Official Series Description


Lab Data Summary

Aggregate lab data for the GOULDING soil series. This aggregation is based on all pedons with a current taxon name of GOULDING, 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 GOULDING 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
15UCD561102156-CA-11-021GOULDING2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties39.3962708,-122.6411057
15UCD654515065-CA-45-150xGOULDING4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties40.6143608,-122.5506668

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the GOULDING 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 GOULDING 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 GOULDING 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 GOULDING 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 GOULDING 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 GOULDING 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 GOULDING 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 hills figure.

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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 GOULDING, 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 GOULDING 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
Neuns-Bamtush-Goulding association, 30 to 50 percent slopes61015573461657hhd5ca01119991:24000
Neuns-Marpa-Goulding complex, 30 to 50 percent slopes59012706461650hhcyca01119991:24000
Neuns-Sheetiron-Goulding complex, 30 to 50 percent slopes591691461651hhczca01119991:24000
Neuns-Goulding-Sheetiron complex, 50 to 75 percent slopes59228461652hhd0ca01119991:24000
Goulding rocky loam, 50 to 65 percent slopesGoF1156458638hd7sca02119611:20000
Goulding rocky loam, 30 to 50 percent slopesGoE322458637hd7rca02119611:20000
Goulding clay loam, 30 to 50 percent slopesGgFsn225816497wdmmca05519741:24000
Goulding clay loam, 15 to 30 percent slopesGgEsn89816496wdmlca05519741:24000
Goulding cobbly clay loam, 30 to 50 percent slopesGlFsn67816501wdmrca05519741:24000
Goulding cobbly clay loam, 30 to 50 percent slopes, erodedGlF2sn37816502wdmsca05519741:24000
Goulding cobbly clay loam, 5 to 15 percent slopesGlDsn35816499wdmpca05519741:24000
Goulding cobbly clay loam, 15 to 30 percent slopesGlEsn9816500wdmqca05519741:24000
Goulding clay loam, 50 to 75 percent slopesGgGsn3816498wdmnca05519741:24000
Goulding clay loam, 30 to 50 percent slopesGgF12896459737hfd7ca09719681:20000
Goulding cobbly clay loam, 15 to 30 percent slopesGlE10551459741hfdcca09719681:20000
Goulding cobbly clay loam, 30 to 50 percent slopesGlF9949459742hfddca09719681:20000
Goulding-Toomes complex, 9 to 50 percent slopesGoF7910459745hfdhca09719681:20000
Goulding cobbly clay loam, 5 to 15 percent slopesGlD6042459740hfdbca09719681:20000
Goulding clay loam, 15 to 30 percent slopesGgE5492459736hfd6ca09719681:20000
Goulding clay loam, 50 to 75 percent slopesGgG2657459739hfd9ca09719681:20000
Goulding clay loam, 5 to 15 percent slopesGgD2597459735hfd5ca09719681:20000
Goulding clay loam, 30 to 50 percent slopes, erodedGgF21567459738hfd8ca09719681:20000
Goulding cobbly clay loam, 50 to 75 percent slopesGlG836459744hfdgca09719681:20000
Goulding cobbly clay loam, 30 to 50 percent slopes, erodedGlF2453459743hfdfca09719681:20000
GOULDING-VITZTHUM-VANVOR COMPLEX, 50 TO 75 PERCENT SLOPES1465728466049hmyvca60619901:24000
PARDALOE-GOULDING COMPLEX, 50 TO 75 PERCENT SLOPES1864164466086hn01ca60619901:24000
HOOSIMBIM-GOULDING COMPLEX, 50 TO 75 PERCENT SLOPES1591131466062hmz8ca60619901:24000
GOULDING-HOLKAT VARIANT-MARPA VARIANT COMPLEX, 50 TO 75 PERCENT SLOPES145767466047hmysca60619901:24000
MARPA VARIANT-GOULDING-HOLKAT VARIANT COMPLEX, 30 TO 50 PERCENT SLOPES173745466074hmznca60619901:24000
Goulding very rocky loam, 50 to 70 percent slopes, erodedGeF213042459997hfnmca60719671:20000
Goulding very rocky loam, 30 to 50 percent slopes, erodedGeE29856459996hfnlca60719671:20000
Goulding very stony loam, 10 to 30 percent slopesGdD6995459995hfnkca60719671:20000
Goulding stony loam, 50 to 65 percent slopesGgF2201460745hgfrca64519611:20000
Goulding stony loam, 30 to 50 percent slopesGgE1921460744hgfqca64519611:20000
Rock outcrop-Goulding family complex, 40 to 80 percent slopes.259st7190609421zfxca70219841:24000
Goulding family-Rock outcrop complex, 50 to 80 percent slopes8541720470683hssbca70719831:24000
Neuns-Goulding families association, 60 to 80 percent slopes.20937240470807hsxbca70719831:24000
Marpa-Goulding families association, 40 to 60 percent slopes.17936691470777hswcca70719831:24000
Goulding family, 40 to 60 percent slopes.8033459470678hss5ca70719831:24000
Goulding-Neuns families association, 50 to 80 percent slopes.8425019470682hss9ca70719831:24000
Rock outcrop-Goulding family complex, 40 to 80 percent slopes.25923985470857hsyyca70719831:24000
Goulding family, 60 to 80 percent slopes8117225470679hss6ca70719831:24000
Neuns-Goulding families association, 40 to 60 percent slopes.20812099470806hsx9ca70719831:24000
Holland-Goulding families association, 40 to 60 percent slopes.10211879470700hsswca70719831:24000
Goulding-Marpa families association, 40 to 60 percent slopes.836746470681hss8ca70719831:24000
Marpa-Goulding families association, 60 to 80 percent slopes.1804881470778hswdca70719831:24000
Marpa-Goulding families association, 20 to 40 percent slopes.1784628470776hswbca70719831:24000
Goulding-Holland families association, 40 to 60 percent slopes.824052470680hss7ca70719831:24000
Pardaloe-Goulding complex, 50 to 75 percent slopes186tw3378186883020qnvca70719831:24000
Goulding family, 20 to 40 percent slopes.791769470677hss4ca70719831:24000
Parrish-Goulding families complex, 20 to 60 percent slopes.2441611470842hsygca70719831:24000
Holland-Goulding families association, 60 to 80 percent slopes.1031073470701hssxca70719831:24000
Holland-Goulding families association, 20 to 40 percent slopes.101984470699hssvca70719831:24000
Hoosimbim-Goulding complex, 50 to 75 percent slopes159tw830186879020qmkca70719831:24000
Goulding-Vitzthum-Vanvor complex, 50 to 75 percent slopes146tw497186876520qlrca70719831:24000
Goulding very rocky loam, 50 to 70 percent slopes, erodedGeF2sh466186839020q6nca70719831:24000
Goulding very rocky loam, 30 to 50 percent slopes, erodedGeE2sh132186838820q6lca70719831:24000
Marpa variant-Goulding-Holkat variant complex, 30 to 50 percent slopes173tw76186881320qn9ca70719831:24000
Goulding stony loam, 30 to 50 percent slopesGgEtc8186828520q38ca70719831:24000
Goulding stony loam, 50 to 65 percent slopesGgFtc2186828720q3bca70719831:24000
Goulding family-Rock outcrop complex, 50 to 80 percent slopes85st50127478812q3rqca70920101:24000
Olete-Kilburn-Goulding families complex, 30 to 50 percent slopesSgF4748779906v5k8ca77619811:24000
Olete-Goulding families-Rubble land association, 50 to 100 percent slopesSgG2033779907v5k9ca77619811:24000
Olete-Goulding families-Rubble land association, 50 to 100 percent slopesSgG15880471671htt6ca77719811:24000
Olete-Goulding families. association, 30 to 50 percent slopesFaF13990471641hts7ca77719811:24000
Olete-Goulding families association, 15 to 30 percent slopesFaE12105471640hts6ca77719811:24000
Olete-Kilburn-Goulding families complex, 30 to 50 percent slopesSgF6075471670htt5ca77719811:24000

Map of Series Extent

Approximate geographic distribution of the GOULDING 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 .