Soil Data Explorer - CHASEBURG

Official Series Description

Lab Data Summary

Aggregate lab data for the CHASEBURG soil series. This aggregation is based on all pedons with a current taxon name of CHASEBURG, 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 CHASEBURG 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
104	X53-142-1	S1982IA105002NEED TO CHANGE ID!	Chaseburg	2	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	42.2590337,-91.2031605
105	UMN1215	S1970MN0491215	Chaseburg	3	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	44.3870811,-92.6162491
105	UMN1251	S1971MN0451251	Chaseburg	3	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	43.6454659,-92.2336273
105	UMN1541	S1972MN1691541	Chaseburg	3	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	44.120018,-91.9993668
105	X22-142-1	S1973IA043002	Chaseburg	2	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	42.8409194,-91.5647877
105	UMN2082	S1975MN055060	Chaseburg	3	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	43.7058071,-91.3863883
105	UMN1960	S1975MN1091960	Chaseburg	3	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	43.9308853,-92.2088776
105	X49-142-2	S1982IA097001	Chaseburg	2	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	42.1670252,-90.8930409
105	X3-142-1	S1986IA005001	Chaseburg	2	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	43.4914321,-91.4371339
105	X49-87-4	S1987IA097001	Chaseburg	2	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	42.1177827,-90.4990928
105	X49-87-3	S1987IA097002	Chaseburg	2	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	42.0466472,-90.8567213
n/a	X49-142-1	S1985IA097001	Chaseburg	2	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	n/a

Water Balance

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

Soil series sharing subgroup-level classification with CHASEBURG, 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. IA-2011-05-31-19 | Dubuque County - 1986

   Typical pattern of soils and underlying material in the Fayette-Nordness association (Soil Survey of Dubuque County, Iowa; 1986).

2. IA-2011-05-31-20 | Dubuque County - 1986

   Typical pattern of soils and underlying material in the Fayette-Rozetta-Eleroy association (Soil Survey of Dubuque County, Iowa; 1986).

3. IA-2011-05-31-23 | Dubuque County - 1986

   Typical pattern of soils and underlying material in the Chelsea-Sogn-Lamont association (Soil Survey of Dubuque County, Iowa; 1986).

4. IA-2011-05-31-24 | Dubuque County - 1986

   A cross section of a typical pattern of soils and underlying material in a landscape controlled by limestone and shale (Soil Survey of Dubuque County, Iowa; 1986).

5. IA-2011-05-31-50 | Jackson County - 1992

   Typical pattern of soils and parent material in the Fayette-Nordness-Rock outcrop association (Soil Survey of Jackson County, Iowa; 1992).

6. IA-2011-05-31-51 | Jackson County - 1992

   Typical pattern of soils and parent material in the Downs-Fayette association (Soil Survey of Jackson County, Iowa; 1992).

7. IA-2011-05-31-53 | Jackson County - 1992

   Typical pattern of soils and parent material in the Walford-Atterberry-Downs association (Soil Survey of Jackson County, Iowa; 1992).

8. IA-2011-06-01-01 | Jones County - 1991

   Typical pattern of soils and parent material in the Fayette-Downs-Exette association (Soil Survey of Jones County, Iowa; 1991).

9. IA-2011-06-01-03 | Jones County - 1991

   Typical pattern of soils and parent material in the Fayette-Nordness-Rock outcrop association (Soil Survey of Jones County, Iowa; 1991).

10. MN-2012-02-06-04 | Olmsted County - March 1980

    Pattern of soils and underlying material in the Mt. Carroll-Marlean-Arenzville association (Soil Survey of Olmsted County, Minnesota; March 1980).

Map Units

Map units containing CHASEBURG 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
Arenzville-Chaseburg complex, 1 to 5 percent slopes	129B	1995	402345	2tc4l	ia005	1992	1:15840
Chaseburg silt loam, 0 to 2 percent slopes	142	517	2774733	2syk8	ia005	1992	1:15840
Arenzville-Chaseburg complex, 1 to 5 percent slopes	129B	6112	404203	2tc4l	ia043	1979	1:15840
Chaseburg silt loam, moderately well drained, 0 to 2 percent slopes	142	317	2774735	2syk9	ia043	1979	1:15840
Arenzville-Chaseburg complex, 1 to 5 percent slopes	129B	13449	404348	2tc4l	ia045	1978	1:15840
Chaseburg silt loam, moderately well drained, 0 to 2 percent slopes	142	10725	2774736	2syk9	ia045	1978	1:15840
Chaseburg silt loam, 2 to 5 percent slopes	142B	1090	2914145	fkrh	ia045	1978	1:15840
Chaseburg silt loam, channeled, 0 to 2 percent slopes	1142	588	404333	fkr0	ia045	1978	1:15840
Arenzville-Chaseburg complex, 1 to 5 percent slopes	129B	3134	404979	2tc4l	ia055	1984	1:15840
Arenzville-Chaseburg complex, 1 to 5 percent slopes	129B	12966	405375	2tc4l	ia061	1983	1:15840
Chaseburg silt loam, moderately well drained, 0 to 2 percent slopes	142	5337	2774737	2syk9	ia061	1983	1:15840
Arenzville-Chaseburg complex, 1 to 5 percent slopes	129B	2167	405695	2tc4l	ia065	1975	1:15840
Chaseburg silt loam, 0 to 2 percent slopes	142	12584	2774734	2syk8	ia097	1988	1:15840
Arenzville-Chaseburg complex, 1 to 5 percent slopes	129B	9174	407450	2tc4l	ia097	1988	1:15840
Chaseburg-Perks complex, 0 to 2 percent slopes	128	2643	407448	fnzh	ia097	1988	1:15840
Arenzville-Chaseburg complex, 1 to 5 percent slopes	129B	12732	408086	2tc4l	ia105	1988	1:15840
Perks-Chaseburg complex, 0 to 2 percent slopes, frequently flooded	315	7615	408138	30qvs	ia105	1988	1:15840
Chaseburg silt loam, 0 to 2 percent slopes	142	4613	408089	2syk8	ia105	1988	1:15840
Chaseburg and Judson silt loams, 2 to 6 percent slopes	Cb	12553	2216705	2ddnm	mn045	2008	1:12000
Chaseburg and Judson silt loams, 0 to 1 percent slopes	Ca	3381	2216704	2ddnl	mn045	2008	1:12000
Chaseburg silt loam, 2 to 12 percent slopes, frequently flooded	N620B	3995	1675879	1t7wm	mn049	2007	1:12000
Chaseburg silt loam, channeled, 2 to 6 percent slopes	1861B	2774	398239	fcdf	mn055	1981	1:15840
Chaseburg silt loam, moderately well drained, 0 to 2 percent slopes	19	8727	400724	2syk9	mn109	1977	1:15840
Chaseburg silt loam, moderately well drained, 2 to 6 percent slopes	ChB	5766	2216307	2tc4n	mn157	2008	1:12000
Chaseburg silt loam, moderately well drained, 0 to 2 percent slopes	ChA	5735	2216306	2syk9	mn157	2008	1:12000
Chaseburg fine sandy loam, 2 to 6 percent slopes	CaB	193	2216305	2dd7q	mn157	2008	1:12000
Chaseburg silt loam, moderately well drained, 0 to 2 percent slopes	19	3249	429001	2syk9	mn169	1987	1:20000
Chaseburg silt loam, channeled	1861	1584	428999	gddp	mn169	1987	1:20000
Chaseburg silt loam, 1 to 4 percent slopes, occasionally flooded	616B	5529	2561686	h6x7	wi011	1960	1:20000
Chaseburg silt loam, 4 to 12 percent slopes, occasionally flooded	616C	1910	2561689	2qr2d	wi011	1960	1:20000
Chaseburg silt loam, 1 to 4 percent slopes, occasionally flooded	616B	4394	2504299	h6x7	wi023	1960	1:12000
Chaseburg silt loam, moderately well drained, 2 to 6 percent slopes	ChB	1288	753470	2tc4n	wi025	1972	1:15840
Chaseburg silt loam, 1 to 4 percent slopes, occasionally flooded	616B	1703	2504300	h6x7	wi033	2003	1:15840
Chaseburg silt loam, 1 to 4 percent slopes, occasionally flooded	616B	66	3099663	h6x7	wi035	1974	1:15840
Chaseburg silt loam, moderately well drained, 2 to 6 percent slopes	ChB	7241	424145	2tc4n	wi043	1959	1:20000
Chaseburg silt loam, moderately well drained, 0 to 2 percent slopes	ChA	6417	2774741	2syk9	wi043	1959	1:20000
Chaseburg silt loam, 6 to 15 percent slopes	ChC	852	424146	g7c4	wi043	1959	1:20000
Chaseburg silt loam, moderately well drained, 2 to 6 percent slopes	ChB	5372	425210	2tc4n	wi045	1969	1:12000
Chaseburg and Arenzville silt loams, 0 to 2 percent slopes	Cn	794	425212	2tc4m	wi045	1969	1:12000
Chaseburg silt loam, 6 to 12 percent slopes, rarely flooded	ChC	101	425211	g8gh	wi045	1969	1:12000
Chaseburg silt loam, moderately well drained, 2 to 6 percent slopes	616B	6187	2806634	2tc4n	wi049	1960	1:20000
Chaseburg silt loam, moderately well drained, 0 to 2 percent slopes	ChA	2926	2774742	2syk9	wi049	1960	1:20000
Chaseburg silt loam, 4 to 12 percent slopes, occasionally flooded	616C	145	2809836	2qr2d	wi049	1960	1:20000
Chaseburg silt loam, 1 to 4 percent slopes, occasionally flooded	616B	1	2561555	h6x7	wi057	1987	1:15840
Chaseburg silt loam, moderately well drained, 2 to 6 percent slopes	ChB	7226	424752	2tc4n	wi065	1964	1:15840
Chaseburg silt loam, moderately well drained, 0 to 2 percent slopes	ChA	1192	2774743	2syk9	wi065	1964	1:15840
Chaseburg silt loam, 1 to 4 percent slopes, occasionally flooded	616B	1932	2685134	h6x7	wi081	1981	1:15840
Chaseburg silt loam, 1 to 4 percent slopes, occasionally flooded	616B	2357	2504301	h6x7	wi091	1998	1:12000
Chaseburg silt loam, till plain, 1 to 6 percent slopes, occasionally flooded	892B	4025	1700385	1v2d4	wi093	2006	1:12000
Chaseburg silt loam, 1 to 4 percent slopes, occasionally flooded	616B	912	1691013	1trmt	wi093	2006	1:12000
Chaseburg silt loam, moderately well drained, 0 to 2 percent slopes	ChA	3586	423134	2syk9	wi111	1977	1:15840
Chaseburg silt loam, 1 to 4 percent slopes, occasionally flooded	616B	3	2683485	h6x7	wi121	1969	1:15840
Chaseburg silt loam, 1 to 4 percent slopes, occasionally flooded	616B	5089	2504302	h6x7	wi123	1965	1:12000

Map of Series Extent

Approximate geographic distribution of the CHASEBURG 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).