Soil Data Explorer - BROOKINGS

Official Series Description

Lab Data Summary

Aggregate lab data for the BROOKINGS soil series. This aggregation is based on all pedons with a current taxon name of BROOKINGS, 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 BROOKINGS 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
102A	40A2411	S1957SD029001	Brookings	3	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	44.8327599,-97.1192398
102A	95P0214	S1994SD011009	Brookings	7	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	44.4158325,-96.7275009

Water Balance

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

Competing Series

Soil series competing with BROOKINGS 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 BROOKINGS 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 BROOKINGS 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 hills figure.

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

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

Soil series sharing subgroup-level classification with BROOKINGS, 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. SD-2010-11-01-02 | Brookings County - 2004

   Typical pattern of soils and parent material in the Kranzburg-Brookings association (Soil Survey of Brookings County, South Dakota; 2004).

2. SD-2010-11-01-09 | Hamlin County - 2003

   Typical pattern of soils and underlying material in the Kranzburg-Brookings association (Soil Survey of Hamlin County, South Dakota; 2003).

3. SD-2012-03-15-02 | Codington County - December 1966

   Diagram showing the relative position of the major soils in association 3 (Soil Survey of Codington County, SD; 1966).

4. SD-2012-03-15-17 | Day County - August 1997

   Typical pattern of soils and underlying material in the Harmony-Aberdee-Nahon and Kranzburg-Brookings associations (Soil Survey of Day County, SD; 1997).

5. SD-2012-03-15-27 | Deuel County - November 1997

   Typical pattern of soils and parent material in the Kranzburg-Brookings association (Soil Survey of Deuel County, SD; 1997).

6. SD-2012-03-15-81 | Minnehaha County - June 1964

   Block diagram showing the geographical association of the soils in association 9. Here, the soils formed in loess and till (Soil Survey of Minnehaha County, SD; 1964).

7. SD-2012-03-15-84 | Moody County - April 1989

   Pattern of soils and parent material in the Kranzburg-Houdek association (Soil Survey of Moody County, SD; 1989).

Map Units

Map units containing BROOKINGS 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
Kranzburg-Brookings silty clay loams, 1 to 6 percent slopes	J90B	17916	991439	2wkp4	mn081	2007	1:12000
Brookings silty clay loam, 0 to 2 percent slopes	J71A	6895	991432	2wkp5	mn081	2007	1:12000
Vienna-Brookings complex, 1 to 6 percent slopes	J79B	1186	991442	2wkpx	mn081	2007	1:12000
Vienna-Brookings complex, 1 to 6 percent slopes	J79B	3978	988905	2wkpx	mn101	2008	1:12000
Kranzburg-Brookings silty clay loams, 1 to 6 percent slopes	J90B	1	1947682	2wkp4	mn101	2008	1:12000
Kranzburg-Brookings silty clay loams, 1 to 6 percent slopes	J90B	54508	780322	2wkp4	mn117	2005	1:12000
Brookings silty clay loam, 0 to 2 percent slopes	J71A	46211	780265	2wkp5	mn117	2005	1:12000
Vienna-Brookings complex, 1 to 6 percent slopes	J79B	3789	780668	2wkpx	mn117	2005	1:12000
Kranzburg-Brookings silty clay loams, 1 to 6 percent slopes	KrB	29703	418768	2wkp4	sd011	1995	1:24000
Kranzburg-Brookings silty clay loams, 0 to 2 percent slopes	KrA	20378	418767	2wkp2	sd011	1995	1:24000
Vienna-Brookings complex, 1 to 6 percent slopes	VbB	12908	418818	2wkpx	sd011	1995	1:24000
Vienna-Brookings complex, 0 to 2 percent slopes	VbA	9686	418817	2wkpw	sd011	1995	1:24000
Brookings silty clay loam, 0 to 2 percent slopes	Bf	3556	418724	2wkp5	sd011	1995	1:24000
Kranzburg-Brookings silt loams, 0 to 2 percent slopes	G790A	8681	2797820	2sd5q	sd013	1987	1:20000
Kranzburg-Brookings-Buse complex, 0 to 6 percent slopes	G792B	2721	2797822	2sd5x	sd013	1987	1:20000
Kranzburg-Brookings silt loams, 2 to 6 percent slopes	G790B	404	2797821	2sd5r	sd013	1987	1:20000
Vienna-Brookings complex, 1 to 6 percent slopes	Z192B	28105	2765246	2wkpx	sd029	2006	1:12000
Vienna-Brookings complex, 0 to 2 percent slopes	Z192A	19321	2765245	2wkpw	sd029	2006	1:12000
Kranzburg-Brookings silty clay loams, 0 to 2 percent slopes	J143A	16463	1684436	2wkp2	sd029	2006	1:12000
Kranzburg-Brookings silty clay loams, 1 to 6 percent slopes	J143B	8233	1684438	2wkp4	sd029	2006	1:12000
Brookings silty clay loam, 0 to 2 percent slopes	Z190A	2374	2765244	2wkp5	sd029	2006	1:12000
Kranzburg-Brookings silt loams, 0 to 2 percent slopes	G790A	32151	2798526	2sd5q	sd037	1992	1:20000
Kranzburg-Brookings-Buse complex, 0 to 6 percent slopes	G792B	11853	2798528	2sd5x	sd037	1992	1:20000
Kranzburg-Brookings silt loams, 2 to 6 percent slopes	G790B	3061	2798527	2sd5r	sd037	1992	1:20000
Vienna-Brookings complex, 1 to 6 percent slopes	VoB	2082	417142	2wkpx	sd037	1992	1:20000
Vienna-Brookings complex, 0 to 2 percent slopes	VoA	510	417141	2wkpw	sd037	1992	1:20000
Kranzburg-Brookings-Buse complex, 1 to 6 percent slopes	KrB	56	417092	g00l	sd037	1992	1:20000
Kranzburg-Brookings silt loams, 0 to 2 percent slopes	Ks	37	417093	g00m	sd037	1992	1:20000
Kranzburg-Brookings silty clay loams, 1 to 6 percent slopes	KrB	34581	416867	2wkp4	sd039	1992	1:20000
Vienna-Brookings complex, 1 to 6 percent slopes	VtB	22547	416911	2wkpx	sd039	1992	1:20000
Kranzburg-Brookings silty clay loams, 0 to 2 percent slopes	KrA	15185	416866	2wkp2	sd039	1992	1:20000
Vienna-Brookings complex, 0 to 2 percent slopes	VrA	7437	416910	2wkpw	sd039	1992	1:20000
Brookings silty clay loam, 0 to 2 percent slopes	Br	1571	416839	2wkp5	sd039	1992	1:20000
Kranzburg-Brookings silty clay loams, 2 to 9 percent slopes	KrC	1276	416868	fzsc	sd039	1992	1:20000
Vienna-Brookings complex, 1 to 6 percent slopes	Z192B	13515	2712902	2wkpx	sd051	1977	1:20000
Vienna-Brookings complex, 0 to 2 percent slopes	Z192A	10027	2712901	2wkpw	sd051	1977	1:20000
Brookings silty clay loam, 0 to 2 percent slopes	Z190A	602	2712900	2wkp5	sd051	1977	1:20000
Vienna-Brookings complex, 1 to 6 percent slopes	VbB	17531	417319	2wkpx	sd057	1992	1:20000
Kranzburg-Brookings silty clay loams, 1 to 6 percent slopes	KrB	6115	417283	2wkp4	sd057	1992	1:20000
Vienna-Brookings complex, 0 to 2 percent slopes	VbA	5074	417318	2wkpw	sd057	1992	1:20000
Kranzburg-Brookings silty clay loams, 0 to 2 percent slopes	KrA	1941	417282	2wkp2	sd057	1992	1:20000
Brookings silty clay loam, 0 to 2 percent slopes	Bs	559	417255	2wkp5	sd057	1992	1:20000
Vienna-Brookings complex, 1 to 6 percent slopes	VbB	2204	417521	2wkpx	sd077	1992	1:20000
Vienna-Brookings complex, 0 to 2 percent slopes	VbA	834	417520	2wkpw	sd077	1992	1:20000
Kranzburg-Brookings silt loams, 0 to 2 percent slopes	G790A	12841	2799374	2sd5q	sd091	1970	1:20000
Kranzburg-Brookings silt loams, 2 to 6 percent slopes	G790B	8494	2799375	2sd5r	sd091	1970	1:20000
Kranzburg-Brookings-Buse complex, 0 to 6 percent slopes	G792B	1525	2799380	2sd5x	sd091	1970	1:20000
Kranzburg-Brookings silty clay loams, 1 to 6 percent slopes	KaB	18313	418340	2wkp4	sd101	1985	1:20000
Kranzburg-Brookings silty clay loams, 0 to 2 percent slopes	KbA	3020	418341	2wkp2	sd101	1985	1:20000
Vienna-Brookings complex, 1 to 6 percent slopes	Z192B	8683	2712797	2wkpx	sd109	1977	1:20000
Vienna-Brookings complex, 0 to 2 percent slopes	Z192A	2978	2712796	2wkpw	sd109	1977	1:20000
Kranzburg-Brookings silt loams, 0 to 2 percent slopes	G790A	6888	2800034	2sd5q	sd115	1997	1:24000
Kranzburg-Brookings-Buse complex, 0 to 6 percent slopes	G792B	5557	2800036	2sd5x	sd115	1997	1:24000
Kranzburg-Brookings silt loams, 2 to 6 percent slopes	G790B	314	2800035	2sd5r	sd115	1997	1:24000

Map of Series Extent

Approximate geographic distribution of the BROOKINGS 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).