	776	2378287	2ktsy	ny069	2012	1:12000
Collamer silt loam, 3 to 8 percent slopes	CoB	514	293915	9vv4	ny071	1976	1:15840
Collamer silt loam, 8 to 15 percent slopes	CoC	151	293916	9vv5	ny071	1976	1:15840
Collamer silt loam, 15 to 25 percent slopes	CoD	150	293917	9vv6	ny071	1976	1:15840
Collamer silt loam, 2 to 6 percent slopes	CmB	11063	294019	9vyh	ny073	1973	1:15840
Arkport-Collamer complex, 6 to 20 percent slopes	AsD	1098	293999	9vxv	ny073	1973	1:15840
Collamer silt loam, 0 to 2 percent slopes	CmA	926	294018	9vyg	ny073	1973	1:15840
Collamer silt loam, 6 to 12 percent slopes, severely eroded	CmC3	580	294020	9vyj	ny073	1973	1:15840
Collamer silt loam, 3 to 8 percent slopes	CrB	384	294599	9wk6	ny097	1976	1:15840
Collamer silt loam, 0 to 3 percent slopes	CrA	133	294598	9wk5	ny097	1976	1:15840
Collamer silt loam, 2 to 6 percent slopes	ClB	2692	294701	9wnh	ny099	1966	1:15840
Collamer silt loam, 0 to 2 percent slopes	ClA	2496	294700	9wng	ny099	1966	1:15840
Collamer silt loam, moderately shallow variant, 2 to 6 percent slopes	CoB	402	294703	9wnk	ny099	1966	1:15840
Collamer silt loam, moderately shallow variant, 0 to 2 percent slopes	CoA	186	294702	9wnj	ny099	1966	1:15840
Collamer silt loam, 6 to 12 percent slopes	ClC	70	294697	9wnc	ny099	1966	1:15840
Collamer silt loam, rolling	CoC	740	294799	9wrn	ny101	1972	1:15840
Hudson and Collamer silt loams, 2 to 6 percent slopes	HwB	844	295629	9xmf	ny109	1963	1:20000
Collamer silt loam, 2 to 6 percent slopes	CrB	3550	295714	9xq5	ny117	1972	1:15840
Collamer silt loam, 3 to 8 percent slopes	CoB	907	295331	9x9t	ny121	1969	1:20000
Collamer silt loam, 8 to 15 percent slopes	CoC	818	295332	9x9v	ny121	1969	1:20000
Collamer silt loam, 15 to 25 percent slopes	CoD	489	295333	9x9w	ny121	1969	1:20000
Collamer silt loam, 3 to 8 percent slopes	CsB	139	289256	9pzv	ny605	1981	1:24000
Collamer silt loam, till substratum, 3 to 8 percent slopes	CtB	54	289258	9pzx	ny605	1981	1:24000
Collamer silt loam, 8 to 15 percent slopes	CsC	22	289257	9pzw	ny605	1981	1:24000
Collamer silt loam, 2 to 6 percent slopes	CnB	6352	292985	9tw4	ny664	1968	1:15840
Collamer silt loam, 0 to 2 percent slopes	CnA	3823	292984	9tw3	ny664	1968	1:15840
Collamer silt loam, 15 to 25 percent slopes	CoD	82	2633108	2rg8p	pa049	2012	1:12000
Collamer silt loam, 8 to 15 percent slopes	CoC	40	2633109	2rg8q	pa049	2012	1:12000

Map of Series Extent

Approximate geographic distribution of the COLLAMER 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).