Soil Data Explorer - MERIDIAN

Official Series Description

Lab Data Summary

Aggregate lab data for the MERIDIAN soil series. This aggregation is based on all pedons with a current taxon name of MERIDIAN, 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 MERIDIAN 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	UMN1160	S1970MN0491160	Meridian	3	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	44.207325,-92.6598434
105	UMN1159	S1970MN0491159	Meridian	3	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	44.3071136,-92.8433151
105	78P0216	S1977WI017001	Meridian	4	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	44.8731036,-91.5678578

Water Balance

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

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

Soil series sharing subgroup-level classification with MERIDIAN, 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-2012-03-22-02 | Buffalo County - March 1962

   Soil associations and relief in Buffalo County. 1. Silty soils of the rolling limestone uplands and Steep stony and rocky land: Dubuque, Fayette, Steep stony and rocky land. 2. Loamy soils of the rolling to hilly sandstone uplands: Gale, Hixton. 3. Sandy soils of the rolling to hilly sandstone uplands: Boone, Hixton. 4. Sandy soils of stream terraces: Sparta, Plainfield. 5. Silty soils of stream terraces: Bertrand, Richwood. 6. Loamy terrace soils underlain by sand on stream terraces: Meridian, Tell. 7. Wet organic and mineral soils of bottom lands: Peat and Muck, Ettrick, Wallkill. 8. Soils of overflow bottom lands: Loamy alluvial lands, Marsh (Soil Survey of Bayfield County, WI; 1961).

2. WI-2012-03-23-02 | Iowa County - July 1962

   Two landscapes of terrace soils showing the relationship of the major soils. The upper illustration shows silty soils, and the lower one, sandy soils. By Soil Survey Division, University of Wisconsin (Soil Survey of Iowa County, WI; 1962).

3. WI-2012-03-23-24 | Monroe County - June 1984

   Relationship of soils and parent material in the Billett-Impact map unit (Soil Survey of Monroe County, WI; 1984).

Map Units

Map units containing MERIDIAN 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
Meridian loam, 0 to 3 percent slopes	M513A	1120	1384957	1hh51	mn039	2005	1:12000
Meridian fine sandy loam, 2 to 6 percent slopes	Mc	473	2216759	2ddqc	mn045	2008	1:12000
Meridian silt loam, 0 to 3 percent slopes	N607A	1956	1670219	1t201	mn049	2007	1:12000
Meridian silt loam, 6 to 12 percent slopes, moderately eroded	N607C2	444	1690744	1trc4	mn049	2007	1:12000
Meridian, till substratum-Bassett complex, 6 to 12 percent slopes, moderately eroded	M536C2	411	1670153	1t1xx	mn049	2007	1:12000
Meridian, till substratum-Bassett complex, 12 to 18 percent slopes, moderately eroded	M536D2	337	1670154	1t1xy	mn049	2007	1:12000
Meridian silt loam, 12 to 18 percent slopes, moderately eroded	N607D2	242	1690743	1trc3	mn049	2007	1:12000
Meridian-Bassett complex, 18 to 35 percent slopes	M537E	139	1670173	1t1yk	mn049	2007	1:12000
Meridian sandy loam, 2 to 6 percent slopes	MdB	528	2216396	2ddbn	mn157	2008	1:12000
Meridian sandy loam, 0 to 2 percent slopes	MdA	507	2216395	2ddbm	mn157	2008	1:12000
Meridian sandy loam, 6 to 12 percent slopes, moderately eroded	MdC2	155	2216399	2ddbr	mn157	2008	1:12000
Meridian silt loam, 2 to 6 percent slopes, moderately eroded	423B2	232	2561787	1vgbf	wi011	1960	1:12000
Meridian silt loam, 0 to 3 percent slopes	423A	197	2639462	1vgbd	wi011	1960	1:12000
Meridian silt loam, 6 to 12 percent slopes, moderately eroded	423C2	51	2561786	g0w1	wi011	1960	1:12000
Meridian loam, 2 to 6 percent slopes	MlB	4217	421554	g4nj	wi017	1985	1:15840
Meridian loam, moderately well drained, 0 to 3 percent slopes	MmA	1993	421555	g4nk	wi017	1985	1:15840
Meridian loam, 0 to 2 percent slopes	MlA	1618	421553	g4nh	wi017	1985	1:15840
Meridian silt loam, 2 to 6 percent slopes, moderately eroded	423B2	131	2504048	1vgbf	wi023	1960	1:12000
Meridian silt loam, 0 to 3 percent slopes	423A	29	2504045	1vgbd	wi023	1960	1:12000
Meridian silt loam, 6 to 12 percent slopes, moderately eroded	423C2	17	2504052	g0w1	wi023	1960	1:12000
Meridian loam, 0 to 2 percent slopes	MeA	1631	753539	t93q	wi025	1972	1:15840
Meridian loam, 2 to 6 percent slopes	MeB	1315	753540	t93r	wi025	1972	1:15840
Meridian silt loam, 0 to 3 percent slopes	423A	1452	2504046	1vgbd	wi033	2003	1:12000
Meridian silt loam, 2 to 6 percent slopes, moderately eroded	423B2	1122	2504049	1vgbf	wi033	2003	1:12000
Meridian silt loam, 6 to 12 percent slopes, moderately eroded	423C2	10	2504053	g0w1	wi033	2003	1:12000
Meridian silt loam, 2 to 6 percent slopes, moderately eroded	423B2	4797	3099704	1vgbf	wi035	1974	1:12000
Meridian silt loam, 0 to 3 percent slopes	423A	2041	3099703	1vgbd	wi035	1974	1:12000
Meridian silt loam, 6 to 12 percent slopes, moderately eroded	423C2	1732	3099644	g0w1	wi035	1974	1:12000
Meridian fine sandy loam, 2 to 6 percent slopes, moderately eroded	MfB2	337	424301	g7j4	wi043	1959	1:20000
Meridian fine sandy loam, 10 to 15 percent slopes, moderately eroded	MfD2	274	424304	g7j7	wi043	1959	1:20000
Meridian fine sandy loam, 0 to 2 percent slopes	MfA	260	424299	g7j2	wi043	1959	1:20000
Meridian loam, 2 to 6 percent slopes	MmB	215	424306	g7j9	wi043	1959	1:20000
Meridian loam, 0 to 2 percent slopes	MmA	205	424305	g7j8	wi043	1959	1:20000
Meridian fine sandy loam, 6 to 10 percent slopes, moderately eroded	MfC2	181	424302	g7j5	wi043	1959	1:20000
Meridian loam, 2 to 6 percent slopes, moderately eroded	MmB2	141	424307	g7jb	wi043	1959	1:20000
Meridian fine sandy loam, 2 to 6 percent slopes	MfB	119	424300	g7j3	wi043	1959	1:20000
Meridian loam, 10 to 15 percent slopes, moderately eroded	MmD2	33	424309	g7jd	wi043	1959	1:20000
Meridian loam, 6 to 10 percent slopes, moderately eroded	MmC2	23	424308	g7jc	wi043	1959	1:20000
Meridian loam, 2 to 6 percent slopes, moderately eroded	MlB2	1047	425301	g8kd	wi045	1969	1:12000
Meridian loam, 0 to 2 percent slopes	MlA	616	425300	g8kc	wi045	1969	1:12000
Meridian loam, 6 to 12 percent slopes, moderately eroded	MlC2	244	425302	g8kf	wi045	1969	1:12000
Meridian silt loam, 2 to 6 percent slopes, moderately eroded	423B2	261	2774824	1vgbf	wi049	1960	1:20000
Meridian silt loam, 0 to 3 percent slopes	423A	181	2774823	1vgbd	wi049	1960	1:20000
Meridian silt loam, 6 to 12 percent slopes, moderately eroded	423C2	95	2774809	g0w1	wi049	1960	1:20000
Meridian loam, 2 to 6 percent slopes	MdB	193	424847	g82r	wi065	1964	1:15840
Meridian sandy loam, 2 to 6 percent slopes	MeB	142	424849	g82t	wi065	1964	1:15840
Meridian loam, 0 to 2 percent slopes	MdA	99	424846	g82q	wi065	1964	1:15840
Meridian sandy loam, 0 to 2 percent slopes	MeA	43	424848	g82s	wi065	1964	1:15840
Meridian silt loam, 0 to 3 percent slopes	423A	750	2504047	1vgbd	wi091	1998	1:12000
Meridian silt loam, 2 to 6 percent slopes, moderately eroded	423B2	502	2504050	1vgbf	wi091	1998	1:12000
Meridian silt loam, cobbly substratum, 0 to 2 percent slopes	391A	2097	1701118	1v34s	wi093	2006	1:12000
Meridian silt loam, strath terrace, 2 to 6 percent slopes, moderately eroded	300B2	842	1697578	1tzgl	wi093	2006	1:12000
Meridian silt loam, strath terrace, 0 to 2 percent slopes	300A	315	1697577	1tzgk	wi093	2006	1:12000
Meridian silt loam, 2 to 6 percent slopes, moderately eroded	423B2	300	1690951	1trkt	wi093	2006	1:12000
Meridian silt loam, strath terrace, 6 to 12 percent slopes, moderately eroded	300C2	174	1701124	1v34z	wi093	2006	1:12000
Meridian silt loam, 0 to 3 percent slopes	423A	73	1703595	1v5qp	wi093	2006	1:12000
Meridian silt loam, 6 to 12 percent slopes, moderately eroded	423C2	12	1703596	1v5qq	wi093	2006	1:12000
Meridian silt loam, 2 to 6 percent slopes, moderately eroded	423B2	113	2639542	1vgbf	wi121	1969	1:12000
Meridian silt loam, 0 to 3 percent slopes	423A	76	2639541	1vgbd	wi121	1969	1:12000
Meridian silt loam, 6 to 12 percent slopes, moderately eroded	423C2	4	2683471	g0w1	wi121	1969	1:12000
Meridian silt loam, 6 to 12 percent slopes, moderately eroded	423C2	11	2504054	g0w1	wi123	1965	1:12000
Meridian silt loam, 2 to 6 percent slopes, moderately eroded	423B2	5	2504051	1vgbf	wi123	1965	1:12000

Map of Series Extent

Approximate geographic distribution of the MERIDIAN 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).