Official Series Description


Lab Data Summary

Aggregate lab data for the FLANLY soil series. This aggregation is based on all pedons with a current taxon name of FLANLY, 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 FLANLY 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
18UCD755502975-CA-55-029xFlanly4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties37.920573,-120.30341
18UCD755503175-CA-55-031xFlanly3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties37.8829739,-120.3830093
1886P017685CA115011Flanly6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties39.3898811,-121.2268753
22AUCD755502675-CA-55-026xFlanly3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties37.7735339,-120.2149866
22A11N6750R11CA109001Flanly6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties37.7736111,-120.2144444

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the FLANLY 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 FLANLY 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 FLANLY 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 FLANLY 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 flats position figure.

Competing Series

Soil series competing with FLANLY 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 FLANLY 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 FLANLY 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.

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

Soil series sharing subgroup-level classification with FLANLY, 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 FLANLY 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
Flanly-Swedesflat-Rackerby , 15 to 30 percent slopes5848169749431t4v6ca61220051:24000
Parkshill-Flanly-Hurleton , 2 to 15 percent slopes5776175461540hh8dca61220051:24000
Flanly-Swedesflat , 2 to 15 percent slopes5784491461539hh8cca61220051:24000
Flanly-Sommeyflat , 2 to 15 percent slopes5852387749430t4v5ca61220051:24000
Flanly sandy loam, 30 to 50 percent slopes151yu162767855ts0jca61220051:24000
Flanly sandy loam, 8 to 15 percent slopes149yu714081261j88fca61220051:24000
Flanly sandy loam, 8 to 15 percent slopes1493865460458hg4hca61819911:24000
Flanly sandy loam, 15 to 30 percent slopes1503165460459hg4jca61819911:24000
Flanly-Orose-Verjeles complex, 3 to 8 percent slopes1532975460462hg4mca61819911:24000
Flanly sandy loam, 30 to 50 percent slopes1512055460460hg4kca61819911:24000
Flanly-Orose-Verjeles complex, 8 to 15 percent slopes1541300460463hg4nca61819911:24000
Flanly sandy loam, 3 to 8 percent slopes148980460457hg4gca61819911:24000
Flanly-Rock outcrop complex, 50 to 75 percent slopes152805460461hg4lca61819911:24000
Flanly sandy loam, 8 to 15 percent slopes149220640468phg8ca61919701:24000
Sierra-Flanly complex, 30 to 60 percent slopes6075601723997702lk4yca63020181:24000
Sierra-Flanly complex, 15 to 65 percent slopes6078384829247012x4c6ca63020181:24000
Sierra-Flanly complex, 3 to 15 percent slopes6071262024412532myb3ca63020181:24000
Flanly loam, 8 to 30 percent slopes6079209429247392x4c9ca63020181:24000
Flanly-Verjeles complex, 0 to 8 percent slopes6072196829247382x4c8ca63020181:24000
Urban land-Sierra-Flanly complex, 3 to 25 percent slopes9011158124037212lp8dca63020181:24000
Sierra-Flanly complex, 3 to 15 percent slopes607126629250122myb3ca64919671:24000
Sierra-Flanly complex, 30 to 60 percent slopes60756629249882lk4yca64919671:24000
Flanly loam, 8 to 30 percent slopes60792029249892x4c9ca64919671:24000
Flanly-Verjeles complex, 0 to 8 percent slopes6072329249862x4c8ca64919671:24000

Map of Series Extent

Approximate geographic distribution of the FLANLY 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 .