Soil Data Explorer - MIVIDA

Official Series Description

Lab Data Summary

Aggregate lab data for the MIVIDA soil series. This aggregation is based on all pedons with a current taxon name of MIVIDA, 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 MIVIDA 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
35	82P0785	82UT037005	Mivida	7	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	37.3552818,-109.741806
48A	92P0909	92UT037163C	Mivida	6	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	37.8460007,-109.901001

Water Balance

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

Competing Series

Soil series competing with MIVIDA 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 MIVIDA 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 MIVIDA 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 MIVIDA, 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 MIVIDA 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
Mivida fine sandy loam, 5 to 15 percent slopes	59	3599	502085	jvg9	co675	1986	1:24000
Mivida very fine sandy loam, 1 to 6 percent slopes	65	5279	503759	jx69	ut616	1983	1:24000
Mivida gravelly fine sandy loam, 3 to 8 percent slopes	66	2266	503760	jx6b	ut616	1983	1:24000
Mivida very stony fine sandy loam, 1 to 3 percent slopes	67	1999	503761	jx6c	ut616	1983	1:24000
Mivida loamy fine sand, 1 to 4 percent slopes	098	2065	504872	jyc6	ut623	2011	1:24000
Mivida loamy fine sand	54	3045	55183	1vf3	ut631	1982	1:24000
Mivida-Goblin complex	55	574	55184	1vf4	ut631	1982	1:24000
Mivida variant very cobbly very fine sandy loam, 15 to 40 percent slopes	56	494	55185	1vf5	ut631	1982	1:24000
Mivida fine sandy loam, 2 to 8 percent slopes	52	8858	55374	1vm8	ut633	1983	1:24000
Mivida fine sandy loam, 2 to 10 percent slopes	95	1392	504494	jxz0	ut636	1984	1:24000
Milok-Mivida complex	24	24589	55447	1vpm	ut638	1985	1:24000
Mivida-Pastern-Rock outcrop complex, 1 to 8 percent slopes	27	16080	55450	1vpq	ut638	1985	1:24000
Mivida fine sandy loam, 1 to 6 percent slopes	26	5105	55449	1vpp	ut638	1985	1:24000
Mivida fine sandy loam, moist, 1 to 8 percent slopes	77	54	2484393	2pd6q	ut638	1985	1:24000
Mido-Mivida-Sazi complex, 2 to 15 percent slopes	51	3782	2397992	2lh9l	ut642		1:63360
Mivida-Barx, dry complex, 1 to 8 percent slopes	54	361	2433235	2mnzg	ut642		1:63360
Mivida loamy fine sand, 1 to 4 percent slopes	44	1621	2556036	2qdrh	ut685	1990	1:24000
Mivida-Gish-Cannonville complex, 2 to 15 percent slopes	45	172	2515004	2qdr0	ut685	1990	1:24000
Mikim-Mivida, moist, complex, 3 to 15 percent slopes	41	132	2507454	2q70q	ut685	1990	1:24000
Mido-Mivida complex, 2 to 15 percent slopes	5122	8150	59794	206v	ut686	2004	1:24000
Mivida-Barx, dry complex, 1 to 8 percent slopes	5055	5864	59817	207l	ut686	2004	1:24000
Earlweed-Mivida complex, 2 to 20 percent slopes	5058	1506	59820	207p	ut686	2004	1:24000
Mivida-Yarts, moist complex, 2 to 8 percent slopes	5059	1382	59821	207q	ut686	2004	1:24000

Map of Series Extent

Approximate geographic distribution of the MIVIDA 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).