Official Series Description


Lab Data Summary

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

There are insufficient data to create the lab data summary figure.


Water Balance

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

Click the image to view it full size.



Click the image to view it full size.

Sibling Summary

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

There are insufficient data to create the sibling sketch figure.

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

There are insufficient data to create the annual climate figure.

Geomorphic description summaries for the KINTLA 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 .

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.

Competing Series

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

There are insufficient data to create the competing sketch figure.

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

There are insufficient data to create the annual climate figure.

Geomorphic description summaries for the KINTLA 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.

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 KINTLA, 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 KINTLA 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
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
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
Kintla-Kintla families, very gravelly medial silt loam complex, weakly weathered high elevation broadly convex mountain slopes, metasedimentary belt geology, south aspects, sparsely timbered2lg3s3629368152lg3sid60819941:24000
Kintla-Kintla families, very gravelly medial silt loam-Rock outcrop complex, weakly weathered high elevation broadly convex mountain slopes, metasedimentary belt geology, south aspects2lg3t329367762lg3tid60819941:24000
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
Kintla-Kintla families, very gravelly medial silt loam complex, weakly weathered high elevation broadly convex mountain slopes, metasedimentary belt geology, south aspects, sparsely timbered4063812523968512lg3sid6701:24000
Kintla-Goatrock families, complex, weakly weathered belt geology, lower sideslopes toeslopes and stream bottoms of incised drainages, north aspects, fern glades4431973723968662lg48id6701:24000
Kintla-Vaywood families, complex, weakly weathered metasedimentary belt geology, high elevation mountain ridges and upper slopes, north aspects4401442123968632lg45id6701:24000
Kintla-Goatrock families, complex, weakly weathered belt geology, lower sideslopes toeslopes and stream bottoms of incised drainages along slopes, north aspects4111208023968572lg3zid6701:24000
Kintla-Kintla families, very gravelly medial silt loam-Rock outcrop complex, weakly weathered high elevation broadly convex mountain slopes, metasedimentary belt geology, south aspects407901623968522lg3tid6701:24000
Kintla-Vaywood families, complex, weakly weathered metasedimentary belt geology, high elevation mountain ridges and upper slopes, south aspects441674123968642lg46id6701:24000
Kintla-Goatrock families, complex, weakly weathered belt geology, lower sideslopes toeslopes and stream bottoms of incised drainages along slopes, south aspects412457223968582lg40id6701:24000
Kintla-Goatrock families, complex, weakly weathered metasedimentary belt geology, dissected stream headlands, north aspects41374123968592lg41id6701:24000
Kintla-Goatrock families, complex, weakly weathered metasedimentary belt geology, dissected stream headlands, south aspects41449523968602lg42id6701:24000
Kintla family-Rock outcrop complex, weakly weathered metasedimentary belt geology, high elevation mountain ridges and upper slopes, south aspects44224323968652lg47id6701:24000
Typic Haplocryands-Rock outcrop complex, cirque headwalls2x6tc5430444882x6tcid6701:24000
Typic Haplocryands-Rock outcrop complex, cirque headwalls40QA9685828090812tr57mt60319891:24000
Typic Haplocryands-Constance family-Rock outcrop complex, steep subalpine mountain slopes41QA4157228090832tr59mt60319891:24000
Typic Haplocryands-Rock outcrop complex, cirque headwalls40QA143631648572tr57mt63419881:24000
Typic Haplocryands-Constance family-Rock outcrop complex, steep subalpine mountain slopes41QA2331648582tr59mt63419881:24000
Typic Haplocryands-Rock outcrop complex, cirque headwalls40QA372829953422tr57mt63819851:24000
Typic Haplocryands-Constance family-Rock outcrop complex, steep subalpine mountain slopes41QA34129953432tr59mt63819851:24000
Typic Haplocryands-Rock outcrop complex, cirque headwalls40QA11329953812tr57mt64419951:24000
Typic Haplocryands-Constance family-Rock outcrop complex, steep subalpine mountain slopes41QA44229954252tr59mt65119971:24000
Typic Haplocryands-Rock outcrop complex, cirque headwalls40QA10429954242tr57mt65119971:24000
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 KINTLA 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 .