Soil Data Explorer - WAINOLA

Official Series Description

Lab Data Summary

Aggregate lab data for the WAINOLA soil series. This aggregation is based on all pedons with a current taxon name of WAINOLA, 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 WAINOLA were used in the calculation. Source: KSSL snapshot (updated 2020-03-18). Methods used to assemble the KSSL snapshot used by SoilWeb / SDE

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

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the WAINOLA 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 WAINOLA series. Sketches are arranged according to their subgroup-level taxonomic structure. Source: SSURGO snapshot (updated 2024-02-21), parsed OSD records (updated 2023-10-06) and snapshot of SC database (updated 2023-10-02).

Select annual climate data summaries for the WAINOLA 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 WAINOLA 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 WAINOLA share the same family level classification in Soil Taxonomy. Source: parsed OSD records (updated 2023-10-06) and snapshot of the SC database (updated 2023-10-02).

Select annual climate data summaries for the WAINOLA 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 WAINOLA 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 WAINOLA, 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. MI-2010-09-07-09 | Mackinac County - 1997

   Typical pattern of soils and parent material in the Leafriver-Croswell-Wainola association (Soil Survey of Mackinac County, Michigan; 1997).

2. MI-2012-02-06-36 | Mackinac County - 1997

   Typical pattern of soils and parent material in the Leafriver-Croswell-Wainola association (Soil Survey of Mackinac County, Michigan; 1997).

3. MI-2012-02-06-38 | Menominee County - September 1989

   Typical pattern of soils and parent material in the Deford-Wainola-Rousseau map unit (Soil Survey of Menominee County, Michigan; September 1989).

4. NY-2010-09-28-04 | Clinton County - 2006

   Typical pattern of deltaic sands and associated soils in the Champlain-Adams-Croghan general soil map unit (Soil Survey of Clinton County, New York; 2006).

5. NY-2010-09-28-31 | Akwesasne Territory: St. Regis Mohawk Reservation - 2005

   One of three major rivers flows through Akwesasne. The Raquetter River sliced through glacial till ridges (consisting of Grenville, Hogansburg, and Malone soils) and deposited fine-grained sands at varying depths over silt, clay, or loamy till. The silt and clay sediments of Adjidaumo and Muskellunge soils are remnants of proglacial lake and marine environments (Soil Survey of Akwesasne Territory; St. Regis Mohawk Reservation; 2005).

6. WI-2012-03-23-18 | Marinette County - February 1991

   Pattern of soils and parent material in the Wainola-Deford association (Soil Survey of Marinette County, WI; 1991).

Map Units

Map units containing WAINOLA 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
Wainola loamy fine sand, 0 to 2 percent slopes	WaA	607	189297	6bzc	mi011	1964	1:20000
Wainola loamy fine sand, 2 to 6 percent slopes	WaB	171	189298	6bzd	mi011	1964	1:20000
Wainola-Kinross-Rousseau complex, 0 to 35 percent slopes	48E	14871	415157	fy05	mi033	1989	1:15840
Kinross-Wainola complex, 0 to 3 percent slopes	137A	9803	415093	fxy3	mi033	1989	1:15840
Wainola fine sand, 0 to 3 percent slopes	49A	4436	415158	2zytr	mi033	1989	1:15840
Dawson-Deer Park-Wainola complex, 0 to 50 percent slopes	154F	2662	415112	fxyq	mi033	1989	1:15840
Wainola fine sand, 0 to 3 percent slopes	49A	1646	1588125	2zytr	mi041	1969	1:24000
Wainola loamy fine sand, outwash plain, 0 to 3 percent slopes	985A	2557	3340046	2zyts	mi043	1985	1:20000
Wainola fine sand, 0 to 3 percent slopes	47A	54	415222	fy28	mi043	1985	1:20000
Wainola loamy fine sand, 0 to 6 percent slopes	WaB	780	189378	6c1z	mi047	1968	1:20000
Wainola-Deford association	WD	1419	189865	6ckp	mi051	1966	1:15840
Wainola-Trap Falls complex, 0 to 3 percent slopes	293A	37	1456172	1kw89	mi053	2007	1:24000
Manido-Wainola complex, 0 to 4 percent slopes	8235B	1314	2485004	2pdvf	mi061	1989	1:20000
Wainola-Ingalls-Liminga complex, terrace, 1 to 55 percent slopes	8152F	196	2484793	2pdmm	mi061	1989	1:20000
Wainola fine sand, 0 to 2 percent slopes	8153A	144	2484794	2pdmn	mi061	1989	1:20000
Leafriver-Croswell-Wainola complex, 0 to 6 percent slopes	172B	15854	416349	fz7m	mi097	1994	1:20000
Wainola-Leafriver-Pullup complex, 0 to 35 percent slopes	48E	2446	416408	fz9j	mi097	1994	1:20000
Wainola fine sand, 0 to 3 percent slopes	49A	2212	416409	2zytr	mi097	1994	1:20000
Croswell-Wainola complex, 0 to 6 percent slopes	88B	1752	416430	fzb7	mi097	1994	1:20000
Wainola-Deford fine sands, 0 to 2 percent slopes	WdA	24	2508668	6924	mi099	1967	1:20000
Wainola loamy fine sand, 0 to 2 percent slopes	WaA	1	2508667	6923	mi099	1967	1:20000
Deford-Wainola-Rousseau complex, 0 to 12 percent slopes	45C	35413	415481	fybm	mi109	1985	1:20000
Wainola fine sand, 0 to 3 percent slopes	49A	4615	3340048	2zytr	mi109	1985	1:20000
Wainola fine sand, 0 to 3 percent slopes	22A	1213	415460	fy9y	mi109	1985	1:20000
Wainola-Deford association	WD	34	2673566	6ckp	mi111	1976	1:15840
Manido-Wainola complex, 0 to 4 percent slopes	8235B	851	1674872	1t6v4	mi131	2007	1:24000
Wainola fine sand, 0 to 2 percent slopes	8153A	708	1674843	1t6t6	mi131	2007	1:24000
Wainola-Trap Falls complex, 0 to 3 percent slopes	8293A	456	1674898	1t6vz	mi131	2007	1:24000
Wainola-Ingalls-Liminga complex, terrace, 1 to 55 percent slopes	8152F	12	1674842	1t6t5	mi131	2007	1:24000
Wainola-Deford fine sands, 0 to 2 percent slopes	WdA	25418	187461	6924	mi147	1969	1:20000
Wainola-Tobico complex, 0 to 3 percent slopes	WnA	3250	187462	6925	mi147	1969	1:20000
Wainola loamy fine sand, 0 to 2 percent slopes	WaA	451	187460	6923	mi147	1969	1:20000
Wainola-Deford fine sands, 0 to 2 percent slopes	WfA	25	2508316	6924	mi151	1955	1:15840
Neconish-Kinross-Wainola complex, 0 to 6 percent slopes	525B	8560	1457046	1kx5h	mi153	2007	1:24000
Neconish-Deford, rarely flooded-Wainola complex, 0 to 6 percent slopes	491B	2490	1611820	1r376	mi153	2007	1:24000
Deer Park-Dawson-Wainola complex, 0 to 60 percent slopes	80F	995	1610311	1r1nj	mi153	2007	1:24000
Wainola loamy fine sand	Wn	4559	290254	9r11	ny019	1995	1:24000
Wainola loamy fine sand	33	73	296054	9y24	ny689	1999	1:24000
Wainola loamy fine sand	Wa	2254	422284	g5f2	wi029	1975	1:15840
Wainola loamy fine sand, 0 to 3 percent slopes	WaA	1102	422360	g5hj	wi061	1978	1:15840
Wainola fine sand, 0 to 3 percent slopes	49A	18179	3340049	2zytr	wi075	1987	1:20000
Wainola loamy fine sand, outwash plain, 0 to 3 percent slopes	985A	2821	3340050	2zyts	wi075	1987	1:20000
Wainola loamy fine sand, 0 to 3 percent slopes	WaA	1440	422456	g5lm	wi075	1987	1:20000
Wainola loamy fine sand, outwash plain, 0 to 3 percent slopes	985A	390	395876	2zyts	wi078	1998	1:12000
Wainola loamy fine sand, 0 to 3 percent slopes	WaA	12200	422522	g5nr	wi083	1985	1:15840
Wainola loamy fine sand, outwash plain, 0 to 3 percent slopes	985A	9056	3340053	2zyts	wi083	1985	1:15840
Wainola fine sand, 0 to 3 percent slopes	49A	7709	3340052	2zytr	wi083	1985	1:15840
Wainola loamy fine sand, 0 to 3 percent slopes	WaA	12199	422606	g5rg	wi087	1975	1:15840
Wainola fine sand, 0 to 3 percent slopes	WaA	6228	422646	g5sr	wi115	1981	1:15840
Wainola loamy fine sand, outwash plain, 0 to 3 percent slopes	985A	2977	3340054	2zyts	wi115	1981	1:15840
Wainola loamy fine sand	Wa	4375	422758	g5xc	wi135	1982	1:15840

Map of Series Extent

Approximate geographic distribution of the WAINOLA 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).