Official Series Description


Lab Data Summary

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

Click the image to view it full size.

Pedons used in the lab summary:

MLRALab IDPedon IDTaxonnameCINSSL / NASIS ReportsLink To SoilWeb GMap
3085P062584CA029020Helendale5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties35.637207,-117.8036804

Water Balance

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

Click the image to view it full size.



Click the image to view it full size.

Sibling Summary

Siblings are those soil series that occur together in map units, in this case with the HELENDALE series. Sketches are arranged according to their subgroup-level taxonomic structure. Source: SSURGO snapshot , parsed OSD records and snapshot of SC database .

Click the image to view it full size.

Select annual climate data summaries for the HELENDALE series and siblings. 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 HELENDALE 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 .

Click the image to view it full size.

Click the image to view it full size.

Click the image to view it full size.

Click the image to view it full size.

Click the image to view it full size.

Competing Series

Soil series competing with HELENDALE share the same family level classification in Soil Taxonomy. Source: parsed OSD records and snapshot of the SC database .

Click the image to view it full size.

Select annual climate data summaries for the HELENDALE 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 HELENDALE 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 .

Click the image to view it full size.

Click the image to view it full size.

Click the image to view it full size.

Click the image to view it full size.

Click the image to view it full size.

Soil series sharing subgroup-level classification with HELENDALE, 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 HELENDALE 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
Helendale loamy sand, 2 to 5 percent slopes11513815461687hhf4ca66919971:24000
Helendale-Cajon complex, 2 to 9 percent slopes1187980461691hhf8ca66919971:24000
Helendale-Sparkhule complex, 2 to 15 percent slopes1197700461692hhf9ca66919971:24000
Helendale loamy sand, 0 to 2 percent slopes1146065461686hhf3ca66919971:24000
Norob-Helendale complex, 2 to 5 percent slopes1383740461725hhgcca66919971:24000
Helendale-Cajon complex, 2 to 5 percent slopes1171765461689hhf6ca66919971:24000
Helendale-Randsburg complex, 0 to 5 percent slopes1201015461693hhfbca66919971:24000
Helendale fine sandy loam, 0 to 1 percent slopes116840461688hhf5ca66919971:24000
HELENDALE-BRYMAN LOAMY SANDS, 2 TO 5 PERCENT SLOPES*13343500463952hks6ca67119781:24000
HELENDALE LOAMY SAND, 2 TO 5 PERCENT SLOPES13216600463951hks5ca67119781:24000
HELENDALE LOAMY SAND, 0 TO 2 PERCENT SLOPES1319200463950hks4ca67119781:24000
Langwell-Rock outcrop-Helendale complex, 4 to 30 percent slopes3242124325052092pz5jca79420121:24000
Helendale-Desertqueen association, 4 to 15 percent slopes4071112725051952pz51ca79420121:24000
Gravesumit-Helendale complex, 1 to 4 percent slopes406484225052002pz57ca79420121:24000
Silvermine-Helendale-Burntshack association, 1 to 15 percent slopes404142025174152qb1gca79420121:24000
Helendale-Caruthers-Castaneda complex, 1 to 4 percent slopes4146607333908362s10jca79520231:24000
Helendale-Cajon complex, 0 to 5 percent slopes2072960488112jcxkca80219961:24000
Centennial-Helendale complex, 2 to 9 percent slopes1622808488055jcvqca80219961:24000
Helendale-Cajon complex, dry, 0 to 5 percent slopes208954488113jcxlca80219961:24000

Map of Series Extent

Approximate geographic distribution of the HELENDALE 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 .