Official Series Description


Lab Data Summary

Aggregate lab data for the DANLEY soil series. This aggregation is based on all pedons with a current taxon name of DANLEY, 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 DANLEY 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
14089P042688NY099004Danley3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties42.5722237,-76.8183365
14040A0269S1959NY109004Danley4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties42.4130554,-76.5747223

Water Balance

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

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.

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

Competing Series

Soil series competing with DANLEY 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 DANLEY series and competing. 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 DANLEY 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.

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 DANLEY, 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. NY-2012-02-15-42 | Seneca County - April 1972

    Cross section of Darien-Angola association (Soil Survey of Seneca County, New York; April 1972).

Map Units

Map units containing DANLEY 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
Danley silt loam, 3 to 8 percent slopesDaB22202907899rl9ny02919791:15840
Danley silt loam, 8 to 15 percent slopesDaC8882907909rlbny02919791:15840
Danley silt loam, 15 to 25 percent slopesDaD4582907919rlcny02919791:15840
Danley silt loam, 3 to 8 percent slopesDcB13292918059sn2ny04519811:15840
Danley silt loam, 8 to 15 percent slopesDcC9222918069sn3ny04519811:15840
Danley silt loam, 15 to 25 percent slopesDcD3332918079sn4ny04519811:15840
Danley silt loam, 8 to 15 percent slopes70C183431128612yfvxny05120191:24000
Danley silt loam, 15 to 25 percent slopes70D29731128622yfvyny05120191:24000
Danley-Lansing complex, 3 to 8 percent slopes106B211124542362w3mkny06920121:12000
Danley and Nunda soils, 15 to 25 percent slopesDaD8632942029w4dny07719931:24000
Danley and Nunda soils, 8 to 15 percent slopesDaC8022942019w4cny07719931:24000
Danley and Nunda soils, 3 to 8 percent slopesDaB3382942009w4bny07719931:24000
Darien-Danley-Cazenovia silt loams, 3 to 8 percent slopesDdB119502947099wnrny09919661:15840
Danley silty clay loam, 15 to 25 percent slopes, erodedDlD313062953429xb5ny12119691:20000
Danley silt loam, 8 to 15 percent slopesDeC7982953419xb4ny12119691:20000
Danley silt loam, 3 to 8 percent slopesDeB7692953409xb3ny12119691:20000
Danley silty clay loam, 25 to 40 percent slopes, erodedDlE32392953439xb6ny12119691:20000

Map of Series Extent

Approximate geographic distribution of the DANLEY 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 .