Soil Data Explorer - HILLFIELD

Official Series Description

Lab Data Summary

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

Competing Series

Soil series competing with HILLFIELD 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 HILLFIELD 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 HILLFIELD 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 HILLFIELD, 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 HILLFIELD 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
Hillfield-Kucera complex, 4 to 30 percent slopes	38	2198	485631	j9bj	id715	1994	1:24000
Hillfield-Kucera complex, 30 to 50 percent slopes	39	938	485632	j9bk	id715	1994	1:24000
HILLFIELD-TIMPANOGOS SILT LOAMS, 10 TO 30 PERCENT SLOPES, ERODED	HhE2	1250	482744	j6bd	ut603	1968	1:20000
MCMURDIE-HILLFIELD SILT LOAMS, 10 TO 30 PERCENT SLOPES, ERODED	MdE2	639	482778	j6ch	ut603	1968	1:20000
HILLFIELD SILT LOAM, 20 TO 30 PERCENT SLOPES, ERODED	HgE2	301	482743	j6bc	ut603	1968	1:20000
Hillfield-Timpanogos-Parleys complex, 30 to 60 percent slopes, eroded	HTG2	1706	481568	j53g	ut607	1965	1:15840
Hillfield-Timpanogos-Parleys complex, 20 to 30 percent slopes, eroded	HTF2	658	481567	j53f	ut607	1965	1:15840
Hillfield-Marriott complex, 30 to 60 percent slopes, eroded	HMG2	421	481566	j53d	ut607	1965	1:15840
Hillfield soils, 10 to 20 percent slopes, eroded	HnE2	415	481573	j53m	ut607	1965	1:15840
Hillfield soils, 6 to 10 percent slopes, eroded	HnD2	58	481572	j53l	ut607	1965	1:15840
Hillfield silt loam, 2 to 5 percent slopes	HeC	696	482523	j638	ut608	1981	1:24000
Hillfield-Sterling complex, 8 to 25 percent slopes	8023	101	2981368	2tjt8	ut608	1981	1:24000
Hillfield loam, 1 to 3 percent slopes	HlB	3328	482924	j6j6	ut612	1967	1:20000
Hillfield-Taylorsville complex, 6 to 30 percent slopes	HtF2	2521	482926	j6j8	ut612	1967	1:20000
Hillfield loam, 3 to 6 percent slopes	HlC	1235	482925	j6j7	ut612	1967	1:20000
Hillfield loam, 0 to 1 percent slopes	HlA	856	482923	j6j5	ut612	1967	1:20000
Hillfield sandy loam, 2 to 6 percent slopes	HfC	548	482922	j6j4	ut612	1967	1:20000
Rawnjay-Hillfield-Sterling complex, 10 to 40 percent slopes	8015	513	2981390	2tjt0	ut612	1967	1:20000
Hillfield-Sterling complex, 8 to 25 percent slopes	8023	7	2981385	2tjt8	ut612	1967	1:20000
Welby-Hillfield silt loams, 6 to 10 percent slopes	WhD	1181	483403	j70n	ut621	1966	1:20000
Hillfield-Sterling complex, 20 to 35 percent slopes	HOF	1033	483303	j6xf	ut621	1966	1:20000
Hillfield-Welby silt loams, 6 to 35 percent slopes	HpF	888	483306	j6xj	ut621	1966	1:20000
Hillfield-Layton complex, 30 to 60 percent slopes	HNG	622	483302	j6xd	ut621	1966	1:20000
Welby-Hillfield silt loams, 10 to 30 percent slopes	WhE	605	483404	j70p	ut621	1966	1:20000
Hillfield silt loam, 10 to 20 percent slopes	HmE	594	483304	j6xg	ut621	1966	1:20000
Hillfield silt loam, 20 to 30 percent slopes	HmF	248	483305	j6xh	ut621	1966	1:20000
Hillfield-Sterling complex, 8 to 25 percent slopes	8023	132	2981397	2tjt8	ut621	1966	1:20000
Rawnjay-Hillfield-Sterling complex, 10 to 40 percent slopes	8015	42	2981400	2tjt0	ut621	1966	1:20000

Map of Series Extent

Approximate geographic distribution of the HILLFIELD 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).