Soil Data Explorer - WAYLAND

Official Series Description

Lab Data Summary

Aggregate lab data for the WAYLAND soil series. This aggregation is based on all pedons with a current taxon name of WAYLAND, 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 WAYLAND 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.

Pedons used in the lab summary:

MLRA	Lab ID	Pedon ID	Taxonname	CI	NSSL / NASIS Reports	Link To SoilWeb GMap
140	04N0374	S03NY003014	Wayland	6	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	42.0455551,-77.9341354
n/a	AB-070	1955-OH007-070	Wayland	2	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	n/a
n/a	CO-115	1959-OH029-115	Wayland	3	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	n/a
n/a	CO-130	1960-OH029-130	Wayland	3	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	n/a
n/a	MH-043	1964-OH099-043	Wayland	3	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 WAYLAND 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 WAYLAND 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 WAYLAND 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 WAYLAND 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).

Competing Series

Soil series competing with WAYLAND 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 WAYLAND 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 WAYLAND 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 WAYLAND, 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. NY-2010-09-28-24 | Otsego County - 2006

   The relationship between the soils and underlying material in the Wayland-Canadaigua-Raynham general soil map unit and the Otego-Chenango-Scio general soil map unit (Soil Survey of Otsego County, New York; 2006).

2. NY-2012-02-15-22 | Genesee County - March 1969

   Cross section showing typical soil pattern in the Palmyra association (Soil Survey of Genesee County, New York; March 1969).

3. NY-2012-02-16-06 | Wyoming County - April 1974

   Typical pattern of soils in association 13 (Soil Survey of Wyoming County, New York; April 1974).

4. OH-2012-02-16-17 | Columbiana County - February 1968

   A schematic drawing showing the relationship of soils on the Wisconsin glacial outwash plain (in the valley to the right) and on the Wisconsin till plain (Soil Survey of Columbiana County, Ohio; February 1968).

5. PA-2012-03-13-63 | Mercer County - April 1971

   Relationship of soils and underlying material in association 1 (Soil Survey of Mercer County, PA; 1971).

6. PA-2012-03-13-64 | Mercer County - April 1971

   Relationship of soils and underlying material in associations 2 and 3 (Soil Survey of Mercer County, PA; 1971).

7. PA-2012-03-13-70 | Monroe County - August 1981

   Typical pattern of soils and underlying material in the Wyoming-Chenango-Pope map unit (Soil Survey of Monroe County, PA; 1981).

8. PA-2012-03-14-30 | Warren and Forest Counties - October 1985

   Typical landscape and underlying material of the Hazleton-Cookport-Cavode map unit (Soil Survey of Warren and Forest Counties, PA; 1985).

9. PA-2012-03-14-31 | Warren and Forest Counties - October 1985

   Typical landscape and underlying material of the Hanover-Alvira-Shelmadine map unit (Soil Survey of Warren and Forest Counties, PA; 1985).

Map Units

Map units containing WAYLAND 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
Wayland soils complex, non-calcareous substratum, 0 to 3 percent slopes, frequently flooded	Wo	2743	288816	2srgt	ny001	1985	1:15840
Wayland soils complex, 0 to 3 percent slopes, frequently flooded	5A	4419	1859966	2srgv	ny003	2013	1:24000
Wayland soils complex, 0 to 3 percent slopes, frequently flooded	Wd	9481	289220	2srgv	ny007	1966	1:15840
Wayland soils complex, 0 to 3 percent slopes, frequently flooded	5	3361	289623	2srgv	ny009	2002	1:24000
Wayland soils complex, 0 to 3 percent slopes, frequently flooded	Wy	6395	289906	2srgv	ny013	1988	1:15840
Wayland soils complex, non-calcareous substratum, 0 to 3 percent slopes, frequently flooded	Wa	4967	290056	2srgt	ny017	1982	1:15840
Wayland soils complex, non-calcareous substratum, 0 to 3 percent slopes, frequently flooded	5A	4627	2760834	2srgt	ny023	2014	1:12000
Wayland-Natchaug complex, 0 to 2 percent slopes, frequently flooded	6A	1474	2723115	2rwd5	ny023	2014	1:12000
Wayland silt loam	Wy	16557	290731	9rjf	ny027	1992	1:24000
Wayland soils complex, 0 to 3 percent slopes, frequently flooded	Wd	11183	290942	2srgv	ny029	1979	1:15840
Rumney and Wayland fine sandy loams, 0 to 2 percent slopes	Rea	1079	2677530	bmfc	ny033	2018	1:24000
Rumney and Wayland fine sandy loams, high bottoms, 0 to 2 percent slopes	Rfa	220	2677556	bmfd	ny033	2018	1:24000
Wayland soils complex, 0 to 3 percent slopes, frequently flooded	Wy	6195	634210	2srgv	ny037	2004	1:24000
Wayland soils complex, non-calcareous substratum, 0 to 3 percent slopes, frequently flooded	Wa	1602	291745	2srgt	ny039	1985	1:24000
Wayland soils complex, 0 to 3 percent slopes, frequently flooded	Wd	1811	2518405	2srgv	ny043	2018	1:24000
Wayland silt loam	We	2258	291932	9ss5	ny045	1981	1:15840
Wayland-Teel-Palms association, 0 to 3 percent slopes, frequently flooded	9197A	225	964997	11d4y	ny045	1981	1:15840
Wayland silt loam, 0 to 2 percent slopes	WcA	1288	2677807	bmpb	ny049	2018	1:24000
Wayland silty clay loam, 0 to 3 percent slopes, frequently flooded	10A	6550	3105640	2y9v2	ny051	2019	1:24000
Wayland soils complex, non-calcareous substratum, 0 to 3 percent slopes, frequently flooded	5A	362	3100306	2srgt	ny051	2019	1:24000
Wayland soils complex, 0 to 3 percent slopes, frequently flooded	Wn	12298	292653	2srgv	ny053	1975	1:15840
Wayland soils complex, 0 to 3 percent slopes, frequently flooded	Wg	6693	292777	2srgv	ny055	1967	1:15840
Wayland soils complex, 0 to 3 percent slopes, frequently flooded	Wy	1557	292903	2srgv	ny057	1973	1:24000
Wayland soils complex, 0 to 3 percent slopes, frequently flooded	7	7359	293475	2srgv	ny065	1993	1:24000
Wayland soils complex, 0 to 3 percent slopes, frequently flooded	Wn	8236	293673	2srgv	ny067	1973	1:20000
Wayland soils complex, 0 to 3 percent slopes, frequently flooded	5A	6703	2421204	2srgv	ny069	2012	1:12000
Wayland soils complex, non-calcareous substratum, 0 to 3 percent slopes, frequently flooded	Wd	10159	293990	2srgt	ny071	1976	1:15840
Wayland soils complex, 0 to 3 percent slopes, frequently flooded	Wy	1773	294085	2srgv	ny073	1973	1:15840
Wayland soils complex, 0 to 3 percent slopes, frequently flooded	Wg	5578	294316	2srgv	ny077	1993	1:24000
Wayland soils complex, 0 to 3 percent slopes, frequently flooded	Wy	1362	309669	2srgv	ny093	1973	1:15840
Wayland soils complex, non-calcareous substratum, 0 to 3 percent slopes, frequently flooded	Wa	1592	294567	2srgt	ny095	1965	1:15840
Wayland soils complex, non-calcareous substratum, 0 to 3 percent slopes, frequently flooded	Wy	1553	294671	2srgt	ny097	1976	1:15840
Wayland soils complex, non-calcareous substratum, 0 to 3 percent slopes, frequently flooded	Wn	10446	294863	2srgt	ny101	1972	1:15840
Wayland soils complex, non-calcareous substratum, 0 to 3 percent slopes, frequently flooded	Wd	2842	295153	2srgt	ny105	1984	1:15840
Wayland soils complex, 0 to 3 percent slopes, frequently flooded	Ws	8015	295690	2srgv	ny109	1963	1:20000
Wayland soils complex, non-calcareous substratum, 0 to 3 percent slopes, frequently flooded	Wb	2792	295566	2srgt	ny111	1974	1:15840
Wayland mucky silt loam	Wc	963	295567	9xkf	ny111	1974	1:15840
Wayland soils complex, 0 to 3 percent slopes, frequently flooded	Wd	8403	295793	2srgv	ny117	1972	1:15840
Wayland soils complex, 0 to 3 percent slopes, frequently flooded	Wn	2766	295439	2srgv	ny121	1969	1:20000
Wayland soils complex, 0 to 3 percent slopes, frequently flooded	5A	2384	1407903	2srgv	ny123	1948	1:12000
Wayland soils complex, 0 to 3 percent slopes, frequently flooded	Wd	675	289337	2srgv	ny605	1981	1:24000
Wayland soils complex, 0 to 3 percent slopes, frequently flooded	Wa	2511	293058	2srgv	ny664	1968	1:15840
Wayland silt loam	Wc	8239	816833	wdzg	oh099	1966	1:15840
Wayland silt loam	Wd	3062	288098	9nsh	oh151	1967	1:15840
Wayland silt loam	Wd	164	2217049	2df0q	oh169	1981	1:15840
Wayland silty clay loam	Wa	636	3098655	2y180	pa025	1960	1:20000
Wayland silt loam	Wa	1616	296491	9yj7	pa079	1974	1:20000
Wayland silt loam, coarse variant	Wa	21252	296264	9y8x	pa085	1967	1:20000
Wayland silty clay loam	Wb	2343	296369	9yd9	pa089	1975	1:20000
Wayland and Wyalusing soils, 0 to 3 percent slopes, frequently flooded	WaA	2041	2433759	2z5wr	pa105	1953	1:24000
Wayland silty clay loam	Wa	1385	297172	9z76	pa117	1973	1:20000
Wayland silt loam	Wa	17387	539270	l34t	pa609	1979	1:20000

Map of Series Extent

Approximate geographic distribution of the WAYLAND 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).