Soil Data Explorer - NOBSCOT

Official Series Description

Lab Data Summary

Aggregate lab data for the NOBSCOT soil series. This aggregation is based on all pedons with a current taxon name of NOBSCOT, 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 NOBSCOT 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
78C	00P1360	s2000ok-055-005 nobscot	nobscot	7	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	35.1033401489258,-99.4581527709961

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the NOBSCOT 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 NOBSCOT 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 NOBSCOT 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 NOBSCOT 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 NOBSCOT 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 NOBSCOT 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 NOBSCOT 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 NOBSCOT, 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

Click a link below to display the diagram. Note that these diagrams may be from multiple survey areas.

1. OK-2012-02-16-04 | Blaine County - February 1968

   Typical pattern of soils in associations 1, 3, 4, and 6 (Soil Survey of Blaine County, Oklahoma; February 1968).

2. OK-2012-02-16-25 | Dewey County - December 1963

   Typical pattern of the dominant soils in association 3 (Soil Survey of Dewey County, Oklahoma; December 1963).

3. OK-2012-02-16-29 | Ellis County - April 1966

   Major soils of association 4 (Soil Survey of Ellis County, Oklahoma; April 1966).

4. OK-2012-02-16-35 | Greer County - March 1967

   Major soils in soil association 1, and their relation to the landscape (Soil Survey of Greer County, Oklahoma; March 1967).

5. OK-2012-02-16-52 | Jackson County - June 1961

   Typical pattern of Miles, Enterprise, Tivoli, and associated soil (Soil Survey of Jackson County, Oklahoma; June 1961).

6. OK-2012-02-17-12 | Major County - October 1968

   Soil associations in the central part of the county (Soil Survey of Major County, Oklahoma; October 1968).

7. OK-2012-02-17-13 | Major County - October 1968

   Cross section along a line extending across the middle of the county from the western to the eastern boundary (Soil Survey of Major County, Oklahoma; October 1968).

8. OK-2012-02-17-39 | Roger Mills County - August 1963

   Typical pattern of soils in associations 1 and 2 (Soil Survey of Roger Mills County, Oklahoma; August 1963).

9. OK-2012-02-17-62 | Woodward County - November 1963

   Typical pattern of soils of the Nobscot-Brownfield association (Soil Survey of Woodward County, Oklahoma; November 1963).

10. TX-2010-11-03-50 | King County - 2007

    Typical pattern of the Grandfield-Shrewder-Devol and Delwin-Nobscot general soil map units (Soil Survey of King County, Texas; 2007).

11. TX-2012-03-20-16 | Childress County - July 1963

    Soils developed in sandy outwash material (Soil Survey of Childress County, TX; 1963).

Map Units

Map units containing NOBSCOT 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
Nobscot sand, 0 to 5 percent slopes	36	50289	381673	2t6p9	ok009	1978	1:24000
Delwin-Nobscot complex, 0 to 3 percent slopes	15	41739	381650	dt49	ok009	1978	1:24000
Nobscot sand, 5 to 20 percent slopes	37	3975	381674	2t6pn	ok009	1978	1:24000
Nobscot and Delwin soils, 2 to 5 percent slopes, gullied	38	3011	381675	dt53	ok009	1978	1:24000
Nobscot sand, 0 to 5 percent slopes	NstC	36577	381750	2t6p9	ok011	1965	1:24000
Nobscot sand, 5 to 20 percent slopes	NcD	1882	381752	2t6pn	ok011	1965	1:24000
Nobscot sand, 5 to 20 percent slopes	NoE	36711	382383	2t6pn	ok043	1961	1:24000
Nobscot-Grandfield complex, 0 to 5 percent slopes	NpC	19964	382384	dtwz	ok043	1961	1:24000
Nobscot and Grandfield soils, 3 to 12 percent slopes, severely eroded	Er	2966	382370	dtwj	ok043	1961	1:24000
Nobscot-Delwin complex, 1 to 5 percent slopes	NbC	63737	382449	dtz2	ok045	1963	1:24000
Nobscot sand, 5 to 20 percent slopes	NoE	42726	382451	2t6pn	ok045	1963	1:24000
Nobscot-Delwin complex, 3 to 8 percent slopes, severely eroded MLRA 78C	Nc3	2592	382450	2t6pr	ok045	1963	1:24000
Nobscot fine sand, 2 to 5 percent slopes, severely eroded	Bg	638	382420	dty4	ok045	1963	1:24000
Nobscot sand, 0 to 5 percent slopes	NstC	4155	653901	2t6p9	ok055	2005	1:24000
Nobscot sand, 5 to 20 percent slopes	46	2441	975480	2t6pn	ok057	1982	1:24000
Nobscot sand, 0 to 5 percent slopes	45	1910	975479	2t6p9	ok057	1982	1:24000
Nobscot sand, 5 to 20 percent slopes	NcD	72766	383841	2t6pn	ok093	1965	1:24000
Nobscot sand, 0 to 5 percent slopes	NcC	20045	383840	2t6p9	ok093	1965	1:24000
Nobscot-Eda complex, 5 to 20 percent slopes	NpD	11064	383843	2t6pp	ok093	1965	1:24000
Nobscot-Eda complex, 3 to 5 percent slopes	NpC	3246	383842	2t6pq	ok093	1965	1:24000
Nobscot and Delwin soils, 3 to 8 percent slopes	NbC	43337	384756	dxch	ok129	1961	1:24000
Nobscot and Delwin soils, 0 to 3 percent slopes	NbB	42739	384755	dxcg	ok129	1961	1:24000
Nobscot sand, 0 to 5 percent slopes	NaB	26828	384754	2t6p9	ok129	1961	1:24000
Nobscot, Delwin, and Grandfield soils, 3 to 8 percent slopes, severely eroded	Er	22776	384738	dxbx	ok129	1961	1:24000
Grandfield-Nobscot complex, 8 to 15 percent slopes	MnE	19273	384752	30l0f	ok129	1961	1:24000
Grandfield-Nobscot complex, 5 to 8 percent slopes	MnD	8550	384751	30l0d	ok129	1961	1:24000
Nobscot and Delwin soils, 3 to 8 percent slopes, eroded	Nc2	2662	384757	dxcj	ok129	1961	1:24000
Nobscot-Eufaula complex, 5 to 12 percent slopes	NeD	23685	385285	dxxk	ok153	1961	1:24000
Nobscot-Eda complex, 5 to 20 percent slopes	NpE	18057	385287	2t6pp	ok153	1961	1:24000
Nobscot-Delwin complex, 3 to 5 percent slopes	NbC	15534	385283	dxxh	ok153	1961	1:24000
Nobscot-Eda complex, 3 to 5 percent slopes	NpC	5148	385286	2t6pq	ok153	1961	1:24000
Nobscot-Delwin complex, 3 to 8 percent slopes, severely eroded MLRA 78C	Nc3	1378	385284	2t6pr	ok153	1961	1:24000
Devol and Nobscot soils, severely eroded	Sn3	8394	363841	d6lt	tx075	1961	1:20000
Devol and Nobscot soils, hummocky	SnD	5769	363842	d6lv	tx075	1961	1:20000
Heatly-Nobscot complex, 0 to 5 percent slopes	Bn	10752	364094	2vt8d	tx087	1965	1:20000
Nobscot fine sand	No	15880	364606	d7dh	tx101	1969	1:20000
Heatly-Nobscot complex, 0 to 5 percent slopes	BW	53226	365109	2vt8d	tx125	1965	1:20000
Nobscot fine sand, 1 to 8 percent slopes	Nb	2764	365191	d80c	tx129	1975	1:24000
Nobscot fine sand, 0 to 5 percent slopes	NoC	5250	378345	dppp	tx169	1965	1:24000
Nobscot fine sand	Nb	2530	366953	d9v6	tx191	1965	1:20000
Nobscot fine sand, undulating	No	2100	367152	db1m	tx197	1965	1:20000
Devol-Nobscot complex, 1 to 3 percent slopes	DeNB	16688	2713435	2r5rx	tx207	1960	1:20000
Nobscot-Devol complex, 3 to 8 percent slopes	NoDC	5055	2713443	2r5ry	tx207	1960	1:20000
Tivoli-Nobscot complex, 5 to 15 percent slopes	TvND	694	2713444	2r5rz	tx207	1960	1:20000
Nobscot fine sand	No	12702	368243	dc5t	tx253	1966	1:20000
Nobscot soils and blown-out land	Ns	959	368244	dc5v	tx253	1966	1:20000
Heatly-Nobscot complex, 0 to 5 percent slopes	Nb	101131	368491	2vt8d	tx263	1968	1:31680
Nobscot and Tivoli soils, undulating	NtB	418	368492	dcfv	tx263	1968	1:31680
Nobscot sand, 1 to 5 percent slopes	NoC	2692	368600	dckb	tx269	1999	1:31680
Devol-Nobscot complex, 1 to 3 percent slopes	DeNB	5500	2713436	2r5rx	tx275	1975	1:24000
Nobscot soils, 3 to 12 percent slopes	NoE	10276	370882	dfxy	tx345	1972	1:24000
Nobscot association	NS	49086	372290	dhdc	tx433	1970	1:24000
Devol-Nobscot complex, 1 to 3 percent slopes	DeNB	69	2713437	2r5rx	tx433	1970	1:24000
Nobscot sand, 0 to 5 percent slopes	PtB	50577	373323	2t6p9	tx483	1970	1:24000

Map of Series Extent

Approximate geographic distribution of the NOBSCOT 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).