Official Series Description


Lab Data Summary

Aggregate lab data for the LONNIEBEE soil series. This aggregation is based on all pedons with a current taxon name of LONNIEBEE, 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 LONNIEBEE 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 LONNIEBEE 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 LONNIEBEE 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 LONNIEBEE 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 LONNIEBEE 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 LONNIEBEE 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 LONNIEBEE 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 LONNIEBEE 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 flats position figure.

Soil series sharing subgroup-level classification with LONNIEBEE, 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 LONNIEBEE 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
Lonniebee-Tamarron family-Graysill family complex, 40 to 70 percent slopes202C6105507535k143co6501:24000
Lonniebee, very stony-Storm-Como, extremely stony families, complex, 15 to 60 percent slopes6280F57831692502v2sjmt60019691:24000
Storm, very stony-Lonniebee, stony-Garlet families, complex, 15 to 60 percent slopes6370F9531692652v2shmt60019691:24000
Lonniebee, bouldery-Wesdy, very stony-Booneville complex, 8 to 35 percent slopes, landslides746E442625125502pphymt61220111:24000
Lonniebee, stony-Kegsprings-Slidemountain, extremely stony complex, 25 to 60 percent slopes747F135825125512pphzmt61220111:24000
Kegsprings, very stony-Lonniebee-Cowood, extremely stony complex, 25 to 50 percent slopes748F117425125522ppj0mt61220111:24000
Lonniebee, stony-Kegsprings-Slidemountain, extremely stony complex, 25 to 60 percent slopes747F526334692pphzmt61420121:24000
Yellowmule-Lonniebee, stony complex, 15 to 45 percent slopes294E317715538256pbmt62219971:24000
Lonniebee-Cowood complex, 15 to 35 percent slopes593E104915561256xrmt62219971:24000
Lonniebee-Cowood complex, 35 to 60 percent slopes593F97715561356xsmt62219971:24000
Yellowmule-Lonniebee complex, 35 to 60 percent slopes, stony294F77815538356pcmt62219971:24000
Lonniebee-Cowood complex, warm, 40 to 70 percent slopes794G528155730571kmt62219971:24000
Yellowmule-Lonniebee, stony-Redlodge complex, 4 to 15 percent slopes294D19315538156p9mt62219971:24000
Storm, very stony-Lonniebee, stony-Garlet families, complex, 15 to 60 percent slopes6370F73030941122v2shmt63019911:24000
Lonniebee, stony-Helmville, extremely stony-Currycreek families, complex, 25 to 60 percent slopes6270F68530941092v2sdmt63019911:24000
Lonniebee, extremely stony-Garlet-Kamack, very stony families, complex, 25 to 60 percent slopes6375F1330941112v2sgmt63019911:24000
Jaegie, very stony-Lonniebee, extremely stony-Jefflake, stony families, complex, 1 to 8 percent slopes1251C1497224841542pcz0mt6321:24000
Lonniebee-Como, very stony-Cowood, extremely stony families, complex, 4 to 15 percent slopes1251D1458424841562pcz2mt6321:24000
Lonnibee, stony-Cowood, very stony-Worock, stony families, complex, 30 to 60 percent slopes1266F1120424852342pf2vmt6321:24000
Lonnibee, stony-Cowood, very stony-Worock, stony families, complex, 15 to 35 percent slopes1266E886324852332pf2tmt6321:24000
Cowood, very rubbly-Lonniebee, very stony-Como, very stony families, complex, 4 to 15 percent slopes1219D875426044352r6xhmt6321:24000
Lonniebee, very stony-Storm-Como, extremely stony families, complex, 15 to 60 percent slopes6280F653728384402v2sjmt6321:24000
Jefflake, very stony-Wetpark-Lonniebee, very stony families, complex, 8 to 35 percent slopes2251E555026044322r6xfmt6321:24000
Lonniebee-Stemple-Cowood, stony complex, 20 to 60 percent slopes403F533525128811sd6hmt6321:24000
Lonniebee, stony-Helmville, extremely stony-Currycreek families, complex, 25 to 60 percent slopes6270F529628384362v2sdmt6321:24000
Storm, very stony-Lonniebee, stony-Garlet families, complex, 15 to 60 percent slopes6370F436628384392v2shmt6321:24000
Storm, rubbly-Cowood, rubbly families-Rock outcrop complex, 35 to 70 percent slopes6340G376129110392w758mt6321:24000
Lonniebee-Redfern-Worock families, complex, 25 to 60 percent slopes1276F236524853622pf6zmt6321:24000
Lonniebee-Worock families, complex, 15 to 35 percent slopes1276E220824853612pf6ymt6321:24000
Lonniebee, extremely stony-Garlet-Kamack, very stony families, complex, 25 to 60 percent slopes6375F171528384382v2sgmt6321:24000
Jefflake-Yellowmule-Lonniebee, very stony families, complex, 0 to 8 percent slopes2252C153226044362r6xlmt6321:24000
Owlcan-Lonniebee, very stony-Wetpark families, complex, 4 to 35 percent slopes, landslides6252E136528384432v2spmt6321:24000
Redfern, stony-Mountedith, very stony-Lonniebee, stony families, complex, 4 to 30 percent slopes1269E48328324412v10smt6321:24000
Risingwolf-Nooney, stony-Lonniebee family, complex, 35 to 60 percent slopes2400F3384042316lgmt6331:24000
Nooney, very stony-Lonniebee family-Rock outcrop complex, 35 to 60 percent slopes2440F3384044316lkmt6331:24000
Lonniebee-Cowood complex, warm, 40 to 70 percent slopes1891051465724xj4mt63619831:24000
Lonniebee-Cowood complex, 35 to 60 percent slopes188911465574xhnmt63619831:24000
Lonniebee-Cowood complex, 15 to 35 percent slopes187751465564xhmmt63619831:24000
Lonniebee-Stemple-Cowood, stony complex, 20 to 60 percent slopes403F676216502381sd6hmt63720141:24000
Lonniebee-Como, very stony-Cowood, extremely stony families, complex, 4 to 15 percent slopes1251D63324965522pcz2mt63720141:24000
Muggins, moderately deep-Lonniebie families, complex, 10 to 50 percent slopes33414437152010535kwy66320121:24000

Map of Series Extent

Approximate geographic distribution of the LONNIEBEE 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 .