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 . Methods used to assemble the KSSL snapshot used by SoilWeb / SDE

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Pedons used in the lab summary:

MLRALab IDPedon IDTaxonnameCINSSL / NASIS ReportsLink To SoilWeb GMap
15UCD541701054-CA-17-010xHENNEKE3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.7737999,-122.5855026
15UCD561101256-CA-11-012HENNEKE2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties39.7525139,-122.5831985
1578P045678CA033021Henneke6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.7640495,-122.5971832
1593P018092CA099004Henneke6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties37.3105555,-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.

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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 , parsed OSD records and snapshot of SC database .

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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 .

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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 .

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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 and snapshot of the SC database .

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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 .

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 .

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 .

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 slopes54914567461646hhctca01119991:24000
Henneke-Montara-Rock outcrop complex, 10 to 50 percent slopes, MLRA 15545145334616622xcb0ca01119991:24000
Henneke-Okiota complex, 10 to 50 percent slopes54871264616452xcb1ca01119991:24000
Okiota-Dubakella-Henneke complex, 15 to 50 percent slopes542883461663hhdcca01119991:24000
Henneke stony clay loam, 30 to 65 percent slopesHcE11515458642hd7xca02119611:20000
Henneke stony clay loam, 10 to 30 percent slopesHcD730458641hd7wca02119611:20000
Stonyford-Henneke complex, 30 to 65 percent slopesSvE222458870hdh8ca02119611:20000
Henneke very gravelly clay loam, 15 to 50 percent slope s1231465461784hhj8ca03119801:24000
Henneke very gravelly clay loam, 5 to 15 percent slopes122477461783hhj7ca03119801:24000
Henneke-Montara-Rock outcrop complex, 10 to 50 percent slopes, MLRA 15142310464595452xcb0ca03319851:24000
Henneke-Okiota complex, 10 to 50 percent slopes143100734595462xcb1ca03319851:24000
Okiota-Henneke-Dubakella association, 15 to 50 percent slopes1939632459596hf7pca03319851:24000
Okiota-Henneke complex, 5 to 30 percent slopes1925922459595hf7nca03319851:24000
Henneke-Montara complex, 8 to 15 percent slopes141972459544hf60ca03319851:24000
Henneke gravelly loam, 30 to 75 percent slopes154n11216068921qy37ca03319851:24000
Henneke stony clay loam, 15 to 50 percent slopes1293065459421hf21ca04119791:24000
Henneke extremely stony clay loam, 15 to 75 percent slopesHcF7375455626h93mca05319721:24000
Henneke gravelly loam, 30 to 75 percent slopes15452995458978hdlrca05519741:24000
Henneke-Montara-Rock outcrop complex, 10 to 50 percent slopes, MLRA 15142l20648138272xcb0ca05519741:24000
Henneke gravelly loam, 4 to 46 percent slopes, MLRA 1515318204589772xc9zca05519741:24000
Henneke-Okiota complex, 10 to 50 percent slopes143l2938138282xcb1ca05519741:24000
Okiota-Henneke complex, 5 to 30 percent slopes192l235813832w9vnca05519741:24000
Okiota-Henneke-Dubakella association, 15 to 50 percent slopes193l117813833w9vpca05519741:24000
Henneke gravelly loam, 30 to 75 percent slopes, erodedHgG2sn33816509wdn0ca05519741:24000
Henneke fine gravelly loam, 15 to 50 percent slopes, er odedHnF23025456209h9qfca06919651:20000
Henneke soils, 15 to 75 percent slopes, severely erodedHsG32083456210h9qgca06919651:20000
Henneke gravelly loam, 30 to 75 percent slopes, erodedHgG211997459762hff1ca09719681:20000
Henneke gravelly loam, 4 to 46 percent slopes, MLRA 15HgE14924597612xc9zca09719681:20000
Henneke-Montara-Rock outcrop complex, 10 to 50 percent slopes, MLRA 15142l3666951032xcb0ca11319681:20000
Henneke gravelly loam, 30 to 75 percent slopes154n303765508tpktca11319681:20000
Henneke very rocky loam, 15 to 60 percent slopesHaF1343460002hfnsca60719671:20000
Henneke rocky loam, erodedHnF26761456585hb3kca60919631:20000
Henneke-Rock outcrop complex, 5 to 50 percent slopes148770460312hfzsca62019751:24000
Henneke very rocky loam, 3 to 51 percent slopesHaD2064462357hj3rca62819631:20000
Henneke-Hentine-Rock outcrop complex, 30 to 70 percent slopes6826075467000hnyjca64219981:24000
Hentine-Henneke-Rock outcrop complex, 30 to 70 percent slopes6872220467004hnynca64219981:24000
Hentine-Rock outcrop-Henneke complex, 30 to 70 percent slopes6832135467001hnykca64219981:24000
Hentine-Henneke complex, 30 to 70 percent slopes684615467002hnylca64219981:24000
Henneke stony loam, 30 to 65 percent slopesHeE15664460751hgfyca64519611:20000
Henneke stony loam, landslips, 10 to 30 percent slopesHfD728460752hgfzca64519611:20000
Henneke stony loam, landslips, 30 to 65 percent slopesHfE510460753hgg0ca64519611:20000
Henneke stony loam, 10 to 30 percent slopesHeD483460750hgfxca64519611:20000
Hentine-Henneke complex, 30 to 70 percent slopes684ws1664699655rh1jca64619671:24000
Henneke rocky clay loam, 30 to 75 percent slopes, severely erodedHeG31143457003hbk1ca64619671:24000
Hentine-Henneke-Rock outcrop complex, 30 to 70 percent slopes687ws22817079wf7dca64619671:24000
Henneke extremely rocky clay loam, 15 to 75 percent slopesHaG6306463266hk22ca64919671:24000
Henneke-Rock outcrop complex, 15 to 75 percent slopes14611180457118hbnrca66419771:24000
Henneke-Rock outcrop complex, 15 to 75 percent slopes1517450457254hbt4ca66519771:24000
Henneke-Montara complex, 15 to 50 percent slopes1367771461021hgqnca68719851:24000
Henneke-Montara complex, 50 to 75 percent slopes1371948461022hgqpca68719851:24000
Henneke-Dubakella families complex, 40 to 60 percent slopes.91115470687hssgca70719831:24000
Henneke very rocky loam, 15 to 60 percent slopesHaFsh97186839420q6sca70719831:24000
Henneke stony loam, 30 to 65 percent slopesHeEtc30186869820qjlca70719831:24000
Henneke-Montara complex, 15 to 50 percent slopes136me852747835hgqnca70920101:24000
Diablo-Altamont-Henneke families association, 10 to 60 percent slopes515134465318hm68ca77219811:24000
Cuesta-Henneke families complex, 15 to 60 percent slopes47035465307hm5xca77219811:24000
Agua Dulce-Henneke-Cuesta families complex, 40 to 70 percent slopes24164465285hm56ca77219811:24000

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 .