Soil Data Explorer - NOONAN

Official Series Description

Lab Data Summary

Aggregate lab data for the NOONAN soil series. This aggregation is based on all pedons with a current taxon name of NOONAN, 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 NOONAN 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
53A	89P0284	88ND013057	Noonan	5	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	48.9169082641602,-102.813369750977
53A	89P0295	88ND023061	Noonan	5	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	48.9552421569824,-103.026153564453
53A	89P0287	88ND023063	Noonan	5	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	48.9044075012207,-103.237548828125
53A	92P0707	92ND023155	Noonan	8	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	48.9547222,-102.9838889
53A	89P0283	S1988ND013056	Noonan	5	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	48.9072227,-102.8708344
53A	89P0286	S1988ND023062	Noonan	5	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	48.9655571,-103.2441635
53A	91P0203	S1990ND023127	Noonan	6	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	48.9180565,-103.2244415
53B	79P0019	78ND029001	Noonan	7	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	46.032470703125,-100.026573181152
53B	90P0297	89ND023105	Noonan	6	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	48.7925,-103.3616667
54	89P0762	88ND053091	Noonan	4	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	47.9860725402832,-102.897804260254

Water Balance

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

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

Soil series sharing subgroup-level classification with NOONAN, 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. ND-2010-09-27-05 | Burke County - 2003

   Typical pattern of soils and underlying material in the Noonan-Niobell association (Soil Survey of Burke County, North Dakota; 2003).

2. ND-2012-02-07-27 | Divide County - 2002

   Typical pattern of soils and underlying material in the Williams-Niobell-Noonan association (Soil Survey of Divide County, North Dakota; 2002).

3. ND-2012-02-07-28 | Divide County - 2002

   Typical pattern of soils and underlying material in the Noonan-Niobell association (Soil Survey of Divide County, North Dakota; 2002).

4. ND-2012-02-07-33 | Dunn County - April 1982

   Typical pattern of soils and underlying material in the Williams-Amor-Arnegard association (Soil Survey of Dunn County, North Dakota; April 1982).

5. SD-2012-03-14-11 | Brown County - April 1993

   Typical pattern of soils and parent material in the Niobell-Noonan-Williams association (Soil Survey of Brown County, SD; 1993).

6. SD-2012-03-15-32 | Faulk County - January 1984

   Pattern of soils and parent material in the Williams-Bowbells association (Soil Survey of Faulk County, SD; 1984).

7. SD-2012-03-15-34 | Faulk County - January 1984

   Pattern of soils and parent material in the Max-Niobell-Noonan association (Soil Survey of Faulk County, SD; 1984).

Map Units

Map units containing NOONAN 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
Shambo-Noonan loams, 4 to 15 percent slopes	131C	4645	342871	chsc	mt011	1992	1:24000
Bearpaw-Noonan complex, 0 to 4 percent slopes	673B	2627	344243	2vysv	mt051	1992	1:24000
Bearpaw-Noonan complex, 0 to 4 percent slopes	673B	2154	345239	2vysv	mt101	1992	1:24000
Bearpaw-Noonan complex, 0 to 4 percent slopes	673A	1012	346879	2vysv	mt615	1992	1:24000
Noonan-Niobell loams, 0 to 6 percent slopes	2179	58448	341120	cfyw	nd013	1991	1:24000
Miranda-Noonan loams, 0 to 3 percent slopes	2181	34340	341122	cfyy	nd013	1991	1:24000
Niobell-Noonan-Tonka complex, 0 to 3 percent slopes	2180	27705	341121	cfyx	nd013	1991	1:24000
Noonan-Niobell-Williams loams, 0 to 6 percent slopes	C665B	103	2564060	2q2k9	nd013	1991	1:24000
Miranda-Noonan loams, 0 to 3 percent slopes	C557A	100	2564064	2q2kh	nd013	1991	1:24000
Miranda-Noonan loams, 3 to 6 percent slopes	C557B	9	2595623	2q2kg	nd013	1991	1:24000
Niobell-Noonan loams, 0 to 3 percent slopes	C661A	6689	2564189	2q77l	nd015	1967	1:20000
Niobell-Noonan loams, 3 to 6 percent slopes	C661B	5117	2564146	2q52b	nd015	1967	1:20000
Miranda-Noonan loams, 3 to 6 percent slopes	C557B	1125	2494660	2q2kg	nd015	1967	1:20000
Miranda-Noonan loams, 0 to 3 percent slopes	C557A	468	2567049	2q2kh	nd015	1967	1:20000
Williams-Noonan loams, 0 to 6 percent slopes	C772B	40	2595633	2q2jj	nd015	1967	1:20000
Williams-Noonan loams, 0 to 6 percent slopes	C772B	16	2595431	2q2jj	nd021	1989	1:20000
Noonan-Niobell loams, 0 to 6 percent slopes	2179	38896	341320	cg5b	nd023	1992	1:24000
Noonan-Niobell-Tonka complex, 0 to 3 percent slopes	2282	23775	341336	cg5v	nd023	1992	1:24000
Miranda-Noonan loams, 0 to 3 percent slopes	2181	9878	341321	cg5c	nd023	1992	1:24000
Noonan-Niobell-Williams loams, 0 to 6 percent slopes	C665B	5067	2564250	2q2k9	nd023	1992	1:24000
Niobell-Noonan-Tonka complex, 0 to 6 percent slopes	2283	4412	341337	cg5w	nd023	1992	1:24000
Niobell-Noonan-Tonka complex, 0 to 6 percent slopes	C669B	2857	2564251	2q2kc	nd023	1992	1:24000
Miranda-Noonan loams, 0 to 3 percent slopes	C557A	1505	2564252	2q2kh	nd023	1992	1:24000
Noonan-Niobell-Tonka complex, 0 to 3 percent slopes	C669A	1098	2564246	2q2k8	nd023	1992	1:24000
Williams-Noonan loams, 3 to 6 percent slopes	E3520B	1684	2707227	2qkx8	nd025	1981	1:20000
Noonan-Williams-Niobell loams, 6 to 9 percent slopes	E3521C	708	2707228	d32w	nd025	1981	1:20000
Noonan-Niobell-Williams loams, 3 to 6 percent slopes	E3517B	24	2758487	d32v	nd025	1981	1:20000
Noonan-Flaxton fine sandy loams, 3 to 6 percent slopes	E3748B	7	2758490	2qkx1	nd025	1981	1:20000
Noonan-Niobell-Williams loams, 0 to 6 percent slopes	C665B	11582	2596921	2q2k9	nd029	1979	1:20000
Bearpaw-Noonan loams, 0 to 6 percent slopes	C198B	197	2595792	2q2qr	nd029	1979	1:20000
Williams-Noonan loams, 0 to 6 percent slopes	C772B	119	2595795	2q2jj	nd029	1979	1:20000
Miranda-Noonan loams, 3 to 6 percent slopes	C557B	79	2595803	2q2kg	nd029	1979	1:20000
Niobell-Noonan loams, 3 to 6 percent slopes	C661B	8	2595450	2q52b	nd029	1979	1:20000
Williams-Noonan loams, 0 to 6 percent slopes	C772B	4739	2564388	2q2jj	nd043	1985	1:20000
Miranda-Noonan loams, 3 to 6 percent slopes	C557B	3566	2494661	2q2kg	nd043	1985	1:20000
Miranda-Noonan loams, 0 to 3 percent slopes	C557A	3155	2595477	2q2kh	nd043	1985	1:20000
Niobell-Noonan loams, 0 to 3 percent slopes	C661A	334	2596681	2q77l	nd043	1985	1:20000
Niobell-Noonan loams, 3 to 6 percent slopes	C661B	192	2596668	2q52b	nd043	1985	1:20000
Noonan-Miranda loams, 0 to 6 percent slopes	C556B	209	2566459	2q58s	nd045	1966	1:20000
Noonan-Niobell-Williams loams, 0 to 6 percent slopes	C665B	121	2596955	2q2k9	nd045	1966	1:20000
Noonan-Niobell-Williams loams, 0 to 6 percent slopes	C665B	6457	2596966	2q2k9	nd047	1992	1:20000
Bearpaw-Noonan loams, 0 to 6 percent slopes	C198B	12156	2566562	2q2qr	nd051	1992	1:24000
Noonan-Niobell-Williams loams, 0 to 6 percent slopes	C665B	4777	2596978	2q2k9	nd051	1992	1:24000
Niobell-Noonan loams, 3 to 6 percent slopes	C661B	57	2596741	2q52b	nd051	1992	1:24000
Niobell-Noonan loams, 0 to 3 percent slopes	C661A	16	2596757	2q77l	nd051	1992	1:24000
Williams-Noonan loams, 0 to 6 percent slopes	C772B	4	2596728	2q2jj	nd051	1992	1:24000
Noonan-Niobell-Williams loams, 3 to 6 percent slopes	E3517B	5885	2715106	d32v	nd053	2003	1:24000
Noonan-Williams-Niobell loams, 6 to 9 percent slopes	E3521C	1610	2715107	d32w	nd053	2003	1:24000
Noonan-Niobell-Williams loams, 0 to 3 percent slopes	E3517A	843	2715105	2qz93	nd053	2003	1:24000
Noonan-Miranda loams, 0 to 6 percent slopes	C556B	931	2566699	2q58s	nd055	1974	1:20000
Noonan-Miranda loams, 6 to 15 percent slopes	E3515D	234	2662482	2qkx7	nd055	1974	1:20000
Noonan-Miranda loams, 0 to 6 percent slopes	E3515B	191	2662481	2qkx6	nd055	1974	1:20000
Noonan-Flaxton fine sandy loams, 3 to 6 percent slopes	E3748B	4158	2699295	2qkx1	nd057	1976	1:20000
Noonan-Niobell-Williams loams, 3 to 6 percent slopes	E3517B	2253	2699297	d32v	nd057	1976	1:20000
Noonan-Niobell-Williams loams, 0 to 3 percent slopes	E3517A	64	2699296	2qz93	nd057	1976	1:20000
Noonan-Flaxton fine sandy loams, 0 to 3 percent slopes	E3748A	26	2699294	2qz95	nd057	1976	1:20000
Noonan-Niobell-Williams loams, 0 to 6 percent slopes	C665B	5434	2597007	2q2k9	nd061	1988	1:24000
Miranda-Noonan loams, 3 to 6 percent slopes	C557B	1004	2494662	2q2kg	nd061	1988	1:24000
Miranda-Noonan loams, 0 to 3 percent slopes	C557A	292	2595556	2q2kh	nd061	1988	1:24000
Noonan-Niobell-Williams loams, 3 to 6 percent slopes	E3517B	9	2662504	d32v	nd061	1988	1:24000
Noonan-Miranda loams, 0 to 6 percent slopes	E3515B	4	2662529	2qkx6	nd061	1988	1:24000
Noonan-Flaxton fine sandy loams, 3 to 6 percent slopes	E3748B	545	2525977	2qkx1	nd065	1971	1:20000
Noonan-Flaxton fine sandy loams, 0 to 3 percent slopes	E3748A	118	2525976	2qz95	nd065	1971	1:20000
Niobell-Noonan loams, 3 to 6 percent slopes	C661B	7211	2566801	2q52b	nd083	1990	1:20000
Miranda-Noonan loams, 0 to 3 percent slopes	C557A	2669	2566788	2q2kh	nd083	1990	1:20000
Noonan-Niobell-Williams loams, 0 to 6 percent slopes	C665B	869	2597019	2q2k9	nd083	1990	1:20000
Niobell-Noonan loams, 0 to 3 percent slopes	C661A	2444	2566881	2q77l	nd093	1990	1:24000
Noonan-Miranda loams, 0 to 6 percent slopes	C556B	656	2566862	2q58s	nd093	1990	1:24000
Williams-Noonan loams, 0 to 6 percent slopes	C772B	190	2597024	2q2jj	nd093	1990	1:24000
Noonan-Niobell loams	Nn	1147	352533	ctv1	nd101	1967	1:20000
Noonan-Niobell-Williams loams, 0 to 6 percent slopes	C665B	1056	2566893	2q2k9	nd101	1967	1:20000
Noonan-Miranda complex	Nm	276	352532	ctv0	nd101	1967	1:20000
Noonan-Miranda loams, 0 to 6 percent slopes	C556B	158	2566926	2q58s	nd101	1967	1:20000
Miranda-Noonan loams, 0 to 3 percent slopes	C557A	987	2595705	2q2kh	nd103	1966	1:12000
Noonan-Niobell-Williams loams, 0 to 6 percent slopes	C665B	60	2661650	2q2k9	nd103	1966	1:12000
Williams-Noonan loams, 0 to 6 percent slopes	C772B	38	2661647	2q2jj	nd103	1966	1:12000
Miranda-Noonan loams, 3 to 6 percent slopes	C557B	1	2595704	2q2kg	nd103	1966	1:12000
Noonan-Niobell-Williams loams, 0 to 6 percent slopes	C665B	2	2596781	2q2k9	nd105	1993	1:24000
Niobell-Noonan loams, 3 to 6 percent slopes	C661B	40631	2765572	2q52b	sd013	1987	1:20000
Noonan-Miranda loams, 0 to 6 percent slopes	C556B	28568	2765576	2q58s	sd013	1987	1:20000
Williams-Noonan loams, 0 to 6 percent slopes	C772B	2282	2765558	2q2jj	sd013	1987	1:20000
Niobell-Noonan loams, 0 to 3 percent slopes	C661A	662	2765580	2q77l	sd013	1987	1:20000
Williams-Noonan loams, 0 to 6 percent slopes	C772B	3814	2797860	2q2jj	sd021	1978	1:20000
Noonan-Niobell-Williams loams, 0 to 6 percent slopes	C665B	319	2797870	2q2k9	sd021	1978	1:20000
Noonan-Miranda loams, 0 to 6 percent slopes	C556B	194	2797897	2q58s	sd021	1978	1:20000
Williams-Noonan loams, 0 to 4 percent slopes	5	108	354717	cx3h	sd021	1978	1:20000
Niobell-Noonan loams, 3 to 6 percent slopes	C661B	8	2797893	2q52b	sd021	1978	1:20000
Niobell-Noonan loams, 3 to 6 percent slopes	C661B	66478	2798568	2q52b	sd045	1973	1:20000
Noonan-Miranda loams, 0 to 6 percent slopes	C556B	11787	2798572	2q58s	sd045	1973	1:20000
Williams-Bowbells-Noonan loams, 3 to 6 percent slopes	C773B	16215	2798653	2shzg	sd049	1981	1:20000
Max-Niobell-Noonan loams, 3 to 6 percent slopes	C672B	11313	2798672	2rrr7	sd049	1981	1:20000
Noonan-Miranda loams, 0 to 6 percent slopes	C556B	7293	2798642	2q58s	sd049	1981	1:20000
Niobell-Noonan-Max loams, 0 to 3 percent slopes	C650A	6817	2798669	2rrr2	sd049	1981	1:20000
Niobell-Noonan loams, 0 to 3 percent slopes	C661A	3386	2798646	2q77l	sd049	1981	1:20000
Niobell-Noonan-Max loams, 0 to 3 percent slopes	NbA	2844	355185	cxll	sd049	1981	1:20000
Bearpaw-Noonan loams, 0 to 3 percent slopes	C199A	2180	2798660	2rrq3	sd049	1981	1:20000
Bearpaw-Noonan loams, 3 to 6 percent slopes	C199B	805	2798661	2rrq4	sd049	1981	1:20000
Niobell-Noonan loams, 3 to 6 percent slopes	C661B	56	2798638	2q52b	sd049	1981	1:20000
Niobell-Noonan loams, 3 to 6 percent slopes	C661B	41399	2798724	2q52b	sd089	1980	1:20000
Noonan-Miranda loams, 0 to 6 percent slopes	C556B	20909	2798734	2q58s	sd089	1980	1:20000
Noonan gravelly substratum, loam, 0 to 2 percent slopes	C331A	1211	2798762	2rrq8	sd089	1980	1:20000
Niobell-Noonan loams, 0 to 3 percent slopes	C661A	471	2798744	2q77l	sd089	1980	1:20000
Noonan-Niobell-Williams loams, 0 to 6 percent slopes	C665B	90	2798699	2q2k9	sd089	1980	1:20000
Niobell-Noonan loams, 0 to 3 percent slopes	C661A	436	2799468	2q77l	sd107	1983	1:20000
Bearpaw-Noonan loams, 0 to 3 percent slopes	C199A	191	2799475	2rrq3	sd107	1983	1:20000
Bearpaw-Noonan loams, 3 to 6 percent slopes	C199B	181	2799476	2rrq4	sd107	1983	1:20000
Niobell-Noonan loams, 0 to 3 percent slopes	C661A	1975	2799505	2q77l	sd115	1997	1:24000
Niobell-Noonan-Heil complex, 0 to 3 percent slopes	C668A	1570	2799520	2rrr6	sd115	1997	1:24000
Noonan-Miranda loams, 0 to 6 percent slopes	C556B	1054	2799501	2q58s	sd115	1997	1:24000
Max-Niobell-Noonan loams, 3 to 6 percent slopes	C672B	347	2799521	2rrr7	sd115	1997	1:24000
Niobell-Noonan-Max loams, 0 to 3 percent slopes	C650A	273	2799519	2rrr2	sd115	1997	1:24000
Niobell-Noonan loams, 0 to 3 percent slopes	C661A	4325	2800111	2q77l	sd129	1975	1:20000
Niobell-Noonan loams, 3 to 6 percent slopes	C661B	1231	2800101	2q52b	sd129	1975	1:20000
Noonan-Miranda loams, 0 to 6 percent slopes	C556B	1065	2800105	2q58s	sd129	1975	1:20000

Map of Series Extent

Approximate geographic distribution of the NOONAN 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).