Soil Data Explorer - PARKER

Official Series Description

Lab Data Summary

Aggregate lab data for the PARKER soil series. This aggregation is based on all pedons with a current taxon name of PARKER, 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 PARKER 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
148	00P0095	99MD510003	Parker	6	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	39.3028583,-76.6912111

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the PARKER 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 PARKER 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 PARKER 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 PARKER 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 terrace figure.

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

Competing Series

Soil series competing with PARKER 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 PARKER 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 PARKER 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 PARKER, 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 PARKER 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
Parker gravelly loam, 8 to 25 percent slopes, very stony	PaD	1	3347301	2zhhq	de003	2009	1:24000
Parker gravelly loam, 25 to 55 percent slopes, very stony	PaF	1	3347302	2zhhp	de003	2009	1:24000
Parker cobbly loam, 18 to 40 percent slopes, extremely stony	ParEe	13867	1482827	1ls04	nj019	1970	1:24000
Parker cobbly loam, 3 to 15 percent slopes	ParC	9805	548645	ldx7	nj019	1970	1:24000
Gladstone and Parker soils, 8 to 15 percent slopes, extremely stony	GKAPCC	6268	1033913	13pw1	nj019	1970	1:24000
Parker cobbly loam, 15 to 25 percent slopes	ParD	3904	548646	ldx8	nj019	1970	1:24000
Parker-Gladstone complex, 0 to 15 percent slopes, extremely stony	PauCc	15700	1480285	1lpc4	nj027	1974	1:24000
Parker gravelly sandy loam, 3 to 15 percent slopes	PaoC	8677	298520	b0mp	nj027	1974	1:24000
Parker-Gladstone complex, 15 to 25 percent slopes, extremely stony	PauDc	8613	1480286	1lpc5	nj027	1974	1:24000
Parker-Rock outcrop complex, 25 to 45 percent slopes	PawE	6444	298524	b0mt	nj027	1974	1:24000
Parker very gravelly sandy loam, 15 to 25 percent slopes	PapD	2434	298521	b0mq	nj027	1974	1:24000
Parker cobbly loam, 3 to 15 percent slopes	ParC	310	1482962	1ls4h	nj027	1974	1:24000
Gladstone and Parker soils, 8 to 15 percent slopes, extremely stony	GKAPCC	200	1482960	1ls4f	nj027	1974	1:24000
Parker cobbly loam, 18 to 40 percent slopes, extremely stony	ParEe	133	1482963	1ls4j	nj027	1974	1:24000
Parker cobbly loam, 15 to 25 percent slopes	ParD	52	1482964	1ls4k	nj027	1974	1:24000
Parker-Gladstone complex, 15 to 25 percent slopes, very stony	PauDb	1201	1034040	13q04	nj035	1972	1:24000
Parker very gravelly sandy loam, 3 to 15 percent slopes	PapC	980	548506	ldrr	nj035	1972	1:24000
Parker very gravelly sandy loam, 25 to 45 percent slopes, rocky	PapFg	449	548504	ldrp	nj035	1972	1:24000
Parker very gravelly sandy loam, 15 to 25 percent slopes	PapD	142	1405063	1j52m	nj035	1972	1:24000
Parker-Gladstone complex, 15 to 25 percent slopes, extremely stony	PauDc	81	1034041	13q05	nj035	1972	1:24000
Parker-Gladstone complex, 0 to 15 percent slopes, extremely stony	PauCc	64	1034034	13pzy	nj035	1972	1:24000
Parker-Rock outcrop complex, 25 to 45 percent slopes	PawE	55	548555	ldtb	nj035	1972	1:24000
Parker gravelly sandy loam, 3 to 15 percent slopes	PaoC	12	548505	ldrq	nj035	1972	1:24000
Parker-Rock outcrop complex, 45 to 65 percent slopes	PawF	7487	1896061	21n08	nj041	2007	1:12000
Parker gravelly sandy loam, 15 to 25 percent slopes	PaoD	4487	298375	b0h0	nj041	2007	1:12000
Parker-Rock outcrop complex, 25 to 45 percent slopes	PawE	1010	1896062	21n09	nj041	2007	1:12000
Parker gravelly sandy loam, 3 to 15 percent slopes	PaoC	96	1710223	1vdmh	nj041	2007	1:12000
Gladstone-Parker gravelly loams, 15 to 25 percent slopes	GnD	66	1947960	23d0f	pa017	1997	1:24000
Gladstone-Parker gravelly loams, 15 to 25 percent slopes	GeD	4103	1599929	1qpvm	pa029	2008	1:24000
Parker gravelly loam, 8 to 15 percent slopes	PaC	3161	868631	y4wc	pa029	2008	1:24000
Parker gravelly loam, 15 to 25 percent slopes	PaD	2910	868630	y4wb	pa029	2008	1:24000
Parker gravelly loam, 25 to 35 percent slopes	PaE	1780	868629	y4w9	pa029	2008	1:24000
Parker gravelly loam, 3 to 8 percent slopes	PaB	1044	868632	y4wd	pa029	2008	1:24000
Parker gravelly loam, 35 to 60 percent slopes	PaF	551	868860	y53r	pa029	2008	1:24000
Parker loam, 8 to 25 percent slopes, extremely stony	PbD	385	868627	y4w7	pa029	2008	1:24000
Parker loam, 25 to 60 percent slopes, extremely stony	PbF	164	868626	y4w6	pa029	2008	1:24000
Parker loam, 0 to 8 percent slopes, extremely stony	PbB	82	868628	y4w8	pa029	2008	1:24000
Urban land-Parker complex, 8 to 25 percent slopes	UrvD	79	1611965	1r3cw	pa029	2008	1:24000
Urban land-Parker complex, 0 to 8 percent slopes	UrvB	22	1611964	1r3cv	pa029	2008	1:24000
Parker gravelly loam, 25 to 35 percent slopes	PbE	585	984449	2zhhh	pa045	1960	1:20000
Gladstone-Parker complex, 0 to 8 percent slopes	GfB	288	2396182	30chb	pa045	1960	1:20000
Parker gravelly loam, 15 to 25 percent slopes	PbD	263	984446	2yh31	pa045	1960	1:20000
Parker gravelly loam, 8 to 25 percent slopes, very stony	PaD	245	984451	2zhhq	pa045	1960	1:20000
Parker gravelly loam, 25 to 55 percent slopes, very stony	PaF	169	984452	2zhhp	pa045	1960	1:20000
Parker gravelly loam, 8 to 15 percent slopes	PbC	120	984443	2zhhk	pa045	1960	1:20000
Parker gravelly loam, 3 to 8 percent slopes	PbB	41	984442	2zhhj	pa045	1960	1:20000
Parker gravelly loam, 0 to 8 percent slopes, very stony	PaB	3	984450	2zhhn	pa045	1960	1:20000
Gladstone-Parker gravelly loams, 15 to 25 percent slopes	GgD	24	1947970	23d0r	pa077	1997	1:24000
Parker gravelly loam, 8 to 15 percent slopes	PaC	614	2397962	2lh8m	pa091	2008	1:12000
Parker loam, 8 to 25 percent slopes, extremely stony	PbD	531	2397968	2lh8t	pa091	2008	1:12000
Parker gravelly loam, 25 to 35 percent slopes	PaE	360	2397965	2lh8q	pa091	2008	1:12000
Parker gravelly loam, 15 to 25 percent slopes	PaD	297	2397964	2lh8p	pa091	2008	1:12000
Parker loam, 25 to 60 percent slopes, extremely stony	PbF	226	2397969	2lh8v	pa091	2008	1:12000
Parker gravelly loam, 3 to 8 percent slopes	PaB	196	2397961	2lh8l	pa091	2008	1:12000
Parker loam, 0 to 8 percent slopes, extremely stony	PbB	50	2397966	2lh8r	pa091	2008	1:12000
Gladstone-Parker gravelly loams, 15 to 25 percent slopes	GnD	1888	1946672	23bnw	pa095	2007	1:12000
Parker very stony loam, 25 to 45 percent slopes	66E	12580	516440	kbdc	va003	1981	1:15840
Parker extremely stony loam, 25 to 60 percent slopes	67E	6100	516442	kbdf	va003	1981	1:15840
Parker very stony loam, 15 to 25 percent slopes	66D	2320	516439	kbdb	va003	1981	1:15840
Parker very stony loam, 7 to 15 percent slopes	66C	700	516438	kbd9	va003	1981	1:15840
Parker extremely stony loam, 15 to 25 percent slopes	67D	550	516441	kbdd	va003	1981	1:15840
Parker extremely stony loam, 25 to 70 percent slopes	PrE	14348	516905	kbwc	va079	1983	1:15840
Chester and Parker soils, very stony, 15 to 25 percent slopes	CmD	2877	516882	kbvm	va079	1983	1:15840
Chester and Parker soils, very stony, 7 to 15 percent slopes	CmC	620	516881	kbvl	va079	1983	1:15840
Parker-Glenelg complex, 25 to 50 percent slopes	26E	4498	517100	kc2n	va121	1980	1:15840
Parker-Glenelg complex, 15 to 25 percent slopes	26D	1371	517099	kc2m	va121	1980	1:15840
Parker-Rock outcrop complex, 25 to 50 percent slopes	27E	1027	517101	kc2p	va121	1980	1:15840
Parker-Glenelg complex, 7 to 15 percent slopes	26C	759	517098	kc2l	va121	1980	1:15840

Map of Series Extent

Approximate geographic distribution of the PARKER 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).