Soil Data Explorer - LAKEWOOD

Official Series Description

Lab Data Summary

Aggregate lab data for the LAKEWOOD soil series. This aggregation is based on all pedons with a current taxon name of LAKEWOOD, 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 LAKEWOOD were used in the calculation. Source: KSSL snapshot (updated 2020-03-13). Methods used to assemble the KSSL snapshot used by SoilWeb / SDE

There are insufficient data to create the lab data summary figure.

Pedons used in the lab summary:

MLRA	Lab ID	Pedon ID	Taxonname	CI	NSSL / NASIS Reports	Link To SoilWeb GMap
153D	87P0132	86NJ005001	Lakewood	6	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	39.8041649,-74.8569412
153D	95P0316	94NJ001003	Lakewood	6	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	39.5402794,-74.6022186
153D	95P0317	94NJ001004	Lakewood	5	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	39.541111,-74.6033325
n/a	40A5368	S1973NJ029002	Lakewood	7	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	n/a
n/a	40A5369	S1973NJ029002A	Lakewood	6	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	n/a
n/a	40A5370	S1973NJ029002B	Lakewood	6	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	n/a
n/a	40A5380	S1973NJ029006	Lakewood	4	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	n/a
n/a	40A5381	S1973NJ029006A	Lakewood	6	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	n/a
n/a	40A5382	S1973NJ029006B	Lakewood	6	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	n/a
n/a	40A5383	S1973NJ029007	Lakewood	7	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	n/a
n/a	40A5384	S1973NJ029007A	Lakewood	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 LAKEWOOD 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 LAKEWOOD 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 LAKEWOOD 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 LAKEWOOD 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 LAKEWOOD 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 LAKEWOOD 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).

There are insufficient data to create the annual climate figure.

Geomorphic description summaries for the LAKEWOOD 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 2D hillslope position 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 LAKEWOOD, 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-2012-04-26-09 | Seminole County - June 1966

   Cross section of Seminole County showing the relationship between the geologic strata and artesian and nonartesian water, and the relative position of some of the sandy soils to the ground water table (Soil Survey of Seminole County, Florida; June 1966).

2. NJ-2010-09-13-02 | Cumberland County -

   Typical relationship of the soils, landform position, and parent material of soils that formed in sandy materials and organic deposits. The excessively drained Evesboro and Lakewood soils are in the higher landform positions. The very poorly drained Berryland, Mullica, and Manahawkin soils are in the lowest landform positions. The moderately well drained Galloway and Lakehurst soils are in the intermediate landform positions, but higher than the poorly drained Atsion soils (Soil Survey of Cumberland County, New Jersey).

3. NJ-2010-09-13-03 | Gloucester County -

   (Soil Survey of Gloucester County, New Jersey)

Map Units

Map units containing LAKEWOOD 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
Lakewood sand, 0 to 5 percent slopes	LkB	4558	328162	c0gw	al003	1961	1:20000
Lakewood coarse sand, thick surface, 5 to 8 percent slopes	LxC	560	124640	45pn	ga191	1960	1:20000
Lakewood (kureb) coarse sand, 5 to 8 percent slopes	LBC	155	125086	4651	ga305	1962	1:20000
Lakewood sand, 0 to 5 percent sand	LasB	10223	745846	t13k	nj001	1975	1:24000
Lakewood sand, 5 to 10 percent sand	LasC	518	745847	t13l	nj001	1975	1:24000
Lakewood sand, 0 to 5 percent slopes	LasB	20144	697799	rf3n	nj005	1967	1:24000
Lakewood sand, loamy substratum, 0 to 5 percent slopes	LashB	9536	697803	rf3s	nj005	1967	1:24000
Lakehurst-Lakewood sands, 0 to 5 percent slopes	LanB	5798	697797	rf3l	nj005	1967	1:24000
Lakewood fine sand, 0 to 5 percent slopes	LatB	3647	697804	rf3t	nj005	1967	1:24000
Lakewood sand, thick surface, 0 to 5 percent slopes	LasfB	2553	697802	rf3r	nj005	1967	1:24000
Lakewood sand, 5 to 10 percent slopes	LasC	2296	697800	rf3p	nj005	1967	1:24000
Lakewood fine sand, loamy substratum, 0 to 5 percent slopes	LathB	1384	697806	rf3w	nj005	1967	1:24000
Lakehurst-Lakewood sands, loamy substrata, 0 to 5 percent slopes	LanhB	1331	697798	rf3m	nj005	1967	1:24000
Lakewood sand, 10 to 15 percent slopes	LasD	301	697801	rf3q	nj005	1967	1:24000
Lakewood fine sand, 5 to 10 percent slopes	LatC	112	697805	rf3v	nj005	1967	1:24000
Lakewood sand, 0 to 5 percent slopes	LasB	3692	710877	rvqj	nj007	1964	1:12000
Lakehurst-Lakewood sands, 0 to 5 percent slopes	LanB	3183	710876	rvqh	nj007	1964	1:12000
Lakewood fine sand, 0 to 5 percent slopes	LatB	2454	710879	rvql	nj007	1964	1:12000
Lakewood sand, 5 to 10 percent slopes	LasC	1032	710878	rvqk	nj007	1964	1:12000
Lakewood fine sand, 5 to 10 percent slopes	LatC	184	710880	rvqm	nj007	1964	1:12000
Lakewood fine sand, 10 to 25 percent slopes	LatD	88	710881	rvqn	nj007	1964	1:12000
Lakewood sand, 0 to 5 percent slopes	LasB	2080	135841	4kbz	nj011	2003	1:24000
Lakewood-Quakerbridge complex, 0 to 5 percent slopes	LatvB	1402	1089500	15kq5	nj015	2004	1:24000
Lakewood sand, 0 to 5 percent slopes	LasB	985	1089498	15kq3	nj015	2004	1:24000
Lakewood sand, 5 to 10 percent slopes	LasC	424	135402	4jwt	nj023	1985	1:24000
Lakewood sand, 0 to 5 percent slopes	LasB	3	606508	nc3s	nj023	1985	1:24000
Lakewood sand, 0 to 5 percent slopes	LasB	8309	134797	4j89	nj025	1985	1:24000
Lakewood sand, 5 to 10 percent slopes	LasC	1232	134798	4j8b	nj025	1985	1:24000
Lakewood sand, 0 to 5 percent slopes	LasB	39801	697532	rdv1	nj029	1978	1:24000
Lakewood sand, 5 to 10 percent slopes	LasC	5223	697533	rdv2	nj029	1978	1:24000
Lakewood sand, thick surface, 0 to 5 percent slopes	LasfB	145	697616	rdxr	nj029	1978	1:24000
Lakewood sand, loamy substratum, 0 to 5 percent slopes	LashB	17	697602	rdx9	nj029	1978	1:24000

Map of Series Extent

Approximate geographic distribution of the LAKEWOOD 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).