Soil Data Explorer - DUBAKELLA

Official Series Description

Lab Data Summary

Aggregate lab data for the DUBAKELLA soil series. This aggregation is based on all pedons with a current taxon name of DUBAKELLA, 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 DUBAKELLA 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
22A	UCD6758125	67-CA-58-125x	DUBAKELLA	2	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	39.4962425,-121.2014008
22A	UCD6858127	68-CA-58-127x	DUBAKELLA	3	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	39.5109596,-121.1919937
22A	68C0115	S1968CA057036	DUBAKELLA	6	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	39.2661095,-121.0588913
5	UCD5852015	58-CA-52-015	DUBAKELLA	2	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	40.2489243,-122.8924713
5	UCD6012008	60-CA-12-008x	DUBAKELLA	2	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	41.0224686,-123.7329865
5	74C0064	S1974CA093014	DUBAKELLA	6	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	41.6911125,-122.7127762

Water Balance

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

There are insufficient data to create the annual climate figure.

Geomorphic description summaries for the DUBAKELLA 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 2D hillslope position figure.

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

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

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 DUBAKELLA, 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 DUBAKELLA 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
Okiota-Dubakella-Henneke complex, 15 to 50 percent slopes	542	883	461663	hhdc	ca011	1999	1:24000
Dubakella stony loam, 30 to 50 percent slopes	DuE	68	458632	hd7l	ca021	1961	1:20000
Okiota-Henneke-Dubakella association, 15 to 50 percent slopes	193	9632	459596	hf7p	ca033	1985	1:24000
Okiota-Henneke-Dubakella association, 15 to 50 percent slopes	193l	117	813833	w9vp	ca055	1974	1:24000
Dubakella-Ipish complex, 30 to 50 percent slopes	144	8350	459053	hdp5	ca602	1978	1:24000
Rock outcrop-Dubakella complex, 30 to 50 percent slopes	213	3050	459122	hdrd	ca602	1978	1:24000
Dubakella-Ipish complex, 5 to 30 percent slopes	143	2980	459052	hdp4	ca602	1978	1:24000
DUBAKELLA COBBLY CLAY LOAM, 30 TO 50 PERCENT SLOPES	139	1093	466039	hmyj	ca606	1990	1:24000
WEITCHPEC-DUBAKELLA COMPLEX, 30 TO 50 PERCENT SLOPES	210	627	466112	hn0w	ca606	1990	1:24000
DUBAKELLA COBBLY CLAY LOAM, 50 TO 75 PERCENT SLOPES	140	515	466040	hmyk	ca606	1990	1:24000
DUBAKELLA STONY LOAM, 30 TO 50 PERCENT SLOPES	141	490	466042	hmym	ca606	1990	1:24000
DUBAKELLA COBBLY CLAY LOAM, 15 TO 30 PERCENT SLOPES	138	213	466038	hmyh	ca606	1990	1:24000
Rock outcrop-Dubakella complex, 5 to 50 percent slopes	RrE	1992	460241	hfxh	ca619	1970	1:24000
Dubakella, shallow variant-Rock outcrop complex, 2 to 50 percent slopes	DrE	1374	460209	hfwg	ca619	1970	1:24000
Dubakella very stony loam, 9 to 50 percent slopes	143	1950	460307	hfzm	ca620	1975	1:24000
Dubakella stony loam, 30 to 50 percent slopes	DyE	4023	460738	hgfj	ca645	1961	1:20000
Neuns-Dubakella complex, 30 to 50 percent slopes	NpE	551	460879	hgl2	ca645	1961	1:20000
Dubakella stony loam, 10 to 30 percent slopes	DyD	286	460737	hgfh	ca645	1961	1:20000
Dubakella family, 30 to 70 percent slopes.	122	10422	470343	hsfc	ca702	1984	1:24000
Lithic Mollic Haploxeralfs-Dubakella family association, 15 to 70 percent slopes.	155	8418	470376	hsgf	ca702	1984	1:24000
Dubakella-Ipish complex, 5 to 30 percent slopes	143sc	541	1905893	21z7f	ca702	1984	1:24000
Dubakella-Ipish complex, 30 to 50 percent slopes	144sc	308	1905895	21z7h	ca702	1984	1:24000
Rock outcrop-Dubakella-Weitchpec familes complex, 40 to 60 percent slopes.	256st	147	1906090	21zfs	ca702	1984	1:24000
Rock outcrop-Dubakella complex, 30 to 50 percent slopes	213sc	50	1905960	21z9l	ca702	1984	1:24000
Dubakella-Weitchpec families complex, 20 to 40 percent slopes.	47	6818	470645	hsr3	ca707	1983	1:24000
Rock outcrop-Dubakella-Weitchpec familes complex, 40 to 60 percent slopes.	256	5754	470854	hsyv	ca707	1983	1:24000
Ishi Pishi, deep-Dubakella families complex, 20 to 40 percent slopes.	152	3210	470750	hsvh	ca707	1983	1:24000
Dubakella family, 40 to 60 percent slopes.	44	3050	470642	hsr0	ca707	1983	1:24000
Dubakella-Weitchpec families complex, 40 to 60 percent slopes.	48	2937	470646	hsr4	ca707	1983	1:24000
Dubakella family-Rock outcrop complex, 20 to 40 percent slopes.	46	2548	470644	hsr2	ca707	1983	1:24000
Dunsmuir-Dubakella-Weitchpec families complex, 40 to 60 percent slopes.	52	2201	470650	hsr8	ca707	1983	1:24000
Beaughton-Dubakella families complex, 20 to 40 percent slopes.	13	2155	470611	hsq0	ca707	1983	1:24000
Dubakella-Beaughton families complex, 30 to 70 percent slopes.	45	2140	470643	hsr1	ca707	1983	1:24000
Weitchpec-Dubakella families complex, 20 to 40 percent slopes.	344	1806	470942	ht1p	ca707	1983	1:24000
Dubakella family, 20 to 40 percent slopes.	43	1418	470641	hsqz	ca707	1983	1:24000
Dubakella-Ipish complex, 30 to 50 percent slopes	144sc	1115	1867662	20pg5	ca707	1983	1:24000
Dubakella stony loam, 30 to 50 percent slopes	DyEtc	736	1868283	20q36	ca707	1983	1:24000
Rock outcrop-Dubakella complex, 30 to 50 percent slopes	213sc	628	1867690	20ph2	ca707	1983	1:24000
Dubakella cobbly clay loam, 30 to 50 percent slopes	139tw	362	1868760	20qll	ca707	1983	1:24000
Dubakella--Weitchpec families complex, 60 to 80 percent slopes.	49	337	470647	hsr5	ca707	1983	1:24000
Henneke-Dubakella families complex, 40 to 60 percent slopes.	91	115	470687	hssg	ca707	1983	1:24000
Dubakella-Ipish complex, 5 to 30 percent slopes	143sc	67	1867661	20pg4	ca707	1983	1:24000
Dubakella cobbly clay loam, 15 to 30 percent slopes	138tw	65	1868758	20qlj	ca707	1983	1:24000
Dubakella stony loam, 10 to 30 percent slopes	DyDtc	38	1868281	20q34	ca707	1983	1:24000
Dubakella very gravelly loam, 10 to 30 percent slopes	132	870	2747797	2q1yn	ca709	2010	1:24000
Rock outcrop-Dubakella family complex, 70 to 100 percent slopes.	240	12428	471249	htcl	ca713	1984	1:24000
Dubakella family, 30 to 50 percent slopes.	145	4556	471154	ht8j	ca713	1984	1:24000
Dubakella family, 2 to 30 percent slopes.	144	4157	471153	ht8h	ca713	1984	1:24000
Dubakella family, 50 to 70 percent slopes.	146	2496	471155	ht8k	ca713	1984	1:24000
Dubakella family, 20 to 70 percent slopes, slumped.	147	542	471156	ht8l	ca713	1984	1:24000
Dubakella-Rock outcrop complex, 20 to 80 percent slopes.	148	532	471157	ht8m	ca713	1984	1:24000
Rock outcrop-Dubakella-Dubakella variant complex, 40 to 75 perce nt slopes	RDG	6672	464784	hln1	ca719	1982	1:24000
Dubakella-Dubakella variant-Rock outcrop complex, 30 to 50 percent slopes	DUF	2744	464642	hlhg	ca719	1982	1:24000
Forbes-Dubakella complex, 2 to 30 percent slopes	ISE	1366	464698	hlk8	ca719	1982	1:24000
Forbes-Dubakella complex, 30 to 50 percent slopes	ISF	1361	464700	hlkb	ca719	1982	1:24000
Dubakella-Dubakella variant-Rock outcrop complex, 2 to 30 percent slopes	DUE	1050	464641	hlhf	ca719	1982	1:24000
Rock outcrop-Dubakella-Dubakella variant complex, 2 to 40 percen t slopes	RDE	856	464783	hln0	ca719	1982	1:24000
Forbes-Dubakella complex, 2 to 30 percent slopes, altered	ISE5	613	464699	hlk9	ca719	1982	1:24000
Dubakella very stony loam, 9 to 50 percent slopes	143pc	60	1585910	1q78d	ca719	1982	1:24000
Dubakella-Cornutt-Pearsoll complex, 20 to 60 percent south slopes	94F	943	65577	267d	or015	1995	1:24000
Cornutt-Dubakella complex, 35 to 55 percent south slopes	21F	28020	469447	hrhg	or033	1979	1:20000
Dubakella-Pearsoll complex, 35 to 70 percent south slopes	29F	20541	469456	hrhr	or033	1979	1:20000
Dubakella-Pearsoll complex, 35 to 75 percent north slopes	28F	16876	469455	hrhq	or033	1979	1:20000
Cornutt-Dubakella complex, 35 to 55 percent north slopes	20F	12569	469446	hrhf	or033	1979	1:20000
Eightlar-Dubakella complex, 35 to 65 percent north slopes	32F	6688	469461	hrhx	or033	1979	1:20000
Eightlar-Dubakella complex, 35 to 65 percent south slopes	33F	6147	469462	hrhy	or033	1979	1:20000
Cornutt-Dubakella complex, 20 to 35 percent slopes	19E	4024	469442	hrh9	or033	1979	1:20000
Cornutt-Dubakella complex, 7 to 20 percent slopes	19D	1122	469441	hrh8	or033	1979	1:20000
Dubakella very stony clay loam, rocky, 35 to 70 percent slopes	50G	727	469744	hrt1	or632	1989	1:20000
Dubakella very stony clay loam, rocky, 12 to 35 percent slopes	50E	667	469743	hrt0	or632	1989	1:20000
Pearsoll-Dubakella complex, rocky, 20 to 60 percent slopes	140G	442	469610	hrnq	or632	1989	1:20000
Pearsoll-Dubakella complex, 30 to 70 percent south slopes	186F	10383	66505	276b	or649	1994	1:24000
Dubakella-Pearsoll complex, 30 to 70 percent north slopes	68F	3246	67033	27rc	or649	1994	1:24000
Dubakella-Pearsoll complex, 5 to 30 percent slopes	67E	2465	67022	27r0	or649	1994	1:24000
Dubakella very stony clay loam, 30 to 60 percent north slopes	65F	431	67019	27qx	or649	1994	1:24000
Dubakella very stony clay loam, 30 to 60 percent south slopes	66F	360	67021	27qz	or649	1994	1:24000

Map of Series Extent

Approximate geographic distribution of the DUBAKELLA 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).