Official Series Description


Lab Data Summary

Aggregate lab data for the MORROW soil series. This aggregation is based on all pedons with a current taxon name of MORROW, 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 MORROW 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 MORROW 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 MORROW 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 MORROW 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 MORROW 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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Click the image to view it full size.

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

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

Competing Series

Soil series competing with MORROW 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 MORROW 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 MORROW 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.

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

Soil series sharing subgroup-level classification with MORROW, 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-2010-11-05-02 | Douglas County - 2008

    Cross-section view of soils that formed in residuum and colluvium or loess over older loess over basalt and receive 12 to 15 inches of precipitation (Soil Survey of Douglas County, Washington; 2008).

  2. WA-2010-11-05-08 | Klickitat County - 2009

    Representative landscape cross section of the Van Nostern-Morrow-Bakeoven general soil map unit (Soil Survey of Klickitat County, Washington; 2009).

  3. WA-2012-05-11-43 | Douglas County - May 2008

    Cross-section of soils that formed in residuum and colluvium or loess over older loess over basalt and receive 12 to 15 inches of precipitation (Soil Survey of Douglas County, Washington; May 2008).

  4. WA-2012-05-11-46 | Klickitat County Area - December 2009

    Representative landscape cross-section of general soil map unit 9 (Soil Survey of Klickitat County Area, Washington; December 2009).

Map Units

Map units containing MORROW 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
Morrow silt loam, 1 to 7 percent slopes18B363906104621j7or02119781:24000
Bakeoven-Morrow complex, 2 to 20 percent slopes3D194006108621kjor02119781:24000
Morrow silt loam, 7 to 12 percent slopes18C91676104721j8or02119781:24000
Morrow silt loam, 20 to 35 percent north slopes19E68016104921jbor02119781:24000
Morrow silt loam, 12 to 20 percent north slopes19D40336104821j9or02119781:24000
Morrow-Lickskillet complex, 20 to 30 percent slopes21E3466105221jfor02119781:24000
Morrow silt loam, 12 to 20 percent south slopes20D2686105121jdor02119781:24000
Bakeoven-Morrow complex, 2 to 20 percent slopes3D310046132521t7or64819771:24000
Morrow silt loam, 20 to 35 percent north slopes32E246646131521sxor64819771:24000
Morrow silt loam, 1 to 7 percent slopes31B160526131221stor64819771:24000
Morrow silt loam, 7 to 12 percent slopes31C122856131321svor64819771:24000
Morrow silt loam, 12 to 20 percent north slopes32D116196131421swor64819771:24000
Morrow silt loam, 20 to 30 percent south slopes33E39786131721szor64819771:24000
Morrow silt loam, 12 to 20 percent south slopes33D8046131621syor64819771:24000
Morrow silt loam, 1 to 7 percent slopes56B24831645202549or66719841:20000
Morrow-Bakeoven complex, 2 to 20 percent slopes59D2066464525254gor66719841:20000
Morrow silt loam, 7 to 12 percent slopes56C1072064521254bor66719841:20000
Morrow silt loam, 12 to 20 percent north slopes57D627164523254dor66719841:20000
Morrow silt loam, 20 to 35 percent slopes56E595264522254cor66719841:20000
Morrow silt loam, 12 to 20 percent south slopes58D68164524254for66719841:20000
Morrow silt loam, 20 to 35 percent north slopes19Emg203933916332krkror6771:24000
Bakeoven-Morrow complex, 2 to 20 percent slopes3Dmg1531339164021bq0or6771:24000
Morrow silt loam, 7 to 12 percent slopes18Cmg101833916582krk9or6771:24000
Morrow-Lickskillet complex, 20 to 30 percent slopes21Emg61333916692lk67or6771:24000
Morrow silt loam, 1 to 7 percent slopes18Bmg586339167921bq1or6771:24000
Morrow silt loam, 12 to 20 percent north slopes19Dmg46033916742krkgor6771:24000
Morrow silt loam, 12 to 20 percent south slopes20Dmg9333916612lk66or6771:24000
Argabak-Morrow complex, 0 to 30 percent slopes285955701057rjhrwa01719981:12000
Broadax-Morrow-Spofford complex, 3 to 8 percent slopes682558701059rjhtwa01719981:12000
Broadax-Morrow-Spofford complex, 8 to 15 percent slopes692489701162rjm4wa01719981:12000
Morrow silt loam, 3 to 8 percent slopes2391730700928rjclwa01719981:12000
Morrow-Argabak complex, 3 to 8 percent slopes2411471700932rjcqwa01719981:12000
Morrow silt loam, 8 to 15 percent slopes240956700929rjcmwa01719981:12000
Morrow-Argabak complex, 8 to 15 percent slopes242951700934rjcswa01719981:12000
Morrow-Argabak-Badge complex, 15 to 30 percent slopes243720701053rjhmwa01719981:12000
Morrow silt loam, 0 to 3 percent slopes238231700926rjcjwa01719981:12000
Morrow silt loam, 2 to 5 percent slopes1508034761802k8fwa63920031:24000
Morrow-Bakeoven complex, 2 to 15 percent slopes1556729761822k8hwa63920031:24000
Morrow silt loam, 5 to 10 percent slopes151680761812k8gwa63920031:24000

Map of Series Extent

Approximate geographic distribution of the MORROW 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 .