Official Series Description


Lab Data Summary

Aggregate lab data for the KEKAWAKA soil series. This aggregation is based on all pedons with a current taxon name of KEKAWAKA, 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 KEKAWAKA 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
580P052179CA045129Kekawaka7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties39.3836098,-123.2702789

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the KEKAWAKA 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 KEKAWAKA 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 KEKAWAKA series and siblings. Series are sorted according to hierarchical clustering of median values. Source: SSURGO map unit geometry and 1981-2010, 800m PRISM data .

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Geomorphic description summaries for the KEKAWAKA 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 terrace figure.

There are insufficient data to create the 3D flats position figure.

Competing Series

Soil series competing with KEKAWAKA 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 KEKAWAKA series and competing. Series are sorted according to hierarchical clustering of median values. Source: SSURGO map unit geometry and 1981-2010, 800m PRISM data .

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Geomorphic description summaries for the KEKAWAKA 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 .

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There are insufficient data to create the 3D hills figure.

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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 KEKAWAKA, 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

Click a link below to display the diagram. Note that these diagrams may be from multiple survey areas.

  1. CA-2011-05-27-03 | Mendocino County, Eastern Part, and Trinity County, Southwestern Part - 1991

    Pattern of active, metastable, and stable slopes (Soil Survey of Mendocino County, Eastern Part, and Trinity County, Southwestern Part, California; 1991).

Map Units

Map units containing KEKAWAKA 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
Sanhedrin-Kekawaka-Speaker complex, 30 to 50 percent slopes20235752459605hf7zca03319851:24000
Sanhedrin-Kekawaka-Speaker complex, 15 to 30 percent slopes2012655459604hf7yca03319851:24000
Sanhedrin-Kekawaka-Speaker complex, 30 to 50 percent slopes202l24813834w9vqca05519741:24000
Hopland-Sanhedrin-Kekawaka complex, 50 to 75 percent slopes425151470157hgr0ca60120111:24000
Sanhedrin-Kekawaka-Speaker complex, 30 to 50 percent slopes19453284461079hgsjca68719851:24000
Hopland-Sanhedrin-Kekawaka complex, 30 to 50 percent slopes14630839461031hgqzca68719851:24000
Sanhedrin-Kekawaka-Speaker complex, 50 to 75 percent slopes19512356461080hgskca68719851:24000
Hopland-Sanhedrin-Kekawaka complex, 50 to 75 percent slopes14712306461032hgr0ca68719851:24000
Sanhedrin-Kekawaka-Speaker complex, 2 to 30 percent slopes1938204461078hgshca68719851:24000
Hopland-Sanhedrin-Kekawaka complex, 15 to 30 percent slopes1455249461030hgqyca68719851:24000
Kekawaka-Casabonne-Wohly complex, 30 to 50 percent slopes1554980461040hgr8ca68719851:24000
Pardaloe-Kekawaka-Casabonne complex, 50 to 75 percent slopes1723547461057hgrtca68719851:24000
Kekawaka-Casabonne-Wohly loams, 15 to 30 percent slopes1542163461039hgr7ca68719851:24000
Hopland-Sanhedrin-Kekawaka complex, 30 to 50 percent slopes146em16117011381v35fca70119841:24000
Sanhedrin-Kekawaka-Speaker complex, 30 to 50 percent slopes194em6917011451v35nca70119841:24000
Sanhedrin-Kekawaka-Speaker complex, 30 to 50 percent slopes194me13052747853hgsjca70920101:24000
Hopland-Sanhedrin-Kekawaka complex, 50 to 75 percent slopes147me672747840hgr0ca70920101:24000
Hopland-Sanhedrin-Kekawaka complex, 15 to 30 percent slopes145me362747838hgqyca70920101:24000
Sanhedrin-Kekawaka-Speaker complex, 2 to 30 percent slopes193me242747852hgshca70920101:24000
Hopland-Sanhedrin-Kekawaka complex, 30 to 50 percent slopes146me1427478392q203ca70920101:24000

Map of Series Extent

Approximate geographic distribution of the KEKAWAKA 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 .