Official Series Description


Lab Data Summary

Aggregate lab data for the VONID soil series. This aggregation is based on all pedons with a current taxon name of VONID, 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 VONID 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
6990P00381999CO073047OSDVonid7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.5797222,-104.0372222

Water Balance

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

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Competing Series

Soil series competing with VONID 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 VONID 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 VONID 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 .

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There are insufficient data to create the 3D mountains figure.

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Click the image to view it full size.

Soil series sharing subgroup-level classification with VONID, 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 VONID 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
Vonid sandy loam, 0 to 5 percent slopesVnB1115626110512rgqcco01119651:15840
Vonid sandy loam, 0 to 5 percent slopes, dryVoC620126110522rgqdco01119651:15840
Vonid soils, 1 to 6 percent slopes, erodedVs2389727665412t50xco01119651:15840
Valent-Vonid complex, 1 to 15 percent slopes, dry60887327664672rgs9co01719851:24000
Vonid loamy sand, 1 to 5 percent slopes62475627667132rgq9co01719851:24000
Vonid-Fort sandy loams, 1 to 9 percent slopes61195127667102t51cco01719851:24000
Vonid sandy loam, 0 to 5 percent slopesVnC4309926110532rgqcco02519651:15840
Vonid sandy loam, 0 to 5 percent slopes, dryVoC1949826110542rgqdco02519651:15840
Valent-Vonid complex, 1 to 15 percent slopes, dryVtV1923227664452rgs9co02519651:15840
Vonid-Oterodry sandy loams, 3 to 9 percent slopesVoD774127665462t50yco02519651:15840
Vonid-Oterodry sandy loams, 1 to 6 percent slopes, erodedVs2764627665432t50wco02519651:15840
Vonid loamy sand, 1 to 5 percent slopesVaB641026110362rgq9co02519651:15840
Valent-Vonid complex, 1 to 15 percent slopes, dry74341527664682rgs9co06119771:24000
Vonid-Fort sandy loams, 1 to 9 percent slopes401393127667172t51cco06119771:24000
Vonid sandy loam, 0 to 5 percent slopes45668526110572rgqcco06119771:24000
Vonid sandy loam, 0 to 5 percent slopes2043280726110562rgqcco07320011:24000
Vonid loamy sand, 1 to 5 percent slopes2032662026110352rgq9co07320011:24000
Valent-Vonid complex, 1 to 15 percent slopes, dry1961440827664462rgs9co07320011:24000
Vonid-Karval-Midway complex, 5 to 25 percent slopes206130201052873jkcco07320011:24000
Vonid sandy loam, 5 to 12 percent slopes205105141052863jkbco07320011:24000
Vonid-Midway complex, 3 to 12 percent slopes20755971052883jkdco07320011:24000
Vonid-Seldom sandy loams, 3 to 25 percent slopes20840781052893jkfco07320011:24000
Vonid sandy loam, 0 to 5 percent slopes, dryVdC2971326110502rgqdco08919661:15840
Vonid soils, 1 to 6 percent slopes, erodedVs2309127665422t50xco09919631:15840
Vonid sandy loam, 0 to 5 percent slopes1172102126110602rgqcco62519751:24000
Olney-Vonid soils, 1 to 6 percent slopes, eroded12314403954252t51dco62519751:24000
Vonid loamy sand, 1 to 5 percent slopesVn2586626110332rgq9co62619741:24000
Vonid sandy loam, 0 to 5 percent slopesVo1950826110582rgqcco62619741:24000
Vonid-Oterodry sandy loams, 1 to 6 percent slopes, erodedVs2894027665442t50wco62619741:24000
Vonid sandy loam, 0 to 5 percent slopes, dryVoC763926110592rgqdco62619741:24000
Vonid sandy loam, 0 to 5 percent slopesVoC280426706302rgqcco62719801:24000
Vonid sandy loam, 0 to 5 percent slopesVoC819326110552rgqcco62820081:24000
Gapmesa-Vonid-Kaiar complex, 2 to 8 percent slopesZaB755017048341v70nut0131:24000
Cambria-Eaglenest-Vonid complex, 2 to 10 percent slopesB21231709482wxmzwy6031:24000
Cambria-Eaglenest-Vonid complex, 2 to 10 percent slopes221229691052wxmzwy6291:24000
Vonalee-Vonid complex, 4 to 12 percent slopes231331332332ynlrwy6291:24000
Maysdorf-Hiland-like-Vonid complex, 3 to 12 percent slopes222031332502ynm9wy6291:24000
Vonid-Cascajo-Zigweid complex, 1 to 4 percent slopes113232066322zc4hwy6291:24000
Sedgran-like-Vonid complex, 6 to 20 percent slopes534632066482zc50wy6291:24000
Taluce-like-Vonid complex, 1 to 6 percent slopes521529119582y4ydwy6291:24000
Maysdorf-Shingle-Vonid complex, 6 to 25 percent slopes32224834512pc7bwy6291:24000

Map of Series Extent

Approximate geographic distribution of the VONID 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 .