Soil Data Explorer - BURKHARDT

Official Series Description

Lab Data Summary

Aggregate lab data for the BURKHARDT soil series. This aggregation is based on all pedons with a current taxon name of BURKHARDT, 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 BURKHARDT 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
104	X65285-2-1	S1962IA065005	Burkhardt	2	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	43.0629006,-92.0623559
104	X65285-2-1B	S1962IA065006	Burkhardt	2	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	43.056249,-92.07734
104	X45-285-1	S1965IA089916	Burkhardt	2	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	43.29525,-92.20419
104	X28-285B-1	S1979IA055003	Burkhardt	2	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	42.5338143,-91.5626198
105	78IL085012	1978IL085012	Burkhardt	1	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	42.4841417,-90.4419278
105	X23-285-1	S1972IA045001	Burkhardt	3	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	41.9025504,-90.181652
105	78P0219	S1977WI017005	Burkhardt	4	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	44.8576532,-91.4567152
105	93P0380	S1992WI033004	Burkhardt	6	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	44.8066673,-91.7311096
90B	98P0080	S1979WI017002	Burkhardt	4	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	44.9806,-91.37681
91A	UMN2415	S1977MN037008 (2415)	Burkhardt	2	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	44.6927872,-92.7672729

Water Balance

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

Soil series sharing subgroup-level classification with BURKHARDT, 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. WI-2010-11-08-07 | Pepin County - 2002

   Typical pattern of soils and parent material in the Finchford-Plainfield-Burkhardt and Algansee-Kalmarville-Scotah associations (Soil Survey of Pepin County, Wisconsin; 2002).

2. WI-2012-03-23-30 | Pepin County - March 1964

   Cross section showing the geology and the associated soils in Pepin County (Soil Survey of Pepin County, WI; 1964).

Map Units

Map units containing BURKHARDT 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
Burkhardt sandy loam, 2 to 9 percent slopes	285C	319	402866	fj6p	ia011	1977	1:15840
Burkhardt-Bassett-Chelsea complex, 18 to 60 percent slopes	1285G	345	473078	30qwj	ia013	2001	1:12000
Burkhardt sandy loam, 0 to 2 percent slopes, rarely flooded	285	418	2220245	2djbt	ia017	2008	1:12000
Burkhardt sandy loam, 2 to 9 percent slopes, rarely flooded	285C	298	2220246	2djbv	ia017	2008	1:12000
Burkhardt-Saude complex, 2 to 5 percent slopes	241B	2266	403225	fjl8	ia019	1978	1:15840
Saude-Burkhardt complex, 2 to 9 percent slopes, moderately eroded	241C2	1520	403384	fjrd	ia023	1978	1:15840
Burkhardt sandy loam, 2 to 9 percent slopes	285C	569	403390	fjrl	ia023	1978	1:15840
Saude-Burkhardt complex, 9 to 18 percent slopes, moderately eroded	241E2	270	403385	fjrf	ia023	1978	1:15840
Burkhardt sandy loam, 2 to 5 percent slopes	285B	1586	404019	fkdw	ia037	1989	1:15840
Burkhardt sandy loam, 5 to 14 percent slopes	285D	951	404022	fkdz	ia037	1989	1:15840
Burkhardt sandy loam, 0 to 2 percent slopes	285	475	404018	fkdv	ia037	1989	1:15840
Burkhardt sandy loam, 5 to 14 percent slopes	285D	483	404398	fkt3	ia045	1978	1:15840
Burkhardt sandy loam, 14 to 25 percent slopes, moderately erode	285F2	449	404399	fkt4	ia045	1978	1:15840
Burkhardt sandy loam, 2 to 5 percent slopes	285B	141	404397	fkt2	ia045	1978	1:15840
Burkhardt-Saude complex, 2 to 5 percent slopes	241B	2325	405029	flgg	ia055	1984	1:15840
Burkhardt sandy loam, 2 to 5 percent slopes	285B	361	405032	flgk	ia055	1984	1:15840
Burkhardt sandy loam, 5 to 14 percent slopes	285D	194	405414	flvw	ia061	1983	1:15840
Burkhardt sandy loam, 2 to 5 percent slopes	285B	1211	405754	fm6v	ia065	1975	1:15840
Burkhardt sandy loam, 5 to 9 percent slopes, moderately eroded	285C2	967	405755	fm6w	ia065	1975	1:15840
Burkhardt sandy loam, 0 to 2 percent slopes	285	243	405753	fm6t	ia065	1975	1:15840
Burkhardt sandy loam, 9 to 18 percent slopes, moderately eroded	285E2	197	405756	fm6x	ia065	1975	1:15840
Burkhardt sandy loam, 5 to 9 percent slopes	285C	817	405902	fmcm	ia067	1989	1:15840
Burkhardt sandy loam, 2 to 5 percent slopes	285B	788	405901	fmcl	ia067	1989	1:15840
Burkhardt sandy loam, 14 to 30 percent slopes	285F	192	405904	fmcp	ia067	1989	1:15840
Burkhardt sandy loam, 3 to 9 percent slopes	285C	569	406937	fng0	ia089	1969	1:15840
Burkhardt sandy loam, 5 to 9 percent slopes	285C	339	407990	fpjz	ia103	1979	1:15840
Burkhardt sandy loam, 9 to 14 percent slopes, moderately eroded	285D2	489	408598	fq5l	ia113	1970	1:15840
Burkhardt sandy loam, 2 to 9 percent slopes	285C	306	408597	fq5k	ia113	1970	1:15840
Burkhardt sandy loam, 3 to 9 percent slopes	285C	362	409660	fr8v	ia131	1971	1:15840
Burkhardt sandy loam, 0 to 3 percent slopes	285	143	409659	fr8t	ia131	1971	1:15840
Burkhardt loam, 14 to 25 percent slopes	285F	842	1399089	1hyvx	ia191	2005	1:12000
Burkhardt loam, 2 to 5 percent slopes	285B	129	437382	gp43	ia191	2005	1:12000
Burkhardt-Saude complex, 0 to 2 percent slopes	961A	765	198770	6nty	il161	2002	1:12000
Burkhardt sandy loam, 6 to 12 percent slopes	151C	1769	396781	f9wd	mn037	1980	1:15840
Burkhardt sandy loam, 12 to 18 percent slopes	151D	730	396782	f9wf	mn037	1980	1:15840
Burkhardt sandy loam, very gravelly substratum, 0 to 3 percent slopes	N628A	1439	1690742	1trc2	mn049	2007	1:12000
Burkhardt sandy loam, 0 to 6 percent slopes	N623B	520	1690451	1tr1p	mn049	2007	1:12000
Burkhardt loam, 0 to 2 percent slopes	BrA	1060	2216299	2dd7j	mn157	2008	1:12000
Burkhardt sandy loam, 0 to 2 percent slopes	BtA	1053	2216301	2dd7l	mn157	2008	1:12000
Burkhardt sandy loam, 2 to 6 percent slopes	BtB	447	2216302	2dd7m	mn157	2008	1:12000
Burkhardt sandy loam, 6 to 12 percent slopes, moderately eroded	BtC2	240	2216304	2dd7p	mn157	2008	1:12000
Burkhardt loam, 2 to 6 percent slopes	BrB	176	2216300	2dd7k	mn157	2008	1:12000
Burkhardt gravelly sandy loam, 2 to 6 percent slopes	BkB	144	2216298	2dd7h	mn157	2008	1:12000
Burkhardt gravelly sandy loam, 0 to 2 percent slopes	BkA	115	2216297	2dd7g	mn157	2008	1:12000
Burkhardt sandy loam, 0 to 3 percent slopes	151	929	1677061	1t93r	mn163	1978	1:15840
Burkhardt sandy loam, 3 to 9 percent slopes	151B	597	1677062	1t93s	mn163	1978	1:15840
Burkhardt sandy loam, 0 to 3 percent slopes	453A	380	2561687	1vgbr	wi011	1960	1:12000
Burkhardt sandy loam, 2 to 6 percent slopes	453B	346	2561688	1vgbs	wi011	1960	1:12000
Burkhardt sandy loam, 0 to 3 percent slopes	BuA	9986	421501	g4lt	wi017	1985	1:15840
Burkhardt sandy loam, 2 to 6 percent slopes	453B	1306	2518441	1vgbs	wi033	2003	1:12000
Burkhardt sandy loam, 0 to 3 percent slopes	453A	782	2517809	1vgbr	wi033	2003	1:12000
Burkhardt sandy loam, 0 to 3 percent slopes	453A	225	3099714	1vgbr	wi035	1974	1:12000
Burkhardt sandy loam, 0 to 3 percent slopes	453A	3511	2517810	1vgbr	wi091	1998	1:12000
Burkhardt sandy loam, 2 to 6 percent slopes	453B	382	2518442	1vgbs	wi091	1998	1:12000
Burkhardt sandy loam, 0 to 3 percent slopes	453A	620	1691012	1trms	wi093	2006	1:12000
Burkhardt sandy loam, 2 to 6 percent slopes	453B	257	1703737	1v5w8	wi093	2006	1:12000
Burkhardt sandy loam, 2 to 6 percent slopes	BpB	3241	421151	g47j	wi095	1978	1:15840
Burkhardt sandy loam, 0 to 2 percent slopes	BpA	2359	421150	g47h	wi095	1978	1:15840
Burkhardt sandy loam, 6 to 12 percent slopes, eroded	BpC2	1164	421152	g47k	wi095	1978	1:15840
Burkhardt-Sattre complex, 6 to 12 percent slopes, eroded	BxC2	10977	422120	g57s	wi109	1975	1:15840
Burkhardt-Sattre complex, 12 to 30 percent slopes, eroded	BxD2	8754	422121	g57t	wi109	1975	1:15840
Burkhardt-Sattre complex, 2 to 6 percent slopes	BxB	4693	422119	g57r	wi109	1975	1:15840
Burkhardt sandy loam, 6 to 12 percent slopes, eroded	BrC2	2388	422118	g57q	wi109	1975	1:15840
Burkhardt sandy loam, 1 to 6 percent slopes	BrB	2348	422117	g57p	wi109	1975	1:15840

Map of Series Extent

Approximate geographic distribution of the BURKHARDT 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).