Official Series Description


Lab Data Summary

Aggregate lab data for the BARTLE soil series. This aggregation is based on all pedons with a current taxon name of BARTLE, 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 BARTLE 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
114ADA67031967IN027003Bartle2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.6704611,-86.9607778
114BBA69011969IN005001Bartle2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties39.1766667,-86.0025722
114BDC78041978IN031004Bartle2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties39.2468694,-85.3420778
114BJN80061980IN071006Bartle2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.9557389,-85.8162167
114BRI79082017IN137002Bartle2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties39.2422333,-85.3307278
114B90P00452017IN143001Bartle5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.6666679,-85.7663879
120BMT80062016IN101001Bartle2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.6463444,-86.8667833
120BOR77042016IN117002Bartle2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.4724889,-86.6684639
120CWS79021979IN175002Bartle3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.5626,-85.8956389
120CLW80022015IN093004Bartle3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.9539139,-86.3403556
120CBR82052016IN013002Bartle2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties39.1961639,-86.3477333
n/aRO-0851959-OH141-085Bartle2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Propertiesn/a

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the BARTLE 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 BARTLE 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 BARTLE 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 BARTLE 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 BARTLE 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 BARTLE 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 BARTLE 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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Click the image to view it full size.

There are insufficient data to create the 3D mountains figure.

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Click the image to view it full size.

Soil series sharing subgroup-level classification with BARTLE, 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 BARTLE 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
Bartle silt loam, 0 to 2 percent slopesBbhA308024390585sxin00520021:12000
Bartle-Pekin silt loams, 2 to 6 percent slopesBbiB65824389485skin00520021:12000
Bartle silt loam, 0 to 3 percent slopesBa690535581kz9tin01319851:15840
Bartle silt loam, 0 to 2 percent slopesBbhA4616513721sfd2in01319851:15840
Bartle-Pekin silt loams, 2 to 6 percent slopesBbiB1516513731sfd3in01319851:15840
Bartle silt loam, 0 to 2 percent slopesBbhA19212107477299in01920011:12000
Bartle silt loam, 0 to 2 percent slopesBbhA27616525632zs58in02519701:20000
Bartle silt loamBa108761629285gjrin02719691:20000
Bartle silt loam, 0 to 3 percent slopesBaA20516006331qqlbin02919791:15840
Bartle silt loam, 0 to 2 percent slopesBa12135356172zs58in03719781:15840
Bartle silt loam, 0 to 2 percent slopesBbhA4091851362zs58in04320001:12000
Bartle silt loam, 0 to 2 percent slopesBb7321615202zs58in05519841:15840
Bartle silt loam, 0 to 2 percent slopesBbhA2097806642zs58in06120071:12000
Bartle silt loam, 0 to 2 percent slopesBbhA1143620185ntbzin07119851:15840
Bartle silt loam, 0 to 2 percent slopesBaA1896866011hz3in07719821:15840
Bartle silt loam, 0 to 2 percent slopesBbhA992633177p7w2in07920101:12000
Bartle silt loam, 0 to 2 percent slopes, rarely floodedBbhAQ240616515282zs59in09319821:15840
Bartle silt loam, 0 to 2 percent slopesBbhA38517081122zs58in10119841:15840
Bartle silt loam, 0 to 2 percent slopesBa13405355162zs58in10519791:15840
Bartle silt loamBd5331631935gt9in10919791:15840
Bartle silt loam, 0 to 3 percent slopesBaA25816005251qqgvin11519791:15840
Bartle silt loam, 0 to 2 percent slopesBbhA32314429652zs58in11719801:15840
Bartle silt loamBa2031618895fg7in12519831:15840
Bartle silt loamBa2751598205c9hin13319791:15840
Bartle silt loam, 0 to 2 percent slopesBaA73814796171lnnlin13719821:15840
Bartle silt loam, 0 to 2 percent slopesBbhA9561655875k9jin14319951:12000
Bartle silt loam, 2 to 4 percent slopesBbhB5071655885k9kin14319951:12000
Bartle silt loam, 0 to 2 percent slopes, rarely floodedBa17131600112zs59in14719661:15840
Bartle silt loamBa10051627335gbgin16319721:15840
Bartle silt loamBa10031596505c40in16719711:20000
Bartle silt loamBa25241599435cfgin17319761:15840
Bartle silt loam, 0 to 2 percent slopesBa32995354542zs58in17519841:15840

Map of Series Extent

Approximate geographic distribution of the BARTLE 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 .