Soil Data Explorer - PARKHILL

Official Series Description

Lab Data Summary

Aggregate lab data for the PARKHILL soil series. This aggregation is based on all pedons with a current taxon name of PARKHILL, 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 PARKHILL 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
98	84P0561	S1984MI073001	Parkhill	7	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	43.5099983,-84.726387
98	84P0562	S1984MI073002	Parkhill	7	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	43.6880569,-84.6505585
98	85P0675	S1985MI057001	Parkhill	7	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	43.1286125,-84.4252777
98	09N1087	S2008MI057006	Parkhill	6	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	43.1190083,-84.4137167
98	09N0064	S2008MI147004	Parkhill	6	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	43.1635833,-82.6438417
99	84P0563	S1984MI057001	Parkhill	7	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	43.3533325,-84.444725
99	07N0680	S2007MI057013	Parkhill	5	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	43.2991083,-84.4496222
99	09N0069	S2007MI057017	Parkhill	1	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	43.3472611,-84.4072361
99	09N1086	S2008MI057007	Parkhill	7	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	43.3281639,-84.4609361
99	09N1077	S2009MI091003	Parkhill	6	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	41.7174778,-83.976625
99	09N1078	S2009MI091004	Parkhill	6	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	41.7188444,-83.9380417

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the PARKHILL 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 PARKHILL 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 PARKHILL 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 PARKHILL 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.

There are insufficient data to create the 3D terrace figure.

Competing Series

Soil series competing with PARKHILL 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 PARKHILL 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 PARKHILL 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 PARKHILL, 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 PARKHILL 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
Parkhill loam, non dense till subsoil, 0 to 2 percent slopes	33	4319	186092	2w5mp	mi015	1988	1:15840
Parkhill loam, 0 to 1 percent slopes	111	84	2507998	2tx84	mi017	1978	1:20000
Parkhill loam, non dense till subsoil, 0 to 2 percent slopes	Pr	31775	186395	2w5mp	mi037	1974	1:15840
Parkhill loam, 0 to 1 percent slopes	Pk	3741	2994137	2tx84	mi037	1974	1:15840
Parkhill loam, non dense till subsoil, 0 to 2 percent slopes	Pr	26354	186249	2w5mp	mi045	1974	1:15840
Parkhill-Selfridge complex, 0 to 2 percent slopes	PcB	6	2399409	2whvy	mi049	1967	1:20000
Parkhill loam, 0 to 1 percent slopes	Pa	2	2399410	2tx84	mi049	1967	1:20000
Parkhill-Poseyville complex, 0 to 3 percent slopes	PbA	1	2399407	2ljs7	mi049	1967	1:20000
Parkhill loam, 0 to 1 percent slopes	Pa	5224	189841	2tx84	mi051	1966	1:15840
Parkhill loam, 0 to 1 percent slopes	Ph	60952	187028	2tx84	mi057	1975	1:12000
Parkhill loam, non dense till subsoil, 0 to 2 percent slopes	PhA	21696	2998376	2w5mp	mi057	1975	1:12000
Conover-Parkhill complex, 0 to 3 percent slopes	CvraeA	3083	3117286	2y14q	mi057	1975	1:12000
Capac variant-Parkhill complex, 0 to 2 percent slopes	CcA	43	187005	68lf	mi057	1975	1:12000
Parkhill-Selfridge complex, 0 to 2 percent slopes	PcB	14	2673591	2whvy	mi057	1975	1:12000
Parkhill-Conover loams, 0 to 3 percent slopes	PkhabA	8	3117288	2y14n	mi057	1975	1:12000
Parkhill loam, 0 to 1 percent slopes	58	4058	186808	2tx84	mi063	1978	1:20000
Parkhill loam, non dense till subsoil, 0 to 2 percent slopes	Bw	24755	187904	2w5mp	mi067	1965	1:15840
Parkhill loam, 0 to 1 percent slopes	40	11193	186626	2tx84	mi073	1983	1:15840
Parkhill loam, non dense till subsoil, 0 to 2 percent slopes	40A	5499	2998374	2w5mp	mi073	1983	1:15840
Parkhill loam, non dense till subsoil, 0 to 2 percent slopes	38	5139	187140	2w5mp	mi081	1984	1:15840
Parkhill loam, 0 to 1 percent slopes	Pc	493	2508415	2tx84	mi087	1966	1:15840
Parkhill loam and clay loam, 0 to 2 percent slopes	PdA	125	2508416	6b0t	mi087	1966	1:15840
Parkhill loam, 0 to 1 percent slopes	Pa	17250	187676	2tx84	mi099	1967	1:20000
Ensley-Parkhill complex	Ep	4850	187641	697y	mi099	1967	1:20000
Parkhill-Urban land complex, 0 to 2 percent slopes	PkhuaA	10	3015245	2v13r	mi099	1967	1:20000
Parkhill loam, non dense till subsoil, 0 to 2 percent slopes	15	719	192467	2w5mp	mi105	1992	1:15840
Parkhill loam, 0 to 1 percent slopes	Pa	20099	186644	2tx84	mi111	1976	1:15840
Parkhill-Conover loams, 0 to 3 percent slopes	PkhabA	158	3117263	2y14n	mi111	1976	1:15840
Parkhill-Selfridge complex, 0 to 2 percent slopes	PbB	128	2673552	2whvy	mi111	1976	1:15840
Parkhill loam, non dense till subsoil, 0 to 2 percent slopes	53	1349	186499	2w5mp	mi123	1990	1:15840
Ensley-Parkhill complex	138	2	2508694	697y	mi125	1980	1:15840
Parkhill loam, 0 to 1 percent slopes	24	51453	186667	2tx84	mi145	1991	1:15840
Parkhill-Selfridge complex, 0 to 2 percent slopes	22B	16082	186665	2whvy	mi145	1991	1:15840
Parkhill-Conover loams, 0 to 3 percent slopes	PkhabA	6942	3117255	2y14n	mi145	1991	1:15840
Urban land-Parkhill complex, 0 to 3 percent slopes	99A	4456	186712	688z	mi145	1991	1:15840
Parkhill-Poseyville complex, 0 to 3 percent slopes	84A	1203	186703	688p	mi145	1991	1:15840
Parkhill loam, 0 to 1 percent slopes	Pc	47591	187445	2tx84	mi147	1969	1:20000
Conover-Parkhill loams, 0 to 2 percent slopes	CwA	12497	187409	690g	mi147	1969	1:20000
Metamora-Parkhill complex, 0 to 2 percent slopes	MhA	8135	187431	6915	mi147	1969	1:20000
Parkhill loam and clay loam, 0 to 2 percent slopes	PdA0	101476	188381	6b0t	mi151	1955	1:15840
Parkhill loam, 0 to 1 percent slopes	PcA0	70264	188379	2tx84	mi151	1955	1:15840
Parkhill loam and mucky loam, 0 to 2 percent slopes	PeA0	26867	188382	6b0v	mi151	1955	1:15840
Parkhill loam, 2 to 6 percent slopes, slightly eroded	PcB1	211	188380	6b0s	mi151	1955	1:15840
Parkhill loam, 0 to 1 percent slopes	Pr	9	2399159	2tx84	mi155	1967	1:12000
Parkhill loam, 0 to 1 percent slopes	120A	425	2508118	2tx84	mi157	1984	1:15840
Parkhill loam and clay loam, 0 to 2 percent slopes	117A	149	2508115	6b0t	mi157	1984	1:15840
Avoca-Urban land-Parkhill complex, 0 to 4 percent slopes	AvoucB	4644	3015164	2v146	mi163	1974	1:12000
Parkhill-Urban land complex, 0 to 2 percent slopes	PkhuaA	578	3015155	2v13r	mi163	1974	1:12000
Avoca-Parkhill sandy loams, 0 to 4 percent slopes	AvohcB	136	3015182	2wht8	mi163	1974	1:12000
Parkhill sandy loam, 0 to 2 percent slopes	PkhhaA	37	3015207	2whv2	mi163	1974	1:12000
Parkhill loam, non dense till subsoil, 0 to 2 percent slopes	15	599	631167	2w5mp	mi614	2005	1:12000

Map of Series Extent

Approximate geographic distribution of the PARKHILL 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).