Soil Data Explorer - NEWHAN

Official Series Description

Lab Data Summary

Aggregate lab data for the NEWHAN soil series. This aggregation is based on all pedons with a current taxon name of NEWHAN, 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 NEWHAN were used in the calculation. Source: KSSL snapshot (updated 2020-03-13). 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
152A	S66_025	1980-FL131-S66_025	Newhan	3	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	30.3718662,-86.3412094
152A	S23_014	1989-FL045-S23_014	Newhan	3	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	29.7492981,-85.3995972
153B	S45_002	1984-FL089-S45_002	Newhan	3	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	30.5697918,-81.4446716
153B	VPI0434	V1992-VA810-434	Newhan	3	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	36.9092293,-75.9980621
153B	VPI0437	V1992-VA810-437	Newhan	3	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	36.5593033,-75.8702011
n/a	VPI0435	V1992-VA810-435	Newhan	1	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	n/a
n/a	VPI0436	V1992-VA810-436	Newhan	2	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 NEWHAN 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 NEWHAN series. Sketches are arranged according to their subgroup-level taxonomic structure. Source: SSURGO snapshot (updated 2024-02-21), parsed OSD records (updated 2023-10-02) and snapshot of SC database (updated 2023-10-02).

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

Select annual climate data summaries for the NEWHAN 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).

Geomorphic description summaries for the NEWHAN 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 3D mountains figure.

Soil series sharing subgroup-level classification with NEWHAN, 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. FL-2011-05-31-08 | City of Jacksonville, Duval County - 1978

   Typical pattern of soils and parent material in an area of the Fripp-Corolla-Mandarin, Cornelia-Mandarin-Leon, and Tisonia-Maurepas general soil map units. The soils of these map units support native vegetation (Soil Survey of City of Jacksonville, Duval County, Florida; 1978).

2. FL-2011-05-31-12 | Nassau County - 1991

   Typical pattern of soils and parent material in an area of the Kureb-Fripp-Newhan and Mandarin-Echaw map units (Soil Survey of Nassau County, Florida; 1991).

Map Units

Map units containing NEWHAN 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
Newhan-Duckston complex, 0 to 8 percent slopes, rarely flooded, gulf	NdC	839	2995037	2x5ql	al097	2018	1:24000
Urban land-Duckston-Newhan complex, 0 to 8 percent slopes, rarely flooded, gulf	UdC	537	2995036	2x5qk	al097	2018	1:24000
Fripp-Newhan complex, 5 to 30 percent slopes, rarely flooded, gulf	FnE	75	2995035	2x5qj	al097	2018	1:24000
Newhan-Corolla, rarely flooded, complex, gently undulating to hilly, 2 to 20 percent slopes	42	230	738854	ssv0	fl031	1996	1:24000
Newhan-Corolla complex, rolling, rarely flooded	8	3180	1425316	1jv4y	fl033	1998	1:24000
Newhan-Corolla complex, 2 to 30 percent slopes	40	1822	1477094	2w4gq	fl037	1990	1:20000
Newhan-Corolla complex, 2 to 30 percent slopes	47	446	1472767	2w4gq	fl045	1997	1:24000
Newhan-Corolla, rarely flooded, fine sands, rolling	12	695	132898	4g91	fl089	1989	1:15840
Newhan-Corolla complex, 2 to 30 percent slopes	18	4320	1444700	2w4gq	fl091	1989	1:20000
Newhan-Corolla complex, 2 to 30 percent slopes	49	570	823796	2w4gq	fl113	1978	1:24000
Newhan-Corolla sands, rolling	54	1170	324026	bw5g	fl131	1985	1:20000
Newhan-Duckston complex, 0 to 8 percent slopes, rarely flooded, gulf	NdC	247	3121735	2x5ql	ms045	1979	1:20000
Newhan-Duckston complex, 0 to 8 percent slopes, rarely flooded, gulf	Su	951	3121736	2x5ql	ms047	1971	1:20000
Newhan-Duckston complex, 0 to 8 percent slopes, rarely flooded, gulf	386	839	3121737	2x5ql	ms059	1997	1:24000
Newhan fine sand, 2 to 30 percent slopes	NeE	4682	115550	3w7f	nc019	1983	1:24000
Newhan fine sand, dredged, 2 to 30 percent slopes	NhE	3823	115551	3w7g	nc019	1983	1:24000
Newhan-Corolla complex, 0 to 30 percent slopes	Nc	2748	115609	3w9b	nc031	1984	1:24000
Newhan fine sand, dredged, 2 to 30 percent slopes	Nd	2165	115610	3w9c	nc031	1984	1:24000
Newhan fine sand, 2 to 30 percent slopes	Nh	1296	115612	3w9f	nc031	1984	1:24000
Beaches-Newhan complex, 0 to 30 percent slopes	Bn	1067	115574	3w86	nc031	1984	1:24000
Newhan-Urban land complex, 0 to 8 percent slopes	Ne	495	115611	3w9d	nc031	1984	1:24000
Beaches-Newhan association	BN	1715	112105	3rn9	nc053	1980	1:20000
Newhan fine sand, 0 to 10 percent slopes	NeC	1358	112120	3rns	nc053	1980	1:20000
Newhan-Corolla complex, 0 to 10 percent slopes	NhC	1025	112121	3rnt	nc053	1980	1:20000
Dune land-Newhan complex, 2 to 40 percent slopes	DwD	915	112118	3rnq	nc053	1980	1:20000
Newhan fine sand, 0 to 10 percent slopes	NeC	5773	110985	3qh5	nc055	1987	1:24000
Beaches-Newhan complex, 0 to 25 percent slopes	BnD	4565	110968	3qgm	nc055	1987	1:24000
Newhan-Corolla complex, 0 to 10 percent slopes	NhC	2011	110986	3qh6	nc055	1987	1:24000
Dune land-Newhan complex, 2 to 40 percent slopes	DwE	1087	110978	3qgy	nc055	1987	1:24000
Newhan-Urban land complex, 0 to 10 percent slopes	NuC	477	110987	3qh7	nc055	1987	1:24000
Beaches-Newhan complex, 3 to 50 percent slopes, flooded	BeE	1204	113271	3svx	nc095	1996	1:24000
Newhan fine sand, 6 to 25 percent slopes, rarely flooded	NaD	348	113296	3swq	nc095	1996	1:24000
Newhan-Corolla complex, 0 to 15 percent slopes, rarely flooded	NcC	305	113297	3swr	nc095	1996	1:24000
Newhan fine sand	Nh	3845	116049	3wrj	nc129	1974	1:15840
Newhan-Beaches complex, 0 to 30 percent slopes	NeE	2092	116091	3wsw	nc133	1984	1:24000
Newhan-Corolla-Urban land complex, 0 to 30 percent slopes	NnE	950	116093	3wsy	nc133	1984	1:24000
Newhan fine sand, dredged, 2 to 10 percent slopes	NfC	863	116092	3wsx	nc133	1984	1:24000
Newhan-Corolla-Urban land complex, 0 to 30 percent slopes	NmE	1186	116185	3wwx	nc141	1986	1:24000
Newhan-Corolla complex, 0 to 30 percent slopes	NkE	671	116184	3www	nc141	1986	1:24000
Newhan fine sand, dredged, 2 to 10 percent slopes	NhC	612	116183	3wwv	nc141	1986	1:24000
Newhan sand, 0 to 6 percent slopes	38B	1710	639589	pgjx	sc043	1980	1:20000
Newhan fine sand, 0 to 6 percent slopes	NhB	2930	130159	4cfp	sc051	1983	1:20000
Coastal beaches and dune land	Co	6209	138272	4mwd	sc690	1967	1:24000
Newhan fine sand, 2 to 30 percent slopes	22E	1915	120898	41sy	va810	1982	1:15840
Newhan-Corolla fine sands, 0 to 15 percent slopes	23C	1250	120899	41sz	va810	1982	1:15840

Map of Series Extent

Approximate geographic distribution of the NEWHAN 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).