Official Series Description


Lab Data Summary

Aggregate lab data for the HUGO soil series. This aggregation is based on all pedons with a current taxon name of HUGO, 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 HUGO 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
4BUCD541200654-CA-12-006xHUGO3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties40.4245567,-124.1300049
4BUCD634901163-CA-49-011xHUGO3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.5948296,-123.1914139
4B40A2989S1957CA081001Hugo3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties37.4113884,-122.3291702
5UCD601200660-CA-12-006xHUGO3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties41.0874519,-123.6199036

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the HUGO 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 HUGO 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 HUGO 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 HUGO 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 HUGO 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 HUGO 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 HUGO 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 HUGO, 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-2012-05-09-16 | San Mateo Area - May 1961

    Southwest to northeast cross section, at Pigeon Point, showing relationship of geologic formations, land forms, and soil series. Prepared by R. J. Arkley, University of California, Department of Soils and Plant Nutritions (Soil Survey of San Mateo Area, California; May 1961).

Map Units

Map units containing HUGO 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
Hugo loam, moderately deep, 30 to 50 percent slopesHtE976458657hd8dca02119611:20000
Hugo loam, moderately deep, 10 to 30 percent slopesHtD204458656hd8cca02119611:20000
Hugo loam, 20 to 50 percent slopesHrE171458655hd8bca02119611:20000
Hugo loam, moderately deep, 50 to 65 percent slopesHtF166458658hd8fca02119611:20000
Hugo very gravelly loam, 50 to 75 percent slopesHkG89565459765hff4ca09719681:20000
Hugo-Josephine complex, 50 to 75 percent slopesHnG33672459772hffcca09719681:20000
Hugo loam, 30 to 50 percent slopesHhF24143459763hff2ca09719681:20000
Hugo-Atwell complex, 50 to 75 percent slopesHlG9737459768hff7ca09719681:20000
Hugo very gravelly loam, 30 to 50 percent slopesHkF7364459764hff3ca09719681:20000
Hugo-Atwell complex, 30 to 50 percent slopesHlF4023459767hff6ca09719681:20000
Hugo-Hely complex, 50 to 75 percent slopesHsG3745459777hffjca09719681:20000
Hugo-Josephine complex, 9 to 30 percent slopesHnE3418459771hffbca09719681:20000
Hugo very gravelly loam, 50 to 75 percent slopes, erodedHkG22030459766hff5ca09719681:20000
Hugo-Josephine complex, 50 to 75 percent slopes, erodedHnG21916459773hffdca09719681:20000
Hugo-Boomer complex, 50 to 75 percent slopesHmG1831459770hff9ca09719681:20000
Hugo-Laughlin complex, 30 to 75 percent slopesHoG1379459774hfffca09719681:20000
Hugo-Los Gatos complex, 50 to 75 percent slopesHrG989459775hffgca09719681:20000
Hugo-Boomer complex, 30 to 50 percent slopesHmF901459769hff8ca09719681:20000
Hugo-Hely complex, 30 to 50 percent slopesHsF463459776hffhca09719681:20000
Hugo and Josephine sandy loams, very steepHyF14600456427h9ygca63719581:15000
Hugo and Josephine loams, very steepHuF12330456420h9y7ca63719581:15000
Hugo and Josephine sandy loams, very steep, erodedHyF26209456428h9yhca63719581:15000
Hugo and Josephine sandy loams, steep, erodedHyE21771456426h9yfca63719581:15000
Hugo and Josephine loams, steepHuE1288456418h9y5ca63719581:15000
Hugo and Josephine sandy loams, steepHyE873456425h9ydca63719581:15000
Hugo and Josephine sandy loams, moderately steep, erodedHyD2596456424h9ycca63719581:15000
Hugo and Josephine loams, moderately steepHuD436456416h9y3ca63719581:15000
Hugo and Josephine loams, moderately steep, erodedHuD2347456417h9y4ca63719581:15000
Hugo and Josephine loams, steep, erodedHuE2289456419h9y6ca63719581:15000
Hugo and Josephine loams, very deep, slopingHvC280456422h9y9ca63719581:15000
Hugo and Josephine loams, slopingHuC167456415h9y2ca63719581:15000
Hugo and Josephine sandy loams, sloping, erodedHyC2114456423h9ybca63719581:15000
Hugo and Josephine sandy loams, very deep, moderately steepHzD96456430h9ykca63719581:15000
Hugo and Josephine sandy loams, very deep, slopingHzC79456429h9yjca63719581:15000
Hugo and Josephine loams, very deep, gently slopingHvB30456421h9y8ca63719581:15000
Hugo gravelly sandy loam, 30 to 50 percent slopesHuE744460761hgg8ca64519611:20000
Hugo gravelly sandy loam, 50 to 65 percent slopesHuF417460762hgg9ca64519611:20000
Clallam family, moderately deep-Hugo family, deep,maymen family association, 35 to 70 percent slopes24575838470240hsb1ca70119841:24000
Hugo family, moderately deep, 50 to 70 percent slopes27245063470257hsblca70119841:24000
Clallam-Hugo-Holland families association, deep, dry, 35 to 70 percent slopes26543422470254hsbhca70119841:24000
Clallam-Hugo-Holland families association, deep, 35 to 70 percent slopes26632863470255hsbjca70119841:24000
Hugo family, moderately deep-Maymen family complex, 50 to 70 percent slopes32111444470272hsc2ca70119841:24000
Hugo family, moderately deep-Rock outcrop, metasedimentary complex, 50 to 70 percent slopes27410119470259hsbnca70119841:24000
Hugo family, deep-Clallam family, moderately deep association, 25 to 70 percent slopes2409724470235hs9wca70119841:24000
Hugo family, moderately deep, 30 to 50 percent slopes2713852470256hsbkca70119841:24000
Wapal family, moderately deep-Hugo family, deep, dioritic association, 20 to 65 percent slopes5542721470320hsdmca70119841:24000
Hugo family, deep, dioritic, 15 to 35 percent slopes5602521470321hsdnca70119841:24000
Hugo family, deep, 30 to 50 percent slopes3242230470275hsc5ca70119841:24000
Skalan-hugo families association, deep, 25 to 65 percent slopes2321455470230hs9qca70119841:24000
Hugo family, moderately deep-holland, deep complex, 30 to 50 percent slopes3271232470278hsc8ca70119841:24000
Hugo family, moderately deep-Maymen family complex, 30 to 50 percent slopes3201007470271hsc1ca70119841:24000
Hugo family, moderately deep, 50 to 70 percent slopes.272sr1059190617321zjgca70219841:24000
Hugo family, moderately deep-Maymen family complex, 50 to 70 percent slopes.321sr607190579921z4dca70219841:24000
Hugo family, moderately deep-Maymen family complex, 30 to 50 percent slopes,320sr37190579721z4bca70219841:24000
Neuns-Hugo families complex, 40 to 60 percent slopes.21623311470814hsxkca70719831:24000
Hugo-Neuns families complex, 40 to 60 percent slopes.13815420470736hsv1ca70719831:24000
Holland, deep-Hugo families complex, 20 to 40 percent slopes.12111356470719hsthca70719831:24000
Hugo family, 15 to 40 percent slopes.1319410470729hsttca70719831:24000
Hugo family, moderately deep, 40 to 60 percent slopes.1407417470738hsv3ca70719831:24000
Hugo-Holland, deep families complex, 20 to 40 percent slopes.1367376470734hstzca70719831:24000
Neuns-Hugo families complex, 60 to 80 percent slopes.2177264470815hsxlca70719831:24000
Hugo-Neuns families complex, 20 to 40 percent slopes.1377235470735hsv0ca70719831:24000
Hugo, moderately deep-Neuns families complex, 60 to 80 percent slopes.1437116470741hsv6ca70719831:24000
Hugo family, 40 to 60 percent slopes.1325653470730hstvca70719831:24000
Hohmann-Hugo families complex, 40 to 60 percent slopes.955341470691hsslca70719831:24000
Holland, deep-Hugo families complex, 40 to 60 percent slopes.1225265470720hstjca70719831:24000
Huntmount-Hugo-Marpa, deep families complex, 15 to 45 percent slopes.1454841470743hsv8ca70719831:24000
Hugo, moderately deep-Holland families complex, 40 to 60 percent slopes.1414166470739hsv4ca70719831:24000
Hugo-Chaix families complex, 60 to 80 percent slopes.1353755470733hstyca70719831:24000
Hugo-Neuns families complex, 60 to 80 percent slopes.1393534470737hsv2ca70719831:24000
Hugo family, 60 to 80 percent slopes.1332706470731hstwca70719831:24000
Hugo-Chaix families complex, 40 to 60 percent slopes.1342537470732hstxca70719831:24000
Hugo, moderately deep-Holland, deep families complex, 20 to 40 percent slopes.1422442470740hsv5ca70719831:24000
Chawanakee-Hugo families association, 60 to 80 percent slopes.262346470624hsqfca70719831:24000
Neuns-Hugo families complex, 20 to 40 percent slopes.2152114470813hsxjca70719831:24000
Neuns, deep-Hugo families complex, 20 to 40 percent slopes.2271565470825hsxxca70719831:24000
Chaix-Hugo families complex, 20 to 40 percent slopes.221486470620hsq9ca70719831:24000
Clallam-Hugo-Holland families association, deep, dry, 35 to 70 percent slopes.265sr657186820020q0jca70719831:24000
Clallam-Hugo-Holland families association, deep, 35 to 70 percent slopes.266sr486186820220q0lca70719831:24000
Hugo family, moderately deep, 50 to 70 percent slopes.272sr8186820420q0nca70719831:24000
Hugo loam, moderately deep, 10 to 30 percent slopesHtDgl9827478972q419ca70920101:24000
Hugo-Holland, deep-Wilder families complex, 5 to 35 per cent slopes1453778465021hlwpca73119811:24000
Hugo-Holland, deep-Wilder families complex, 35 to 50 pe rcent slopes1461848465022hlwqca73119811:24000

Map of Series Extent

Approximate geographic distribution of the HUGO 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 .