Soil Data Explorer - MANNING

Official Series Description

Lab Data Summary

Aggregate lab data for the MANNING soil series. This aggregation is based on all pedons with a current taxon name of MANNING, 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 MANNING 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
53B	89P0142	88ND105117	Manning	5	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	48.5549583435059,-103.644508361816
54	40A0081	58ND089001	Manning	7	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	46.8613471984863,-102.902793884277
54	72ND011001	72ND011001	Manning	4	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	46.1480124,-103.1830731

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the MANNING 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 MANNING series. Sketches are arranged according to their subgroup-level taxonomic structure. Source: SSURGO snapshot (updated 2024-02-21), parsed OSD records (updated 2023-10-02) and snapshot of SC database (updated 2023-10-02).

Select annual climate data summaries for the MANNING 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 2023-10-09).

Geomorphic description summaries for the MANNING 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 2023-10-04).

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

Competing Series

Soil series competing with MANNING share the same family level classification in Soil Taxonomy. Source: parsed OSD records (updated 2023-10-02) and snapshot of the SC database (updated 2023-10-02).

Select annual climate data summaries for the MANNING 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 2023-10-09).

There are insufficient data to create the annual climate figure.

Geomorphic description summaries for the MANNING 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 2023-10-04).

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 MANNING, 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 2023-10-02).

Block Diagrams

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

1. ND-2010-09-27-14 | Morton County - 2002

   Typical pattern of soils and underlying materials in the Straw-Parshall-Manning-Stady association (Soil Survey of Morton County, North Dakota; 2002).

2. ND-2012-02-08-33 | Mountrail County - June 1991

   Typical pattern of soils and parent material in the Manning-Livona-Lihen association (Soil Survey of Mountrail County, North Dakota; June 1991).

3. ND-2012-02-08-53 | Stark County - February 1968

   Diagram showinig the relationship of some of the major soils in Stark County (Soil Survey of Stark County, North Dakota; February 1968).

Map Units

Map units containing MANNING 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
Manning coarse sandy loam, 0 to 6 percent slopes	MaB	26336	348860	cq0k	mt091	1971	1:24000
Parshall, gravelly substratum-Manning fine sandy loams, 0 to 2 percent slopes	E4581A	3957	2755669	2qz8v	nd001	1983	1:20000
Manning fine sandy loam, 0 to 2 percent slopes	E4585A	3782	2525760	1vzwd	nd001	1983	1:20000
Parshall, gravelly substratum-Manning fine sandy loams, 2 to 6 percent slopes	E4581B	3452	2755670	2r4fn	nd001	1983	1:20000
Manning fine sandy loam, 2 to 6 percent slopes	E4585B	2259	2525761	1vzwf	nd001	1983	1:20000
Manning-Schaller-Wabek complex, 6 to 35 percent slopes	E4561F	145	2525773	2r4ff	nd001	1983	1:20000
Manning-Wabek complex, 6 to 9 percent slopes	E4559C	104	2755665	2r4fd	nd001	1983	1:20000
Manning-Schaller-Wabek complex, 6 to 35 percent slopes	E4561F	2265	2707110	2r4ff	nd007	1998	1:24000
Manning fine sandy loam, 2 to 6 percent slopes	E4585B	1735	2707111	1vzwf	nd007	1998	1:24000
Manning fine sandy loam, 0 to 2 percent slopes	E4585A	318	1715194	1vzwd	nd007	1998	1:24000
Parshall, gravelly substratum-Manning fine sandy loams, 2 to 6 percent slopes	E4581B	28	2758437	2r4fn	nd007	1998	1:24000
Manning-Schaller-Wabek complex, 6 to 35 percent slopes	E4561F	2966	2563580	2r4ff	nd011	1969	1:20000
Manning fine sandy loam, 0 to 2 percent slopes	E4585A	2208	2563578	1vzwd	nd011	1969	1:20000
Manning fine sandy loam, 2 to 6 percent slopes	E4585B	1612	2563579	1vzwf	nd011	1969	1:20000
Manning-Wabek complex, 6 to 9 percent slopes	E4559C	915	2563581	2r4fd	nd011	1969	1:20000
Parshall, gravelly substratum-Manning fine sandy loams, 0 to 2 percent slopes	E4581A	195	2758459	2qz8v	nd011	1969	1:20000
Manning fine sandy loam, 2 to 6 percent slopes	MaB	131	992857	12b4n	nd011	1969	1:20000
Lehr, Manning, and Wabek soils, 6 to 9 percent slopes	LmC	103	992855	12b4l	nd011	1969	1:20000
Manning fine sandy loam, 0 to 2 percent slopes	MaA	99	992856	12b4m	nd011	1969	1:20000
Manning-Schaller-Wabek complex, 6 to 35 percent slopes	E4561F	3958	2707258	2r4ff	nd025	1981	1:20000
Manning fine sandy loam, 2 to 6 percent slopes	E4585B	2808	1714661	1vzwf	nd025	1981	1:20000
Manning-Wabek complex, 6 to 9 percent slopes	E4559C	1422	2707257	2r4fd	nd025	1981	1:20000
Parshall, gravelly substratum-Manning fine sandy loams, 2 to 6 percent slopes	E4581B	330	2758475	2r4fn	nd025	1981	1:20000
Manning fine sandy loam, 0 to 2 percent slopes	E4585A	216	2707259	1vzwd	nd025	1981	1:20000
Parshall, gravelly substratum-Manning fine sandy loams, 0 to 2 percent slopes	E4581A	170	2758474	2qz8v	nd025	1981	1:20000
Manning fine sandy loam, 0 to 6 percent slopes	C840B	536	2564331	2q536	nd029	1979	1:20000
Manning fine sandy loam, 2 to 6 percent slopes	E4585B	344	2661789	1vzwf	nd029	1979	1:20000
Manning-Schaller-Wabek complex, 6 to 35 percent slopes	E4561F	18026	2525893	2r4ff	nd037	1985	1:20000
Manning fine sandy loam, 2 to 6 percent slopes	E4585B	6570	2525894	1vzwf	nd037	1985	1:20000
Manning fine sandy loam, 0 to 2 percent slopes	E4585A	4550	1715509	1vzwd	nd037	1985	1:20000
Parshall, gravelly substratum-Manning fine sandy loams, 0 to 2 percent slopes	E4581A	1665	2759660	2qz8v	nd037	1985	1:20000
Parshall, gravelly substratum-Manning fine sandy loams, 2 to 6 percent slopes	E4581B	1517	2759661	2r4fn	nd037	1985	1:20000
Manning-Wabek complex, 6 to 9 percent slopes	E4559C	15	2759656	2r4fd	nd037	1985	1:20000
Manning-Schaller-Wabek complex, 6 to 35 percent slopes	E4561F	6875	2525824	2r4ff	nd041	1986	1:20000
Parshall, gravelly substratum-Manning fine sandy loams, 2 to 6 percent slopes	E4581B	5635	2525826	2r4fn	nd041	1986	1:20000
Manning fine sandy loam, 2 to 6 percent slopes	E4585B	4512	2525827	1vzwf	nd041	1986	1:20000
Manning fine sandy loam, 0 to 2 percent slopes	E4585A	4181	1718611	1vzwd	nd041	1986	1:20000
Parshall, gravelly substratum-Manning fine sandy loams, 0 to 2 percent slopes	E4581A	2675	2525825	2qz8v	nd041	1986	1:20000
Manning-Wabek complex, 6 to 9 percent slopes	E4559C	21	2755691	2r4fd	nd041	1986	1:20000
Manning fine sandy loam, 0 to 6 percent slopes	C840B	124	2596709	2q536	nd047	1992	1:20000
Manning fine sandy loam, 0 to 6 percent slopes	C840B	294	2596749	2q536	nd051	1992	1:24000
Manning-Schaller-Wabek complex, 6 to 35 percent slopes	E4561F	4383	2699359	2r4ff	nd053	2003	1:24000
Manning fine sandy loam, 2 to 6 percent slopes	E4585B	1733	2699361	1vzwf	nd053	2003	1:24000
Manning fine sandy loam, 0 to 2 percent slopes	E4585A	113	2699360	1vzwd	nd053	2003	1:24000
Parshall, gravelly substratum-Manning fine sandy loams, 2 to 6 percent slopes	E4581B	250	2755735	2r4fn	nd057	1976	1:20000
Parshall, gravelly substratum-Manning fine sandy loams, 0 to 2 percent slopes	E4581A	67	2755734	2qz8v	nd057	1976	1:20000
Manning fine sandy loam, 2 to 6 percent slopes	E4585B	4099	2699186	1vzwf	nd059	1998	1:20000
Wabek-Manning complex, 6 to 15 percent slopes	E4555D	3319	2699227	cdph	nd059	1998	1:20000
Manning fine sandy loam, 0 to 2 percent slopes	E4585A	623	2699185	1vzwd	nd059	1998	1:20000
Manning-Wabek complex, 6 to 9 percent slopes	E4559C	379	2759682	2r4fd	nd059	1998	1:20000
Parshall, gravelly substratum-Manning fine sandy loams, 0 to 2 percent slopes	E4581A	369	2759686	2qz8v	nd059	1998	1:20000
Manning-Schaller-Wabek complex, 6 to 35 percent slopes	E4561F	86	2759683	2r4ff	nd059	1998	1:20000
Parshall, gravelly substratum-Manning fine sandy loams, 2 to 6 percent slopes	E4581B	470	2755719	2r4fn	nd065	1971	1:20000
Parshall, gravelly substratum-Manning fine sandy loams, 0 to 2 percent slopes	E4581A	31	2755718	2qz8v	nd065	1971	1:20000
Manning-Schaller-Wabek complex, 6 to 35 percent slopes	E4561F	6924	2699106	2r4ff	nd085	1992	1:24000
Manning fine sandy loam, 0 to 2 percent slopes	E4585A	2629	2699104	1vzwd	nd085	1992	1:24000
Manning fine sandy loam, 2 to 6 percent slopes	E4585B	2206	2699105	1vzwf	nd085	1992	1:24000
Manning-Wabek complex, 6 to 9 percent slopes	E4559C	991	2699107	2r4fd	nd085	1992	1:24000
Parshall, gravelly substratum-Manning fine sandy loams, 0 to 2 percent slopes	E4581A	837	2759708	2qz8v	nd085	1992	1:24000
Parshall, gravelly substratum-Manning fine sandy loams, 2 to 6 percent slopes	E4581B	784	2759709	2r4fn	nd085	1992	1:24000
Manning-Schaller-Wabek complex, 6 to 35 percent slopes	E4561F	9079	2715868	2r4ff	nd087	1974	1:20000
Manning-Wabek complex, 6 to 9 percent slopes	E4559C	2732	2715867	2r4fd	nd087	1974	1:20000
Manning fine sandy loam, 2 to 6 percent slopes	E4585B	2046	2715872	1vzwf	nd087	1974	1:20000
Manning fine sandy loam, 0 to 2 percent slopes	E4585A	1430	2715871	1vzwd	nd087	1974	1:20000
Parshall, gravelly substratum-Manning fine sandy loams, 2 to 6 percent slopes	E4581B	291	2758511	2r4fn	nd087	1974	1:20000
Parshall, gravelly substratum-Manning fine sandy loams, 0 to 2 percent slopes	E4581A	55	2758510	2qz8v	nd087	1974	1:20000
Manning-Schaller-Wabek complex, 6 to 35 percent slopes	E4561F	8255	2716021	2r4ff	nd089	1965	1:20000
Manning fine sandy loam, 0 to 2 percent slopes	E4585A	5145	1713579	1vzwd	nd089	1965	1:20000
Manning fine sandy loam, 2 to 6 percent slopes	E4585B	4701	1713580	1vzwf	nd089	1965	1:20000
Parshall, gravelly substratum-Manning fine sandy loams, 0 to 2 percent slopes	E4581A	238	2759690	2qz8v	nd089	1965	1:20000
Parshall, gravelly substratum-Manning fine sandy loams, 2 to 6 percent slopes	E4581B	38	2759691	2r4fn	nd089	1965	1:20000
Manning sandy loam, nearly level	MgA	84	352522	cttp	nd101	1967	1:20000
Manning sandy loam, undulating	MgB	54	352523	cttq	nd101	1967	1:20000
Manning fine sandy loam, 0 to 6 percent slopes	MaB	7729	354636	cx0w	sd105	1977	1:24000

Map of Series Extent

Approximate geographic distribution of the MANNING 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 2023-10-04).