Soil Data Explorer - DUXBURY

Official Series Description

Lab Data Summary

Aggregate lab data for the DUXBURY soil series. This aggregation is based on all pedons with a current taxon name of DUXBURY, 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 DUXBURY 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
n/a	40A4134	S1977VT015005	DUXBURY	4	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	n/a
n/a	40A4136	S1977VT015007	DUXBURY	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 DUXBURY 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 DUXBURY 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 DUXBURY 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 DUXBURY 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).

Competing Series

Soil series competing with DUXBURY 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 DUXBURY 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 DUXBURY 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 mountains figure.

Soil series sharing subgroup-level classification with DUXBURY, 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 DUXBURY 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
Duxbury fine sandy loam, 3 to 15 percent slopes, very stony	350B	1093	319789	bqrs	ny031	2007	1:24000
Duxbury fine sandy loam, 3 to 8 percent slopes	DxB	761	291299	9s3r	ny031	2007	1:24000
Colton-Duxbury-Adams complex, 3 to 15 percent slopes	376C	135	2517672	2q6h5	ny033	2018	1:24000
Duxbury fine sandy loam, 3 to 15 percent slopes	350B	93	2427908	2mhfm	ny033	2018	1:24000
Colton-Duxbury-Adams complex, 0 to 3 percent slopes	376A	46	1913214	226vl	ny033	2018	1:24000
Colton-Duxbury-Dawson complex, 15 to 35 percent slopes	380D	42	2679499	9wv5	ny033	2018	1:24000
Colton-Duxbury-Adams complex, 3 to 15 percent slopes	376C	6	3118067	2q6h5	ny035	2007	1:24000
Colton-Duxbury-Adams complex, 3 to 15 percent slopes	376C	3372	2514986	2q6h5	ny043	2018	1:24000
Duxbury fine sandy loam, 3 to 15 percent slopes	350B	713	2514984	2mhfm	ny043	2018	1:24000
Colton-Duxbury-Adams complex, 0 to 3 percent slopes	376A	167	2518239	226vl	ny043	2018	1:24000
Colton-Duxbury-Dawson complex, 0 to 15 percent slopes	380B	76	2677573	9wv4	ny043	2018	1:24000
Colton-Duxbury-Adams complex, 15 to 35 percent slopes	376D	51	2677572	9wv3	ny043	2018	1:24000
Colton-Duxbury-Adams complex, 3 to 15 percent slopes	376C	326	2517671	2q6h5	ny049	2018	1:24000
Colton-Duxbury-Adams complex, 0 to 3 percent slopes	376A	189	2516833	226vl	ny049	2018	1:24000
Colton-Duxbury-Adams complex, 3 to 15 percent slopes	376C	48792	294874	9wv2	ny089	1990	1:24000
Colton-Duxbury-Dawson complex, 15 to 35 percent slopes	380D	18376	294877	9wv5	ny089	1990	1:24000
Colton-Duxbury-Adams complex, 15 to 35 percent slopes	376D	17232	294875	9wv3	ny089	1990	1:24000
Colton-Duxbury-Dawson complex, 0 to 15 percent slopes	380B	12997	294876	9wv4	ny089	1990	1:24000
Colton-Duxbury complex, 2 to 8 percent slopes	CgB	4416	294915	9wwd	ny089	1990	1:24000
Colton-Duxbury-Adams complex, 0 to 3 percent slopes	376A	3938	294873	9wv1	ny089	1990	1:24000
Colton-Duxbury complex, rolling	CgC	2320	294916	9wwf	ny089	1990	1:24000
Colton-Duxbury complex, hilly	CgD	1478	294917	9wwg	ny089	1990	1:24000
Colton-Duxbury complex, 3 to 8 percent slopes	32B	1022	282892	9hck	vt005	2006	1:20000
Colton-Duxbury complex, 25 to 60 percent slopes	32E	681	282895	9hcn	vt005	2006	1:20000
Colton-Duxbury complex, 15 to 25 percent slopes	32D	570	282894	9hcm	vt005	2006	1:20000
Colton-Duxbury complex, 8 to 15 percent slopes	32C	371	282893	9hcl	vt005	2006	1:20000
Colton-Duxbury complex, 0 to 3 percent slopes	32A	229	282891	9hcj	vt005	2006	1:20000
Colton-Duxbury complex, 15 to 25 percent slopes	32D	1257	1401062	1j0xk	vt009	2012	1:
Colton-Duxbury complex, 3 to 8 percent slopes	32B	1241	1401060	1j0xh	vt009	2012	1:
Colton-Duxbury complex, 8 to 15 percent slopes	32C	1158	1401061	1j0xj	vt009	2012	1:
Colton-Duxbury complex, 25 to 60 percent slopes	32E	630	1401063	1j0xl	vt009	2012	1:
Colton-Duxbury complex, 0 to 3 percent slopes	32A	527	1401059	1j0xg	vt009	2012	1:
Colton-Duxbury complex, 2 to 8 percent slopes	CoB	7468	281899	9gbj	vt015	1979	1:20000
Colton-Duxbury complex, 25 to 50 percent slopes	CoE	5894	281902	9gbm	vt015	1979	1:20000
Colton-Duxbury complex, 8 to 15 percent slopes	CoC	4479	281900	9gbk	vt015	1979	1:20000
Colton-Duxbury complex, 15 to 25 percent slopes	CoD	2377	281901	9gbl	vt015	1979	1:20000
Colton-Duxbury complex, 3 to 8 percent slopes	38B	2524	283469	9hz5	vt019	2005	1:20000
Colton-Duxbury complex, 25 to 60 percent slopes	38E	1483	283472	9hz8	vt019	2005	1:20000
Colton-Duxbury complex, 15 to 25 percent slopes	38D	1334	283471	9hz7	vt019	2005	1:20000
Colton-Duxbury complex, 8 to 15 percent slopes	38C	1137	283470	9hz6	vt019	2005	1:20000
Colton-Duxbury complex, 0 to 3 percent slopes	38A	675	283468	9hz4	vt019	2005	1:20000
Colton-Duxbury complex, 8 to 15 percent slopes, very stony	56C	1573	282378	9gtz	vt021	1985	1:20000
Duxbury-Colton complex, 2 to 8 percent slopes	57B	1557	282381	9gv2	vt021	1985	1:20000
Colton-Duxbury complex, 25 to 50 percent slopes, very stony	56E	1471	282380	9gv1	vt021	1985	1:20000
Colton-Duxbury complex, 2 to 8 percent slopes, very stony	56B	1249	282377	9gty	vt021	1985	1:20000
Colton-Duxbury complex, 8 to 15 percent slopes	58C	1246	282386	9gv7	vt021	1985	1:20000
Colton-Duxbury complex, 15 to 25 percent slopes, very stony	56D	1060	282379	9gv0	vt021	1985	1:20000
Colton-Duxbury complex, 15 to 25 percent slopes	58D	770	282387	9gv8	vt021	1985	1:20000

Map of Series Extent

Approximate geographic distribution of the DUXBURY 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).