Official Series Description


Lab Data Summary

Aggregate lab data for the CHEHALIS soil series. This aggregation is based on all pedons with a current taxon name of CHEHALIS, 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 CHEHALIS were used in the calculation. Source: KSSL snapshot . Methods used to assemble the KSSL snapshot used by SoilWeb / SDE

Click the image to view it full size.

Pedons used in the lab summary:

MLRALab IDPedon IDTaxonnameCINSSL / NASIS ReportsLink To SoilWeb GMap
291P074791OR047001Chehalis5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties45.0583344,-123.0333328
200P0500S1999OR043002Chehalis6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties44.5744438,-123.1411133
206N0228S2005OR003001Chehalis7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties44.3023071,-123.2278519
206N0234S2005OR071006Chehalis7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties45.1336937,-123.0317459
215N0059S2014WA027411Chehalis7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties46.8506133,-123.2724466

Water Balance

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

Click the image to view it full size.



Click the image to view it full size.

Sibling Summary

Siblings are those soil series that occur together in map units, in this case with the CHEHALIS series. Sketches are arranged according to their subgroup-level taxonomic structure. Source: SSURGO snapshot , parsed OSD records and snapshot of SC database .

Click the image to view it full size.

Select annual climate data summaries for the CHEHALIS series and siblings. Series are sorted according to hierarchical clustering of median values. Source: SSURGO map unit geometry and 1981-2010, 800m PRISM data .

Click the image to view it full size.

Geomorphic description summaries for the CHEHALIS 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.

Click the image to view it full size.

Click the image to view it full size.

Competing Series

Soil series competing with CHEHALIS share the same family level classification in Soil Taxonomy. Source: parsed OSD records and snapshot of the SC database .

Click the image to view it full size.

Select annual climate data summaries for the CHEHALIS 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 CHEHALIS 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 CHEHALIS, 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. WA-2012-05-11-18 | Grays Harbor County Area, Pacific County, and Wahkiakum County - July 1986

    Pattern of soils and parent material in general soil map unit 3 (Soil Survey of Grays Harbor County Area, Pacific County, and Wahkiakum County, Washington; July 1986).

  2. WA-2012-05-11-29 | Lewis County Area - May 1987

    Pattern of soils and parent material in the Reed-Chehalis map unit (Soil Survey of Lewis County Area, Washington; May 1987).

Map Units

Map units containing CHEHALIS 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
Chehalis silty clay loam, 0 to 3 percent slopes4010714852892vr8or00320041:24000
Chehalis silt loam, 0 to 3 percent slopes381536852952vrgor00320041:24000
Chehalis silt loam, high precipitation, 0 to 3 percent slopes39482700519rhydor00320041:24000
Chehalis silty clay loam, occasionally flooded1446296230622twor05319771:20000
Chehalis silty clay loam, 0 to 3 percent slopes2002A127111282dgl4or05319771:20000
Chehalis silty clay loam, occasional overflow9582561530220vor06719751:20000
Chehalis silt loam, occasional overflow1017446142021x9or06719751:20000
Chehalis silty clay loam, 0 to 3 percent slopes2002A846527112702dgl4or07119671:24000
Chehalis silt loam, 0 to 3 percent slopes2040A242127113282lkh8or07119671:24000
Chehalis silt loam16229761611223gor61019821:20000
Chehalis silty clay loam, occasionally flooded269349626522361or63719811:20000
Chehalis-Urban land complex27827626532362or63719811:20000
Chehalis silty clay loam21108956427724wgor63919831:20000
Chehalis silty clay loamCh66256407524nyor64319661:20000
Chapman-Chehalis complex, 0 to 3 percent slopes37A66556684127k5or64919941:24000
Chehalis silty clay2682736626sqj4wa01519941:24000
Chehalis silt loam306178736242glzwa62719791:24000
Chehalis-Maytown complex, 0 to 10 percent slopes1224218330158592w94nwa62719791:24000
Maytown-Chehalis-Rennie complex, 0 to 10 percent slopes1223107730158582w94mwa62719791:24000
Chehalis silty clay4810203744412hgbwa64119801:24000
Chehalis silt loam472413744402hg9wa64119801:24000
Chehalis-Maytown complex, 0 to 10 percent slopes122434430158862w94nwa64119801:24000
Maytown-Chehalis-Rennie complex, 0 to 10 percent slopes12237330158852w94mwa64119801:24000
Chehalis silt loam9A484747242hrgwa65319741:24000
Chehalis silt loam26383924546602nd8lwa66719831:24000
Chehalis-Maytown complex, 0 to 10 percent slopes12245530158932w94nwa66719831:24000
Maytown-Chehalis-Rennie complex, 0 to 10 percent slopes12232030159072w94mwa66719831:24000

Map of Series Extent

Approximate geographic distribution of the CHEHALIS 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 .