Official Series Description


Lab Data Summary

Aggregate lab data for the FINSEL soil series. This aggregation is based on all pedons with a current taxon name of FINSEL, 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 FINSEL 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.

Pedons used in the lab summary:

MLRALab IDPedon IDTaxonnameCINSSL / NASIS ReportsLink To SoilWeb GMap
1003N033301ORGCAO077Finsel6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties44.6365776,-119.5808868

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the FINSEL 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 FINSEL 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 FINSEL 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 FINSEL 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 FINSEL 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 FINSEL 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 FINSEL 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 FINSEL, 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 FINSEL 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
Finsel-Camool complex, 20 to 50 percent north slopes4012BO173120162rcqzor60720181:24000
Finsel-Polkbutte complex, 30 to 65 percent north slopes26462273426100132rqor6181:24000
Ateron-Finsel complex, 12 to 50 percent north slopes477E369234260662lk5mor6181:24000
Finsel-Polkbutte complex, 12 to 30 percent north slopes26332993434963132rkor6181:24000
Finsel ashy loam, 12 to 30 percent north slopes086250234260782mldor6181:24000
Longbarn-Wickiser-Finsel complex 10 to 40 percent north slopes007194234375612l8c5or6181:24000
Gwinly-Kishwalk-Finsel complex, 2 to 50 percent slopes166E3123426420znhvor6181:24000
Finsel-Powellbutte-Fopiano complex, 12 to 50 percent north slopes29617434347122lb8ror6181:24000
Hutchley-Kishwalk-Finsel complex, 20 to 50 percent slopes4324NO763385407znj5or62620181:24000
Hutchley-Kishwalk-Finsel complex, 20 to 50 percent slopes212E180573426043znj5or6271:24000
Finsel-Camool complex, 20 to 50 percent north slopes204E131123425014rcqzor6271:24000
Ateron-Kishwalk-Finsel complex, 20 to 50 percent slopes231E227534263632m79dor6271:24000
Gwinly-Kishwalk-Finsel complex, 2 to 50 percent slopes166E16893426417znhvor6271:24000
Finsel-Luckycreek complex, MLRA 9, 2 to 20 percent slopes234C108934295412mhwjor6271:24000
Finsel-Camool-Rock outcrop complex, 40 to 90 percent north slopes204F4253425019rcr0or6271:24000
Hutchley-Finsel-Bocker complex, 20 to 50 percent slopes211E3593432103znj3or6271:24000
Finsel-Camool complex, 20 to 50 percent north slopes204E80493421705rcqzor6771:24000
Finsel-Camool-Rock outcrop complex, 40 to 90 percent north slopes204F61483421736rcr0or6771:24000
Observation-Finsel-Ateron complex, 10 to 30 percent north slopes476C61273421737261m7or6771:24000
Ateron-Finsel complex, 12 to 50 percent north slopes477E266834218112lk5mor6771:24000
Finsel ashy loam, 12 to 30 percent north slopes086177334218862mldor6771:24000
Finsel-Polkbutte complex, 30 to 65 percent north slopes2647373424440132rqor6771:24000

Map of Series Extent

Approximate geographic distribution of the FINSEL 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 .