Soil Data Explorer - ROLLINGSTONE

Official Series Description

Lab Data Summary

Aggregate lab data for the ROLLINGSTONE soil series. This aggregation is based on all pedons with a current taxon name of ROLLINGSTONE, 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 ROLLINGSTONE were used in the calculation. Source: KSSL snapshot (updated 2020-03-18). 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
105	87P0067	86IA005036	Rollingstone	7	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	43.4497223,-91.3722229
105	87P0074	86IA005043	Rollingstone	7	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	43.4897232,-91.3527756
105	UMN2952	S1979MN0552952	Rollingstone	3	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	43.8166008,-91.351532
105	UMN2953	S1979MN1692953	Rollingstone	3	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	43.8577995,-91.3182831
105	UMN3299	S1980MN1693299	Rollingstone	2	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	43.8723257,-91.435831
105	X61215C2	S1983IA061030	Rollingstone	2	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	42.4087184,-90.6020543
105	X49-915-1	S1983IA097001	Rollingstone	2	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	42.1972159,-90.7351388
105	X3-9-43	S1986IA005043	Rollingstone	2	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	43.4897232,-91.3527756
105	11N0307	S2005WI011002	Rollingstone	6	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	44.4014053,-91.5615234

Water Balance

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

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

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

Competing Series

Soil series competing with ROLLINGSTONE 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 ROLLINGSTONE 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 ROLLINGSTONE 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 ROLLINGSTONE, 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. IA-2011-05-31-54 | Jackson County - 1992

   A cross section indicating the major kinds of parent material in Jackson County (Soil Survey of Jackson County, Iowa; 1992).

Map Units

Map units containing ROLLINGSTONE 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
Rollingstone silt loam, 9 to 14 percent slopes, moderately eroded	915D2	1443	405486	fly6	ia061	1983	1:15840
Rollingstone silt loam, 5 to 9 percent slopes, moderately eroded	915C2	263	405485	fly5	ia061	1983	1:15840
Rollingstone silt loam, 5 to 9 percent slopes	915C	249	405484	fly4	ia061	1983	1:15840
Donatus-Rollingstone silt loams, 9 to 14 percent slopes, moderately eroded	939D2	2823	407577	fp3n	ia097	1988	1:15840
Donatus-Rollingstone silt loams, 14 to 18 percent slopes, moderately eroded	939E2	1027	407578	fp3p	ia097	1988	1:15840
Donatus-Rollingstone silt loams, 18 to 25 percent slopes, moderately eroded	939F2	683	407580	fp3r	ia097	1988	1:15840
Donatus-Rollingstone silt loams, 18 to 25 percent slopes	939F	620	407579	fp3q	ia097	1988	1:15840
Donatus-Rollingstone silt loams, 9 to 14 percent slopes	939D	392	407576	fp3m	ia097	1988	1:15840
Nodine-Rollingstone silt loams, 12 to 20 percent slopes, eroded	586D2	14757	398306	fcgl	mn055	1981	1:15840
Nodine-Rollingstone silt loams, 4 to 12 percent slopes, eroded	586C2	2703	398305	fcgk	mn055	1981	1:15840
Rollingstone silt loam, 12 to 20 percent slopes	198D	4738	429016	gdf7	mn169	1987	1:20000
Rollingstone silt loam, 3 to 12 percent slopes	198C	2461	429015	gdf6	mn169	1987	1:20000
Nodine-Rollingstone silt loams, 4 to 12 percent slopes	586C	1619	429077	gdh6	mn169	1987	1:20000
Nodine-Rollingstone silt loams, 12 to 20 percent slopes	586D	1217	429078	gdh7	mn169	1987	1:20000

Map of Series Extent

Approximate geographic distribution of the ROLLINGSTONE 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).