Official Series Description


Lab Data Summary

Aggregate lab data for the KILLARNEY soil series. This aggregation is based on all pedons with a current taxon name of KILLARNEY, 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 KILLARNEY 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
116AM95613111995MO203011MKillarney4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties37.1720361,-91.2565917
116AM95613131995MO203013MKillarney4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties37.1707972,-91.2564389
116AM97613421997MO203042MKillarney4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties37.1249917,-91.235025
116AM98613041998MO203004MKillarney4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties37.1262861,-91.1983667
116AM98613131998MO203013MKillarney4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties37.1257722,-91.1830583
116AM98613141998MO203014MKillarney4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties37.1280528,-91.1865611
116AM98613221998MO203022MKillarney4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties37.1157528,-91.23795
116CM88123011988MO123001MKillarney3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties37.4828339,-90.345108
116CM88123051988MO123005MKillarney3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties37.4711113,-90.632225
116CM88123101988MO123010MKillarney3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties37.4731102,-90.4381638
116CM99223121999MO223030Killarney4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties37.2229156,-90.5015488
116CM99223151999MO223031Killarney4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties37.2230721,-90.5013733
116CM99223141999MO223033Killarney4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties37.2216873,-90.5029373
116CM00221122000MO221275Killarney4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties37.8085556,-90.7166672
116CM00221132000MO221276Killarney4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties37.8083878,-90.7170029

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the KILLARNEY 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 KILLARNEY 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 KILLARNEY 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 KILLARNEY 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 KILLARNEY 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 KILLARNEY 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 KILLARNEY 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 KILLARNEY, 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. MO-2010-09-08-08 | Madison County - 2005

    Typical pattern of soils and parent material in the Irondale-Killarney-Trackler association (Soil Survey of Madison County, Missouri; 2005).

Map Units

Map units containing KILLARNEY 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
Killarney-Frenchmill complex, 15 to 45 percent slopes, rubbly770003625011112t7hlmo01720041:24000
Killarney-Frenchmill complex, 15 to 45 percent slopes, rubbly7700060525011182t7hlmo03519881:24000
Killarney-Frenchmill complex, 15 to 45 percent slopes, rubbly770002607225011122t7hlmo09319881:24000
Mudlick-Irondale-Killarney complex, 15 to 45 percent slopes, rocky, extremely bouldery77012118625012252vxpqmo09319881:24000
Killarney-Frenchmill complex, 15 to 45 percent slopes, rubbly770001727325011132t7hlmo12319991:24000
Killarney-Frenchmill complex, 15 to 45 percent slopes, rubbly77000318925011142t7hlmo17920041:24000
Mudlick-Irondale-Killarney complex, 15 to 45 percent slopes, rocky, extremely bouldery77012143125012262vxpqmo17920041:24000
Killarney-Frenchmill complex, 15 to 45 percent slopes, rubbly77000177725011152t7hlmo18719791:24000
Killarney-Frenchmill complex, 15 to 45 percent slopes, rubbly77000279225011192t7hlmo20320041:24000
Killarney-Frenchmill complex, 15 to 45 percent slopes, rubbly77000133125011162t7hlmo22120031:24000
Mudlick-Irondale-Killarney complex, 15 to 45 percent slopes, rocky, extremely bouldery77012918225012242vxpqmo22320041:24000
Killarney-Frenchmill complex, 15 to 45 percent slopes, rubbly77000229825011172t7hlmo22320041:24000

Map of Series Extent

Approximate geographic distribution of the KILLARNEY 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 .