Official Series Description


Lab Data Summary

Aggregate lab data for the HESPERUS soil series. This aggregation is based on all pedons with a current taxon name of HESPERUS, 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 HESPERUS 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
3585P071484NM045015Hesperus6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties36.0161095,-108.8533325
3693P064393CO083001Hesperus7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties37.2383347,-108.3933334
3682P0135S1981NM039010HESPERUS7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties36.933918,-106.5978241
48A81P062481CO045002Hesperus7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties39.5111122,-108.7983322
5179P036479CO023001Hesperus7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties37.0097237,-105.5291672

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the HESPERUS 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 HESPERUS 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 HESPERUS 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 HESPERUS 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 HESPERUS 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 HESPERUS series and competing. 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 HESPERUS 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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Soil series sharing subgroup-level classification with HESPERUS, 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 HESPERUS 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
Pagoda-Hesperus complex, 12 to 40 percent slopes174186509537k36pco66019941:24000
Hesperus-Empedrado, moist-Pagoda complex, 35 to 55 percent slopes160134509520k364co66019941:24000
Hesperus-Empedrado, moist-Pagoda complex, 5 to 35 percent slopes159130509519k363co66019941:24000
Hesperus-Pagoda complex, 3 to 12 percent slopes16132509522k366co66019941:24000
Fughes-Hesperus complex, 3 to 12 percent slopes1459509502k35kco66019941:24000
Hesperus-Pastorius family-Chamita complex, 1 to 5 percent slopes118A374784447vb8rco66820181:24000
Hesperus loam, 3 to 12 percent slopes3911698582991ynmco66919821:24000
Hesperus sandy loam, 3 to 12 percent slopes551513576751y0hco67119971:24000
Hesperus loam, 3 to 6 percent slopes531151576731y0fco67119971:24000
Hesperus loam, 6 to 12 percent slopes54709576741y0gco67119971:24000
Hesperus loam, 0 to 3 percent slopes52311576702wqyhco67119971:24000
Hesperus loam, 0 to 3 percent slopes28247376772wqyhco67220031:24000
Hesperus, stony-Morapos-Nortez complex, 3 to 25 percent slopesMC542173170443k09qco67519861:24000
Hesperus, stony-Morapos-Nortez complex, 3 to 25 percent slopesMC54923170475k09qco67619831:24000
Hesperus, stony-Morapos-Nortez complex, 3 to 25 percent slopes5416469506748k09qco68019701:31680
Hesperus-Empedrado, moist-Pagoda complex, 5 to 35 percent slopes261353506718k08rco68019701:31680
Hesperus-Empedrado, moist-Pagoda complex 5 to 35 percent slopes4754614496709jnvwco68219861:24000
Hesperus-Empedrado, moist-Pagoda complex, 35 to 55 percent slopes4812012496710jnvxco68219861:24000
Hesperus-Pagoda complex, 3 to 12 percent slopes498377496711jnvyco68219861:24000
Pagoda-Hesperus complex, 12 to 40 percent slopes535876496716jnw3co68219861:24000
Debeque-Hesperus complex, 5 to 25 percent slopes303840496691jnv9co68219861:24000
Fughes-Hesperus complex, 3 to 12 percent slopes392957496700jnvlco68219861:24000
Hesperus-Empedrado, moist-Pagoda complex, 5 to 35 percent slopesMC2612583170521k08rco68219861:24000
Hesperus fine sandy loam, dry, 2 to 15 percent slopes996873497280jpg9co68619921:31680
Hesperus loam, 3 to 25 percent slopes, very stony1011657497060jp76co68619921:31680
Hesperus loam, 15 to 50 percent slopes1001551497059jp75co68619921:31680
Hesperus-Dula, frequently flooded-Pastorius complex, 0 to 15 percent slopesHeC117430438422sdk8nm63019771:48000
Hesperus-Pastorius-Chamita, frequently flooded complex, 0 to 5 percent slopesHpC2430438432tdjynm63019771:48000
Hesperus-Tularosa association, strongly slopingHT732566681wz0nm63619701:31680
Hesperus sandy loam, 1 to 3 percent slopesHb6896375690dly1nm63819811:31680
Firo-Hesperus association, hillyFH5507375686dlxxnm63819811:31680
Hesperus sandy loam, 3 to 8 percent slopesHc4075375691dly2nm63819811:31680
Hesperus-Pastorius-Chamita complex, 0 to 5 percent slopes11811433561711wfznm65019891:24000
Hesperus-Dula, frequently flooded-Pastorius complex, 0 to 15 percent slopesHeC514727213932sdk8nm6721:24000
Hesperus-Pastorius-Chamita, frequently flooded complex, 0 to 5 percent slopesHpC347427212752tdjynm6721:24000
Hesperus-Dula, frequently flooded-Pastorius complex, 0 to 15 percent slopesHeC351929345122sdk8nm6781:24000
Hesperus-Pastorius-Chamita, frequently flooded complex, 0 to 5 percent slopesHpC292529345132tdjynm6781:24000
Firo-Hesperus association, 5 to 25 percent slopesFHD28229344922whl0nm6781:24000
Hesperus, stony-Morapos-Nortez complex, 3 to 25 percent slopesMC543543202651k09qut63319831:24000
Elbuck, extremely stony-Hesperus families complex, cool, 10 to 40 percent slopes52326693512504k69dut6461:24000
Hesperus-Zillion families complex, 0 to 15 percent slopes2207766512439k679ut6461:24000
Hesperus variant-Reget association, 10 to 65 percent slopes1633269361156d3t6wy63319871:24000
Tymosling-Hesperus complex, 5 to 30 percent slopes -- draft8604322228434352tsbcwy7231:24000
Bondoe-Hesperus complex, 5 to 30 percent slopes -- draft8602243828091372ts9swy7231:24000

Map of Series Extent

Approximate geographic distribution of the HESPERUS 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 .