Soil Data Explorer - HAZELAIR

Official Series Description

Lab Data Summary

Aggregate lab data for the HAZELAIR soil series. This aggregation is based on all pedons with a current taxon name of HAZELAIR, 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 HAZELAIR were used in the calculation. Source: KSSL snapshot (updated 2020-03-18). 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
2	40A5467	S1962OR071013	Hazelair	5	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	45.372776,-123.1577759
2	40A5441	S1962OR071014	Hazelair	6	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	45.3311119,-123.1333313

Water Balance

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

Competing Series

Soil series competing with HAZELAIR 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 HAZELAIR 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 HAZELAIR 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 hills 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 HAZELAIR, 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. OR-2012-05-10-22 | Yamhill County - January 1974

   Pattern of soils of association 7 on terraces and low foothills of the Coast Range (Soil Survey of Yamhill County, Oregon; January 1974).

Map Units

Map units containing HAZELAIR 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
Hazelair silty clay loam, 2 to 12 percent slopes	77	47	85229	2vpb	or003	2004	1:24000
Hazelair silty clay loam, 7 to 20 percent slopes	80	36	618944	ns1y	or003	2004	1:24000
Hazelair silty clay loam, 20 to 30 percent slopes	79	31	85314	2vs2	or003	2004	1:24000
Hazelair silty clay loam, 12 to 20 percent slopes	78	13	85237	2vpl	or003	2004	1:24000
Hazelair silt loam, 3 to 12 percent slopes	29C	3836	62329	22vm	or053	1977	1:20000
Hazelair silt loam, 12 to 20 percent slopes	29D	1881	62330	22vn	or053	1977	1:20000
Hazelair silty clay loam, 2 to 12 percent slopes	2706C	229	2711166	1j8bg	or053	1977	1:20000
Hazelair silt loam, 20 to 30 percent slopes	29E	101	62331	22vp	or053	1977	1:20000
Hazelair silty clay loam, 2 to 12 percent slopes	2706C	720	2711408	1j8bg	or071	1967	1:24000
Hazelair-Witham complex, 2 to 12 percent slopes	2825C	518	2711280	2p8tl	or071	1967	1:24000
Hazelair silty clay loam, 12 to 20 percent slopes	2706D	183	2711330	1j8bh	or071	1967	1:24000
Hazelair-Witham complex, 12 to 20 percent slopes	2825D	31	2731446	2p8tn	or071	1967	1:24000
Hazelair silty clay loam, 20 to 30 percent slopes	2706E	5	2711420	1qkwd	or071	1967	1:24000
Dixonville-Philomath-Hazelair complex, 12 to 35 percent slopes	43E	19947	62680	236y	or637	1981	1:20000
Hazelair silty clay loam, 7 to 20 percent slopes	52D	11413	62693	237c	or637	1981	1:20000
Dixonville-Philomath-Hazelair complex, 3 to 12 percent slopes	43C	10336	62679	236x	or637	1981	1:20000
Hazelair silty clay loam, 2 to 7 percent slopes	52B	5736	62692	237b	or637	1981	1:20000
Urban land-Hazelair-Dixonville complex, 3 to 12 percent slopes	127C	2094	62607	234l	or637	1981	1:20000
Dixonville-Hazelair-Urban land complex, 12 to 35 percent slopes	42E	794	62678	236w	or637	1981	1:20000
Hazelair silty clay loam, 2 to 7 percent slopes	43B	8000	64312	24xl	or639	1983	1:20000
Hazelair silty clay loam, 7 to 20 percent slopes	43D	5715	64313	24xm	or639	1983	1:20000
Dixonville-Philomath-Hazelair complex, 12 to 35 percent slopes	35E	5215	64301	24x7	or639	1983	1:20000
Dixonville-Philomath-Hazelair complex, 3 to 12 percent slopes	35C	3935	64300	24x6	or639	1983	1:20000
Hazelair silt loam, 2 to 6 percent slopes	HaB	755	64091	24pg	or643	1966	1:20000
Hazelair silt loam, 6 to 20 percent slopes	HaD	731	64092	24ph	or643	1966	1:20000
Hazelair silty clay loam, 2 to 15 percent slopes, eroded	HcD2	710	64093	24pj	or643	1966	1:20000

Map of Series Extent

Approximate geographic distribution of the HAZELAIR 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).