Official Series Description


Lab Data Summary

Aggregate lab data for the DAMERON soil series. This aggregation is based on all pedons with a current taxon name of DAMERON, 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 DAMERON 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
115BM86195061986MO195006mDameron3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties39.0047222,-93.1616667
115BM89163241989MO163024Dameron2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.4562611,-91.0013083
115BM90019191990MO019019Dameron4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.7353588,-92.3034483
115BM90053361990MO053036Dameron4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.7521111,-92.6464167
115BM90163921990MO163092Dameron2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.9672203,-92.3450012
115BM90163931990MO163093Dameron2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.9672203,-92.3450012
115BM91019871991MO019087Dameron4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties39.0284306,-92.3705915
115BM91019901991MO019090Dameron4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.8230997,-92.3093329
115BM91019951991MO019095Dameron4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties39.13891,-92.3075887
115BM92019061992MO019006Dameron4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.8561156,-92.3347722
115BM03019112003MO019011DAMERON4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.7356111,-92.2061944
115CM04163502004MO163050DAMERON4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties39.4597222,-91.2905556
116AM90053071990MO053007DAMERON4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.68725,-92.6824444
116AM90053391990MO053039Dameron4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.7583056,-92.7603583
116AM90053421990MO053042Dameron4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.7517778,-92.8676667
116AM90161101990MO161010Dameron4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties37.968,-91.7282
116AM91161121991MO161012Dameron4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties37.9954,-91.8576
116AM93161121993MO161012Dameron4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.006,-91.7873
116AM94161091994MO161009Dameron4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.0133333,-91.7658333
116AM97125261997MO125026Dameron4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.1299224,-92.1152749
116BM90057011990MO057001Dameron4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties37.3810944,-93.8764167
116BM92057251992MO057025Dameron4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties37.4173306,-93.7572667
116BM92057781992MO057078Dameron4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties37.4051444,-93.7417778
116BM92057801992MO057080Dameron4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties37.4060111,-93.7429833
116BM93057221993MO057034Dameron4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties37.4347222,-93.6269444
116BM98097031998MO097003Dameron4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties37.22485,-94.4274556
116CM95223021995MO223002Dameron4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties37.2724991,-90.4749985

Water Balance

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

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Competing Series

Soil series competing with DAMERON 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 DAMERON 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 DAMERON 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 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 DAMERON, 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 DAMERON 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
Dameron silt loam, 1 to 3 percent slopes, frequently flooded67014725798822qs33mo01119691:24000
Cedargap-Dameron complex, 0 to 2 percent slopes, frequently flooded660171649184817669vmo01919981:24000
Cedargap-Dameron complex, 1 to 3 percent slopes, frequently flooded67013147525754382r0c9mo01919981:24000
Dameron silt loam, 1 to 3 percent slopes, frequently flooded670146226730442rt12mo03920011:24000
Dameron silt loam, 0 to 3 percent slopes, occasionally flooded66077490425337422qp9hmo05319931:24000
Dameron silt loam, 1 to 4 percent slopes, occasionally flooded66135305626882562qs37mo05319931:24000
Dameron silt loam, 1 to 3 percent slopes, frequently flooded67014636026730582rt12mo05719961:24000
Dameron silt loam, 0 to 2 percent slopes, frequently flooded66001289825334582qp83mo05719961:24000
Dameron silt loam, 1 to 3 percent slopes, frequently flooded670148526730732rt12mo07719791:24000
Dameron silt loam, clayey substratum, 1 to 3 percent slopes, frequently flooded78753198524876272t7gzmo09319881:24000
Dameron silt loam, clayey substratum, 0 to 3 percent slopes, frequently flooded7875113949012632t7fnmo09319881:24000
Dameron silt loam, 1 to 3 percent slopes, frequently flooded6701446826731182rt12mo10919791:24000
Dameron silt loam, 0 to 2 percent slopes, frequently flooded6600136225334572qp83mo10919791:24000
Dameron silt loam, 1 to 4 percent slopes, occasionally flooded66135305425755542qs37mo11319851:24000
Dameron silt loam, 0 to 2 percent slopes, frequently flooded66001187025755552qp83mo11319851:24000
Dameron silt loam, 0 to 3 percent slopes, occasionally flooded6607740125337402qp9hmo11319851:24000
Dameron silt loam, 0 to 3 percent slopes, occasionally flooded6607742825337392qp9hmo13519621:24000
Dameron silt loam, 1 to 4 percent slopes, occasionally flooded6613536026882592qs37mo13519621:24000
Dameron silt loam, 1 to 3 percent slopes, frequently flooded670144026731352rt12mo14119961:24000
Dameron silt loam, 1 to 3 percent slopes, frequently flooded67014575625799162qs33mo15919901:24000
Dameron silt loam, 0 to 2 percent slopes, frequently flooded6600126125334522qp83mo15919901:24000
Dameron, occasionally flooded-Cedargap, frequently flooded complex, 0 to 3 percent slopes660784250889294yvcxmo16319911:24000
Cedargap-Dameron complex, 1 to 3 percent slopes, frequently flooded67013234226882352r0c9mo16319911:24000
Dameron silt loam, 1 to 3 percent slopes, frequently flooded670146826731582rt12mo16719931:24000
Dameron silt loam, 1 to 4 percent slopes, occasionally flooded66135146325446272qs37mo19519891:24000
Dameron silt loam, 0 to 3 percent slopes, occasionally flooded6607712225337412qp9hmo19519891:24000
Dameron silt loam, 1 to 3 percent slopes, frequently flooded670145125446172qs33mo19519891:24000
Dameron silt loam, 0 to 2 percent slopes, frequently flooded660012925334542qp83mo19519891:24000
Dameron silt loam, 0 to 2 percent slopes, frequently flooded66001944025334552qp83mo22519881:24000
Dameron silt loam, 1 to 3 percent slopes, frequently flooded67014177126731982rt12mo22519881:24000

Map of Series Extent

Approximate geographic distribution of the DAMERON 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 .