Soil Data Explorer - PINEHILL

Official Series Description

Lab Data Summary

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

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the PINEHILL 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 PINEHILL 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 PINEHILL 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 PINEHILL 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 PINEHILL 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 PINEHILL 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 PINEHILL 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 mountains figure.

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

Soil series sharing subgroup-level classification with PINEHILL, 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 PINEHILL 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
Pinehill loam, 2 to 8 percent slopes	64C	8148	343604	cjk0	mt017	1995	1:24000
Pinehill-Absher complex, 2 to 15 percent slopes	641D	4674	343601	cjjx	mt017	1995	1:24000
Creed-Pinehill loams, 2 to 8 percent slopes	811C	2786	343693	cjmw	mt017	1995	1:24000
Pinehill loam, 0 to 2 percent slopes	64A	1547	343603	cjjz	mt017	1995	1:24000
Pinehill loam, 8 to 15 percent slopes	64D	953	343605	cjk1	mt017	1995	1:24000
Pinehill-Weingart-Gerdrum complex, 0 to 6 percent slopes	993C	60	343834	cjsf	mt017	1995	1:24000
Pinelli loam, 2 to 8 percent slopes	104	2567	344780	ckry	mt079	1986	1:24000
Pinelli-Weingart-Gerdrum complex, 0 to 6 percent slopes	105	1484	344781	ckrz	mt079	1986	1:24000
Pinelli loam, 0 to 2 percent slopes	103	792	344779	ckrx	mt079	1986	1:24000
Vanstel-Pinehill complex, 0 to 6 percent slopes	332	240	1387777	1hl30	mt643	1967	1:20000
Pinehill clay loam, 0 to 6 percent slopes	305	137	1387768	1hl2q	mt643	1967	1:20000
Pinehill complex, 0 to 6 percent slopes	307	126	1387770	1hl2s	mt643	1967	1:20000
Pinehill-Pylon loams, 3 to 15 percent slopes	308	59	1387771	1hl2t	mt643	1967	1:20000
Pinehill-Pylon clay loams, 3 to 15 percent slopes	306	29	1387769	1hl2r	mt643	1967	1:20000
Mantlemine-Pinehill, stony-Peta complex, 4 to 50 percent slopes	9453		3203087	2zbsl	wy629		1:24000
Kremlin-Pinehill complex, 4 to 25 percent slopes	9458		3203108	2zbt9	wy629		1:24000
Coyoteflats-Pinehill complex, 6 to 15 percent slopes	2350		3250476	2zv71	wy629		1:24000
Amalia-like-Scravo, very stony-Pinehill complex, 15 to 50 percent slopes	4409		3170958	2z1zn	wy629		1:24000
Pinehill-Yamacall-Hawksell-like complex, 4 to 25 percent slopes	5361		3203069	2zbs0	wy629		1:24000
Shooter-Pinehill complex 0 to 7 percent slopes	744		3410471	31g8v	wy630		1:24000
Golphco-Pinehill complex, 6 to 25 percent slopes	5521	5197	2370691	2kkwx	wy635		1:24000
Pinehill-Pylon clay loams, 3 to 15 percent slopes	306	2796	817561	wfqy	wy705	2003	1:24000
Pinehill-Pylon loams, 3 to 15 percent slopes	308	2136	817552	wfqn	wy705	2003	1:24000
Pinehill complex, 0 to 6 percent slopes	307	1019	817550	wfql	wy705	2003	1:24000
Pinehill clay loam, 0 to 6 percent slopes	305	632	817559	wfqw	wy705	2003	1:24000
Vanstel-Pinehill complex, 0 to 6 percent slopes	332	332	817569	wfr6	wy705	2003	1:24000

Map of Series Extent

Approximate geographic distribution of the PINEHILL 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).