Official Series Description


Lab Data Summary

Aggregate lab data for the HALEBURU soil series. This aggregation is based on all pedons with a current taxon name of HALEBURU, 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 HALEBURU were used in the calculation. Source: KSSL snapshot . 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 HALEBURU 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 HALEBURU 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 HALEBURU 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 HALEBURU 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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Competing Series

Soil series competing with HALEBURU 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 HALEBURU series and competing. Series are sorted according to hierarchical clustering of median values. Source: SSURGO map unit geometry and 1981-2010, 800m PRISM data .

Click the image to view it full size.

Geomorphic description summaries for the HALEBURU 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 .

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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 HALEBURU, 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

No block diagrams are available.

Map Units

Map units containing HALEBURU 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
Haleburu-Noble Pass complex, 15 to 50 percent slopes3401211514034531j3dpca6981:24000
Haleburu-Rock outcrop association, 8 to 50 percent slopes341166914034881j3ftca6981:24000
Haleburu association, 2 to 30 percent slopes341017614034871j3fsca6981:24000
Haleburu-Noble Pass complex, 15 to 50 percent slopes406304973229694hns9ca6991:24000
Sunrock-Haleburu-Lava flows association, 15 to 75 percent slopes141127573229661hnr7ca6991:24000
Haleburu-Upspring complex, 8 to 50 percent slopes40389933229634hnqcca6991:24000
Haleburu association, 8 to 30 percent slopes, extremely stony40058173229678hnrsca6991:24000
Haleburu-Arizo association, 2 to 15 percent slopes40144023229612hnpnca6991:24000
Sunrock-Haleburu association, 8 to 30 percent slopes, very stony14336933229663hnr9ca6991:24000
Cajon-Gravesumit-Haleburu complex, 2 to 50 percent slopes36021003229690hns5ca6991:24000
Haleburu-Rubble land complex, 30 to 75 percent slopes4171467027836432ss1sca79520231:24000
Haleburu-Winkel complex, 2 to 8 percent slopes3901219633908532zlpfca79520231:24000
Haleburu association3412378186074620g82ca8051:24000
Goldroad-Haleburu-Rock outcrop associationGHF931917124541vgygnv60819671:24000
Sunrock-Haleburu-Rock outcrop association54165082468906hqy0nv75520061:24000
Nipton-Haleburu-Rock outcrop association14124580468819hqv6nv75520061:24000
Haleburu-Crosgrain-Rock outcrop association75024328468950hqzfnv75520061:24000
Haleburu-Hiddensun association75414976468954hqzknv75520061:24000
Haleburu-Nipton association, dry14710199468825hqvdnv75520061:24000
Haleburu-Seanna association1489894468826hqvfnv75520061:24000
Nipton-Hiddensun-Haleburu association7539614468953hqzjnv75520061:24000
Haleburu association34127032339409120g82nv75520061:24000
Haleburu extremely gravelly sandy loam, 4 to 15 percent slopes1405729468818hqv5nv75520061:24000
Goldroad-Haleburu-Rock outcrop association6135187603166n7mznv75520061:24000
Haleburu-Nipton association1465077468824hqvcnv75520061:24000
Haleburu, extremely cobbly-Hiddensun association1444568468822hqv9nv75520061:24000
Tecopa-Haleburu-Rock outcrop complex, 2 to 50 percent slopes23015606469137hr5gnv78519951:24000
Sunrock-Haleburu-Rock outcrop association541681716810041tf6ynv78819821:24000
Nipton-Hiddensun-Haleburu association753323716810131tf77nv78819821:24000
Nipton-Haleburu-Rock outcrop association141256816809701tf5vnv78819821:24000
Haleburu-Crosgrain-Rock outcrop association4501030469317hrc8nv78819821:24000

Map of Series Extent

Approximate geographic distribution of the HALEBURU 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 .