Official Series Description


Lab Data Summary

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

There are insufficient data to create the lab data summary figure.


Water Balance

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

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There are insufficient data to create the 3D flats position figure.

Soil series sharing subgroup-level classification with PROSSER, 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. WA-2010-11-05-09 | Klickitat County - 2009

    Representative landscape cross section of the soils in the eastern part of the survey area (Soil Survey of Klickitat County, Washington; 2009).

  2. WA-2012-05-11-15 | Benton County Area - July 1971

    Cross section of Benton County, showing the relationship of elevation, precipitation, and major soil series (Soil Survey of Benton County Area, Washington; April 1980).

  3. WA-2012-05-11-47 | Klickitat County Area - December 2009

    Representative landscape cross-section of the soils in the eastern part of the survey area (Soil Survey of Klickitat County Area, Washington; December 2009).

Map Units

Map units containing PROSSER 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
Prosser-Rock outcrop complex, 1 to 5 percent slopes27B3006106121jqor02119781:24000
Prosser-Rock outcrop complex, 1 to 20 percent slopes38D77666132321t5or64819771:24000
Prosser silt loam, 0 to 2 percent slopes37A28886132121t3or64819771:24000
Prosser silt loam, 2 to 7 percent slopes37B4836132221t4or64819771:24000
Prosser silt loam, 20 to 40 percent slopes73E123364552255bor66719841:20000
Prosser silt loam, 12 to 20 percent slopes73D523645512559or66719841:20000
Prosser-Starbuck very rocky very fine sandy loams, 0 to 20 percent slopesPtD213216819428ytwa00119651:20000
Prosser very fine sandy loam, 0 to 20 percent slopesPRC65216818728ylwa00119651:20000
Prosser-Starbuck extremely rocky very fine sandy loams, 0 to 20 percent slopesPuD30556819528yvwa00119651:20000
Prosser-Starbuck very rocky very fine sandy loams, 0 to 20 percent slopesPTC26366819028ypwa00119651:20000
Prosser very fine sandy loam, 2 to 8 percent slopesPrC11126819228yrwa00119651:20000
Prosser-Starbuck very fine sandy loams, 0 to 5 percent slopesPsB7546819328yswa00119651:20000
Prosser-Starbuck very fine sandy loams, 0 to 5 percent slopesPSB7536818928ynwa00119651:20000
Prosser very fine sandy loam, 15 to 30 percent slopes, erodedPRD25706818828ymwa00119651:20000
Prosser very fine sandy loam, 0 to 2 percent slopesPrA2756819128yqwa00119651:20000
Prosser-Starbuck complex, 15 to 45 percent slopes2715699468rgvhwa01719981:12000
Prosser-Starbuck-Rock outcrop complex, 2 to 15 percent slopes8318092718842dsvwa02119941:20000
Starbuck-Prosser-Rock outcrop complex, 15 to 30 percent slopes1699795716062dhwwa02119941:20000
Starbuck-Prosser-Finley complex, 0 to 25 percent slopes1687892716052dhvwa02119941:20000
Prosser silt loam, 2 to 5 percent slopes815707718802dsqwa02119941:20000
Prosser-Starbuck-Rock outcrop complex, droughty, 2 to 15 percent slopes843621718862dsxwa02119941:20000
Prosser silt loam, 0 to 2 percent slopes802742718742dsjwa02119941:20000
Prosser silt loam, 5 to 10 percent slopes821980718822dsswa02119941:20000
Starbuck-Prosser-Rock outcrop complex, droughty, 15 to 30 percent slopes1701612716092dhzwa02119941:20000
Kiona-Prosser-Starbuck complex, 30 to 60 percent slopes48872717632dnywa02119941:20000
Starbuck-Prosser complex, 0 to 15 percent slopes167405716042dhtwa02119941:20000
Prosser fine sandy loam, 2 to 5 percent slopes78317718672ds9wa02119941:20000
Prosser fine sandy loam, 5 to 10 percent slopes7996718692dscwa02119941:20000
Prosser fine sandy loam, 0 to 2 percent slopes7741718662ds8wa02119941:20000
Starbuck-Prosser complex, 0 to 25 percent slopes145244226874129jgwa02519791:24000
Prosser-Starbuck very fine sandy loams, 0 to 15 percent slopes94104376887329nqwa02519791:24000
Prosser-Starbuck complex, 15 to 45 percent slopes9527416887429nrwa02519791:24000
Prosser very fine sandy loam, 2 to 5 percent slopes9016406886929nlwa02519791:24000
Prosser very fine sandy loam, 5 to 10 percent slopes9114786887029nmwa02519791:24000
Prosser very fine sandy loam, 10 to 15 percent slopes9214226887129nnwa02519791:24000
Prosser very fine sandy loam, 0 to 2 percent slopes8913556886729njwa02519791:24000
Prosser very fine sandy loam, 15 to 25 percent slopes936516887229npwa02519791:24000
Prosser silt loam, 2 to 5 percent slopesPoB1444695632bczwa60519651:20000
Prosser silt loam, 5 to 15 percent slopesPoD1136695642bd0wa60519651:20000
Prosser silt loam, 0 to 30 percent slopesPoE1070695652bd1wa60519651:20000
Prosser silt loam, 0 to 2 percent slopesPoA405695622bcywa60519651:20000
Prosser very fine sandy loam, 0 to 15 percent slopes, erodedPrD2287695662bd2wa60519651:20000
Prosser silt loam, 2 to 5 percent slopes2743511762502kbpwa63920031:24000
Prosser-Bakeoven complex, 2 to 15 percent slopes2772633762532kbswa63920031:24000
Prosser silt loam, 5 to 15 percent slopes275852762512kbqwa63920031:24000
Prosser silt loam, 2 to 5 percent slopes19111260861162wlywa67620141:12000
Prosser silt loam, 5 to 12 percent slopes1924370861152wlxwa67620141:12000
Onepennee-Prosser complex, 0 to 12 percent slopes28513280866752x5zwa67620141:12000
Prosser silt loam, 12 to 20 percent slopes1931140861142wlwwa67620141:12000
Starbuck-Prosser complex, 2 to 12 percent slopes3002890866722x5wwa67620141:12000
Fortyday-Prosser complex, 12 to 35 percent slopes2006880866542x59wa67620141:12000
Prosser-Onepennee complex, 0 to 12 percent slopes196710866602x5hwa67620141:12000
Prosser silt loam, 20 to 35 percent slopes194560861132wlvwa67620141:12000
Prosser silt loam, 35 to 45 percent slopes195420861122wltwa67620141:12000
Starbuck-Prosser complex, 12 to 35 percent slopes3003110866702x5twa67620141:12000
Prosser silt loam, 0 to 15 percent slopes9410696906729vzwa67719791:24000
Prosser-Nevo complex, 3 to 15 percent slopes1251686707912cnlwa68119941:24000
Prosser silt loam, 10 to 15 percent slopes1241464707902cnkwa68119941:24000

Map of Series Extent

Approximate geographic distribution of the PROSSER 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 .