Soil Data Explorer - WASEPI

Official Series Description

Lab Data Summary

Aggregate lab data for the WASEPI soil series. This aggregation is based on all pedons with a current taxon name of WASEPI, 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 WASEPI 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
98	86P0922	86MI037001	Wasepi	6	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	42.958889,-84.5916672

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the WASEPI 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 WASEPI 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 WASEPI 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 WASEPI 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 WASEPI 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 WASEPI 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 WASEPI 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 WASEPI, 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. MI-2012-02-06-33 | Kent County - April 1986

   Pattern of soils and underlying material in the Plainfield-Oshtemo-Spinks association (Soil Survey of Kent County, Michigan; April 1986).

Map Units

Map units containing WASEPI 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
Wasepi sandy loam, 0 to 3 percent slopes	WbA	9034	186408	67z5	mi037	1974	1:15840
Wasepi sandy loam, 2 to 6 percent slopes	WeB	32	2437905	2mtv3	mi037	1974	1:15840
Wasepi sandy loam, 0 to 3 percent slopes	WaA	5828	186259	67tc	mi045	1974	1:15840
Wasepi sandy loam, bedrock variant, 0 to 3 percent slopes	WbA	537	186260	67td	mi045	1974	1:15840
Wasepi sandy loam, 0 to 2 percent slopes	WeA	2253	186908	68h9	mi049	1967	1:20000
Wasepi sandy loam, loamy substratum, 0 to 2 percent slopes	WpA	1175	186909	68hb	mi049	1967	1:20000
Fabius-Wasepi sandy loams, 0 to 2 percent slopes	FaA	2	2410027	2lwtt	mi049	1967	1:20000
Wasepi loamy sand, loamy substratum, 0 to 2 percent slopes	40A	4092	186790	68ch	mi063	1978	1:20000
Wasepi sandy loam, 0 to 2 percent slopes	WeA	1	2437776	2mtpy	mi065	1977	1:15840
Wasepi-Brady loamy sands, 0 to 2 percent slopes	WrA	558	188216	69vh	mi067	1965	1:15840
Wasepi-Brady loamy sands, 2 to 6 percent slopes	WrB	374	188217	69vj	mi067	1965	1:15840
Wasepi sandy loam, 0 to 2 percent slopes	WeA	356	188214	69vf	mi067	1965	1:15840
Wasepi sandy loam, 2 to 6 percent slopes	WeB	321	188215	69vg	mi067	1965	1:15840
Wasepi-Brady sandy loams, 0 to 2 percent slopes	WsA	156	188218	69vk	mi067	1965	1:15840
Wasepi-Brady sandy loams, 2 to 6 percent slopes	WsB	135	188219	69vl	mi067	1965	1:15840
Wasepi loamy sand, 0 to 3 percent slopes	16A	4159	186605	685j	mi073	1983	1:15840
Wasepi loamy sand, 0 to 4 percent slopes	27B	5306	187122	68q6	mi081	1984	1:15840
Fabius-Wasepi sandy loams, 0 to 2 percent slopes	FaA	5411	192019	6ft5	mi087	1966	1:15840
Fabius-Wasepi sandy loams, 2 to 6 percent slopes	FaB	1583	192020	6ft6	mi087	1966	1:15840
Wasepi loamy sand, 2 to 6 percent slopes	WsB	1193	192168	6fyz	mi087	1966	1:15840
Wasepi loamy sand, 0 to 2 percent slopes	WsA	829	192167	6fyy	mi087	1966	1:15840
Wasepi sandy loam, 0 to 3 percent slopes	WdA	129	2508514	692h	mi087	1966	1:15840
Wasepi sandy loam, 0 to 2 percent slopes	WeA	4	2409837	2lwmp	mi087	1966	1:15840
Wasepi sandy loam, 0 to 2 percent slopes	WeA	3187	187611	696z	mi093	1968	1:20000
Wasepi sandy loam, 0 to 2 percent slopes	WtA	4438	187698	699s	mi099	1967	1:20000
Wasepi sandy loam, silty subsoil variant, 0 to 4 percent slopes	WuB	2354	187699	699t	mi099	1967	1:20000
Wasepi loamy sand, 0 to 2 percent slopes	WsA	2311	187696	699q	mi099	1967	1:20000
Wasepi-Pipestone complex, 0 to 4 percent slopes	WvB	1135	2673710	2qz6c	mi099	1967	1:20000
Wasepi loamy sand, 2 to 6 percent slopes	WsB	312	187697	699r	mi099	1967	1:20000
Wasepi sandy loam, 0 to 3 percent slopes	WrA	52	2508670	6bh0	mi099	1967	1:20000
Wasepi sandy loam, clay subsoil variant, 0 to 3 percent slopes	WwA	29	2508671	6928	mi099	1967	1:20000
Wasepi-Boyer complex, loamy substratum, 0 to 6 percent slopes	WpB	15	2508669	6927	mi099	1967	1:20000
Wasepi sandy loam, loamy substratum, 0 to 3 percent slopes	44A	1052	187251	68vc	mi115	1980	1:15840
Wasepi sandy loam, 0 to 4 percent slopes	105A	213	2509164	6fgg	mi115	1980	1:15840
Wasepi sandy loam, 0 to 3 percent slopes	17A	5072	188821	6bh0	mi125	1980	1:15840
Wasepi sandy loam, 0 to 2 percent slopes	120A	5	2438227	2mv5h	mi125	1980	1:15840
Wasepi loamy sand, 0 to 2 percent slopes	130A	4	2508683	699q	mi125	1980	1:15840
Wasepi sandy loam, 0 to 2 percent slopes	WsA	1056	192748	6gkp	mi139	1967	1:15840
Wasepi sandy loam, 0 to 3 percent slopes	152A	44	2673617	692h	mi145	1991	1:15840
Wasepi sandy loam, loamy substratum, 0 to 2 percent slopes	127A	31	2399539	2ljxh	mi145	1991	1:15840
Wasepi sandy loam, 0 to 2 percent slopes	126A	27	2399544	2ljxn	mi145	1991	1:15840
Wasepi sandy loam, 0 to 2 percent slopes	WoA	3373	187463	6926	mi147	1969	1:20000
Wasepi-Boyer complex, loamy substratum, 0 to 6 percent slopes	WpB	3123	187464	6927	mi147	1969	1:20000
Wasepi sandy loam, clay subsoil variant, 0 to 3 percent slopes	WsA	2496	187465	6928	mi147	1969	1:20000
Wasepi sandy loam, silty subsoil variant, 0 to 4 percent slopes	WuB	27	2508391	699t	mi147	1969	1:20000
Wasepi-Boyer complex, loamy substratum, 0 to 6 percent slopes	WpB	47	2508321	6927	mi151	1955	1:15840
Wasepi loamy sand, loamy substratum, 0 to 2 percent slopes	WsA	29	2508323	68ch	mi151	1955	1:15840
Wasepi sandy loam, 0 to 3 percent slopes	WrA	11	2508322	692h	mi151	1955	1:15840
Wasepi sandy loam, clay subsoil variant, 0 to 3 percent slopes	WtA	5	2508324	6928	mi151	1955	1:15840
Wasepi loamy sand, 0 to 2 percent slopes	WgA	2	2508317	6fyy	mi151	1955	1:15840
Fabius-Wasepi sandy loams, 0 to 2 percent slopes	FaA	1	2508267	6ft5	mi151	1955	1:15840
Wasepi sandy loam, 0 to 2 percent slopes	WeA	5634	187859	69gz	mi155	1967	1:12000
Wasepi sandy loam, 2 to 6 percent slopes	WeB	2978	187860	69h0	mi155	1967	1:12000
Wasepi sandy loam, 0 to 3 percent slopes	WbA	92	2394501	2lcnz	mi155	1967	1:12000
Wasepi sandy loam, loamy substratum, 0 to 2 percent slopes	WpA	7	2399243	2ljly	mi155	1967	1:12000
Wasepi sandy loam, 0 to 3 percent slopes	19A	13332	187472	692h	mi157	1984	1:15840
Wasepi loamy sand, loamy substratum, 0 to 2 percent slopes	129A	15	2508127	68ch	mi157	1984	1:15840
Wasepi sandy loam, 0 to 4 percent slopes	WaA	11125	191687	6fgg	mi161	1974	1:20000
Wasepi sandy loam, loamy substratum, 0 to 3 percent slopes	WbA	35	2508722	68vc	mi161	1974	1:20000
Wasepi sandy loam, 0 to 4 percent slopes	WdA	5582	3015105	6fgg	mi163	1974	1:12000
Wasepi loamy sand, 0 to 2 percent slopes	WaA	3577	3015074	6bl9	mi163	1974	1:12000
Wasepi loamy sand, loamy substratum, 0 to 2 percent slopes	WeA	2136	3015075	6blb	mi163	1974	1:12000
Wasepi sandy loam, 0 to 3 percent slopes	WcA	3	3015104	6bh0	mi163	1974	1:12000
Wasepi sandy loam, 0 to 3 percent slopes	WaA	583	3268516	g624	wi015	2023	1:15840
Wasepi fine sandy loam, 0 to 3 percent slopes	WcA	993	423380	g6kf	wi021	1972	1:15840
Wasepi sandy loam, 0 to 3 percent slopes	WmA	3692	423842	g71b	wi055	1976	1:15840
Wasepi sandy loam, clayey substratum, 1 to 3 percent slopes	WnA	1773	3268731	g7bh	wi059	2023	1:15840
Wasepi sandy loam, 1 to 3 percent slopes	WmA	189	3268730	g7bg	wi059	2023	1:15840
Wasepi sandy loam, 0 to 3 percent slopes	WaA	4742	3268559	g624	wi071	2023	1:15840
Wasepi sandy loam, 1 to 3 percent slopes	WmA	5	3403377	g970	wi079	2023	1:15840
Wasepi sandy loam, 1 to 3 percent slopes	WmA	354	426025	g99r	wi089	1967	1:15840
Wasepi sandy loam, 1 to 3 percent slopes	WmA	37	3268803	g7bg	wi101	2023	1:15840
Wasepi sandy loam, clayey substratum, 1 to 3 percent slopes	WnA	11	3268829	g7bh	wi101	2023	1:15840
Wasepi sandy loam	Wa	676	423939	g74g	wi117	1974	1:15840
Wasepi sandy loam, 1 to 3 percent slopes	WmA	664	425792	g927	wi131	1967	1:15840
Wasepi sandy loam, 1 to 3 percent slopes	WmA	641	3403481	g970	wi133	2023	1:15840

Map of Series Extent

Approximate geographic distribution of the WASEPI 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).