Soil Data Explorer - DODGEVILLE

Official Series Description

Lab Data Summary

Aggregate lab data for the DODGEVILLE soil series. This aggregation is based on all pedons with a current taxon name of DODGEVILLE, 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 DODGEVILLE 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	X53-803-1	S1984IA105037	Dodgeville	2	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	42.2789198,-91.1622618
105	40A5203	S1977WI049002	DODGEVILLE	7	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	42.9694443,-90.0008316
95B	04N0445	S2003IL177008	Dodgeville	7	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	42.3497238,-89.6302795
n/a	68IL177002	1968IL177002	Dodgeville	4	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	n/a
n/a	X61000-3	S1977IA061999	Dodgeville	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 DODGEVILLE 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 DODGEVILLE 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 DODGEVILLE 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 DODGEVILLE 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 DODGEVILLE 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 DODGEVILLE 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 DODGEVILLE 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 DODGEVILLE, 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-2012-03-23-01 | Iowa County - July 1962

   Two landscapes of upland soils showing the relationship of the major soils. The upper illustration shows soils formed under prairie, and the lower one, soils formed under forest. By Soil Survey Division, University of Wisconsin (Soil Survey of Iowa County, WI; 1962).

Map Units

Map units containing DODGEVILLE 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
Dodgeville silt loam, deep, 2 to 5 percent slopes	204B	172	408578	fq4y	ia113	1970	1:15840
Dodgeville silt loam, deep, 5 to 9 percent slopes	204C	138	408579	fq4z	ia113	1970	1:15840
Rockton and Dodgeville soils, 5 to 10 percent slopes, eroded	566C2	156	1483214	1lsdm	il007	2006	1:12000
Rockton and Dodgeville soils, 2 to 5 percent slopes	566B	141	199863	6pz6	il007	2006	1:12000
Rockton and Dodgeville soils, 10 to 15 percent slopes, eroded	566D2	27	1483215	1lsdn	il007	2006	1:12000
Dodgeville silt loam, 5 to 10 percent slopes, eroded	40C2	12842	1591953	1qfkb	il177	2006	1:12000
Dodgeville silt loam, 10 to 18 percent slopes, eroded	40D2	489	1591955	1qfkd	il177	2006	1:12000
Rockton and Dodgeville soils, 5 to 10 percent slopes, eroded	566C2	5001	174132	5v65	il201	1997	1:12000
Rockton and Dodgeville soils, 2 to 5 percent slopes	566B	3435	174131	5v64	il201	1997	1:12000
Rockton and Dodgeville soils, 10 to 15 percent slopes, eroded	566D2	951	174133	5v66	il201	1997	1:12000
Rockton and Dodgeville silt loams, shallow, 2 to 6 percent slopes	Rm	5427	2216776	2ddqx	mn045	2008	1:12000
Rockton and Dodgeville silt loams, shallow, 7 to 11 percent slopes, moderately eroded	Ro	3151	2216779	2ddr0	mn045	2008	1:12000
Rockton and Dodgeville silt loams, shallow, 12 to 17 percent slopes, moderately eroded	Rp	872	2216777	2ddqy	mn045	2008	1:12000
Rockton and Dodgeville silt loams, shallow, 18 to 35 percent slopes	Rr	480	2216775	2ddqw	mn045	2008	1:12000
Dodgeville silt loam, shallow, 12 to 18 percent slopes, moderately eroded	DgD2	246	2216312	2dd7y	mn157	2008	1:12000
Dodgeville silt loam, 6 to 12 percent slopes, moderately eroded	DdC2	139	2216310	2dd7w	mn157	2008	1:12000
Dodgeville silt loam, 12 to 18 percent slopes, moderately eroded	DdD2	91	2216309	2dd7v	mn157	2008	1:12000
Dodgeville silt loam, shallow, 6 to 12 percent slopes, moderately eroded	DgC2	86	2216314	2dd80	mn157	2008	1:12000
Dodgeville silt loam, shallow, 18 to 35 percent slopes	DgE	75	2216313	2dd7z	mn157	2008	1:12000
Dodgeville silt loam, 6 to 12 percent slopes	DpC	3204	753485	t91z	wi025	1972	1:15840
Dodgeville silt loam, 2 to 6 percent slopes	DpB	2386	753484	t91y	wi025	1972	1:15840
Dodgeville silt loam, 12 to 20 percent slopes, eroded	DpD2	573	753486	t920	wi025	1972	1:15840
Dodgeville silt loam, deep, 6 to 10 percent slopes, moderately eroded	DcC2	4894	424160	g7cl	wi043	1959	1:20000
Dodgeville silt loam, deep, 10 to 15 percent slopes, moderately eroded	DcD2	2921	424161	g7cm	wi043	1959	1:20000
Dodgeville soils, deep, 6 to 10 percent slopes, moderately eroded	DeC2	1626	1454339	1ktc5	wi043	1959	1:20000
Dodgeville soils, deep, 10 to 15 percent slopes, moderately eroded	DeD2	1419	1454340	1ktc6	wi043	1959	1:20000
Dodgeville silt loam, deep, 2 to 6 percent slopes, moderately eroded	DcB2	1373	424158	g7cj	wi043	1959	1:20000
Dodgeville silt loam, 10 to 15 percent slopes, moderately eroded	DbD2	1085	424155	g7cf	wi043	1959	1:20000
Dodgeville soils, 10 to 15 percent slopes, moderately eroded	DdD2	949	1454337	1ktc3	wi043	1959	1:20000
Dodgeville soils, deep, 2 to 6 percent slopes, moderately eroded	DeB2	784	1454338	1ktc4	wi043	1959	1:20000
Dodgeville silt loam, 6 to 10 percent slopes, moderately eroded	DbC2	390	424154	g7cd	wi043	1959	1:20000
Dodgeville silt loam, 15 to 20 percent slopes, moderately eroded	DbE2	301	424156	g7cg	wi043	1959	1:20000
Dodgeville silt loam, deep, 15 to 20 percent slopes, moderately eroded	DcE2	282	1454571	1ktln	wi043	1959	1:20000
Dodgeville soils, 6 to 10 percent slopes, moderately eroded	DdC2	228	1454336	1ktc2	wi043	1959	1:20000
Dodgeville silt loam, 20 to 30 percent slopes, moderately eroded	DbF2	38	424157	g7ch	wi043	1959	1:20000
Dodgeville silt loam, 6 to 12 percent slopes, moderately eroded	DgC2	11705	425222	g8gv	wi045	1969	1:12000
Dodgeville silt loam, 12 to 20 percent slopes, moderately eroded	DgD2	5131	425224	g8gx	wi045	1969	1:12000
Dodgeville silt loam, 2 to 6 percent slopes, moderately eroded	DgB2	3659	425221	g8gt	wi045	1969	1:12000
Dodgeville silt loam, deep, 2 to 6 percent slopes, moderately eroded	DhB2	22959	424540	g7rv	wi049	1960	1:20000
Dodgeville silt loam, deep, 6 to 12 percent slopes, moderately eroded	DhC2	17306	424541	g7rw	wi049	1960	1:20000
Dodgeville silt loam, 6 to 12 percent slopes, moderately eroded	DgC2	16628	424534	g7rn	wi049	1960	1:20000
Sogn and Dodgeville silt loams, shallow, 12 to 20 percent slopes, moderately eroded	SoD2	10245	424708	g7y8	wi049	1960	1:20000
Dodgeville silt loam, 12 to 20 percent slopes, moderately eroded	DgD2	8877	424536	g7rq	wi049	1960	1:20000
Sogn and Dodgeville silt loams, shallow, 6 to 12 percent slopes, moderately eroded	SoC2	2885	424706	g7y6	wi049	1960	1:20000
Dodgeville silt loam, 2 to 6 percent slopes, moderately eroded	DgB2	2647	424532	g7rl	wi049	1960	1:20000
Dodgeville silt loam, deep, 12 to 20 percent slopes, moderately eroded	DhD2	2532	424543	g7ry	wi049	1960	1:20000
Sogn and Dodgeville silt loams, shallow, 20 to 30 percent slopes, moderately eroded	SoE2	1432	424710	g7yb	wi049	1960	1:20000
Dodgeville silt loam, shallow, 6 to 12 percent slopes, moderately eroded	DlC2	1100	424546	g7s1	wi049	1960	1:20000
Dodgeville silt loam, shallow, 12 to 20 percent slopes, moderately eroded	DlD2	1084	424548	g7s3	wi049	1960	1:20000
Dodgeville silt loam, deep, 0 to 2 percent slopes	DhA	437	424538	g7rs	wi049	1960	1:20000
Sogn and Dodgeville silt loams, shallow, 2 to 6 percent slopes, moderately eroded	SoB2	429	424704	g7y4	wi049	1960	1:20000
Dodgeville soils, 6 to 12 percent slopes, moderately eroded	DmC2	285	1454905	1ktyf	wi049	1960	1:20000
Dodgeville silt loam, shallow, 2 to 6 percent slopes, moderately eroded	DlB2	262	424544	g7rz	wi049	1960	1:20000
Dodgeville soils, 12 to 20 percent slopes, moderately eroded	DmD2	214	1454906	1ktyg	wi049	1960	1:20000
Dodgeville silt loam, 20 to 30 percent slopes, moderately eroded	DgE2	31	424537	g7rr	wi049	1960	1:20000
Dodgeville soils, 2 to 6 percent slopes, moderately eroded	DmB2	26	1454904	1ktyd	wi049	1960	1:20000
Dodgeville silt loam, 6 to 12 percent slopes, moderately eroded	DgC2	11062	424765	g803	wi065	1964	1:15840
Dodgeville silt loam, 12 to 20 percent slopes, moderately eroded	DgD2	5114	424767	g805	wi065	1964	1:15840
Dodgeville soils, 6 to 12 percent slopes, moderately eroded	DhC2	1021	1454718	1ktrd	wi065	1964	1:15840
Dodgeville silt loam, 2 to 6 percent slopes, moderately eroded	DgB2	955	424763	g801	wi065	1964	1:15840
Dodgeville soils, 12 to 20 percent slopes, moderately eroded	DhD2	437	1454719	1ktrf	wi065	1964	1:15840
Dodgeville silt loam, 12 to 20 percent slopes, very deep, moderately eroded	130D2	291	2421213	2m8gn	wi123	1965	1:12000

Map of Series Extent

Approximate geographic distribution of the DODGEVILLE 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).