Soil Data Explorer - INGLESIDE

Official Series Description

Lab Data Summary

Aggregate lab data for the INGLESIDE soil series. This aggregation is based on all pedons with a current taxon name of INGLESIDE, 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 INGLESIDE 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
149A	40A0324	S1957NJ015001	Ingleside	2	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	39.6462278,-74.9740583
149A	40A0331	S1959NJ011001	Ingleside	3	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	39.3742806,-75.2640778
149A	95P0268	S1994MD003018	Ingleside	6	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	39.0327797,-76.690834
153C	93P0455	S1992MD035026	Ingleside	7	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	39.1040573,-76.1060028
153D	92P0369	91NJ009002	Ingleside	5	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	39.2222214,-74.8466644
153D	40A0330	S1959NJ009001	Ingleside	4	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	38.9626139,-74.94345
153D	86P0112	S1985MD019007	Ingleside	7	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	38.5780563,-75.992775
153D	93P0471	S1993MD047019	Ingleside	6	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	38.0416679,-75.375
n/a	40A0329	S1958NJ015007	Ingleside	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 INGLESIDE 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 INGLESIDE 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 INGLESIDE 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 INGLESIDE 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 INGLESIDE 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 INGLESIDE 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 INGLESIDE 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 INGLESIDE, 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. NJ-2012-02-14-01 | Cape May County - 2002

   The relationship of soils, landform position, and underlying material in the Downer-Ingleside-Swainton general soil map unit. Evesboro, Fort Mott, and Aura soils are minor components in the map unit (Soil Survey of Cape May County, New Jerser; 2002).

Map Units

Map units containing INGLESIDE 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
Ingleside sandy loam, 2 to 5 percent slopes	IgB	5861	1606073	1qx7t	de001	2006	1:24000
Ingleside sandy loam, 0 to 2 percent slopes	IgA	4798	1606072	1qx7s	de001	2006	1:24000
Ingleside-Hammonton-Fallsington complex, 0 to 5 percent slopes	ImB	2193	1606076	1qx7x	de001	2006	1:24000
Ingleside loamy sand, 2 to 5 percent slopes	IeB	1858	1606071	1qx7r	de001	2006	1:24000
Ingleside loamy sand, 0 to 2 percent slopes	IeA	1540	1606070	1qx7q	de001	2006	1:24000
Ingleside-Urban land complex, 0 to 5 percent slopes	IuB	603	1606077	1qx7y	de001	2006	1:24000
Ingleside sandy loam, 5 to 10 percent slopes	IgC	207	1606075	1qx7w	de001	2006	1:24000
Ingleside-Hammonton-Fallsington complex, 0 to 5 percent slopes	ImB	8951	2479773	2p7dp	de003	2009	1:24000
Ingleside sandy loam, 2 to 5 percent slopes	IgB	1124	2479784	2p7f1	de003	2009	1:24000
Ingleside loamy sand, 0 to 2 percent slopes	IeA	665	2479785	2p7f2	de003	2009	1:24000
Ingleside loamy sand, 2 to 5 percent slopes	IeB	596	2479786	2p7f3	de003	2009	1:24000
Ingleside loamy sand, 0 to 2 percent slopes	IeA	13415	1603423	1qthb	de005	2006	1:24000
Ingleside sandy loam, 0 to 2 percent slopes	IgA	7453	1603425	1qthd	de005	2006	1:24000
Ingleside-Hammonton-Fallsington complex, 0 to 5 percent slopes	ImB	2824	1603427	1qthg	de005	2006	1:24000
Ingleside loamy sand, 2 to 5 percent slopes	IeB	1802	1603424	1qthc	de005	2006	1:24000
Ingleside-Urban land complex, 0 to 5 percent slopes	IuB	757	1603428	1qthh	de005	2006	1:24000
Ingleside sandy loam, 2 to 5 percent slopes	IgB	400	1603426	1qthf	de005	2006	1:24000
Ingleside-Woodstown complex, 5 to 10 percent slopes	IwC	10298	2516875	2pz8d	md009	1967	1:20000
Ingleside loamy sand, 2 to 5 percent slopes	IbB	3751	2516872	2pz89	md009	1967	1:20000
Ingleside-Woodstown complex, 10 to 15 percent slopes	IwD	3490	2516876	2pz8f	md009	1967	1:20000
Ingleside-Evesboro complex, 5 to 10 percent slopes	IeC	805	2516880	2pz8k	md009	1967	1:20000
Ingleside-Woodstown complex, 2 to 5 percent slopes	IwB	601	2516879	2pz8j	md009	1967	1:20000
Ingleside-Galestown complex, 0 to 5 percent slopes	IgB	488	2516877	2pz8g	md009	1967	1:20000
Ingleside loamy sand, 5 to 10 percent slopes	IbC	113	2516873	2pz8b	md009	1967	1:20000
Ingleside loamy sand, 2 to 5 percent slopes	IeB	10382	1600079	1qq0g	md011	2009	1:12000
Ingleside sandy loam, 2 to 5 percent slopes	IgB	9907	1600108	1qq1d	md011	2009	1:12000
Ingleside loamy sand, 0 to 2 percent slopes	IeA	8357	1600078	1qq0f	md011	2009	1:12000
Ingleside sandy loam, 0 to 2 percent slopes	IgA	6529	1600107	1qq1c	md011	2009	1:12000
Ingleside loamy sand, 5 to 10 percent slopes	IeC	1020	2455512	2nf52	md011	2009	1:12000
Ingleside sandy loam, 5 to 10 percent slopes	IgC	48	2452691	2nb72	md011	2009	1:12000
Ingleside-Hammonton-Fallsington complex, 0 to 5 percent slopes	ImB	107	2440572	2mxm4	md015	2009	1:12000
Ingleside sandy loam, 2 to 5 percent slopes	IgB	41	2440582	2mxmg	md015	2009	1:12000
Ingleside sandy loam, 0 to 2 percent slopes	IgA	8017	128946	4b5k	md019	1992	1:15840
Ingleside sandy loam, 2 to 5 percent slopes	IgB	2744	128947	4b5l	md019	1992	1:15840
Ingleside-Hammonton-Fallsington complex, 0 to 5 percent slopes	ImB	17	2702636	1qx7x	md029	1978	1:15840
Ingleside sandy loam, 2 to 5 percent slopes	IgB	12	2702635	1qx7t	md029	1978	1:15840
Ingleside sandy loam, 0 to 2 percent slopes	InA	517	2474814	2p27q	md033	2009	1:12000
Ingleside sandy loam, 2 to 5 percent slopes	IgB	36618	139711	4pct	md035	1995	1:12000
Ingleside sandy loam, 5 to 10 percent slopes	IgC	6733	139712	4pcv	md035	1995	1:12000
Ingleside sandy loam, 0 to 2 percent slopes	IgA	2670	139710	4pcs	md035	1995	1:12000
Ingleside sandy loam, 2 to 5 percent slopes	IgB	1297	1407964	1j836	md039	2006	1:12000
Ingleside-Runclint complex, 5 to 10 percent slopes	IkC	500	1599015	1qnx4	md039	2006	1:12000
Ingleside sandy loam, 0 to 2 percent slopes	IgA	249	1407963	1j835	md039	2006	1:12000
Ingleside sandy loam, 2 to 5 percent slopes	IgB	1842	1712515	1vh0f	md041	2009	1:12000
Ingleside sandy loam, 5 to 10 percent slopes	IgC	555	1882968	216cx	md041	2009	1:12000
Ingleside sandy loam, 0 to 2 percent slopes	IgA	400	1712514	1vh0d	md041	2009	1:12000
Ingleside loamy sand, 2 to 5 percent slopes	IeB	2645	975568	11r4y	md045	2005	1:12000
Ingleside loamy sand, 0 to 2 percent slopes	IeA	1847	975567	11r4x	md045	2005	1:12000
Ingleside loamy sand, 0 to 5 percent slopes, Northern Tidewater Area	IngB	4062	697931	2ztw0	nj005	1967	1:24000
Ingleside loamy sand, 0 to 5 percent slopes, Northern Tidewater Area	IngB	6007	745574	2ztw0	nj009	1997	1:24000
Ingleside sandy loam, 0 to 2 percent slopes	InnA	4662	745575	t0tt	nj009	1997	1:24000
Ingleside loamy sand, 0 to 5 percent slopes, Northern Tidewater Area	IngB	233	697604	2ztw0	nj029	1978	1:24000

Map of Series Extent

Approximate geographic distribution of the INGLESIDE 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).