Soil Data Explorer - HORNELL

Official Series Description

Lab Data Summary

Aggregate lab data for the HORNELL soil series. This aggregation is based on all pedons with a current taxon name of HORNELL, 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 HORNELL 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
n/a	TR-010	1955-OH155-010	Hornell	3	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	n/a
n/a	AB-119	1963-OH007-119	Hornell	4	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	n/a
n/a	CY-005	1976-OH035-005	Hornell	4	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	n/a
n/a	ER-041	1989-OH043-041	Hornell	4	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 HORNELL 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 HORNELL 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 HORNELL 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 HORNELL 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 HORNELL 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 HORNELL 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 HORNELL 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 HORNELL, 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. NY-2012-02-15-07 | Chautauqua County - August 1994

   Soils and parent material on a bedrock escarpment and on a lake plain that includes the Beach Ridge (Soil Survey of Chautauqua County, New York; August 1994).

2. NY-2012-02-15-21 | Genesee County - March 1969

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

3. NY-2012-02-16-03 | Wyoming County - April 1974

   Typical pattern of soils in association 7 (Soil Survey of Wyoming County, New York; April 1974).

4. OH-2010-09-29-02 | Ashtabula County - 2007

   Representative pattern of soils and parent materials in the Conneaut-Painesville-Elnora association (Soil Survey of Ashtabula County, Ohio; 2007).

5. OH-2012-02-16-12 | Ashtabula County - May 1973

   Soil pattern in the Conneaut-Swanton-Claverack soil association (Soil Survey of Ashtabula County, Ohio; May 1973).

Map Units

Map units containing HORNELL 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
Hornell silt loam, 3 to 8 percent slopes	HnB	993	288734	9pg0	ny001	1985	1:15840
Hornell silt loam, 8 to 15 percent slopes	HnC	297	288735	9pg1	ny001	1985	1:15840
Hornell silt loam, 0 to 3 percent slopes	HnA	230	288733	9pfz	ny001	1985	1:15840
Hornell silt loam, 15 to 25 percent slopes	78D	1463	299982	b24v	ny003	2013	1:24000
Hornell silt loam, 8 to 15 percent slopes	78C	1290	299981	b24t	ny003	2013	1:24000
Hornell silt loam, 3 to 8 percent slopes	78B	519	299980	b24s	ny003	2013	1:24000
Hornell silt loam, 25 to 35 percent slopes	78E	402	299983	b24w	ny003	2013	1:24000
Hornell silt loam, 0 to 3 percent slopes	78A	175	299979	b24r	ny003	2013	1:24000
Hornell silt loam, 3 to 8 percent slopes	78B	1311	289703	9qg8	ny009	2002	1:24000
Hornell silt loam, 0 to 3 percent slopes	78A	1194	289702	9qg7	ny009	2002	1:24000
Hornell silt loam, 8 to 15 percent slopes	78C	633	289704	9qg9	ny009	2002	1:24000
Hornell silt loam, 15 to 25 percent slopes	78D	501	289705	9qgb	ny009	2002	1:24000
Hornell and Hudson soils, 35 to 50 percent slopes	78F	494	289707	9qgd	ny009	2002	1:24000
Hornell silt loam, 3 to 8 percent slopes	HrB	6039	289843	9qls	ny013	1988	1:15840
Hornell silt loam, 0 to 3 percent slopes	HrA	3171	289842	9qlr	ny013	1988	1:15840
Hornell silt loam, 8 to 15 percent slopes	HrC	2225	289844	9qlt	ny013	1988	1:15840
Hornell silt loam, 15 to 25 percent slopes	HrD	818	289845	9qlv	ny013	1988	1:15840
Hornell silt loam, 3 to 8 percent slopes	HrB	2436	290823	9rmd	ny029	1979	1:15840
Hornell silt loam, 0 to 3 percent slopes	HrA	1566	290822	9rmc	ny029	1979	1:15840
Hornell silty clay loam, 8 to 15 percent slopes	HsC	951	290824	9rmf	ny029	1979	1:15840
Hornell silty clay loam, 3 to 8 percent slopes, eroded	HoB3	1609	301717	b3yt	ny037	2004	1:24000
Hornell silty clay loam, 8 to 15 percent slopes, eroded	HoC3	520	301718	b3yv	ny037	2004	1:24000
Hornell and Fremont soils, 15 to 25 percent slopes, eroded	HsD3	240	301719	2vzrq	ny037	2004	1:24000
Hornell silt loam, 3 to 8 percent slopes	HtB	4187	2518339	9sx8	ny043	2018	1:24000
Hornell silt loam, 8 to 15 percent slopes	HtC	1903	2518340	9sx9	ny043	2018	1:24000
Hornell silt loam, 0 to 3 percent slopes	HtA	707	2518338	9sx7	ny043	2018	1:24000
Hornell silt loam, 3 to 8 percent slopes	78B	329	3112869	2yfw5	ny051	2019	1:24000
Hornell silt loam, 15 to 25 percent slopes	78D	282	3112871	2yfw7	ny051	2019	1:24000
Hornell silt loam, 8 to 15 percent slopes	78C	168	3112870	2yfw6	ny051	2019	1:24000
Hornell silt loam, 3 to 8 percent slopes	HoB	2223	292825	9tpz	ny057	1973	1:24000
Hornell silt loam, 0 to 3 percent slopes	HoA	22	292824	9tpy	ny057	1973	1:24000
Hornell silt loam, 8 to 15 percent slopes	HoC	11	292826	9tq0	ny057	1973	1:24000
Mosherville-Hornell complex, undulating	MxB	5374	294400	9wbs	ny091	1993	1:24000
Hornell silt loam, 3 to 8 percent slopes	HoB	4523	309582	bd4j	ny093	1973	1:15840
Hornell silt loam, 8 to 15 percent slopes	HoC	966	309583	bd4k	ny093	1973	1:15840
Hornell silt loam, 0 to 3 percent slopes	HoA	516	309581	bd4h	ny093	1973	1:15840
Hornell channery silt loam, 8 to 15 percent slopes	HnC	627	294615	9wkq	ny097	1976	1:15840
Hornell channery silt loam, 15 to 25 percent slopes	HnD	576	294616	9wkr	ny097	1976	1:15840
Hornell channery silt loam, 3 to 8 percent slopes	HnB	99	294614	9wkp	ny097	1976	1:15840
Hornell and Fremont silt loams, 20 to 50 percent slopes	HHE	14543	294809	2vzrr	ny101	1972	1:15840
Hornell-Fremont silt loams, 6 to 12 percent slopes	HfC	14140	294807	2vzrf	ny101	1972	1:15840
Hornell and Fremont silt loams, 12 to 20 percent slopes	HgD	11722	294808	2vzrm	ny101	1972	1:15840
Hornell-Fremont silt loams, 1 to 6 percent slopes	HfB	6163	294806	2vzr8	ny101	1972	1:15840
Hornell and Fremont silty clay loams, 6 to 20 percent slopes, severely eroded	HkD3	810	294810	2vzrg	ny101	1972	1:15840
Hornell silt loam, 3 to 8 percent slopes	HlB	2241	295364	9xbw	ny121	1969	1:20000
Fremont and Hornell soils, 15 to 25 percent slopes	FtD	1016	295354	2vzrp	ny121	1969	1:20000
Hornell silt loam, 8 to 15 percent slopes	HlC	768	295365	9xbx	ny121	1969	1:20000
Hornell silt loam, 0 to 3 percent slopes	HlA	363	295363	9xbv	ny121	1969	1:20000
Fremont and Hornell soils, 25 to 40 percent slopes	FtE	332	295355	2vzrs	ny121	1969	1:20000
Hornell silt loam, 0 to 2 percent slopes	HoA	3221	298900	b10y	oh007	2001	1:12000
Darien-Hornell silt loams, 2 to 6 percent slopes	DhB	982	298887	b10j	oh007	2001	1:12000
Hornell silt loam, 2 to 6 percent slopes	HoB	614	298901	b10z	oh007	2001	1:12000
Hornell-Urban land complex, rolling	HsC	3128	287314	9mz6	oh035	1978	1:15840
Hornell silt loam, 2 to 6 percent slopes	HrB	1762	287311	9mz3	oh035	1978	1:15840
Hornell silt loam, 6 to 12 percent slopes	HrC	1113	287312	9mz4	oh035	1978	1:15840
Hornell silt loam, 12 to 18 percent slopes	HrD	647	287313	9mz5	oh035	1978	1:15840
Hornell silty clay loam, 0 to 2 percent slopes	HsA	3864	172148	5s45	oh043	1998	1:12000
Hornell silt loam, 2 to 6 percent slopes	HrB	240	172147	5s44	oh043	1998	1:12000
Hornell loam, 2 to 6 percent slopes	HpB	147	172146	5s43	oh043	1998	1:12000
Darien-Hornell silt loams complex, 2 to 6 percent slopes	DsB	55	300201	b2cx	oh055	1979	1:15840
Hornell silty clay loam, 0 to 2 percent slopes	HrA	27	1605975	1qx4n	oh077	1988	1:15840
Hornell silt loam, 0 to 2 percent slopes	HrA	427	286855	9mhd	oh085	1976	1:15840
Darien-Hornell silt loams, 2 to 6 percent slopes	DhB	6	1651019	1sf0p	oh085	1976	1:15840
Hornell silt loam, 2 to 6 percent slopes	HrB	4	286854	9mhc	oh085	1976	1:15840
Hornell silt loam, 0 to 2 percent slopes	HzA	367	287770	9nfx	oh093	1972	1:15840
Hornell silt loam, 2 to 6 percent slopes	HzB	299	287771	9nfy	oh093	1972	1:15840
Hornell silt loam, 2 to 6 percent slopes	HoB	599	816775	wdxl	oh099	1966	1:15840
Hornell silt loam, 2 to 6 percent slopes	HzB	4	1412546	1jdw0	oh103	1974	1:15840
Hornell silt loam, 3 to 8 percent slopes	HrB	107	288462	9p57	oh133	1973	1:15840
Hornell silt loam, 2 to 6 percent slopes	HnB	13	2633105	2rg8l	pa049	2012	1:12000
Hornell silt loam, 0 to 2 percent slopes	HnA	7	2633104	2rg8k	pa049	2012	1:12000

Map of Series Extent

Approximate geographic distribution of the HORNELL 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).