Official Series Description


Lab Data Summary

Aggregate lab data for the FARLIN soil series. This aggregation is based on all pedons with a current taxon name of FARLIN, 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 FARLIN were used in the calculation. Source: KSSL snapshot . Methods used to assemble the KSSL snapshot used by SoilWeb / SDE

There are insufficient data to create the lab data summary figure.


Water Balance

Monthly water balance estimated using a leaky-bucket style model for the FARLIN 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 FARLIN 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 FARLIN 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 FARLIN 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 FARLIN 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 FARLIN 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 FARLIN 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 terrace figure.

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

Soil series sharing subgroup-level classification with FARLIN, 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 FARLIN 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
Skaggs-Farlin, stony-Levengood complex, 8 to 25 percent slopes164E1953039571pd3qmt60219631:20000
Farlin-Hardhart, stony-Rock outcrop complex, 25 to 60 percent slopes264F743039580wcj1mt60219631:20000
Hardhart-Farlin, stony-Checkerboard complex, 4 to 15 percent slopes164D373039570pd3jmt60219631:20000
Farlin, stony-Raynesford complex, 8 to 15 percent slopes664D273039577pg6smt60219631:20000
Farlin, stony-Hardhart-Checkerboard, stony complex, 15 to 35 percent slopes664E173039578pghvmt60219631:20000
Farlin-Hardhart, stony-Checkerboard, extremely stony complex, 15 to 60 percent slopes764F103039579pgvymt60219631:20000
Farlin, very bouldery-Farlin, stony complex, 8 to 25 percent slopes14E1971609115nftwmt60420011:24000
Tibson, stony-Farlin, extremely bouldery-Rooset complex, 4 to 15 percent slopes, landslides931D626334702pp9tmt60420011:24000
Hanson, stony-Tropal complex, 8 to 45 percent slopes114F10524037992lpbxmt60520071:24000
Tropal-Farlin, very stony-Rock outcrop complex, 8 to 35 percent slopes812E5324962762mfszmt60520071:24000
Farlin loam, 2 to 15 percent slopes214D2124962882pc5cmt60520071:24000
Crago, very stony-Raynesford-Farlin complex, 8 to 35 percent slopes210E3436797982vsccmt61220111:24000
Farlin loam, 2 to 15 percent slopes214D205724833902pc5cmt61220111:24000
Farlin, stony-Tropal complex, 8 to 45 percent slopes114F177116890991tpn2mt61220111:24000
Farlin, very bouldery-Farlin, stony complex, 8 to 25 percent slopes14E10452597679nftwmt61220111:24000
Tropal-Farlin, very stony-Rock outcrop complex, 8 to 35 percent slopes812E71724263382mfszmt61220111:24000
Tibson, stony-Farlin, extremely bouldery-Rooset complex, 15 to 50 percent slopes, landslides931F414524263022mfrtmt61420121:24000
Tibson, stony-Farlin, very bouldery complex, 8 to 35 percent slopes932E148024263052mfrxmt61420121:24000
Tibson, stony-Farlin, extremely bouldery-Rooset complex, 4 to 15 percent slopes, landslides931D105725174412pp9tmt61420121:24000
Tropal-Farlin, very stony-Rock outcrop complex, 8 to 35 percent slopes812E75125174452mfszmt61420121:24000
Rockisland, very bouldery-Levengood-Farlin, very stony complex, 4 to 15 percent slopes883D33225187382ppbmmt61420121:24000
Farlin-Raynesford complex, 2 to 8 percent slopes527C42624870182pgydmt62420211:24000
Findon, stony-Farlin, very stony-Levengood families, complex, 8 to 35 percent slopes, landslides2105E604626274322rf1smt6321:24000
Farlin-Hardhart, stony-Rock outcrop complex, 25 to 60 percent slopes264F537423927972l9x0mt6321:24000
Skaggs-Farlin, stony-Levengood complex, 8 to 25 percent slopes164E421223927802l9wgmt6321:24000
Farlin, stony-Levengood-Skaggs complex, 15 to 45 percent slopes364F175723928082l9xcmt6321:24000
Farlin, stony-Hardhart-Checkerboard, stony complex, 15 to 35 percent slopes664E155924862732pg5cmt6321:24000
Farlin, stony-Raynesford complex, 8 to 15 percent slopes, 8 to 15 percent slopes664D84124862722pg5bmt6321:24000
Hardhart-Farlin, stony-Checkerboard complex, 4 to 15 percent slopes164D82023927792l9wfmt6321:24000
Farlin-Hardhart, stony-Checkerboard, extremely stony complex, 15 to 60 percent slopes764F8092604444pgvymt6321:24000
Farlin, stony-Findon, very stony complex, 4 to 15 percent slopes358D6692632246v6khmt6321:24000
Farlin-Raynesford complex, 2 to 8 percent slopes527C15025124422pgydmt6321:24000
Tropal-Farlin, very stony-Rock outcrop complex, 8 to 35 percent slopes812E66025370372mfszmt63619831:24000
Farlin-Hardhart, stony-Rock outcrop complex, 25 to 60 percent slopes264F7270815425wcj1mt63720141:24000
Farlin, stony-Levengood-Skaggs complex, 15 to 45 percent slopes364F5746637167pd0smt63720141:24000
Skaggs-Farlin, stony-Levengood complex, 8 to 25 percent slopes164E5020637258pd3qmt63720141:24000
Farlin, stony-Hardhart-Checkerboard, stony complex, 15 to 35 percent slopes664E3480639556pghvmt63720141:24000
Farlin, stony-Raynesford complex, 8 to 15 percent slopes664D2867639275pg6smt63720141:24000
Farlin-Hardhart, stony-Checkerboard, extremely stony complex, 15 to 60 percent slopes764F1941639900pgvymt63720141:24000
Hardhart-Farlin, stony-Checkerboard complex, 4 to 15 percent slopes164D1918637252pd3jmt63720141:24000
Farlin, stony-Roxal-Levengood complex, 8 to 35 percent slopes458E442780870v6kcmt63720141:24000
Farlin, stony-Findon, very stony complex, 4 to 15 percent slopes358D308780874v6khmt63720141:24000

Map of Series Extent

Approximate geographic distribution of the FARLIN 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 .