Official Series Description


Lab Data Summary

Aggregate lab data for the VAYWOOD soil series. This aggregation is based on all pedons with a current taxon name of VAYWOOD, 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 VAYWOOD 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
43A96P00221995ID035005Vaywood6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties46.8155556,-115.7558365
43A16N1995S2016ID079001Vaywood6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties47.55552,-115.82404
43B11N01212010ID049001Vaywood7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties46.4663194,-114.6330833

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the VAYWOOD 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 VAYWOOD 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 VAYWOOD 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 VAYWOOD 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 terrace figure.

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

Competing Series

Soil series competing with VAYWOOD 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 VAYWOOD 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 VAYWOOD 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 .

There are insufficient data to create the 2D hillslope position figure.

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

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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 VAYWOOD, 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 VAYWOOD 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
Vaywood medial silt loam, 15 to 35 percent slopesVa3j165250199954qyid05720131:24000
Vaywood medial silt loam, 35 to 75 percent slopesVa1j136250200054qzid05720131:24000
Kintla-Vaywood families, complex, weakly weathered metasedimentary belt geology, high elevation mountain ridges and upper slopes, north aspects2lg456728508672lg45id60419811:24000
Kintla-Vaywood families, complex, weakly weathered metasedimentary belt geology, high elevation mountain ridges and upper slopes, south aspects2lg46828508682lg46id60419811:24000
Vaywood medial silt loam, 30 to 60 percent slopes50812733099006nvdlid60619761:24000
Vaywood medial silt loam, 15 to 30 percent slopes50801473099005nvdkid60619761:24000
Vaywood medial silt loam, 15 to 35 percent slopes91675115351054qyid60819941:24000
Vaywood-Handoff complex, 15 to 35 percent slopesv2yv28671472222v2yvid60819941:24000
Vaywood medial silt loam, 35 to 75 percent slopes92191515351154qzid60819941:24000
Kintla-Vaywood-Kintla families, slightly acid subsoil complex, weakly weathered high elevation broadly convex mountain slopes, metasedimentary belt geology, north aspects2lg3y6529368032lg3yid60819941:24000
Kintla-Vaywood families, complex, weakly weathered metasedimentary belt geology, high elevation mountain ridges and upper slopes, north aspects2lg455029367732lg45id60819941:24000
Vaywood-Goatrock families, complex, weakly weathered belts, lower sideslopes toeslopes and stream bottoms of incised drainages, south aspects2lg491729367982lg49id60819941:24000
Vaywood-Handoff complex, 15 to 35 percent slopes2412417777413v2yvid61220031:24000
Hucberit-Vaywood complex, 35 to 70 percent slopes1071741777415v2yxid61220031:24000
Vaywood medial silt loam, 35 to 75 percent slopes2401169777412v2ytid61220031:24000
Vaywood, high precipitation-Vaywood, dry complex, 15 to 35 percent slopes239626777414v2ywid61220031:24000
Kintla-Vaywood-Kintla families, slightly acid subsoil complex, weakly weathered high elevation broadly convex mountain slopes, metasedimentary belt geology, north aspects4106951523968562lg3yid6701:24000
Vaywood-Kintla families, complex, weakly weathered high elevation broadly convex mountain slopes, metasedimentary belt geology, south aspects4095937423968552lg3xid6701:24000
Vaywood-Goatrock families, complex, weakly weathered belts, lower sideslopes toeslopes and stream bottoms of incised drainages, south aspects4441550723968672lg49id6701:24000
Kintla-Vaywood families, complex, weakly weathered metasedimentary belt geology, high elevation mountain ridges and upper slopes, north aspects4401442123968632lg45id6701:24000
Kintla-Vaywood families, complex, weakly weathered metasedimentary belt geology, high elevation mountain ridges and upper slopes, south aspects441674123968642lg46id6701:24000
Vaywood-Goatrock-Humic Udivitrands families, complex, weakly weathered belt geology, mid to high elevation broadly convex mountain slopes, north aspects, fern glades452401223970092lg8wid6701:24000
Vaywood-Humic Udivitrands-Goatrock families, complex, weakly weathered belt geology, mid to high elevation broadly convex mountain slopes, south aspects, fern glades451357123970072lg8tid6701:24000
Vaywood-Handoff complex, 15 to 35 percent slopesv2yv5582936846v2yvid6701:24000
Vaywood medial silt loam, 15 to 35 percent slopes54qy424285100754qyid6701:24000
Humic Udivitrands-Vaywood-Goatrock families, complex, weakly weathered belt geology, mid to high elevation broadly convex mountain slopes, south aspects, fern glades45040823970062lg8sid6701:24000
Vaywood medial silt loam, 35 to 75 percent slopes54qz100285100854qzid6701:24000
McCay, Vaywood and Muddycreek families, cirque basins2x6td3130444892x6tdid6701:24000
McCay, Vaywood and Muddycreek families, cirque basins42QA4689028090862tr5dmt60319891:24000
Vaywood family, glacial-valley floors, extremely bouldery46OA3757428090922tr5lmt60319891:24000
Vaywood family, moderately steep glacial-valley trains, extremely bouldery47OA1585428090942tr5nmt60319891:24000
Vaywood family, nivation hollows43QA1499828090872tr5fmt60319891:24000
Vaywood family, very stony-Rock outcrop-Mitten family, extremely stony association, dissected stream breaklands61QD1126128091102tr65mt60319891:24000
Vaywood family, glacial-valley floors, extremely bouldery46OA18929953472tr5lmt63819851:24000
Vaywood family, moderately steep glacial-valley trains, extremely bouldery47OA7429953482tr5nmt63819851:24000
Vaywood family, nivation hollows43QA5929953442tr5fmt63819851:24000
Vaywood family, very stony-Rock outcrop-Mitten family, extremely stony association, dissected stream breaklands61QD3729953602tr65mt63819851:24000
Vaywood family, moderately steep glacial-valley trains, extremely bouldery47OA429953832tr5nmt64419951:24000
Vaywood family, very stony-Rock outcrop-Mitten family, extremely stony association, dissected stream breaklands61QD15429954382tr65mt65119971:24000
Vaywood family, moderately steep glacial-valley trains, extremely bouldery47OA1031648482tr5nmt65119971:24000
Vaywood family, nivation hollows43QA829954272tr5fmt65119971:24000
McCay, Vaywood and Muddycreek families, cirque basins42QA229954262tr5dmt65119971:24000
Katkitos-Vaywood family-Wolftail, occasionally flooded complex, 0 to 15 percent slopes821C218628482752v5v7mt66320171:24000
Vaywood medial silt loam, 30 to 60 percent slopes50811605621196nvdlwa06320121:24000
Vaywood medial silt loam, 15 to 30 percent slopes5080879621195nvdkwa06320121:24000
Kintla-Vaywood families, complex, weakly weathered metasedimentary belt geology, high elevation mountain ridges and upper slopes, north aspects2lg4522028509012lg45wa65119811:24000
Kintla-Vaywood families, complex, weakly weathered metasedimentary belt geology, high elevation mountain ridges and upper slopes, south aspects2lg4614228509212lg46wa65119811:24000
Kintla-Vaywood-Kintla families, slightly acid subsoil complex, weakly weathered high elevation broadly convex mountain slopes, metasedimentary belt geology, north aspects2lg3y4628509332lg3ywa65119811:24000
Vaywood-Kintla families, complex, weakly weathered high elevation broadly convex mountain slopes, metasedimentary belt geology, south aspects2lg3x2628509112lg3xwa65119811:24000

Map of Series Extent

Approximate geographic distribution of the VAYWOOD 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 .