Soil Data Explorer - NUNEMAKER

Official Series Description

Lab Data Summary

Aggregate lab data for the NUNEMAKER soil series. This aggregation is based on all pedons with a current taxon name of NUNEMAKER, 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 NUNEMAKER were used in the calculation. Source: KSSL snapshot (updated 2020-03-18). Methods used to assemble the KSSL snapshot used by SoilWeb / SDE

There are insufficient data to create the lab data summary figure.

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the NUNEMAKER 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 NUNEMAKER series. Sketches are arranged according to their subgroup-level taxonomic structure. Source: SSURGO snapshot (updated 2024-02-21), parsed OSD records (updated 2023-10-06) and snapshot of SC database (updated 2023-10-02).

Select annual climate data summaries for the NUNEMAKER 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 NUNEMAKER 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 NUNEMAKER share the same family level classification in Soil Taxonomy. Source: parsed OSD records (updated 2023-10-06) and snapshot of the SC database (updated 2023-10-02).

Select annual climate data summaries for the NUNEMAKER 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).

Geomorphic description summaries for the NUNEMAKER 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 3D mountains figure.

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

Soil series sharing subgroup-level classification with NUNEMAKER, 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

No block diagrams are available.

Map Units

Map units containing NUNEMAKER 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
Nunemaker clay, 3 to 10 percent slopes	70	2587	502107	jvh0	co675	1986	1:24000
Nunemaker clay loam, 3 to 12 percent slopes	143	1259	497106	jp8p	co686	1992	1:31680
Nunemaker silty clay loam, calcareous, 0 to 4 percent slopes	631B	5795	344236	ck6d	mt051	1992	1:24000
Nunemaker silty clay loam, 0 to 4 percent slopes	63B	4888	344238	ck6g	mt051	1992	1:24000
Nunemaker silty clay loam, calcareous, 4 to 8 percent slopes	631C	921	344237	ck6f	mt051	1992	1:24000
Nunemaker silty clay loam, 4 to 8 percent slopes	63C	603	344239	ck6h	mt051	1992	1:24000
Nunemaker silty clay loam, 0 to 4 percent slopes	29B	14228	345116	cl3s	mt101	1992	1:24000
Nunemaker silty clay loam, 4 to 8 percent slopes	29C	2707	345117	cl3t	mt101	1992	1:24000
Marias-Nunemaker complex, 0 to 4 percent slopes	50B	33583	348694	cpv6	mt657	1990	1:24000
Nunemaker silty clay loam, 0 to 4 percent slopes	250B	16002	348498	cpmw	mt657	1990	1:24000
Ethridge-Nunemaker silty clay loams, 0 to 4 percent slopes	539B	11760	348709	cpvp	mt657	1990	1:24000
Nunemaker silty clay loam, 4 to 8 percent slopes	250C	5403	348499	cpmx	mt657	1990	1:24000
Nunemaker-Marias complex, 4 to 8 percent slopes	550C	2930	348717	cpvy	mt657	1990	1:24000
Nunemaker-Ethridge silty clay loams, 4 to 8 percent slopes	650C	2673	348765	cpxh	mt657	1990	1:24000

Map of Series Extent

Approximate geographic distribution of the NUNEMAKER 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).