Soil Data Explorer - BOTELLA

Official Series Description

Lab Data Summary

Aggregate lab data for the BOTELLA soil series. This aggregation is based on all pedons with a current taxon name of BOTELLA, 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 BOTELLA were used in the calculation. Source: KSSL snapshot (updated 2020-03-13). Methods used to assemble the KSSL snapshot used by SoilWeb / SDE

Pedons used in the lab summary:

MLRA	Lab ID	Pedon ID	Taxonname	CI	NSSL / NASIS Reports	Link To SoilWeb GMap
14	07N0673	05ca085641238	Botella	6	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	37.3551611,-122.0247139
15	80P0063	76CA083002	Botella	7	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	34.6480446,-120.2351227
17	40A3363	S1977CA101016	Botella	2	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	39.0833321,-121.6708298
17	40A3364	S1977CA101025	botella	2	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	39.0258331,-121.651947

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the BOTELLA 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 BOTELLA 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 BOTELLA 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 BOTELLA 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).

Competing Series

Soil series competing with BOTELLA 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 BOTELLA 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 BOTELLA 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).

Soil series sharing subgroup-level classification with BOTELLA, 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

Click a link below to display the diagram. Note that these diagrams may be from multiple survey areas.

1. CA-2011-05-27-10 | San Mateo County, Eastern Part, and San Francisco County - 1991

   Idealized cross section of soils near Redwood City, in the southeastern part of San Mateo County (Soil Survey of San Mateo County, Eastern Part, and San Francisco County, California; 1991).

Map Units

Map units containing BOTELLA 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
Botella clay loam, 0 to 2 percent slopes, MLRA 14	BaA	3555	455765	2tyz5	ca013	1973	1:24000
Botella clay loam, 2 to 9 percent slopes, MLRA 14	BaC	1645	455766	2tyz7	ca013	1973	1:24000
Botella loam, 0 to 2 percent slopes, MLRA 14	BoA	433	456163	2tyz6	ca069	1965	1:20000
Botella loam, 2 to 9 percent slopes, MLRA 14	BoC	422	456164	2tyz9	ca069	1965	1:20000
Botella loam, 0 to 2 percent slopes, MLRA 14	106	4980	456659	2tyz6	ca610	1975	1:24000
Botella loam, sloping, eroded	BeC2	262	456328	h9v8	ca637	1958	1:15000
Botella clay loam, nearly level, cool	BcA	220	456322	2yrfn	ca637	1958	1:15000
Botella loam, 2 to 9 percent slopes, MLRA 14	BeB	193	456327	2tyz9	ca637	1958	1:15000
Botella loam, sloping, seeped	BoC	157	456330	h9vb	ca637	1958	1:15000
Botella loam, gently sloping, imperfectly drained	BdB	114	456326	h9v6	ca637	1958	1:15000
Botella clay loam, sloping, eroded	BcC2	102	456324	h9v4	ca637	1958	1:15000
Botella clay loam, 2 to 9 percent slopes, MLRA 14	BcB	81	456323	2tyz7	ca637	1958	1:15000
Botella loam, nearly level and gently sloping, poorly d rained variant	BfB	68	456329	h9v9	ca637	1958	1:15000
Botella loam, nearly level, imperfectly drained	BdA	52	456325	h9v5	ca637	1958	1:15000
Botella clay loam, 9 to 15 percent slopes	133	4	1404972	1j4zp	ca638	1967	1:24000
Urbanland-Botella complex, 0 to 2 percent slopes	175	3660	1653016	1sh33	ca641	2009	1:24000
Urban land-Botella complex, 2 to 9 percent slopes	176	1372	2027471	261r9	ca641	2009	1:24000
Urban land-Botella complex, 9 to 15 percent slopes	177	886	2390849	2l7w5	ca641	2009	1:24000
Botella sandy loam, 2 to 9 percent slopes, MLRA 14	116	840	457219	2tyz4	ca665	1977	1:24000
Botella loam, 2 to 9 percent slopes, shorter FFD, MLRA 14	450	450	458535	2tz0g	ca667	2003	1:24000
Botella sandy loam, 2 to 9 percent slopes, MLRA 14	470	400	458536	2tyz4	ca667	2003	1:24000
Botella loam, 2 to 15 percent slopes, eroded	BoD2	3553	457346	hbx3	ca672	1966	1:20000
Botella clay loam, 2 to 15 percent slopes, eroded	BtD2	3529	457351	hbx8	ca672	1966	1:20000
Botella clay loam, 2 to 9 percent slopes, MLRA 14	BtC	2271	457350	2tyz7	ca672	1966	1:20000
Botella loam, 2 to 9 percent slopes, MLRA 14	BoC	1977	457345	2tyz9	ca672	1966	1:20000
Botella loam, 0 to 2 percent slopes, MLRA 14	BoA	1535	457343	2tyz6	ca672	1966	1:20000
Botella clay loam, 0 to 2 percent slopes, MLRA 14	BtA	1412	457348	2tyz5	ca672	1966	1:20000
Botella clay loam, 0 to 2 percent slopes, eroded	BtA2	1394	457349	hbx6	ca672	1966	1:20000
Botella loam, 0 to 2 percent slopes, eroded	BoA2	680	457344	hbx1	ca672	1966	1:20000
Botella loam, slightly wet, 0 to 2 percent slopes	BsA	305	457347	hbx4	ca672	1966	1:20000
Botella clay loam, wet, 0 to 2 percent slopes	BwA	273	457352	hbx9	ca672	1966	1:20000
Botella silty clay loam, 2 to 9 percent slopes	BgC	1582	3356340	2zwsw	ca673	1974	1:24000
Botella variant clay loam, 2 to 9 percent slopes, eroded	BkC2	558	457570	hc4b	ca673	1974	1:24000
Botella shaly clay loam, 2 to 9 percent slopes	BhC	306	457569	hc49	ca673	1974	1:24000
Botella variant clay loam, 9 to 15 percent slopes, eroded	BkD2	222	457571	hc4c	ca673	1974	1:24000
Botella silty clay loam, 0 to 2 percent slopes	BgA	129	457567	hc47	ca673	1974	1:24000
Botella clay loam, 2 to 9 percent slopes, warm MAAT, MLRA 19	132	1675	458033	2tyz8	ca678	1974	1:24000
Botella clay loam, 9 to 15 percent slopes	133	1510	458034	hcm9	ca678	1974	1:24000
Botella loam, 2 to 9 percent slopes, warm MAAT, lower MAP, MLRA 19	131	1405	458032	2tyzb	ca678	1974	1:24000
Botella-Urban land complex, 0 to 5 percent slopes	108	6043	455969	h9gp	ca689	1985	1:24000
Botella loam, 0 to 5 percent slopes	107	502	455968	h9gn	ca689	1985	1:24000
Botella loam, 2 to 9 percent slopes, warm MAAT, higher MAP , MLRA 19	320	1435	469935	2tz0h	ca692	2001	1:24000
Lodo-Botella families-Rock outcrop association, 30 to 60 percent slopes	15	40086	465280	hm51	ca772	1981	1:24000
Lodo-Modjeska-Botella families association, 10 to 70 percent slopes	18	27696	465283	hm54	ca772	1981	1:24000
Agua Dulce-Botella-Argonaut families association 20 to 60 percent slopes	1	11799	465274	hm4v	ca772	1981	1:24000
Botella sandy loam, 2 to 9 percent slopes, MLRA 14	470cp	6	1412866	2tyz4	ca772	1981	1:24000
Lodo-Modjeska-Botella families association, 10 to 70 percent slopes	18	159	991370	128lp	ca776	1981	1:24000

Map of Series Extent

Approximate geographic distribution of the BOTELLA 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).