Soil Data Explorer - DOOLEY

Official Series Description

Lab Data Summary

Aggregate lab data for the DOOLEY soil series. This aggregation is based on all pedons with a current taxon name of DOOLEY, 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 DOOLEY 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
54	89P0761	88ND053046	Dooley	4	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	47.8927778,-103.6694444

Water Balance

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

Soil series sharing subgroup-level classification with DOOLEY, 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 DOOLEY 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
Dooley fine sandy loam, 2 to 6 percent slopes	DoB	1349	345333	clbs	mt083	1973	1:24000
Dooley fine sandy loam, 0 to 6 percent slopes	DoB	27537	348843	cq00	mt091	1971	1:24000
Dooley fine sandy loam, 6 to 12 percent slopes	DoC	10394	348844	cq01	mt091	1971	1:24000
Tally-Dooley sandy loams, 0 to 5 percent slopes	63	40708	345582	cllt	mt105	1976	1:24000
Tally-Dooley sandy loams, 5 to 15 percent slopes	64	11316	345583	cllv	mt105	1976	1:24000
Dooley sandy loam, 0 to 4 percent slopes	53	7349	341938	cgt8	mt613	1975	1:24000
Dooley sandy loam, 4 to 8 percent slopes	54	1157	341939	cgt9	mt613	1975	1:24000
Dooley sandy loam, 8 to 15 percent slopes	55	298	341940	cgtb	mt613	1975	1:24000
Dooley sandy loam, 0 to 4 percent slopes	14	92377	348216	cpbs	mt661	1982	1:24000
Dooley-Zahl complex, 3 to 6 percent slopes	2278	8987	341332	cg5q	nd023	1992	1:24000
Parshall-Tally-Dooley fine sandy loams, 0 to 6 percent slopes	2284	3160	341338	cg5x	nd023	1992	1:24000
Dooley sandy loam, 1 to 3 percent slopes	2277	3146	341331	cg5p	nd023	1992	1:24000
Zahl-Dooley complex, 6 to 9 percent slopes	2279	1647	341333	cg5r	nd023	1992	1:24000
Dooley-Zahl complex, 3 to 6 percent slopes	C384B	1640	2564266	2q3hj	nd023	1992	1:24000
Dooley-Lihen-Zahl complex, 9 to 15 percent slopes	2280	1312	341334	cg5s	nd023	1992	1:24000
Dooley-Lihen-Zahl complex, 9 to 15 percent slopes	C386D	669	2564265	2q3hh	nd023	1992	1:24000
Zahl-Dooley-Zahill complex, 6 to 9 percent slopes	C385C	618	2564240	2q2jd	nd023	1992	1:24000
Dooley fine sandy loam, 0 to 3 percent slopes	C380A	323	2595771	2q4wy	nd023	1992	1:24000
Dooley-Zahl complex, 6 to 9 percent slopes	E3703C	12447	2699328	d343	nd053	2003	1:24000
Dooley-Zahl complex, 3 to 6 percent slopes	E3703B	9253	2699327	d342	nd053	2003	1:24000
Dooley fine sandy loam, 3 to 6 percent slopes	E3701B	6173	2525633	d0q5	nd053	2003	1:24000
Dooley-Zahl complex, 9 to 15 percent slopes	E3703D	4640	2699329	d344	nd053	2003	1:24000
Dooley fine sandy loam, 0 to 3 percent slopes	E3701A	1882	2699326	2qz94	nd053	2003	1:24000
Dooley fine sandy loam, 0 to 6 percent slopes	2346	1968	339057	cctb	nd105	1993	1:24000
Dooley fine sandy loam, 0 to 3 percent slopes	C380A	741	2595611	2q4wy	nd105	1993	1:24000
Dooley fine sandy loam, 3 to 6 percent slopes	C380B	473	2595609	2q3hg	nd105	1993	1:24000
Dooley fine sandy loam, 3 to 6 percent slopes	E3701B	85	2662545	d0q5	nd105	1993	1:24000
Dooley-Lihen-Zahl complex, 9 to 15 percent slopes	C386D	10	2596785	2q3hh	nd105	1993	1:24000

Map of Series Extent

Approximate geographic distribution of the DOOLEY 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).