Official Series Description


Lab Data Summary

Aggregate lab data for the GILA soil series. This aggregation is based on all pedons with a current taxon name of GILA, 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 GILA were used in the calculation. Source: KSSL snapshot . Methods used to assemble the KSSL snapshot used by SoilWeb / SDE

Click the image to view it full size.

Pedons used in the lab summary:

MLRALab IDPedon IDTaxonnameCINSSL / NASIS ReportsLink To SoilWeb GMap
3040A3197S1959NV003014GILA5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties36.7125015,-114.6769409
3040A3199S1959NV003015GILA5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties36.7194443,-114.6930542
4240A0197S1967TX141003Gila2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties31.541666,-106.1919479
4288P0056S1987-NM015-001-copyGila5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties32.2168722,-103.9989167
n/a40A0726S1967NM061001GILA2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Propertiesn/a

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the GILA 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.

Click the image to view it full size.



Click the image to view it full size.

Sibling Summary

Siblings are those soil series that occur together in map units, in this case with the GILA series. Sketches are arranged according to their subgroup-level taxonomic structure. Source: SSURGO snapshot , parsed OSD records and snapshot of SC database .

Click the image to view it full size.

Select annual climate data summaries for the GILA series and siblings. 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 GILA 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 .

Click the image to view it full size.

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.

Competing Series

Soil series competing with GILA share the same family level classification in Soil Taxonomy. Source: parsed OSD records and snapshot of the SC database .

Click the image to view it full size.

Select annual climate data summaries for the GILA 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 GILA 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 .

Click the image to view it full size.

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 GILA, 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 GILA 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
Gila-Glendale complex, dry, 1 to 3 percent slopes47412515079101mm38az62720051:24000
Gila-Glendale complex, 1 to 3 percent slopes46119915079091mm37az62720051:24000
Gila soilsGo9150528571s02az63719681:31680
Gila very fine sandy loam, reddish variantGs376802486vy1naz64119651:31680
Gila fine sandy loams543720530911s7maz64519821:24000
Gila-Vinton complex, 0 to 5 percent slopes436834581586mj5vaz66120091:24000
Quiburi-Gila complex, 0 to 3 percent slopes7918506008020j2az66120091:24000
Anthony and Gila gravelly sandy loams, 0 to 2 percent slopesAtA17720535901srqaz66219661:20000
Gila and Glendale soils, 0 to 2 percent slopesGgA10610536151ssjaz66219661:20000
Gila loam, 0 to 2 percent slopesGcA10050536111ssdaz66219661:20000
Continental-Gila gravelly sandy loams, 0 to 5 percent slopesCsB8710536081ss9az66219661:20000
Gila sandy loam, 0 to 2 percent slopesGfA1700536141sshaz66219661:20000
Tidwell, Gila, and Glendale soils, saline, 0 to 2 percent slopesTgA1140536421stdaz66219661:20000
Gila loam, saline, 0 to 2 percent slopesGeA580536131ssgaz66219661:20000
Gila gravelly loam, 0 to 2 percent slopesGbA500536101sscaz66219661:20000
Gila loam, 2 to 5 percent slopesGcB290536121ssfaz66219661:20000
Glendale-Gila complex, 0 to 5 percent slopes, severely eroded1613780544381tn2az66319791:24000
Anthony-Gila complex, 0 to 5 percent slopes25465544421tn6az66319791:24000
Gila fine sandy loam, 0 to 2 percent slopes**141245544361tn0az66319791:24000
Glendale-Gila complex, eroded2329655536641sv3az66419751:24000
Anthony-Gila complex128332536491stmaz66419751:24000
Gila loam2014190536611sv0az66419751:24000
Gila-Anthony-Bluepoint complex216721536621sv1az66419751:24000
Glendale-Gila association, frequently flooded246491536651sv4az66419751:24000
Glendale-Gila complex222878536631sv2az66419751:24000
Gila-Glendale complex, chihuahuan, 0 to 2 percent slopes403330679607qt5taz66620071:24000
Gila-Glendale complex, sonoran, 0 to 2 percent slopes4160016931741ttwjaz66620071:24000
Vinton-Gila complex, chihuahuan, 0 to 3 percent slopes84410802948vyjkaz66620071:24000
Vinton-Gila complex, sonoran, 0 to 3 percent slopes8522516931691ttwcaz66620071:24000
Gila loam, 0 to 1 percent slopesGbA10435543601tkkaz66819681:20000
Gila sandy loamGa1774543591tkjaz66819681:20000
Gila loam, 1 to 3 percent slopesGbB1063543611tklaz66819681:20000
Gila silty clay loamGc528543621tkmaz66819681:20000
Glendale-Gila complex, 0 to 3 percent slopes363426592561znhaz67520091:24000
Glendale-Gila complex, saline-sodic, 0 to 3 percent slopes37252114278031jxr5az67520091:24000
Anthony-Gila complex, 0 to 3 percent slopes51281592581znkaz67520091:24000
Gila sandy loamGA15502570122sprlnm02319671:31680
Gila loamGb3227570162vsrxnm02319671:31680
Gila sandy loamGa6774560251w98nm02919671:24000
Gila loamGm5714560271w9bnm02919671:24000
Gila sandy loam, hummockyGh3081560261w99nm02919671:24000
Gila-Hantz complexGH13724556421vwxnm60019731:24000
Gila loam, 0 to 1 percent slopes mlra 42-1Gb4804556432tm57nm60019731:24000
Gila clay loam MLRA 42Ge3710556462spt3nm60019731:24000
Gila fine sandy loamGA3700556401vwvnm60019731:24000
Gila complex, moderately alkaliGF900556411vwwnm60019731:24000
Gila loam, moderately alkaliGd457556451vx0nm60019731:24000
Gila loam, slightly salineGc260556441vwznm60019731:24000
Gila loam, 0 to 1 percent slopes mlra 42-1Gd8981557902tm57nm61219701:24000
Gila clay loamGk5418557951w1vnm61219701:24000
Gila loam, strongly saline and alkaliGh2140557941w1tnm61219701:24000
Gila loam, slightly salineGe1272557911w1qnm61219701:24000
Gila loam, strongly alkaliGg1156557931w1snm61219701:24000
Gila loam, moderately alkaliGf1113557921w1rnm61219701:24000
Gila clay loam, slightly salineGm785557961w1wnm61219701:24000
Gila loamy fine sandGa643557881w1mnm61219701:24000
Gila clay loam, moderately alkaliGn418557971w1xnm61219701:24000
Gila loamy fine sand, strongly alkaliGc390557891w1nnm61219701:24000
Glendale-Gila complex, nearly level3712438565141wt1nm66019811:48000
Gila variant fine sandy loam, 1 to 3 percent slopes161860592821zpbnm66219791:48000
Anthony-Gila complex, 0 to 2 percent slopes6158997571491xgjnm66419841:24000
Gila clay loam, 0 to 1 percent slopes323588570961xdtnm66419841:24000
Gila clay loam, occasionally flooded, 0 to 1 percent slopes232826570921xdpnm66419841:24000
Gila fine sandy loam, 0 to 1 percent slopes132412570851xdgnm66419841:24000
Gila loam, strongly salineGf2486469373hrf2nv60819671:24000
Gila loamGe1154469372hrf1nv60819671:24000
Gila fine sandGd1003469371hrf0nv60819671:24000
Gila loam, water tableGm369469374hrf3nv60819671:24000
Gila loam, water table, strongly salineGn308469375hrf4nv60819671:24000
Gila-Patrole association157495585341yx6tx38919761:24000
Gila fine sandy loam, saline143891585331yx5tx38919761:24000
Gila soilsGa4909372520dhmstx44319641:31680
Gila fine sandy loamGf7974590121zdmtx47519691:24000
Made land, gila soil materialMg6910696634rcx2tx62419671:31680
Gila loamGc3497696622rcwptx62419671:31680
Gila fine sandy loamGa3202696621rcwntx62419671:31680

Map of Series Extent

Approximate geographic distribution of the GILA 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 .