Soil Data Explorer - DUNKIRK

Official Series Description

Lab Data Summary

Aggregate lab data for the DUNKIRK soil series. This aggregation is based on all pedons with a current taxon name of DUNKIRK, 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 DUNKIRK 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	88P0714	88NY109001A	Dunkirk	6	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	42.4583321,-76.4583359
140	88P0715	88NY109001B	Dunkirk	6	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	42.4583321,-76.4583359

Water Balance

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

There are insufficient data to create the annual climate figure.

Geomorphic description summaries for the DUNKIRK 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 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 DUNKIRK, 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

No block diagrams are available.

Map Units

Map units containing DUNKIRK 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
Dunkirk silt loam, 25 to 35 percent slopes	140E	95	299775	b1y5	ny003	2013	1:24000
Dunkirk silt loam, 25 to 35 percent slopes	140E	1196	289533	9q8s	ny009	2002	1:24000
Dunkirk silt loam, 15 to 25 percent slopes	140D	1067	289532	9q8r	ny009	2002	1:24000
Dunkirk silt loam, 1 to 6 percent slopes	DuB	1293	289389	9q44	ny011	1968	1:15840
Dunkirk silt loam, 6 to 12 percent slopes, eroded	DuC3	819	289390	9q45	ny011	1968	1:15840
Dunkirk soils, 18 to 35 percent slopes	DvE	129	289392	9q47	ny011	1968	1:15840
Dunkirk silt loam, 12 to 18 percent slopes, eroded	DuD3	83	289391	9q46	ny011	1968	1:15840
Dunkirk silt loam, 15 to 25 percent slopes	DkD	385	289820	9ql1	ny013	1988	1:15840
Dunkirk silt loam, 25 to 45 percent slopes	DkE	275	289821	9ql2	ny013	1988	1:15840
Dunkirk silt loam, 8 to 15 percent slopes	DuC	916	316633	bmgz	ny031	2007	1:24000
Factoryville-Dunkirk complex, 25 to 60 percent slopes	FdF	795	1468893	1l9hn	ny031	2007	1:24000
Dunkirk silt loam, 25 to 45 percent slopes	DuE	682	316631	bmgx	ny031	2007	1:24000
Dunkirk silt loam, 15 to 25 percent slopes	DuD	528	316632	bmgy	ny031	2007	1:24000
Dunkirk silt loam, 2 to 6 percent slopes	DuB	2188	301698	b3y6	ny037	2004	1:24000
Dunkirk silt loam, 6 to 12 percent slopes	DuC	1073	301699	b3y7	ny037	2004	1:24000
Arkport and Dunkirk soils, 12 to 20 percent slopes	AsD	400	301671	b3xb	ny037	2004	1:24000
Arkport and Dunkirk soils, 20 to 40 percent slopes	AsE	138	301672	b3xc	ny037	2004	1:24000
Dunkirk silt loam, 2 to 6 percent slopes	SmB	562	2677798	bmp1	ny049	2018	1:24000
Dunkirk silt loam, 0 to 6 percent slopes	HkB	496	2677714	bmld	ny049	2018	1:24000
Dunkirk silt loam, 6 to 12 percent slopes	SnC	427	2677799	bmp2	ny049	2018	1:24000
Dunkirk silt loam, 0 to 2 percent slopes	SmA	60	2677797	bmp0	ny049	2018	1:24000
Dunkirk silt loam, 15 to 25 percent slopes	33D	397	3105670	2y9w1	ny051	2019	1:24000
Dunkirk silt loam, 8 to 15 percent slopes	33C	319	3105669	2y9w0	ny051	2019	1:24000
Arkport, Dunkirk, and Colonie soils, 20 to 60 percent slopes, eroded	AtF3	7299	292668	9tjx	ny055	1967	1:15840
Dunkirk silt loam, 2 to 6 percent slopes	DuB	1143	292691	9tkn	ny055	1967	1:15840
Arkport-Dunkirk very fine sandy loams, 12 to 25 percent slopes	AsD	1031	292667	9tjw	ny055	1967	1:15840
Dunkirk silt loam, 6 to 12 percent slopes, eroded	DuC3	530	292692	9tkp	ny055	1967	1:15840
Arkport-Dunkirk very fine sandy loams, 2 to 12 percent slopes	AsC	498	292666	9tjv	ny055	1967	1:15840
Dunkirk silt loam, 12 to 20 percent slopes, eroded	DuD3	249	292693	9tkq	ny055	1967	1:15840
Dunkirk silt loam, rolling	DuC	2592	293556	9vgk	ny067	1973	1:20000
Dunkirk silt loam, 3 to 8 percent slopes	33B	1710	2378490	2kv0h	ny069	2012	1:12000
Dunkirk-Arkport complex, 15 to 25 percent slopes	50D	1571	2379129	2kvp3	ny069	2012	1:12000
Dunkirk silt loam, 8 to 15 percent slopes	33C	1064	2378489	2kv0g	ny069	2012	1:12000
Dunkirk-Arkport complex, 8 to 15 percent slopes	50C	739	2378536	2kv1z	ny069	2012	1:12000
Dunkirk silt loam, 0 to 3 percent slopes	33A	637	2378491	2kv0j	ny069	2012	1:12000
Dunkirk silt loam, 15 to 25 percent slopes	33D	569	2378488	2kv0f	ny069	2012	1:12000
Dunkirk fine sandy loam, 3 to 8 percent slopes	32B	421	2378477	2kv02	ny069	2012	1:12000
Dunkirk-Arkport complex, 3 to 8 percent slopes	50B	352	2378537	2kv20	ny069	2012	1:12000
Dunkirk silt loam, 25 to 35 percent slopes	33E	198	2379125	2kvnz	ny069	2012	1:12000
Dunkirk fine sandy loam, 0 to 3 percent slopes	32A	177	2378484	2kv09	ny069	2012	1:12000
Dunkirk and Hudson soils, steep, severely eroded	DUE3	1224	294605	9wkd	ny097	1976	1:15840
Dunkirk silt loam, 3 to 8 percent slopes	DkB	547	294603	9wkb	ny097	1976	1:15840
Dunkirk silt loam, 8 to 15 percent slopes	DkC	142	294604	9wkc	ny097	1976	1:15840
Dunkirk silt loam, 1 to 6 percent slopes	DuB	3636	294710	9wns	ny099	1966	1:15840
Dunkirk silt loam, limestone substratum, 1 to 6 percent slopes	DwB	730	294713	9wnw	ny099	1966	1:15840
Dunkirk silt loam, 6 to 12 percent slopes, eroded	DuC3	552	294711	9wnt	ny099	1966	1:15840
Dunkirk silt loam, 12 to 20 percent slopes	DuD	144	294712	9wnv	ny099	1966	1:15840
Howard-Dunkirk complex, hilly	HpD	2876	294814	9ws4	ny101	1972	1:15840
Dunkirk silt loam, rolling	DuC	1036	294800	9wrp	ny101	1972	1:15840
Dunkirk silt loam, hilly	DuD	256	294801	9wrq	ny101	1972	1:15840
Hudson and Dunkirk soils, 20 to 45 percent slopes	HzE	2322	295630	9xmg	ny109	1963	1:20000
Colonie and Dunkirk soils, hilly	CTE	3182	295706	9xpx	ny117	1972	1:15840
Dunkirk silt loam, 6 to 12 percent slopes, severely eroded	DkC3	722	295720	9xqc	ny117	1972	1:15840
Dunkirk silt loam, 12 to 20 percent slopes	DkD	567	295721	9xqd	ny117	1972	1:15840
Dunkirk silt loam, 2 to 6 percent slopes	DkB	169	295719	9xqb	ny117	1972	1:15840
Dunkirk silt loam, 8 to 15 percent slopes	33C	856	3250291	2kv0g	ny123	1948	1:12000
Dunkirk silt loam, 3 to 8 percent slopes	33B	620	3250292	2kv0h	ny123	1948	1:12000
Dunkirk silt loam, 25 to 35 percent slopes	33E	49	3250299	2kvnz	ny123	1948	1:12000
Dunkirk silt loam, 15 to 25 percent slopes	33D	31	3250290	2kv0f	ny123	1948	1:12000
Dunkirk silt loam, 2 to 6 percent slopes	DuB	789	292989	9tw8	ny664	1968	1:15840
Dunkirk silt loam, 6 to 12 percent slopes, eroded	DuC3	507	292990	9tw9	ny664	1968	1:15840
Dunkirk and Arkport soils, 12 to 20 percent slopes, eroded	DvD3	444	292991	9twb	ny664	1968	1:15840

Map of Series Extent

Approximate geographic distribution of the DUNKIRK 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).