Official Series Description


Lab Data Summary

Aggregate lab data for the MINNIEVILLE soil series. This aggregation is based on all pedons with a current taxon name of MINNIEVILLE, 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 MINNIEVILLE were used in the calculation. Source: KSSL snapshot . Methods used to assemble the KSSL snapshot used by SoilWeb / SDE

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Pedons used in the lab summary:

MLRALab IDPedon IDTaxonnameCINSSL / NASIS ReportsLink To SoilWeb GMap
13604N108604NC097020Minnieville7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties35.8107491,-81.0188904
13699P0448S1999VA141011Minnieville6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties36.8055573,-80.1038895

Water Balance

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

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Sibling Summary

Siblings are those soil series that occur together in map units, in this case with the MINNIEVILLE series. Sketches are arranged according to their subgroup-level taxonomic structure. Source: SSURGO snapshot , parsed OSD records and snapshot of SC database .

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Select annual climate data summaries for the MINNIEVILLE series and siblings. Series are sorted according to hierarchical clustering of median values. Source: SSURGO map unit geometry and 1981-2010, 800m PRISM data .

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Geomorphic description summaries for the MINNIEVILLE 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 .

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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 MINNIEVILLE share the same family level classification in Soil Taxonomy. Source: parsed OSD records and snapshot of the SC database .

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Select annual climate data summaries for the MINNIEVILLE series and competing. Series are sorted according to hierarchical clustering of median values. Source: SSURGO map unit geometry and 1981-2010, 800m PRISM data .

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Geomorphic description summaries for the MINNIEVILLE 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 .

Click the image to view it full size.

Click the image to view it full size.

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 MINNIEVILLE, 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 .

Block Diagrams

No block diagrams are available.

Map Units

Map units containing MINNIEVILLE 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
Minnieville loam, 2 to 7 percent slopes19B46905163152v7hqva00319811:15840
Minnieville loam, 7 to 15 percent slopes19C40305163162v7hrva00319811:15840
Minnieville clay loam, 7 to 15 percent slopes, severely eroded20C317605163202v7hvva00319811:15840
Minnieville loam, 15 to 25 percent slopes19D14105163172v7hsva00319811:15840
Minnieville clay loam, 15 to 25 percent slopes, severely eroded20D311405163212v7hwva00319811:15840
Minnieville clay loam, 2 to 7 percent slopes, severely eroded20B32705163192v7htva00319811:15840
Minnieville loam, 7 to 15 percent slopes23C52041367362vy6wva00920041:24000
Minnieville loam, 2 to 7 percent slopes23B22171367352vtwbva00920041:24000
Minnieville loam, 15 to 25 percent slopes23D17961367372vy6xva00920041:24000
Minnieville clay loam, 7 to 15 percent slopes, severely eroded22C9881367334l8rva00920041:24000
Minnieville clay loam, 15 to 25 percent slopes, severely eroded22D7361367344l8sva00920041:24000
Minnieville clay loam, 2 to 7 percent slopes, severely eroded22B2541367324l8qva00920041:24000
Minnieville loam, 7 to 15 percent slopes9C48401359972xx60va01919851:24000
Minnieville loam, 2 to 7 percent slopes9B47321359962xx5zva01919851:24000
Minnieville loam, 15 to 25 percent slopes9D14101359982xx61va01919851:24000
Minnieville loam, 2 to 7 percent slopes41B51217264002vtwbva04720061:24000
Minnieville loam, 8 to 15 percent slopes27C76965820112vy73va06720041:24000
Minnieville loam, 15 to 25 percent slopes27D53735820122vy6xva06720041:24000
Minnieville-Orenda-Redbrush complex, 8 to 15 percent slopes28C2368582014mjmnva06720041:24000
Minnieville-Orenda-Redbrush complex, 15 to 25 percent slopes28D2331582016mjmqva06720041:24000
Minnieville loam, 25 to 45 percent slopes27E14925820132vy6yva06720041:24000
Minnieville loam, 2 to 8 percent slopes27B8355820102vy72va06720041:24000
Minnieville-Urban land complex, 8 to 15 percent slopes29C267582019mjmtva06720041:24000
Minnieville clay loam, 8 to 15 percent slopes, severely eroded32C3532614728311lflpva08320041:24000
Minnieville clay loam, 2 to 8 percent slopes, severely eroded32B3500414728301lflnva08320041:24000
Minnieville loam, 2 to 8 percent slopes31B305114728292vy72va08320041:24000
Minnieville loam, 7 to 15 percent slopes14C82091223182vy6wva08919951:24000
Minnieville loam, 15 to 25 percent slopes14D31521223192vy6xva08919951:24000
Minnieville loam, 2 to 7 percent slopes14B14371223162vtwbva08919951:24000
Minnieville-Urban land complex, 7 to 15 percent slopes15C87912232030yn2va08919951:24000
Minnieville loam, 7 to 15 percent slopes32C37451370422vy6wva12519921:24000
Minnieville loam, 15 to 25 percent slopes32D28351370432vy6xva12519921:24000
Minnieville loam, 2 to 7 percent slopes32B11071370412vtwbva12519921:24000
Minnieville loam, 25 to 45 percent slopes32E4701370442vy6yva12519921:24000
Minnieville loam, 2 to 7 percent slopes, moderately erodedLlB216951198552zhdqva13719661:15840
Minnieville clay loam, 7 to 15 percent slopes, severely erodedLmC37791198582zhdtva13719661:15840
Minnieville loam, 7 to 15 percent slopes, moderately erodedLlC25301198562zhdrva13719661:15840
Minnieville clay loam, 2 to 7 percent slopes, severely erodedLmB31561198572zhdsva13719661:15840
Minnieville clay loam, 15 to 25 percent slopes, severely erodedLmD3951198592zhdvva13719661:15840
Minnieville loam, 8 to 15 percent slopes33C688314741852vy73va14120081:24000
Minnieville loam, 15 to 25 percent slopes33D354914741862vy6xva14120081:24000
Minnieville loam, 2 to 8 percent slopes33B79414741842vy72va14120081:24000
Minnieville-Redbrush complex, 8 to 15 percent slopes34C643210866828s7kva14120081:24000
Minnieville loam, 25 to 45 percent slopes33E57014741872vy6yva14120081:24000
Minnieville-Redbrush complex, 15 to 25 percent slopes34D442210866928s7lva14120081:24000
Minnieville-Redbrush complex, 2 to 8 percent slopes34B78210866728s7jva14120081:24000
Minnieville clay loam, 7 to 15 percent slopes, severely eroded11C3125851199512yzrtva14319891:24000
Minnieville clay loam, 2 to 7 percent slopes, severely eroded11B385391199502yzrsva14319891:24000
Minnieville loam, 2 to 7 percent slopes10B29421199492yzrrva14319891:24000
Minnieville clay loam, 7 to 15 percent slopes, severely eroded39C3617521194khbqva15319851:15840
Minnieville clay loam, 2 to 7 percent slopes, severely eroded39B3179521193khbpva15319851:15840

Map of Series Extent

Approximate geographic distribution of the MINNIEVILLE 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 .