Official Series Description


Lab Data Summary

Aggregate lab data for the KACHEMAK soil series. This aggregation is based on all pedons with a current taxon name of KACHEMAK, 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 KACHEMAK 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
22483P083883AK122002Kachemak7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties59.6666679,-151.5416718
22483P084183AK122005Kachemak6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties59.7138901,-151.5283356
22483P084283AK122006Kachemak7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties59.7097206,-151.4674988
22487P078387AK122004Kachemak7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties59.7166672,-151.5166626
22440A0619S1960AK122003KACHEMAK5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties59.6769676,-151.5897827
22440A0620S1960AK122004KACHEMAK5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties59.6661377,-151.5486755
n/a87P078487AK122005Kachemak7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Propertiesn/a
n/a87P078587AK122006Kachemak7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Propertiesn/a

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the KACHEMAK 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 KACHEMAK 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 KACHEMAK 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 KACHEMAK 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 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 KACHEMAK 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 KACHEMAK 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 KACHEMAK 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 KACHEMAK, 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 KACHEMAK 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
Kachemak silt loam, 8 to 15 percent slopes574960214880091lyd9ak65220051:25000
Kachemak silt loam, 15 to 25 percent slopes575790414880101lydbak65220051:25000
Kachemak silt loam, 4 to 8 percent slopes573636714880081lyd8ak65220051:25000
Kachemak silt loam, forested, 8 to 15 percent slopes584529914880191lydmak65220051:25000
Kachemak silt loam, 25 to 35 percent slopes576465314880111lydcak65220051:25000
Kachemak silt loam, cool, 8 to 15 percent slopes579387014880141lydgak65220051:25000
Kachemak silt loam, 35 to 45 percent slopes577370214880121lyddak65220051:25000
Kachemak silt loam, cool, 25 to 35 percent slopes581336714880161lydjak65220051:25000
Kachemak, cool-Snowdance complex, 4 to 8 percent slopes587324614880221lydqak65220051:25000
Kachemak silt loam, cool, 15 to 25 percent slopes580324114880151lydhak65220051:25000
Kachemak silt loam, forested, 15 to 25 percent slopes585181614880201lydnak65220051:25000
Kachemak silt loam, forested, 4 to 8 percent slopes583175414880181lydlak65220051:25000
Kachemak, cool-Snowdance complex, 8 to 15 percent slopes588166414880231lydrak65220051:25000
Kachemak silt loam, cool, 4 to 8 percent slopes578166314880131lydfak65220051:25000
Kachemak silt loam, cool, 35 to 45 percent slopes582164514880171lydkak65220051:25000
Kachemak, cool-Snowdance complex, 0 to 4 percent slopes58686814880211lydpak65220051:25000

Map of Series Extent

Approximate geographic distribution of the KACHEMAK 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 .