Soil Data Explorer - SAUGATUCK

Official Series Description

Lab Data Summary

Aggregate lab data for the SAUGATUCK soil series. This aggregation is based on all pedons with a current taxon name of SAUGATUCK, 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 SAUGATUCK 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
144A	40A0492	59NH013002	Saugatuck	5	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	43.125,-71.4416656
144A	92P0989	92NH011001	Saugatuck	6	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	42.8600006,-71.5952759
144A	92P0993	S1992NH011005	Saugatuck	5	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	42.9386101,-71.7372208
90B	89P0060	88WI013022	Saugatuck	5	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	45.8002777,-92.5644455
97	LP7606	1976IN091006	Saugatuck	3	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	41.753175,-86.7572417
97	99P0348	S1999MI159001	SAUGATUCK	6	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	42.3016663,-86.2438889
98	40A5198	1958MI139001	Saugatuck	5	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	42.9705556,-86.1416667
98	40A5651	1958MI139002	Saugatuck	4	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	43.0636111,-86.1530278
98	08N0654	F2008MI121001	Saugatuck	6	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	43.1552505,-86.059639
98	10N0101	F2009MI121005	Saugatuck	6	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	43.1570549,-86.0857468
n/a	89P0059	88MI105001	Saugatuck	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 SAUGATUCK 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 SAUGATUCK 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 SAUGATUCK 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 SAUGATUCK 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 SAUGATUCK 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 SAUGATUCK 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 SAUGATUCK 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 hills figure.

There are insufficient data to create the 3D mountains figure.

There are insufficient data to create the 3D terrace figure.

Soil series sharing subgroup-level classification with SAUGATUCK, 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. NH-2012-02-14-24 | Strafford County - March 1973

   Typical pattern of soils and underlying material in the Hinckley-Windsor-Saugatuck association (Soil Survey of Strafford County, New Hampshire; March 1973).

Map Units

Map units containing SAUGATUCK 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
Saugatuck-Pipestone complex	Sa	795	272689	94rf	in091	1979	1:15840
Saugatuck loamy sand	Sd	2550	315732	bljx	me005	1969	1:24000
Saugatuck sand	Sc	229	189268	6byf	mi011	1964	1:20000
Saugatuck loamy sand	Sb	152	189267	6byd	mi011	1964	1:20000
Saugatuck sand, 0 to 6 percent slopes	SaB	713	190509	6d7g	mi029	1970	1:15840
Saugatuck sand, 0 to 6 percent slopes	ScB	349	189372	6c1s	mi047	1968	1:20000
Saugatuck sand	Sc	534	189859	6ckh	mi051	1966	1:15840
Au Gres-Saugatuck sands, 0 to 2 percent slopes	AsA	845	189389	6c2b	mi055	1963	1:15840
Au Gres-Saugatuck sands, 2 to 6 percent slopes	AsB	189	189390	6c2c	mi055	1963	1:15840
Saugatuck-Jebavy complex, 0 to 3 percent slopes	53A	4830	192568	6gcw	mi105	1992	1:15840
Pipestone-Saugatuck sands, 0 to 4 percent slopes	56B	4253	192572	6gd0	mi105	1992	1:15840
Pipestone-Covert-Saugatuck sands, 0 to 3 percent slopes	PpsaaA	29682	2689438	2rfgv	mi121	1966	1:15840
Pipestone-Covert-Saugatuck sands, 0 to 3 percent slopes	PpsaaA	83	2689463	2rfgv	mi123	1990	1:15840
Saugatuck-Jebavy complex, 0 to 3 percent slopes	48A	5662	189046	6bq8	mi127	1992	1:15840
Pipestone-Covert-Saugatuck sands, 0 to 3 percent slopes	PpsaaA	14	2689471	2rfgv	mi127	1992	1:15840
Saugatuck sand, 0 to 6 percent slopes	ScB	353	190207	6cxq	mi133	1966	1:15840
Pipestone-Covert-Saugatuck sands, 0 to 3 percent slopes	PpsaaA	14872	2689479	2rfgv	mi139	1967	1:15840
Pipestone and Saugatuck loamy sands, 0 to 2 percent slopes	AeA0	711	2673636	2qz3j	mi151	1955	1:15840
Pipestone and Saugatuck loamy sands, 2 to 6 percent slopes, slightly eroded	AeB1	114	2673637	2qz3k	mi151	1955	1:15840
Saugatuck-Jebavy complex, 0 to 3 percent slopes	53A	5750	193261	6h37	mi614	2005	1:12000
Saugatuck sand, 0 to 3 percent slopes	108A	1501	193361	6h6g	mi614	2005	1:12000
Saugatuck loamy sand	Sb	5886	279922	9d8r	nh017	1968	1:20000
Saugatuck loamy sand	Sn	345	281014	9fdz	nh601	1980	1:20000

Map of Series Extent

Approximate geographic distribution of the SAUGATUCK 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).