Official Series Description


Lab Data Summary

Aggregate lab data for the MANZANO soil series. This aggregation is based on all pedons with a current taxon name of MANZANO, 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 MANZANO 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
6910N077710CO055003Manzano8Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties37.6397222,-104.7455
70A94P001093NM007005Manzano7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties36.4644432,-104.9691696
70C92P033091NM057002MANZANO8Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties34.8013878,-106.0555573

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the MANZANO 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 MANZANO 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 MANZANO 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 MANZANO 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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Competing Series

Soil series competing with MANZANO 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 MANZANO 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 MANZANO 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 mountains figure.

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Soil series sharing subgroup-level classification with MANZANO, 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. NM-2012-02-14-01 | Harding County - November 1973

    Typical pattern of soils in association 2 in the northwestern part of the county (Soil Survey of Harding County, New Mexico; November 1973).

  2. NM-2012-02-14-02 | Harding County - November 1973

    Typical pattern of soils in association 8 in the north-central part of the county (Soil Survey of Harding County, New Mexico; November 1973).

  3. NM-2012-02-14-04 | Harding County - November 1973

    Typical pattern of soils in association 11 in the north-central part of the county (Soil Survey of Harding County, New Mexico; November 1973).

Map Units

Map units containing MANZANO 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
Manzano sandy clay loam, 0 to 3 percent slopes361550542091tdpaz63319941:24000
Manzano loam435583496480jnmhco62719801:24000
Manzano fine sandy loam, 0 to 2 percent slopes90104497539jpqnco64119801:24000
Deacon-La Brier-Manzano association, slopingDR54241507732k1bgnm00719741:24000
Manzano association, gently slopingMB3207507756k1c7nm00719741:24000
Riverwash-Manzano complexRz2718507775k1cvnm00719741:24000
Manzano loamMa2477507760k1ccnm00719741:24000
Manzano loam, 0 to 2 percent slopes, rarely flooded7013679375880dm45nm01919881:48000
Manzano loam, 0 to 2 percent slopes1051121375833dm2nnm01919881:48000
Manzano and La Brier soilsMo9304376366dmmvnm02119681:31680
Manzano loamMn8917376365dmmtnm02119681:31680
Manzano sandy loamMm2395376364dmmsnm02119681:31680
Manzano loam, wet variantMr476376367dmmwnm02119681:31680
Kim-Manzano associationKm775943031454dmv7nm05919721:24000
Manzano loamMn434643031458dmvcnm05919721:24000
Kim-Manzano association, moist, 0 to 9 percent slopesKmmD1454230315472xxtjnm05919721:24000
Manzano loam, moist, 0 to 3 percent slopesMnmB873630315522xxv5nm05919721:24000
Manzano loamMz5525556691vxsnm60019731:24000
Manzano loam, gently slopingMC13571375537dls3nm63019771:48000
Manzano clay loam, 1 to 3 percent slopesMd1925375538dls4nm63019771:48000
Gullied land-Manzano complex, gently slopingGB1832375520dlrknm63019771:48000
Manzano fine sandy loam, 1 to 3 percent slopesMb506375536dls2nm63019771:48000
Manzano loam, 0 to 3 percent slopes353779375594dltynm63219811:63360
Manzano loam, 1 to 3 percent slopesMc2021375705dlyjnm63819811:31680
Manzano clay loam, 0 to 2 percent slopes42456960568032tjg6nm64819821:48000
Loarc-Flugle-Manzano association, 1 to 9 percent slopes67554267568441x4pnm64819821:48000
Maia-Manzano complex, 0 to 5 percent slopes2457360562391wj5nm65019891:24000
Manzano loam, gently sloping542369565371wtsnm66019811:48000
Lonti-Manzano association, 1 to 25 percent slopes28113547592951zprnm66219791:48000
Judd-Manzano association, 1 to 15 percent slopes2215670592891zpknm66219791:48000
Manzano-Ruidoso association, 0 to 5 percent slopes3412810593021zpznm66219791:48000
Paymaster-Ellicott-Manzano association, 0 to 5 percent slopes4512322593141zqcnm66219791:48000
Manzano loam, 1 to 3 percent slopes3310634593011zpynm66219791:48000
Manzano loam, 0 to 1 percent slopes321683593001zpxnm66219791:48000
Tesajo-Manzano complex, 1 to 3 percent slopes69539593401zr6nm66219791:48000
Manzano silt loam, 1 to 3 percent slopes42416133571061xf4nm66419841:24000
Amalia-Manzano association, 3 to 50 percent slopesAMF32071507799k1dmnm67019761:24000
Manzano clay loam, 3 to 5 percent slopesMnC5540507843k1g1nm67019761:24000
Manzano clay loam, 0 to 5 percent slopesMNC3644507832k1fpnm67019761:24000
Manzano clay loam, 1 to 3 percent slopesMnB2379507842k1g0nm67019761:24000
Manzano clay loam, 0 to 1 percent slopesMnA2056507841k1fznm67019761:24000
Maia-Manzano, occasionally flooded complex, 0 to 5 percent slopesMmC6227701892tl9znm6721:24000
Manzano loam, 0 to 1 percent slopesMa3404214739361lgrbnm67419651:24000
Manzano loam, saline substratum, 0 to 1 percent slopesMc2542714739381lgrdnm67419651:24000
Prewitt and Manzano soilsPz2248314739641lgs7nm67419651:24000
Manzano loam, 1 to 5 percent slopesMb849714739371lgrcnm67419651:24000
Maia-Manzano, occasionally flooded complex, 0 to 5 percent slopesMmC208529345592tl9znm6781:24000
Manzano loam, 1 to 5 percent slopesMMB4329345602wl1fnm6781:24000
Manzano loam, 1 to 5 percent slopes1002194568541x50nm68219851:24000
Lazarus-Manzano complex, 0 to 8 percent slopes, flooded605383014537781kss2nm68720081:24000

Map of Series Extent

Approximate geographic distribution of the MANZANO 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 .