Official Series Description


Lab Data Summary

Aggregate lab data for the HONDU soil series. This aggregation is based on all pedons with a current taxon name of HONDU, 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 HONDU 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
1093P0356S1992OR063007Hondu6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties44.3702774,-118.2300034
43C97P0548S1997OR059002HONDU6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties45.0097237,-118.5774994

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the HONDU 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 HONDU 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 HONDU 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 HONDU 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 terrace figure.

There are insufficient data to create the 3D flats position figure.

Competing Series

Soil series competing with HONDU 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 HONDU 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 HONDU 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 HONDU, 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 HONDU 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
Hondu-Analulu complex, 15 to 30 percent slopes1307BO5625938661qyyyor60419881:24000
Analulu-McWillar-Hondu complex, 30 to 60 percent slopes7763CO284431203212pgthor60720181:24000
McWillar-Analulu-Hondu complex, 30 to 60 percent slopes7766CO266631202611q6zvor60720181:24000
Analulu-Vogel-Hondu complex, sandstone substratum, 30 to 60 percent slopes2003CO67031204161r00cor60720181:24000
Vogel-Analulu-Hondu complex, 60 to 90 percent slopes7764DO21131206501sgfxor60720181:24000
Hondu-Analulu complex, 15 to 30 percent slopes1307BO10031203791qyyyor60720181:24000
Hondu-Payraise complex, 30 to 60 percent north slopes7719CN6031206331sgdgor60720181:24000
Hondu-Analulu complex, 30 to 60 percent slopes7750CO1231206431sgfdor60720181:24000
Porch-Hondu-Wintercanyon complex, 25 to 60 percent slopes7819CO2259733854642xj8qor62620181:24000
Hondu-Porch-Wintercanyon complex, 30 to 60 percent slopes7820CO1551933854682xj8tor62620181:24000
Porch-Hondu-Wintercanyon complex, 2 to 25 percent slopes7819NO1277633854652xj8por62620181:24000
Hondu-Analulu-Gutridge complex, 30 to 60 percent slopes1358CO1269133852672tz1cor62620181:24000
Hondu-Analulu complex, 15 to 30 percent slopes1307BO964531222021qyyyor62620181:24000
Hondu-Analulu complex, 0 to 15 percent slopes1307AO826233853042tz1gor62620181:24000
Hondu-Analulu complex, 30 to 60 percent slopes7750CO563331224241sgfdor62620181:24000
Hondu-Analulu-Gutridge complex, 15 to 30 percent slopes1358BO561133853062tz1for62620181:24000
Hondu-Analulu-Gutridge complex, 0 to 15 percent slopes1358AO477833854712tz1bor62620181:24000
Hondu-Gutridge-Gerow complex, 0 to 15 percent slopes1358AW440833853052tz1dor62620181:24000
Hondu-Porch-Wintercanyon complex, 15 to 30 percent slopes7820BO351033854672xj8sor62620181:24000
Deck-Hondu-Blackgulch complex, 30 to 60 percent slopes7322CO160231223861sg9hor62620181:24000
Hondu-Deck-Blackgulch complex, 30 to 60 percent slopes7325CO103931223891sg9lor62620181:24000
Hondu-Kettlecreek-Rock outcrop complex, 30 to 60 percent slopes7784CO44131224381sgh6or62620181:24000
Hondu-Analulu-Rock Outcrop complex, landslides, 30 to 60 percent slopes7750CL9833854552xj8wor62620181:24000
Hondu-Payraise complex, 30 to 60 percent north slopes7719CN233854511sgdgor62620181:24000
Hondu-Analulu complex, 30 to 60 percent slopes7750CO1237224375021sgfdor63120181:24000
Hondu-Eastpine complex, 15 to 30 percent slopes7722BO566124374831sgdlor63120181:24000
Hondu-Payraise complex, 30 to 60 percent north slopes7719CN285424868851sgdgor63120181:24000
Hondu-Analulu complex, 15 to 30 percent slopes1307BO197924370741qyyyor63120181:24000
Payraise-Hondu complex, 60 to 90 percent north slopes7720DN118724868861sgdhor63120181:24000
Hondu-Analulu-Vogel complex, 30 to 60 percent slopes7755CO107524375031sgfkor63120181:24000
Kingbolt-Hondu complex, 0 to 15 percent slopes7733AO26624374901sgdwor63120181:24000
Analulu-McWillar-Hondu complex, 30 to 60 percent slopes7763CO18824868972pgthor63120181:24000
Vogel-Analulu-Hondu complex, 60 to 90 percent slopes7764DO14124868981sgfxor63120181:24000
McWillar-Analulu-Hondu complex, 30 to 60 percent slopes7766CO324869001q6zvor63120181:24000
Hondu-Bluecanyon complex, 30 to 60 percent slopes903266227222772sf31or6451:24000
Analulu-Vogel-Hondu complex, sandstone substratum, 30 to 60 percent slopes2003CO5431215151r00cor64819771:24000

Map of Series Extent

Approximate geographic distribution of the HONDU 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 .