Soil Data Explorer - CABOT

Official Series Description

Lab Data Summary

Aggregate lab data for the CABOT soil series. This aggregation is based on all pedons with a current taxon name of CABOT, 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 CABOT 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
143	2013NH605008	2013NH605008	Cabot	1	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	44.0968672,-71.7969906
143	2013NH605009	2013NH605009	Cabot	1	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	44.0878267,-71.7937413
143	2013NH605010	2013NH605010	Cabot	1	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	44.0893015,-71.7945477
143	93P0071	92VT027001	Cabot	6	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	43.9127769,-72.7844467
143	93P0072	92VT027002	Cabot	6	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	43.9147224,-72.7847214
143	10N0728	S09VT007006	Cabot	6	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	44.4220123,-73.0720444
144A	1982MA011001	S1982MA011001	Cabot	3	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	42.65305,-72.6746778
144B	2013NH605043	2013NH605043	Cabot	1	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	44.0768222,-71.8103472
n/a	40A5417	59VT017001	Cabot	6	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	n/a
n/a	40A5418	59VT017003	Cabot	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 CABOT 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 CABOT 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 CABOT 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 CABOT 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 CABOT 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 CABOT 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 CABOT 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 CABOT, 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. VT-2012-03-22-03 | Chittenden County - January 1974

   Relationship of soils in associations 13 and 14 (Soil Survey of Chittenden County, VT; 1974).

Map Units

Map units containing CABOT 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
Cabot-Howland association, 0 to 15 percent slopes	CAB	829	1478426	1lmf5	me619	2005	1:24000
Howland-Cabot association, 0 to 15 percent slopes	HWB	248	1478425	1lmf4	me619	2005	1:24000
Peacham-Wonsqueak-Cabot association, 0 to 8 percent slopes	PCA	7	1478421	1lmf0	me619	2005	1:24000
Howland-Cabot association, gently sloping, very stony	964B	31500	280760	9f4s	nh607	2000	1:24000
Cabot-Howland association, gently sloping, very stony	965B	23124	280761	9f4t	nh607	2000	1:24000
Cabot silt loam, 0 to 8 percent slopes, very stony	590B	11235	280685	2qgwf	nh607	2000	1:24000
Cabot silt loam, 8 to 15 percent slopes, very stony	590C	7795	280687	2qgwg	nh607	2000	1:24000
Peacham-Wonsqueak-Cabot association, nearly level, extremely stony	768A	2061	280741	9f45	nh607	2000	1:24000
Cabot silt loam, 3 to 8 percent slopes	589B	1051	280683	2qgwb	nh607	2000	1:24000
Cabot silt loam, 8 to 15 percent slopes	589C	1011	280684	2qgwc	nh607	2000	1:24000
Cabot silt loam, 0 to 3 percent slopes	589A	163	280682	2qgw9	nh607	2000	1:24000
Cabot silt loam, 0 to 15 percent slopes, very stony	CbC	10494	281238	2ty55	vt001	1967	1:15840
Cabot silt loam, 0 to 8 percent slopes	CaB	509	281237	2ty54	vt001	1967	1:15840
Cabot silt loam, 0 to 8 percent slopes, very stony	113B	3386	281371	2qgwf	vt003	1992	1:20000
Peru-Berkshire-Cabot association, 15 to 35 percent slopes, very stony	413D	1624	281484	2xk0q	vt003	1992	1:20000
Cabot-Carlisle association, undulating, very stony	403B	227	281474	9fwt	vt003	1992	1:20000
Cabot silt loam, 0 to 8 percent slopes, very stony	23B	35737	282874	2qgwf	vt005	2006	1:20000
Cabot silt loam, 8 to 15 percent slopes, very stony	23C	19286	282875	2qgwg	vt005	2006	1:20000
Cabot silt loam, 3 to 8 percent slopes	22B	9550	282872	2qgwb	vt005	2006	1:20000
Colonel-Cabot complex, 3 to 15 percent slopes, extremely bouldery	87C	8042	282996	2w9nr	vt005	2006	1:20000
Cabot silt loam, 8 to 15 percent slopes	22C	5645	282873	2qgwc	vt005	2006	1:20000
Colonel-Cabot complex, 8 to 15 percent slopes, very stony	73C	3541	282973	2w9nn	vt005	2006	1:20000
Cabot silt loam, 0 to 15 percent slopes, extremely bouldery	86C	2032	282995	2qgwd	vt005	2006	1:20000
Colonel-Cabot complex, 3 to 8 percent slopes, very stony	73B	1420	282972	2w9nl	vt005	2006	1:20000
Colonel-Cabot complex, 3 to 8 percent slopes	72B	408	282969	2w9nk	vt005	2006	1:20000
Colonel-Cabot complex, 8 to 15 percent slopes	72C	251	282970	2w9nm	vt005	2006	1:20000
Colonel-Cabot complex, 15 to 35 percent slopes, very stony	73D	213	282974	2w9nq	vt005	2006	1:20000
Colonel-Cabot complex, 15 to 25 percent slopes	72D	8	282971	2w9np	vt005	2006	1:20000
Cabot silt loam, 3 to 25 percent slopes, very stony	CbD	11498	281676	2ty53	vt007	1969	1:15840
Cabot silt loam, 3 to 15 percent slopes	CaC	3258	281674	2ty50	vt007	1969	1:15840
Cabot silt loam, 0 to 3 percent slopes, very stony	CbA	861	281675	2trpc	vt007	1969	1:15840
Cabot silt loam, 0 to 3 percent slopes	CaA	702	281673	2trpb	vt007	1969	1:15840
Cabot-Colonel complex, 8 to 15 percent slopes, very stony	SIE12	72774	2409964	2w9nf	vt009	2012	1:
Cabot silt loam, 0 to 8 percent slopes, very stony	SIE11	52895	2409963	2qgwf	vt009	2012	1:
Tunbridge-Colonel-Cabot complex, 8 to 15 percent slopes, very stony	SIE42	37510	2409976	2w9nt	vt009	2012	1:
Cabot-Colonel complex, 8 to 15 percent slopes	SIE12N	1035	2505002	2w9nj	vt009	2012	1:
Cabot silt loam, 3 to 8 percent slopes	SIE11N	894	2505001	2qgwb	vt009	2012	1:
Tunbridge-Colonel-Cabot complex, 8 to 15 percent slopes, rocky	SIE42N	499	2505007	2w9ns	vt009	2012	1:
Cabot silt loam, 3 to 15 percent slopes, very stony	CbB	24878	281779	2ty52	vt011	1976	1:20000
Cabot silt loam, 0 to 3 percent slopes, very stony	CbA	4489	281778	2trpc	vt011	1976	1:20000
Cabot silt loam, 3 to 8 percent slopes	CaB	1409	281777	2ty51	vt011	1976	1:20000
Cabot silt loam, 0 to 3 percent slopes	CaA	1263	281776	2trpb	vt011	1976	1:20000
Cabot silt loam, 0 to 8 percent slopes, very stony	FrB	12650	281904	2qgwf	vt015	1979	1:20000
Cabot silt loam, 3 to 15 percent slopes, very stony	CbB	37718	279392	2ty56	vt017	1975	1:20000
Cabot silt loam, 0 to 8 percent slopes	CaB	6299	279389	2trpd	vt017	1975	1:20000
Cabot silt loam, 8 to 15 percent slopes	CaC	2704	279390	2qgwc	vt017	1975	1:20000
Cabot silt loam, 15 to 25 percent slopes, very stony	CbD	2050	279393	2ty58	vt017	1975	1:20000
Cabot silt loam, 15 to 25 percent slopes	CaD	214	279391	2ty57	vt017	1975	1:20000
Cabot silt loam, 0 to 8 percent slopes, very stony	59B	53412	283502	2qgwf	vt019	2005	1:20000
Cabot silt loam, 3 to 8 percent slopes	47B	18596	283478	2qgwb	vt019	2005	1:20000
Cabot silt loam, 8 to 15 percent slopes, very stony	59C	17298	283504	2qgwg	vt019	2005	1:20000
Colonel-Cabot complex, 8 to 15 percent slopes, very stony	259C	12805	283435	2w9nn	vt019	2005	1:20000
Colonel-Cabot complex, 3 to 8 percent slopes, very stony	259B	6468	283434	2w9nl	vt019	2005	1:20000
Cabot silt loam, 8 to 15 percent slopes	47C	5584	283479	2qgwc	vt019	2005	1:20000
Colonel-Cabot complex, 3 to 8 percent slopes	247B	4457	283430	2w9nk	vt019	2005	1:20000
Colonel-Cabot complex, 8 to 15 percent slopes	247C	1865	283431	2w9nm	vt019	2005	1:20000
Colonel-Cabot complex, 15 to 35 percent slopes, very stony	259D	1209	283436	2w9nq	vt019	2005	1:20000
Cabot silt loam, 0 to 3 percent slopes	47A	526	283477	2qgw9	vt019	2005	1:20000
Cabot silt loam, 0 to 15 percent slopes, extremely bouldery	359C	57	1400125	2qgwd	vt019	2005	1:20000
Colonel-Cabot complex, 15 to 25 percent slopes	247D	52	283432	2w9np	vt019	2005	1:20000
Brayton-Cabot-Pinnebog association, rolling, very stony	403C	3721	282314	9grx	vt021	1985	1:20000
Mundal-Cabot association, hilly, very stony	703D	2856	282431	9gwp	vt021	1985	1:20000
Cabot silt loam, 0 to 8 percent slopes, very stony	6A	1612	282422	2qgwf	vt021	1985	1:20000
Cabot silt loam, 8 to 15 percent slopes, very stony	18C	11444	282574	2qgwg	vt023	1996	1:20000
Cabot silt loam, 0 to 8 percent slopes, very stony	18B	10625	282573	2qgwf	vt023	1996	1:20000
Cabot silt loam, 3 to 8 percent slopes	17B	7520	282569	2qgwb	vt023	1996	1:20000
Cabot silt loam, 8 to 15 percent slopes	17C	4596	282570	2qgwc	vt023	1996	1:20000
Cabot silt loam, 0 to 8 percent slopes, extremely bouldery	98B	2302	282799	2ty59	vt023	1996	1:20000
Cabot silt loam, 8 to 15 percent slopes, extremely bouldery	98C	1778	282800	2ty5b	vt023	1996	1:20000
Cabot silt loam, 0 to 3 percent slopes	17A	420	282568	2qgw9	vt023	1996	1:20000
Cabot silt loam, 0 to 8 percent slopes, very stony	31B	7298	283184	2qgwf	vt027	2000	1:20000
Cabot silt loam, 0 to 8 percent slopes	30B	3225	283181	2trpd	vt027	2000	1:20000
Cabot silt loam, 8 to 15 percent slopes, very stony	31C	1428	283185	2qgwg	vt027	2000	1:20000
Cabot silt loam, 8 to 15 percent slopes	30C	1087	283182	2qgwc	vt027	2000	1:20000
Cabot-Pondicherry-Wonsqueak association, 0 to 8 percent slopes, very stony	403B	337	283344	2w9r7	vt027	2000	1:20000

Map of Series Extent

Approximate geographic distribution of the CABOT 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).