Soil Data Explorer - MANIDO

Official Series Description

Lab Data Summary

Aggregate lab data for the MANIDO soil series. This aggregation is based on all pedons with a current taxon name of MANIDO, 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 MANIDO 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
92	04N0482	S2003MI053005	Manido	7	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	46.6673965,-89.9570923

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the MANIDO 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 MANIDO series. Sketches are arranged according to their subgroup-level taxonomic structure. Source: SSURGO snapshot (updated 2024-02-21), parsed OSD records (updated 2023-10-02) and snapshot of SC database (updated 2023-10-02).

Select annual climate data summaries for the MANIDO 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 MANIDO 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 MANIDO share the same family level classification in Soil Taxonomy. Source: parsed OSD records (updated 2023-10-02) and snapshot of the SC database (updated 2023-10-02).

Select annual climate data summaries for the MANIDO 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).

There are insufficient data to create the annual climate figure.

Geomorphic description summaries for the MANIDO 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 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 MANIDO, 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

No block diagrams are available.

Map Units

Map units containing MANIDO 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
Manido-Annalake complex, 1 to 6 percent slopes	652B	1352	1456322	1kwf4	mi053	2007	1:24000
Manido-Fence-Gogebic, sandy substratum, complex, 1 to 6 percent slopes	296B	942	1456174	1kw8c	mi053	2007	1:24000
Belding-Manido complex, 1 to 6 percent slopes	460B	482	1456200	1kw96	mi053	2007	1:24000
Manido-Sporley-Gogebic, sandy substratum, complex, 18 to 35 percent slopes	296D	300	1456175	1kw8d	mi053	2007	1:24000
Manido-Richter complex, 0 to 6 percent slopes	292B	175	1456171	1kw88	mi053	2007	1:24000
Manido fine sand, 1 to 6 percent slopes	8142B	3046	2484710	2pdjy	mi061	1989	1:20000
Manido-Wainola complex, 0 to 4 percent slopes	8235B	1314	2485004	2pdvf	mi061	1989	1:20000
Manido fine sand, 6 to 18 percent slopes	8142C	264	2484711	2pdjz	mi061	1989	1:20000
Manido-Kinross complex, 0 to 4 percent slopes	8155	78	2483787	2pcl5	mi061	1989	1:20000
Manido fine sand, 0 to 3 percent slopes	8142A	26	2566037	1kwpl	mi061	1989	1:20000
Manido fine sand, 1 to 6 percent slopes	8142B	3757	1674839	1t6t2	mi131	2007	1:24000
Manido-Kinross complex, 0 to 4 percent slopes	8155	1648	1674844	1t6t7	mi131	2007	1:24000
Manido fine sand, 0 to 3 percent slopes	148A	1365	1456584	1kwpl	mi131	2007	1:24000
Manido-Richter complex, 0 to 6 percent slopes	8292B	1306	1674897	1t6vy	mi131	2007	1:24000
Manido-Wainola complex, 0 to 4 percent slopes	8235B	851	1674872	1t6v4	mi131	2007	1:24000
Manido fine sand, 6 to 18 percent slopes	8142C	145	1674840	1t6t3	mi131	2007	1:24000

Map of Series Extent

Approximate geographic distribution of the MANIDO 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).