Soil Data Explorer - HAZEL

Official Series Description

Lab Data Summary

Aggregate lab data for the HAZEL soil series. This aggregation is based on all pedons with a current taxon name of HAZEL, 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 HAZEL 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
148	00P1094	S2000VA047012	Hazel	3	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	38.524589,-78.011525

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the HAZEL 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 HAZEL 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 HAZEL 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 HAZEL 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 flats position figure.

Competing Series

Soil series competing with HAZEL 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 HAZEL 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).

Geomorphic description summaries for the HAZEL 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 3D terrace figure.

There are insufficient data to create the 3D flats position figure.

Soil series sharing subgroup-level classification with HAZEL, 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

No block diagrams are available.

Map Units

Map units containing HAZEL 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
Weverton-Hazel complex, 15 to 25 percent slopes, very stony	WeD	2439	535094	kyt3	md021	2001	1:12000
Weverton-Hazel complex, 8 to 15 percent slopes, very stony	WeC	1885	535093	kyt2	md021	2001	1:12000
Weverton-Hazel complex, 25 to 45 percent slopes, very stony	WeE	1810	535095	kyt4	md021	2001	1:12000
Hazel channery silt loam, 8 to 15 percent slopes	HnC	1591	534420	ky3c	md043	1998	1:12000
Hazel channery silt loam, 15 to 25 percent slopes	HnD	1092	534423	ky3g	md043	1998	1:12000
Hazel-Rock outcrop complex, 25 to 45 percent slopes	HrE	1030	534439	ky3z	md043	1998	1:12000
Hazel channery silt loam, 3 to 8 percent slopes	HnB	797	534418	ky39	md043	1998	1:12000
Hazel loam, 15 to 25 percent slopes	39D	4550	516370	kbb3	va003	1981	1:15840
Hazel loam, 25 to 45 percent slopes	39E	4530	516371	2yfh2	va003	1981	1:15840
Hazel loam, 25 to 45 percent slopes, very stony	40E	3710	516376	2xxy9	va003	1981	1:15840
Hazel loam, 15 to 25 percent slopes, very stony	40D	910	516375	2xxy8	va003	1981	1:15840
Hazel loam, 7 to 15 percent slopes	39C	770	516369	kbb2	va003	1981	1:15840
Hazel complex, steep	HnE	4690	519229	kf9b	va035	1965	1:15840
Hazel channery complex, steep	HmE	2536	519226	kf97	va035	1965	1:15840
Hazel channery complex, very steep	HmF	1461	519227	kf98	va035	1965	1:15840
Hazel complex, sloping	HnC	1028	519228	kf99	va035	1965	1:15840
Hazel sandy loam, 15 to 25 percent slopes, rocky	25D	6789	1895276	21m5y	va061	2006	1:12000
Hazel-Edgemont complex, 7 to 15 percent slopes, rocky	25C	4831	1895275	21m5x	va061	2006	1:12000
Hazel sandy loam, 25 to 45 percent slopes, very stony	125E	2246	1895421	21mbm	va061	2006	1:12000
Hazel sandy loam, 15 to 25 percent slopes, very stony	125D	1596	1895420	21mbl	va061	2006	1:12000
Hazel sandy loam, 7 to 15 percent slopes, very stony	125C	332	1895419	21mbk	va061	2006	1:12000
Hazel sandy loam, 25 to 45 percent slopes, rocky	25E	326	1895277	21m5z	va061	2006	1:12000
Hazel-Rock outcrop complex, 25 to 45 percent slopes	225E	215	1895434	21mc1	va061	2006	1:12000
Hazel-Rock outcrop complex, 15 to 25 percent slopes	225D	164	1895433	21mc0	va061	2006	1:12000
Hazel loam, 15 to 25 percent slopes	HzD	1135	516895	kbw1	va079	1983	1:15840
Hazel loam, 25 to 45 percent slopes	HzE	313	516896	kbw2	va079	1983	1:15840
Hazel loam, 15 to 25 percent slopes	HaD	6661	517002	kbzh	va113	1967	1:15840
Hazel loam, 25 to 55 percent slopes	HaF	2985	517003	kbzj	va113	1967	1:15840
Hazel loam, 7 to 15 percent slopes	HaC	1208	517001	kbzg	va113	1967	1:15840
Hazel channery loam, 25 to 50 percent slopes	25E	9901	136971	4ljf	va125	1992	1:24000
Hazel loam, 25 to 50 percent slopes, very stony	26E	4043	136978	4ljn	va125	1992	1:24000
Hazel channery loam, 15 to 25 percent slopes	25D	1601	136970	4ljd	va125	1992	1:24000
Hazel loam, 15 to 25 percent slopes, very stony	26D	752	136976	4ljl	va125	1992	1:24000
Hazel channery loam, 7 to 15 percent slopes	25C	217	136969	4ljc	va125	1992	1:24000
Hazel loam, 7 to 15 percent slopes	HaC	1092	119844	40py	va137	1966	1:15840
Hazel loam, 15 to 30 percent slopes	HaD	834	119845	40pz	va137	1966	1:15840
Hazel loam, moderately steep phase	HeD	2357	517437	kcfj	va157	1958	1:20000
Hazel loam, sloping phase	HeC	1135	517436	kcfh	va157	1958	1:20000
Hazel loam, steep phase	HeE	722	517438	kcfk	va157	1958	1:20000
Hazel stony loam, steep phase	HsE	641	517440	kcfm	va157	1958	1:20000
Hazel stony loam, moderately steep phase	HsD	416	517439	kcfl	va157	1958	1:20000
Hazel - Urban land complex, 15 to 25 percent slopes	139D	17	2514316	2qjgy	va540	2011	1:24000
Hazel loam, 15 to 25 percent slopes	39D	6	2496439	kbb3	va540	2011	1:24000
Hazel loam, 25 to 45 percent slopes	39E	6	2496457	2yfh2	va540	2011	1:24000

Map of Series Extent

Approximate geographic distribution of the HAZEL 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).