Soil Data Explorer - LONNIEBEE

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 (updated 2020-03-18). 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.

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 (updated 2024-10-24), parsed OSD records (updated 2024-10-23) and snapshot of SC database (updated 2024-10-23).

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 (updated 2024-10-23).

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 (updated 2024-10-23).

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 (updated 2024-10-23) and snapshot of the SC database (updated 2024-10-23).

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 (updated 2024-10-23).

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 (updated 2024-10-23).

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 (updated 2024-10-23).

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 slopes	202C	6105	507535	k143	co650		1:24000
Lonniebee, very stony-Storm-Como, extremely stony families, complex, 15 to 60 percent slopes	6280F	578	3169250	2v2sj	mt600	1969	1:24000
Storm, very stony-Lonniebee, stony-Garlet families, complex, 15 to 60 percent slopes	6370F	95	3169265	2v2sh	mt600	1969	1:24000
Lonniebee, bouldery-Wesdy, very stony-Booneville complex, 8 to 35 percent slopes, landslides	746E	4426	2512550	2pphy	mt612	2011	1:24000
Lonniebee, stony-Kegsprings-Slidemountain, extremely stony complex, 25 to 60 percent slopes	747F	1358	2512551	2pphz	mt612	2011	1:24000
Kegsprings, very stony-Lonniebee-Cowood, extremely stony complex, 25 to 50 percent slopes	748F	1174	2512552	2ppj0	mt612	2011	1:24000
Lonniebee, stony-Kegsprings-Slidemountain, extremely stony complex, 25 to 60 percent slopes	747F	5	2633469	2pphz	mt614	2012	1:24000
Yellowmule-Lonniebee, stony complex, 15 to 45 percent slopes	294E	3177	155382	56pb	mt622	1997	1:24000
Lonniebee-Cowood complex, 15 to 35 percent slopes	593E	1049	155612	56xr	mt622	1997	1:24000
Lonniebee-Cowood complex, 35 to 60 percent slopes	593F	977	155613	56xs	mt622	1997	1:24000
Yellowmule-Lonniebee complex, 35 to 60 percent slopes, stony	294F	778	155383	56pc	mt622	1997	1:24000
Lonniebee-Cowood complex, warm, 40 to 70 percent slopes	794G	528	155730	571k	mt622	1997	1:24000
Yellowmule-Lonniebee, stony-Redlodge complex, 4 to 15 percent slopes	294D	193	155381	56p9	mt622	1997	1:24000
Storm, very stony-Lonniebee, stony-Garlet families, complex, 15 to 60 percent slopes	6370F	730	3094112	2v2sh	mt630	1991	1:24000
Lonniebee, stony-Helmville, extremely stony-Currycreek families, complex, 25 to 60 percent slopes	6270F	685	3094109	2v2sd	mt630	1991	1:24000
Lonniebee, extremely stony-Garlet-Kamack, very stony families, complex, 25 to 60 percent slopes	6375F	13	3094111	2v2sg	mt630	1991	1:24000
Jaegie, very stony-Lonniebee, extremely stony-Jefflake, stony families, complex, 1 to 8 percent slopes	1251C	14972	2484154	2pcz0	mt632		1:24000
Lonniebee-Como, very stony-Cowood, extremely stony families, complex, 4 to 15 percent slopes	1251D	14584	2484156	2pcz2	mt632		1:24000
Lonnibee, stony-Cowood, very stony-Worock, stony families, complex, 30 to 60 percent slopes	1266F	11204	2485234	2pf2v	mt632		1:24000
Lonnibee, stony-Cowood, very stony-Worock, stony families, complex, 15 to 35 percent slopes	1266E	8863	2485233	2pf2t	mt632		1:24000
Cowood, very rubbly-Lonniebee, very stony-Como, very stony families, complex, 4 to 15 percent slopes	1219D	8754	2604435	2r6xh	mt632		1:24000
Lonniebee, very stony-Storm-Como, extremely stony families, complex, 15 to 60 percent slopes	6280F	6537	2838440	2v2sj	mt632		1:24000
Jefflake, very stony-Wetpark-Lonniebee, very stony families, complex, 8 to 35 percent slopes	2251E	5550	2604432	2r6xf	mt632		1:24000
Lonniebee-Stemple-Cowood, stony complex, 20 to 60 percent slopes	403F	5335	2512881	1sd6h	mt632		1:24000
Lonniebee, stony-Helmville, extremely stony-Currycreek families, complex, 25 to 60 percent slopes	6270F	5296	2838436	2v2sd	mt632		1:24000
Storm, very stony-Lonniebee, stony-Garlet families, complex, 15 to 60 percent slopes	6370F	4366	2838439	2v2sh	mt632		1:24000
Storm, rubbly-Cowood, rubbly families-Rock outcrop complex, 35 to 70 percent slopes	6340G	3761	2911039	2w758	mt632		1:24000
Lonniebee-Redfern-Worock families, complex, 25 to 60 percent slopes	1276F	2365	2485362	2pf6z	mt632		1:24000
Lonniebee-Worock families, complex, 15 to 35 percent slopes	1276E	2208	2485361	2pf6y	mt632		1:24000
Lonniebee, extremely stony-Garlet-Kamack, very stony families, complex, 25 to 60 percent slopes	6375F	1715	2838438	2v2sg	mt632		1:24000
Jefflake-Yellowmule-Lonniebee, very stony families, complex, 0 to 8 percent slopes	2252C	1532	2604436	2r6xl	mt632		1:24000
Owlcan-Lonniebee, very stony-Wetpark families, complex, 4 to 35 percent slopes, landslides	6252E	1365	2838443	2v2sp	mt632		1:24000
Redfern, stony-Mountedith, very stony-Lonniebee, stony families, complex, 4 to 30 percent slopes	1269E	483	2832441	2v10s	mt632		1:24000
Nooney, very stony-Lonniebee family-Rock outcrop complex, 35 to 60 percent slopes	2440F	212852	3384044	316lk	mt633		1:24000
Risingwolf-Nooney, stony-Lonniebee family complex, 35 to 60 percent slopes	2400F	194451	3384042	316lg	mt633		1:24000
Worock-Mikesell-Lonniebee families, complex, 35 to 60 percent slopes	2366F	29188	3384064	316mb	mt633		1:24000
Worock-Lonniebee-Mikesell families, complex, 35 to 60 percent slopes	2466F	5461	3384066	316md	mt633		1:24000
Lonniebee-Cowood complex, warm, 40 to 70 percent slopes	189	105	146572	4xj4	mt636	1983	1:24000
Lonniebee-Cowood complex, 35 to 60 percent slopes	188	91	146557	4xhn	mt636	1983	1:24000
Lonniebee-Cowood complex, 15 to 35 percent slopes	187	75	146556	4xhm	mt636	1983	1:24000
Lonniebee-Stemple-Cowood, stony complex, 20 to 60 percent slopes	403F	6762	1650238	1sd6h	mt637	2014	1:24000
Lonniebee-Como, very stony-Cowood, extremely stony families, complex, 4 to 15 percent slopes	1251D	633	2496552	2pcz2	mt637	2014	1:24000
Muggins, moderately deep-Lonniebie families, complex, 10 to 50 percent slopes	334	14437	152010	535k	wy663	2012	1:24000

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 (updated 2024-10-30).