Official Series Description


Lab Data Summary

Aggregate lab data for the GOODIN soil series. This aggregation is based on all pedons with a current taxon name of GOODIN, 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 GOODIN 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
240A5465S1962OR071004Goodin6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties45.293335,-123.2569427
240A5444S1962OR071005Goodin5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties45.4066658,-123.2852783
240A5445S1962OR071006Goodin5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties45.3488884,-123.2838898
209N0800S2008OR053001Goodin7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties44.9542503,-123.2948608

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the GOODIN 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 GOODIN 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 GOODIN 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 GOODIN 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 GOODIN 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 GOODIN 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 GOODIN 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 flats position figure.

Soil series sharing subgroup-level classification with GOODIN, 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 GOODIN 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
Goodin-Dupee-Chehulpum complex, 12 to 20 percent slopes73666610186ngyfor00320041:24000
Goodin-Dupee-Chehulpum complex, 2 to 12 percent slopes72423610185ngydor00320041:24000
Melbourne-Goodin silty clay loams, 12 to 20 percent slopes2790D7427111221jrw8or06719751:20000
Goodin-Melbourne complex, 2 to 12 percent slopes2789C3427111211jrw1or06719751:20000
Melbourne-Goodin silty clay loams, 30 to 60 percent slopes2790F2627111241jrwbor06719751:20000
Melbourne-Goodin silty clay loams, 20 to 30 percent slopes2790E2527111231jrw9or06719751:20000
Melbourne-Goodin silt loams, 12 to 20 percent slopes2770D1827111131j8cjor06719751:20000
Melbourne-Goodin silt loams, 20 to 30 percent slopes2770E1727111141j8ckor06719751:20000
Melbourne-Goodin silt loams, 30 to 60 percent slopes2770F827111151j8clor06719751:20000
Melbourne-Goodin silt loams, 2 to 12 percent slopes2770C727111121j8chor06719751:20000
Melbourne-Goodin silty clay loams, 12 to 20 percent slopes2790D595527314381jrw8or07119671:24000
Melbourne-Goodin silty clay loams, 20 to 30 percent slopes2790E505927112831jrw9or07119671:24000
Melbourne-Goodin silt loams, 30 to 60 percent slopes2770F378727112751j8clor07119671:24000
Goodin-Melbourne complex, 2 to 12 percent slopes2789C288627113341jrw1or07119671:24000
Melbourne-Goodin silt loams, 20 to 30 percent slopes2770E248527314511j8ckor07119671:24000
Goodin-Melbourne complex, 12 to 20 percent slopes2767D190127113821j8ccor07119671:24000
Melbourne-Goodin silty clay loams, 30 to 60 percent slopes2790F174227113681jrwbor07119671:24000
Goodin silty clay loam, 2 to 12 percent slopes2766C171127113201j8cbor07119671:24000
Melbourne-Goodin silt loams, 12 to 20 percent slopes2770D171127113481j8cjor07119671:24000
Goodin silty clay loam, 12 to 20 percent slopes2766D120627113241vkrcor07119671:24000
Goodin-Melbourne complex, 20 to 30 percent slopes2767E118727112941j8cdor07119671:24000
Goodin-Dupee-Chehulpum complex, 2 to 12 percent slopes, eroded2765C108027113921j8c8or07119671:24000
Goodin-Dupee-Chehulpum complex, 12 to 20 percent slopes, eroded2765D80327113071j8c9or07119671:24000
Goodin-Melbourne complex, 2 to 30 percent slopes2771E59627113841j8cmor07119671:24000
Melbourne-Goodin silt loams, 2 to 12 percent slopes2770C51727112821j8chor07119671:24000
Goodin silty clay loam, 20 to 30 percent slopes2766E26627314472lkgyor07119671:24000
Goodin-Melbourne complex, 30 to 60 percent slopes2767F22627113581j8cfor07119671:24000
Goodin-Witham complex, hummocky, 2 to 25 percent slopes2808D17527113352q3kror07119671:24000
Goodin-Witham complex, hummocky, 2 to 25 percent, stony2818E12127314522q3knor07119671:24000
Goodin silty clay loam, 30 to 60 percent slopes2766F3827113942p8wkor07119671:24000

Map of Series Extent

Approximate geographic distribution of the GOODIN 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 .