Official Series Description


Lab Data Summary

Aggregate lab data for the SPOKANE soil series. This aggregation is based on all pedons with a current taxon name of SPOKANE, 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 SPOKANE 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
43A84P01641983WA019001Spokane7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties48.0047226,-118.8433304
43A96P00731995WA065001Spokane7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties48.1366653,-117.5299988
43A00P07981999WA063005Spokane6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties47.57305,-117.1298139
992P03091991ID061024Spokane6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties46.1899986,-116.5788879

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the SPOKANE 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 SPOKANE 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 SPOKANE 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 SPOKANE 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 SPOKANE 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 SPOKANE 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 SPOKANE 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 SPOKANE, 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 SPOKANE 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
Spokane ashy loam, 5 to 25 percent slopes48113024872932ph78id05720131:24000
Spokane-Rock outcrop complex, 25 to 65 percent slopes4912124872942ph79id05720131:24000
Spokane loam, 30 to 65 percent slopes2npp428508832nppid60419811:24000
Lenz-Spokane-Rock outcrop association, 30 to 55 percent slopes1453611794352nnfid60619761:24000
Spokane loam, 30 to 65 percent slopes1841251794742nppid60619761:24000
Spokane-Moscow association, 35 to 65 percent slopes1851055794752npqid60619761:24000
Spokane ashy loam, moist, 5 to 30 percent slopes183766794732x1z7id60619761:24000
Micapeak-Spokane complex, 30 to 55 percent slopes502711226628912x1zbid60619761:24000
Micapeak-Spokane complex, 15 to 30 percent slopes50267126628902x1z9id60619761:24000
Spokane-Swakane complex, 15 to 30 percent slopes50416830990602wcbid60619761:24000
Spokane-Kramerhill complex, 25 to 40 percent slopes5314582662917nvf4id60619761:24000
Kramerhill-Spokane complex, 8 to 25 percent slopes53133630990572wdzid60619761:24000
Lenz-Spokane complex, 3 to 15 percent slopes5070926628952wfkid60619761:24000
Spokane-Moscow association, 35 to 65 percent slopes2npq69129366392npqid6701:24000
Spokane loam, 30 to 65 percent slopes2npp25729366342nppid6701:24000
Spokane loam, 5 to 30 percent slopes2npn12729366552npnid6701:24000
Spokane-Rock outcrop complex, very steep7290016867229g7wa04319781:24000
Spokane ashy loam, 5 to 30 percent slopes694037686682x1z6wa04319781:24000
Spokane very stony loam, 30 to 55 percent slopes7135756867129g6wa04319781:24000
Spokane very stony loam, 5 to 30 percent slopes706846867029g5wa04319781:24000
Kramerhill-Spokane complex, 8 to 25 percent slopes531311901859312wdzwa06320121:24000
Micapeak-Spokane complex, 15 to 30 percent slopes50264775859022x1z9wa06320121:24000
Lenz-Spokane complex, 3 to 15 percent slopes50704427859492wfkwa06320121:24000
Lenz-Spokane complex, 15 to 30 percent slopes50714085858672wbxwa06320121:24000
Micapeak-Spokane complex, 30 to 55 percent slopes50273212859032x1zbwa06320121:24000
Spokane-Kramerhill complex, 25 to 40 percent slopes53143083621213nvf4wa06320121:24000
Spokane-Swakane complex, 3 to 15 percent slopes50402651680683qv9jwa06320121:24000
Spokane-Swakane complex, 15 to 30 percent slopes50411734858802wcbwa06320121:24000
Spokane-Rock outcrop complex, 30 to 55 percent slopes50371003859402wf8wa06320121:24000
Urban land-Spokane, disturbed complex, 15 to 30 percent slopes719729624252692mdphwa06320121:24000
Spokane-Rock outcrop complex, 40 to 65 percent slopes2241469515819559m2wa06519781:24000
Spokane stony loam, 0 to 40 percent slopes221987115819259lzwa06519781:24000
Spokane-Rock outcrop complex, 0 to 40 percent slopes223889015819459m1wa06519781:24000
Spokane stony loam, 40 to 65 percent slopes222734915819359m0wa06519781:24000
Spokane loam, 25 to 40 percent slopes219723615818959lwwa06519781:24000
Rock outcrop-Spokane complex, 30 to 65 percent slopes196573015816359l1wa06519781:24000
Spokane loam, 0 to 25 percent slopes218545215818859lvwa06519781:24000
Spokane ashy loam, 40 to 65 percent slopes22017651581912x1z5wa06519781:24000
Lenz-Spokane complex, 3 to 15 percent slopes507012126513242wfkwa06519781:24000
Spokane-Swakane complex, 3 to 15 percent slopes5040922651321qv9jwa06519781:24000
Spokane-Rock outcrop complex, 30 to 55 percent slopes50376126513202wf8wa06519781:24000
Micapeak-Spokane complex, 15 to 30 percent slopes50263826513192x1z9wa06519781:24000
Lenz-Spokane complex, 15 to 30 percent slopes50711726513252wbxwa06519781:24000
Spokane loam, 20 to 40 percent slopes44010188705902cg3wa64819871:24000
Spokane loam, 5 to 20 percent slopes4394582705882cg1wa64819871:24000
Spokane ashy loam, 40 to 65 percent slopes4412918705912x1z5wa64819871:24000
Spokane, warm-Skanid, warm complex, 20 to 40 percent slopes4471971705972cgbwa64819871:24000
Spokane, warm-Skanid, warm complex, 5 to 20 percent slopes4461971705962cg9wa64819871:24000
Spokane, warm-Skanid, warm complex, 40 to 65 percent slopes4481838705982cgcwa64819871:24000
Spokane-Rock outcrop complex, 20 to 40 percent slopes4451030705952cg8wa64819871:24000
Spokane loam, warm, 20 to 40 percent slopes442992705922cg5wa64819871:24000
Spokane loam, warm, 40 to 65 percent slopes443659705932cg6wa64819871:24000
Spokane-Rock outcrop complex, 5 to 20 percent slopes444325705942cg7wa64819871:24000

Map of Series Extent

Approximate geographic distribution of the SPOKANE 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 .