Soil Data Explorer - HENNEKE

Official Series Description

Lab Data Summary

Aggregate lab data for the HENNEKE soil series. This aggregation is based on all pedons with a current taxon name of HENNEKE, 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 HENNEKE 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
15	UCD5417010	54-CA-17-010x	HENNEKE	3	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	38.7737999,-122.5855026
15	UCD5611012	56-CA-11-012	HENNEKE	2	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	39.7525139,-122.5831985
15	78P0456	78CA033021	Henneke	6	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	38.7640495,-122.5971832
15	93P0180	92CA099004	Henneke	6	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	37.3105555,-121.3180556

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the HENNEKE 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 HENNEKE 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 HENNEKE 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 HENNEKE 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 HENNEKE 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 HENNEKE 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 HENNEKE 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 HENNEKE, 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-2012-05-08-17 | Alameda Area - March 1966

   The relationship of geologic formations, landforms, and soil series in the Alameda Area (Soil Survey of Alameda Area, California; March, 1966).

Map Units

Map units containing HENNEKE 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
Henneke-Okiota complex, 50 to 75 percent slopes	549	14567	461646	hhct	ca011	1999	1:24000
Henneke-Montara-Rock outcrop complex, 10 to 50 percent slopes, MLRA 15	545	14533	461662	2xcb0	ca011	1999	1:24000
Henneke-Okiota complex, 10 to 50 percent slopes	548	7126	461645	2xcb1	ca011	1999	1:24000
Okiota-Dubakella-Henneke complex, 15 to 50 percent slopes	542	883	461663	hhdc	ca011	1999	1:24000
Henneke stony clay loam, 30 to 65 percent slopes	HcE	11515	458642	hd7x	ca021	1961	1:20000
Henneke stony clay loam, 10 to 30 percent slopes	HcD	730	458641	hd7w	ca021	1961	1:20000
Stonyford-Henneke complex, 30 to 65 percent slopes	SvE	222	458870	hdh8	ca021	1961	1:20000
Henneke very gravelly clay loam, 15 to 50 percent slope s	123	1465	461784	hhj8	ca031	1980	1:24000
Henneke very gravelly clay loam, 5 to 15 percent slopes	122	477	461783	hhj7	ca031	1980	1:24000
Henneke-Montara-Rock outcrop complex, 10 to 50 percent slopes, MLRA 15	142	31046	459545	2xcb0	ca033	1985	1:24000
Henneke-Okiota complex, 10 to 50 percent slopes	143	10073	459546	2xcb1	ca033	1985	1:24000
Okiota-Henneke-Dubakella association, 15 to 50 percent slopes	193	9632	459596	hf7p	ca033	1985	1:24000
Okiota-Henneke complex, 5 to 30 percent slopes	192	5922	459595	hf7n	ca033	1985	1:24000
Henneke-Montara complex, 8 to 15 percent slopes	141	972	459544	hf60	ca033	1985	1:24000
Henneke gravelly loam, 30 to 75 percent slopes	154n	112	1606892	1qy37	ca033	1985	1:24000
Henneke stony clay loam, 15 to 50 percent slopes	129	3065	459421	hf21	ca041	1979	1:24000
Henneke extremely stony clay loam, 15 to 75 percent slopes	HcF	7375	455626	h93m	ca053	1972	1:24000
Henneke gravelly loam, 30 to 75 percent slopes	154	52995	458978	hdlr	ca055	1974	1:24000
Henneke-Montara-Rock outcrop complex, 10 to 50 percent slopes, MLRA 15	142l	2064	813827	2xcb0	ca055	1974	1:24000
Henneke gravelly loam, 4 to 46 percent slopes, MLRA 15	153	1820	458977	2xc9z	ca055	1974	1:24000
Henneke-Okiota complex, 10 to 50 percent slopes	143l	293	813828	2xcb1	ca055	1974	1:24000
Okiota-Henneke complex, 5 to 30 percent slopes	192l	235	813832	w9vn	ca055	1974	1:24000
Okiota-Henneke-Dubakella association, 15 to 50 percent slopes	193l	117	813833	w9vp	ca055	1974	1:24000
Henneke gravelly loam, 30 to 75 percent slopes, eroded	HgG2sn	33	816509	wdn0	ca055	1974	1:24000
Henneke fine gravelly loam, 15 to 50 percent slopes, er oded	HnF2	3025	456209	h9qf	ca069	1965	1:20000
Henneke soils, 15 to 75 percent slopes, severely eroded	HsG3	2083	456210	h9qg	ca069	1965	1:20000
Henneke gravelly loam, 30 to 75 percent slopes, eroded	HgG2	11997	459762	hff1	ca097	1968	1:20000
Henneke gravelly loam, 4 to 46 percent slopes, MLRA 15	HgE	1492	459761	2xc9z	ca097	1968	1:20000
Henneke-Montara-Rock outcrop complex, 10 to 50 percent slopes, MLRA 15	142l	366	695103	2xcb0	ca113	1968	1:20000
Henneke gravelly loam, 30 to 75 percent slopes	154n	303	765508	tpkt	ca113	1968	1:20000
Henneke very rocky loam, 15 to 60 percent slopes	HaF	1343	460002	hfns	ca607	1967	1:20000
Henneke rocky loam, eroded	HnF2	6761	456585	hb3k	ca609	1963	1:20000
Henneke-Rock outcrop complex, 5 to 50 percent slopes	148	770	460312	hfzs	ca620	1975	1:24000
Henneke very rocky loam, 3 to 51 percent slopes	HaD	2064	462357	hj3r	ca628	1963	1:20000
Henneke-Hentine-Rock outcrop complex, 30 to 70 percent slopes	682	6075	467000	hnyj	ca642	1998	1:24000
Hentine-Henneke-Rock outcrop complex, 30 to 70 percent slopes	687	2220	467004	hnyn	ca642	1998	1:24000
Hentine-Rock outcrop-Henneke complex, 30 to 70 percent slopes	683	2135	467001	hnyk	ca642	1998	1:24000
Hentine-Henneke complex, 30 to 70 percent slopes	684	615	467002	hnyl	ca642	1998	1:24000
Henneke stony loam, 30 to 65 percent slopes	HeE	15664	460751	hgfy	ca645	1961	1:20000
Henneke stony loam, landslips, 10 to 30 percent slopes	HfD	728	460752	hgfz	ca645	1961	1:20000
Henneke stony loam, landslips, 30 to 65 percent slopes	HfE	510	460753	hgg0	ca645	1961	1:20000
Henneke stony loam, 10 to 30 percent slopes	HeD	483	460750	hgfx	ca645	1961	1:20000
Hentine-Henneke complex, 30 to 70 percent slopes	684ws	1664	699655	rh1j	ca646	1967	1:24000
Henneke rocky clay loam, 30 to 75 percent slopes, severely eroded	HeG3	1143	457003	hbk1	ca646	1967	1:24000
Hentine-Henneke-Rock outcrop complex, 30 to 70 percent slopes	687ws	22	817079	wf7d	ca646	1967	1:24000
Henneke extremely rocky clay loam, 15 to 75 percent slopes	HaG	6306	463266	hk22	ca649	1967	1:24000
Henneke-Rock outcrop complex, 15 to 75 percent slopes	146	11180	457118	hbnr	ca664	1977	1:24000
Henneke-Rock outcrop complex, 15 to 75 percent slopes	151	7450	457254	hbt4	ca665	1977	1:24000
Henneke-Montara complex, 15 to 50 percent slopes	136	7771	461021	hgqn	ca687	1985	1:24000
Henneke-Montara complex, 50 to 75 percent slopes	137	1948	461022	hgqp	ca687	1985	1:24000
Henneke-Dubakella families complex, 40 to 60 percent slopes.	91	115	470687	hssg	ca707	1983	1:24000
Henneke very rocky loam, 15 to 60 percent slopes	HaFsh	97	1868394	20q6s	ca707	1983	1:24000
Henneke stony loam, 30 to 65 percent slopes	HeEtc	30	1868698	20qjl	ca707	1983	1:24000
Henneke-Montara complex, 15 to 50 percent slopes	136me	85	2747835	hgqn	ca709	2010	1:24000
Diablo-Altamont-Henneke families association, 10 to 60 percent slopes	5	15134	465318	hm68	ca772	1981	1:24000
Cuesta-Henneke families complex, 15 to 60 percent slopes	4	7035	465307	hm5x	ca772	1981	1:24000
Agua Dulce-Henneke-Cuesta families complex, 40 to 70 percent slopes	2	4164	465285	hm56	ca772	1981	1:24000

Map of Series Extent

Approximate geographic distribution of the HENNEKE 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).