Official Series Description


Lab Data Summary

Aggregate lab data for the MCKENZIE soil series. This aggregation is based on all pedons with a current taxon name of MCKENZIE, 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 MCKENZIE 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 MCKENZIE 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 MCKENZIE 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 MCKENZIE 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 MCKENZIE 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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Competing Series

Soil series competing with MCKENZIE 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 MCKENZIE 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 MCKENZIE 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 .

There are insufficient data to create the 2D hillslope position figure.

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

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

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

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Soil series sharing subgroup-level classification with MCKENZIE, 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 MCKENZIE 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
McKenzie silty clay, 0 to 2 percent slopes72A183342690chljmt03320021:24000
McKenzie clay, 0 to 1 percent slopes13A50793438522vystmt04119941:24000
McKenzie clay, 0 to 1 percent slopes5A11903442312vystmt05119921:24000
McKenzie silty clay, 0 to 2 percent slopes21A3482344506pl1ymt06519961:24000
McKenzie silty clay, 0 to 2 percent slopes106299360712d3bwmt06919891:24000
McKenzie clay, 0 to 1 percent slopesMz68813488622zb35mt09119711:24000
McKenzie clay, 0 to 1 percent slopes14A31163450732vystmt10119921:24000
McKenzie clay, saline, 0 to 2 percent slopes141A1903345068cl27mt10119921:24000
Hoven and McKenzie soilsHy20249345456clgrmt10319611:20000
McKenzie-Hoven silty clays, 0 to 1 percent slopesMa432345635clnjmt10919561:31680
McKenzie clay, 0 to 1 percent slopesMk8694345771clsxmt11119661:20000
McKenzie silty clay, 0 to 2 percent slopes21A1662396640pl1ymt11119661:20000
McKenzie clayMo555346075cm3qmt60719701:24000
McKenzie clay, 0 to 1 percent slopes14723493418092vystmt61319751:24000
McKenzie silty clay loam146725341808cgp2mt61319751:24000
McKenzie clay, 0 to 1 percent slopes29A27103476602vystmt64119941:24000
McKenzie silty clay, 0 to 2 percent slopes222205361537d46hmt64919851:24000
McKenzie clay, saline4115139348173cp9dmt65519751:24000
McKenzie clay, 0 to 1 percent slopes38A45083486152vystmt65719901:24000
McKenzie clay, 0 to 1 percent slopes3949113482432zb35mt66119821:24000
McKenzie silty clay, 0 to 2 percent slopes21A1686642969pl1ymt66620081:24000
McKenzie silty clay, 0 to 1 percent slopesE4719A42625635822q64jnd01119691:20000
McKenzie and Heil silty clays, 0 to 1 percent slopesMo25799286712b4znd01119691:20000
McKenzie clay, 0 to 1 percent slopesMn9999286612b4ynd01119691:20000
McKenzie silty clay loam, strongly saline, 0 to 1 percent slopesC18A388025969182q77vnd02319921:24000
McKenzie silty clay, 0 to 1 percent slopesE4719A2827585242q64jnd08719741:20000
McKenzie silty clay loam, strongly saline, 0 to 1 percent slopesC18A185026616462q77vnd10119671:20000
McKenzie clayMn2062353206cvjrsd01919701:24000
McKenzie clayMc1830356180cympsd03119861:24000

Map of Series Extent

Approximate geographic distribution of the MCKENZIE 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 .