Official Series Description


Lab Data Summary

Aggregate lab data for the KAIKLI soil series. This aggregation is based on all pedons with a current taxon name of KAIKLI, 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 KAIKLI 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
22083P082683AK130042Kaikli5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties55.9638901,-133.6125031

Water Balance

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

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 KAIKLI 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 KAIKLI 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 KAIKLI 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 KAIKLI, 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 KAIKLI 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
Kaikli-Kina association, 0 to 40 percent slopes2544516496671np5ak64419941:31680
Kina-Kaikli association, 0 to 40 percent slopes2343784496541nnrak64419941:31680
Maybeso-Kaikli complex, 5 to 60 percent slopes20CDX42544496481nnkak64419941:31680
Kaikli mucky peat, 0 to 35 percent slopes24AC33519496641np2ak64419941:31680
St. Nicholas-Kaikli complex, 5 to 75 percent slopes550CE19565497651nsbak64419941:31680
St. Nicholas-Kaikli complex, 5 to 35 percent slopes550C18937497641ns9ak64419941:31680
Kaikli-Grindall association, 5 to 60 percent slopes86CD18869498261nv9ak64419941:31680
St. Nicholas-Kaikli complex, 35 to 60 percent slopes550D16531497661nscak64419941:31680
Kaikli mucky peat, 35 to 60 percent slopes24D9753496651np3ak64419941:31680
Maybeso-Kaikli complex, 5 to 35 percent slopes20C4754496471nnjak64419941:31680
St. Nicholas-Kaikli complex, 60 to 75 percent slopes550E3962497671nsdak64419941:31680
Maybeso-Kaikli complex, 35 to 60 percent slopes20D2227496491nnlak64419941:31680
McGilvery-Kaikli association, 35 to 60 percent slopes80D1809498091ntrak64419941:31680
Kaikli mucky peat, 60 to 75 percent slopes24E1494496661np4ak64419941:31680
McGilvery-Kaikli association, 60 to 75 percent slopes80E561498101ntsak64419941:31680
Kushneahin-Kaikli complex, 5 to 35 percent slopes6516443495641nkvak64519921:31680
St. Nicholas-Kaikli complex, 5 to 35 percent slopes494250495451nk7ak64519921:31680
Kaikli peat, 35 to 55 percent slopes50D1454495511nkfak64519921:31680
Kaikli peat, 5 to 35 percent slopes50B1445495501nkdak64519921:31680
Tolstoi and Kaikli soils, alpine, 76 to 120 percent slopes3003E170886498491nw1ak64619921:31680
Tolstoi and Kaikli soils, subalpine, 36 to 55 percent slopes3670C73660500231p1nak64619921:31680
Tolstoi, Kaikli, and Lithic Cryorthent soils, alpine, broken, 6 to 35 percent slopes3604B52300499711nzzak64619921:31680
Tolstoi, Kaikli, and Lithic Cryorthent soils, alpine, rounded summit, 6 to 35 percent slopes1204B40543498411nvsak64619921:31680
Sukoi, Kaikli, and Verstovia soils, subalpine, 36 to 55 percent slopes3668C19339500211p1lak64619921:31680
Mitkof-Tolstoi-Kaikli complex, 36 to 55 percent slopes3662C19248500181p1hak64619921:31680
Tolstoi and Kaikli soils, subalpine, 6 to 35 percent slopes1270B16152498421nvtak64619921:31680
Fordsterror-Traitors-Kaikli complex, broken, 36 to 55 percent slopes3660C11176500161p1fak64619921:31680
Kaikli-Chuckriver complex, broken, 36 to 55 percent slopes3642C7143499921p0nak64619921:31680
Kaikli-St. Nicholas complex, broken, 36 to 55 percent slopes3694C7072500291p1vak64619921:31680
Mitkof-Tolstoi-Kaikli complex, broken, 56 to 75 percent slopes3662D3612500191p1jak64619921:31680
Fordsterror-Traitors-Kaikli complex, broken, 56 to 75 percent slopes3660D2967500171p1gak64619921:31680
Fordsterror-Traitors-Kaikli complex, rolling hills, 36 to 55 percent slopes4260C2901500571p2rak64619921:31680
Mitkof-Tolstoi-Kaikli complex, shallowly incised, 56 to 75 percent slopes3262D2249499111ny1ak64619921:31680
Mitkof-Tolstoi-Kaikli complex, smooth, 56 to 75 percent slopes3562D950499561nzhak64619921:31680
Mitkof-Tolstoi-Kaikli complex, deeply incised, 56 to 75 percent slopes3162D912498701nwqak64619921:31680
Kaikli-St. Nicholas complex, shallowly incised, 36 to 55 percent slopes3294C859499131ny3ak64619921:31680
Kaikli-St. Nicholas complex, deeply incised, 36 to 55 percent slopes3194C657498711nwrak64619921:31680
Fordsterror-Traitors-Kaikli complex, smooth, 56 to 75 percent slopes3560D549499551nzgak64619921:31680
Kaikli-St. Nicholas complex, smooth, 36 to 55 percent slopes3594C502499581nzkak64619921:31680
Kaikli-Chuckriver complex, smooth, 36 to 55 percent slopes3542C204499381nyxak64619921:31680
Fordsterror-Traitors-Kaikli complex, shallowly incised, 56 to 75 percent slopes3260D193499101ny0ak64619921:31680
Kaikli-Chuckriver complex, shallowly incised, 36 to 55 percent slopes3242C156498941nxhak64619921:31680
Kaikli-St. Nicholas complex, smooth hills, 36 to 55 percent slopes4494C135500841p3mak64619921:31680
Kaikli-Chuckriver complex, smooth hills, 36 to 55 percent slopes4442C16500771p3dak64619921:31680

Map of Series Extent

Approximate geographic distribution of the KAIKLI 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 .