Official Series Description


Lab Data Summary

Aggregate lab data for the KINA soil series. This aggregation is based on all pedons with a current taxon name of KINA, 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 KINA 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
22083P0118S1982AK280005Kina3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties56.5291672,-132.75

Water Balance

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

There are insufficient data to create the water balance bar figure.



There are insufficient data to create the water balance line figure.

Sibling Summary

Siblings are those soil series that occur together in map units, in this case with the KINA 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 KINA 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 KINA 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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Click the image to view it full size.

Click the image to view it full size.

Click the image to view it full size.

Click the image to view it full size.

Competing Series

Soil series competing with KINA 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 KINA 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 KINA 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 KINA, 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 KINA 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
Kina-Maybeso association, 5 to 35 percent slopes220C211784496521nnpak64419941:31680
Kina peat, 0 to 35 percent slopes8580601498251nv8ak64419941:31680
Kaikli-Kina association, 0 to 40 percent slopes2544516496671np5ak64419941:31680
Kina-Kaikli association, 0 to 40 percent slopes2343784496541nnrak64419941:31680
Kina-McGilvery complex, 5 to 30 percent slopes15719977496341nn3ak64419941:31680
Maybeso-Kina association, 5 to 35 percent slopes92C9177498331nvjak64419941:31680
St. Nicholas-Kina complex, 5 to 35 percent slopes73C8971497921nt6ak64419941:31680
Kina-Kogish-Staney association, 0 to 35 percent slopes730AC6764497911nt5ak64419941:31680
Kina-Grindall complex, 0 to 40 percent slopes836643498171nv0ak64419941:31680
Isidor-Kina association, 0 to 40 percent slopes724916497881nt2ak64419941:31680
Kina-Maybeso association, 35 to 60 percent slopes220D3783496531nnqak64419941:31680
Kina-Kitkun complex, 5 to 35 percent slopes49C2671497361nrdak64419941:31680
Kina-Kitkun complex, 35 to 60 percent slopes49D1232497371nrfak64419941:31680
Kushneahin-Kina association, 3 to 35 percent slopes22139596494761nh0ak64519921:31680
Kina-Kasiana association, sloping lowlands, 6 to 35 percent slopes6174B60239501411p5gak64619921:31680
Kina-Kasiana association, broken, 6 to 35 percent slopes3674B31386500261p1rak64619921:31680
Kina peat, sloping lowlands, 6 to 35 percent slopes6190B22732501421p5hak64619921:31680
Kina peat, broken, 6 to 35 percent slopes3690B22670500281p1tak64619921:31680
Kina-Sukoi association, broken, 6 to 35 percent slopes3672B18067500251p1qak64619921:31680
Kina-Nakwasina association, broken, 6 to 35 percent slopes3677B17439500271p1sak64619921:31680
Kina peat, 0 to 5 percent slopes6290A13423501451p5lak64619921:31680
Kina-Sukoi association, sloping lowlands, 6 to 35 percent slopes6172B9895501391p5dak64619921:31680
Kina-Nakwasina association, dissected footslopes, 6 to 35 percent slopes5277B6163501131p4kak64619921:31680
Kina-Nakwasina association, rolling hills, 6 to 35 percent slopes4277B4782500591p2tak64619921:31680
Kina-Chichagof association, 6 to 35 percent slopes5296B4322501151p4mak64619921:31680
Kina-Spasski association, 6 to 35 percent slopes6173B2571501401p5fak64619921:31680

Map of Series Extent

Approximate geographic distribution of the KINA 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 .