Official Series Description


Lab Data Summary

Aggregate lab data for the GALVA soil series. This aggregation is based on all pedons with a current taxon name of GALVA, 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 GALVA 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
107A85P028984IA0350011Galva5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties42.625,-95.8000031
107A85P029084IA0350012Galva5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties42.625,-95.8000031
107A85P039184IA1670011Galva5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties43.0583344,-96.3472214
107A85P039284IA1670012Galva5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties43.0583344,-96.3472214
107A85P039384IA1670013Galva5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties43.0583344,-96.3472214
107A85P039484IA1670014Galva5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties43.0583344,-96.3472214
107A85P039584IA1670021Galva5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties42.9377785,-96.2850037
107A85P039684IA1670022Galva5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties42.9377708,-96.2850342
107A85P029185IA0350013Galva4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties42.625,-95.8000031
107A85P029285IA0350014Galva4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties42.625,-95.8000031
107A85P042285IA1610011Galva5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties42.3499985,-95.25
107A85P042385IA1610012Galva5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties42.3499985,-95.25
107A85P042485IA1610013Galva5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties42.3499985,-95.25
107A85P042585IA1610014Galva5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties42.3499985,-95.25
107A86P043185IA1670031Galva5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties43.0430565,-96.4316635
107A86P043285IA1670032Galva5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties43.042778,-96.4313889
107A86P043385IA1670033Galva5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties43.0397224,-96.4313889
107A86P043485IA1670034Galva5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties43.042778,-96.4325027
107A86P043585IA1670035Galva5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties43.0424995,-96.4319458
107A86P043685IA1670036Galva5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties43.0424995,-96.4313889
107A87P037587IA1670051Galva5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties43.0166664,-96.2541656
107A87P037687IA1670052Galva5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties43.0166664,-96.2541656
107A87P037787IA1670053Galva5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties43.0166664,-96.2541656
107A87P037887IA1670061Galva5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties43,-96.2527771
107A87P037987IA1670062Galva5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties43,-96.2527771
107A97P0024S1996IA193011Galva6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties42.560585,-95.8331146

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the GALVA 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 GALVA 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 GALVA 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 GALVA 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 mountains figure.

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Click the image to view it full size.

Competing Series

Soil series competing with GALVA 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 GALVA 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 GALVA 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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Click the image to view it full size.

There are insufficient data to create the 3D mountains figure.

Click the image to view it full size.

Click the image to view it full size.

Soil series sharing subgroup-level classification with GALVA, 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. IA-2010-09-03-06 | Woodbury - 2006

    Typical pattern of soils and underlying material in the Galva association (Soil Survey of Woodbury County, Iowa; 2006).

  2. IA-2011-06-01-27 | Osceola County - 1988

    Typical pattern of soils and parent material in the Sac-Primghar association (Soil Survey of Osceola County, Iowa; 1988).

Map Units

Map units containing GALVA 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
Galva silty clay loam, 2 to 5 percent slopes310B216954032922sy4pia02119731:15840
Galva silty clay loam, 0 to 2 percent slopes3109984032912sqpqia02119731:15840
Galva silty clay loam, terrace, 0 to 2 percent slopesT3103534033372sqq5ia02119731:15840
Galva silty clay loam, 5 to 9 percent slopes, eroded310C23274032932sqq2ia02119731:15840
Galva silty clay loam, 2 to 5 percent slopes310B994884039242sy4pia03519871:15840
Galva silty clay loam, 5 to 9 percent slopes, eroded310C2383894039272sqq2ia03519871:15840
Galva silty clay loam, 5 to 9 percent slopes310C274184039262sqq1ia03519871:15840
Galva silty clay loam, 2 to 5 percent slopes, eroded310B2173964039252sqq0ia03519871:15840
Galva silty clay loam, 0 to 2 percent slopes31085514039232sqpqia03519871:15840
Galva silty clay loam, terrace, 0 to 2 percent slopes81059754039632sqq5ia03519871:15840
Galva silty clay loam, 9 to 14 percent slopes, eroded310D238734039282sqq4ia03519871:15840
Galva silty clay loam, terrace, 2 to 5 percent slopes810B28664039642sqq6ia03519871:15840
Galva silty clay loam, terrace, 5 to 9 percent slopes, eroded810C28164039652sqq8ia03519871:15840
Galva silty clay loam, terrace, 0 to 2 percent slopes8105723994242sqq5ia04120021:12000
Galva silty clay loam, terrace, 2 to 5 percent slopes810B753994252sqq6ia04120021:12000
Galva silty clay loam, 2 to 5 percent slopes310B277774071352sy4pia09319891:15840
Galva silty clay loam, 5 to 9 percent slopes, eroded310C2236064071382sqq2ia09319891:15840
Galva silty clay loam, 5 to 9 percent slopes310C189974071372sqq1ia09319891:15840
Galva silty clay loam, 2 to 5 percent slopes, eroded310B273254071362sqq0ia09319891:15840
Galva silty clay loam, 9 to 14 percent slopes, eroded310D259434071402sqq4ia09319891:15840
Galva silty clay loam, terrace, 2 to 5 percent slopes810B28944072152sqq6ia09319891:15840
Galva silty clay loam, terrace, 0 to 2 percent slopes81016194072142sqq5ia09319891:15840
Galva silty clay loam, 0 to 2 percent slopes3108864071342sqpqia09319891:15840
Galva silty clay loam, terrace, 5 to 9 percent slopes, eroded810C25484072182sqq8ia09319891:15840
Galva silty clay loam, 9 to 14 percent slopes310D3504071392sqq3ia09319891:15840
Galva silty clay loam, 2 to 5 percent slopes310B361174090942sy4pia11919731:15840
Galva silty clay loam, 0 to 2 percent slopes310115484090932sqpqia11919731:15840
Galva silty clay loam, 2 to 5 percent slopes, eroded310B2112274090952sqq0ia11919731:15840
Galva silty clay loam, 5 to 9 percent slopes, eroded310C254114090962sqq2ia11919731:15840
Galva silty clay loam, stratified substratum, 0 to 2 percent slopes31150294090972sqq9ia11919731:15840
Galva silty clay loam, stratified substratum, 2 to 5 percent slopes311B12184090982sqqbia11919731:15840
Galva silty clay loam, 2 to 5 percent slopes310B1009854100692sy4pia14119771:15840
Galva silty clay loam, 0 to 2 percent slopes310117594100682sqpqia14119771:15840
Galva silty clay loam, stratified substratum, 0 to 2 percent slopes31161694100712sqq9ia14119771:15840
Galva silty clay loam, stratified substratum, 2 to 5 percent slopes311B12364100722sqqbia14119771:15840
Galva silty clay loam, 5 to 9 percent slopes, eroded310C26544100702sqq2ia14119771:15840
Galva silty clay loam, 2 to 5 percent slopes310B44274101352sy4pia14319851:15840
Galva silty clay loam, 0 to 2 percent slopes31030004101342sqpqia14319851:15840
Galva silty clay loam, stratified substratum, 0 to 2 percent slopes31129744101362sqq9ia14319851:15840
Galva silty clay loam, stratified substratum, 2 to 5 percent slopes311B9564101372sqqbia14319851:15840
Galva silty clay loam, 5 to 9 percent slopes, eroded310C21292074103412sqq2ia14919721:20000
Galva silty clay loam, 2 to 5 percent slopes310B1097034103402sy4pia14919721:20000
Galva silty clay loam, terrace, 2 to 5 percent slopesT310B219924103642sqq6ia14919721:20000
Galva silty clay loam, 9 to 14 percent slopes, eroded310D297924103422sqq4ia14919721:20000
Galva silty clay loam, terrace, 0 to 2 percent slopesT31042984103632sqq5ia14919721:20000
Galva-Wadena complex, 5 to 14 percent slopes, moderately eroded317C21091410343frzwia14919721:20000
Galva silty clay loam, 2 to 5 percent slopes310B501954107922sy4pia16119751:15840
Galva silty clay loam, 5 to 9 percent slopes, eroded310C240624107952sqq2ia16119751:15840
Galva silty clay loam, 5 to 9 percent slopes310C27824107942sqq1ia16119751:15840
Galva silty clay loam, terrace, 0 to 2 percent slopesT31014254108522sqq5ia16119751:15840
Galva silty clay loam, 0 to 2 percent slopes31012114107912sqpqia16119751:15840
Galva silty clay loam, terrace, 2 to 5 percent slopesT310B7254108532sqq6ia16119751:15840
Galva silty clay loam, 2 to 5 percent slopes, eroded310B24684107932sqq0ia16119751:15840
Galva silty clay loam, 2 to 5 percent slopes, eroded310B21085134112162sqq0ia16719871:15840
Galva silty clay loam, 2 to 5 percent slopes310B706164112152sy4pia16719871:15840
Galva silty clay loam, 5 to 9 percent slopes, eroded310C2341954112172sqq2ia16719871:15840
Galva silty clay loam, 0 to 2 percent slopes310186944112142sqpqia16719871:15840
Galva silty clay loam, terrace, 0 to 2 percent slopes810107324112602sqq5ia16719871:15840
Galva silty clay loam, terrace, 2 to 5 percent slopes810B69134112612sqq6ia16719871:15840
Galva silty clay loam, terrace, 2 to 5 percent slopes, eroded810B227264112622sqq7ia16719871:15840
Galva silty clay loam, 9 to 14 percent slopes, eroded310D28374112182sqq4ia16719871:15840
Galva silty clay loam, 5 to 9 percent slopes, eroded310C2125634019912sqq2ia19320031:12000
Galva silty clay loam, 2 to 5 percent slopes310B99464018962sy4pia19320031:12000
Galva silty clay loam, terrace, 2 to 5 percent slopes810B4644413132sqq6ia19320031:12000
Galva silty clay loam, terrace, 5 to 9 percent slopes, eroded810C21244413152sqq8ia19320031:12000
Galva silty clay loam, 2 to 5 percent slopesP15B214630068p4msmn10520041:12000
Galva silty clay loam, 2 to 5 percent slopesP15B9083432724gj8vmn13320021:12000
Galva silty clay loam, 5 to 9 percent slopes, erodedP15C22294327232sqq2mn13320021:12000

Map of Series Extent

Approximate geographic distribution of the GALVA 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 .