Official Series Description


Lab Data Summary

Aggregate lab data for the WAKENDA soil series. This aggregation is based on all pedons with a current taxon name of WAKENDA, 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 WAKENDA 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
107BM87041151987MO041015Wakenda3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties39.3705667,-92.8708833
107BM89041101989MO041010Wakenda4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties39.3280139,-92.8037722
109M87041161987MO041016Wakenda3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties39.4346694,-93.1192194
109M89041061989MO041006Wakenda4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties39.3517278,-92.8443167
109M89041071989MO041007Wakenda4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties39.4078722,-92.8800833
109M89041081989MO041008Wakenda4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties39.4457972,-92.9567556
115BM88163471988MO163047Wakenda2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.9672203,-92.3450012
115BM89041261989MO041026Wakenda4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.9672203,-92.3450012
115BM89053031989MO053003Wakenda4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.9672203,-92.3450012
115BM89053251989MO053025Wakenda4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.9672203,-92.3450012
115BM89053261989MO053026Wakenda4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.9672203,-92.3450012
115BM89163181989MO163018Wakenda2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.4562611,-91.0013083
115BM89163201989MO163020Wakenda2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.4562611,-91.0013083

Water Balance

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

Click the image to view it full size.

Click the image to view it full size.

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.

Soil series sharing subgroup-level classification with WAKENDA, 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 WAKENDA 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
Wakenda silt loam, 2 to 5 percent slopes441B834023786152kv4jil00119971:12000
Wakenda silt loam, 2 to 5 percent slopes441B6442008026qyhil11920011:12000
Wakenda silt loam, 5 to 10 percent slopes, eroded441C21052008056qylil11920011:12000
Wakenda silt loam, 2 to 5 percent slopes441B50032011066r89il14920011:12000
Wakenda silt loam, 2 to 5 percent slopes441B201518302864g4il16319971:12000
Wakenda silt loam, 5 to 10 percent slopes, eroded441C2195718302964g5il16319971:12000
Wakenda silt loam, 2 to 5 percent slopes10151712125282442ql0tmo03319881:24000
Wakenda silt loam, 5 to 9 percent slopes, eroded10153509025282502ql0wmo03319881:24000
Wakenda silt loam, 2 to 5 percent slopes10151916125282432ql0tmo04119921:24000
Wakenda silt loam, 5 to 9 percent slopes, eroded1015381225282492ql0wmo04119921:24000
Wakenda silt loam, 2 to 5 percent slopes10151389425282392ql0tmo05319931:24000
Wakenda silt loam, 5 to 9 percent slopes, eroded10153130325282472ql0wmo05319931:24000
Wakenda silt loam, 2 to 5 percent slopes1015140325282422ql0tmo08919751:24000
Wakenda silt loam, 2 to 5 percent slopes10151336625282412ql0tmo15919901:24000
Wakenda silt loam, 5 to 9 percent slopes10152122925282462ql0vmo15919901:24000
Wakenda silt loam, 2 to 5 percent slopes10151233025282402ql0tmo16319911:24000
Wakenda silt loam, 5 to 9 percent slopes10152148625282452ql0vmo16319911:24000
Wakenda silt loam, 5 to 9 percent slopes, eroded1015324625282482ql0wmo19519891:24000

Map of Series Extent

Approximate geographic distribution of the WAKENDA 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 .