Curtis Monger USDA-NRCS Developments in Soil Taxonomy rice ANTHROPOCENE? Ca
Curtis Monger USDA-NRCS Developments in Soil Taxonomy rice ANTHROPOCENE? Soil sustainability differs across the landscape. Ca
Soil Taxonomy Historical Perspective
Whitney (1909) Soil sustainability differs across the landscape. Stressed soil textures within physiographic regions.
V.V. Dokuchaev Nikolai Sibirtsev Konstantin Glinka Curtis Marbut
Marbut (1935) Soil sustainability differs across the landscape. Stressed profile types within bioclimatic zones.
Soil sustainability differs across the landscape. Podzolic soil From Buol, Hole, McCracken 1973
Guy Smith and Soil Survey Staff (1960) Soil sustainability differs across the landscape. Stresses quantitative definitions based on soil properties.
Zonal origins are still apparent in Soil Taxonomy. Ultisols
Soil Taxonomy A Language for Describing Soils
Taxonomic Divisions fine, smectitic, thermic Vertic Torrifluvent
Taxonomic Divisions fine, smectitic, thermic Vertic Torrifluvent order
Taxonomic Divisions fine, smectitic, thermic Vertic Torrifluvent order suborder
Taxonomic Divisions fine, smectitic, thermic Vertic Torrifluvent order suborder great group
Taxonomic Divisions fine, smectitic, thermic Vertic Torrifluvent order subgroup suborder great group
Taxonomic Divisions fine, smectitic, thermic Vertic Torrifluvent order family subgroup suborder great group
Soil Taxonomy Applied Internationally
Soil Taxonomy applied internationally
Soil Taxonomy Moving Across Scales
Soil sustainability differs across the landscape. SPATIAL SCALES in Soil Taxonomy ELECTRON MICROSCOPE SCALE THIN SECTION SCALE SOIL PROFILE SCALE LAND- SCAPE SCALE GLOBAL SCALE small µm large mm meters km km x 1000s
Soil sustainability differs across the landscape. SPATIAL SCALES in Soil Taxonomy ELECTRON MICROSCOPE SCALE THIN SECTION SCALE SOIL PEDON SCALE LAND- SCAPE SCALE GLOBAL SCALE small µm large mm meters km km x 1000s
Soil sustainability differs across the landscape. SOIL PEDON SCALE Leland Gile Guy Smith Desert Project Tour (c. 1960)
SOIL PEDON SCALE Soil sustainability differs across the landscape. C 2Ab 2Bkb 3Byymb 3Byy1b 3Byy2b
Soil sustainability differs across the landscape. SPATIAL SCALES in Soil Taxonomy ELECTRON MICROSCOPE SCALE THIN SECTION SCALE SOIL PEDON SCALE POLY- PEDON SCALE GLOBAL SCALE small µm large mm meters km km x 1000s
Soil sustainability differs across the landscape. Pedon Polypedon (Soil Individual) Profile
POLYPEDONS WHAT WE MAP gypsic lake bed gypsum inactive parabolic dunes siliceous red sand with coppice dunes
Soil sustainability differs across the landscape. gypsic lake bed B polypedon B B A A B B polypedon A
Soil sustainability differs across the landscape. SPATIAL SCALES in Soil Taxonomy ELECTRON MICROSCOPE SCALE THIN SECTION SCALE SOIL PEDON SCALE POLY- PEDON SCALE GLOBAL SCALE small µm large mm meters km km x 1000s
Soil sustainability differs across the landscape. Mollisols
Aridisols NRCS World Soil Resources
Soil sustainability differs across the landscape. SPATIAL SCALES in Soil Taxonomy ELECTRON MICROSCOPE SCALE THIN SECTION SCALE SOIL PEDON SCALE POLY- PEDON SCALE GLOBAL SCALE small µm large mm meters km km x 1000s
5/19/04 Plane-polarized light Calciargid A pore BA Btk1 Btk2 Btk3 Btk4 2Btk5
5/19/04 Plane-polarized light Calciargid A pore BA Btk1 Btk2 Crossed-polarized Btk3 light Btk4 2Btk5
5/19/04 Plane-polarized light Calciargid A pore BA Btk1 Clay films Btk2 Crossed-polarized Btk3 light Btk4 2Btk5
Soil sustainability differs across the landscape. SPATIAL SCALES in Soil Taxonomy ELECTRON MICROSCOPE SCALE THIN SECTION SCALE SOIL PEDON SCALE POLY- PEDON SCALE GLOBAL SCALE small µm large mm meters km km x 1000s
gypsum crystals in soil From Buck et al. 2006
calcite gyp calcite calcite calcite quartz X-ray diffraction is used to identify minerals calcite Sentry Btkyz3 gyp gyp gyp gyp gyp gyp gyp
long duration millions of years PLATE TECTONICS TEMPORAL SCALES in Soil Taxonomy millennia centuries decades months hours minutes PETROCALCIC HORIZON DEVELOPMENT CLAY ACCUMULATION IN SUBSOIL ORGANIC MATTER ACCUMULATION IN TOPSOIL SALT EFFLORESCENCE SOIL MOISTURE SOIL TEMPERATURE short duration Soil sustainability differs across the landscape.
long duration millions of years PLATE TECTONICS TEMPORAL SCALES in Soil Taxonomy millennia centuries decades months hours minutes PETROCALCIC HORIZON DEVELOPMENT CLAY ACCUMULATION IN SUBSOIL ORGANIC MATTER ACCUMULATION IN TOPSOIL SALT EFFLORESCENCE SOIL MOISTURE SOIL TEMPERATURE short duration Soil sustainability differs across the landscape.
Temperature Change at 1 cm White Sands, NM
long duration millions of years PLATE TECTONICS TEMPORAL SCALES in Soil Taxonomy millennia centuries decades months hours/ weeks minutes PETROCALCIC HORIZON DEVELOPMENT CLAY ACCUMULATION IN SUBSOIL ORGANIC MATTER ACCUMULATION IN TOPSOIL SALT EFFLORESCENCE SOIL MOISTURE SOIL TEMPERATURE short duration Soil sustainability differs across the landscape.
long duration millions of years PLATE TECTONICS TEMPORAL SCALES in Soil Taxonomy millennia centuries decades months hours/ weeks minutes PETROCALCIC HORIZON DEVELOPMENT CLAY ACCUMULATION IN SUBSOIL ORGANIC MATTER ACCUMULATION IN TOPSOIL SALT EFFLORESCENCE SOIL MOISTURE SOIL TEMPERATURE short duration Soil sustainability differs across the landscape.
For Example: Saline playa efflorescence at White Sands
Saline playa efflorescence at White Sands
December 2011
February 2012
May 2012
long duration millions of years PLATE TECTONICS TEMPORAL SCALES in Soil Taxonomy millennia centuries decades months hours/ weeks minutes PETROCALCIC HORIZON DEVELOPMENT CLAY ACCUMULATION IN SUBSOIL ORGANIC MATTER ACCUMULATION IN TOPSOIL SALT EFFLORESCENCE SOIL MOISTURE SOIL TEMPERATURE short duration Soil sustainability differs across the landscape.
long duration millions of years PLATE TECTONICS TEMPORAL SCALES in Soil Taxonomy millennia centuries decades months hours/ weeks minutes PETROCALCIC HORIZON DEVELOPMENT CLAY ACCUMULATION IN SUBSOIL ORGANIC MATTER ACCUMULATION IN TOPSOIL SALT EFFLORESCENCE SOIL MOISTURE SOIL TEMPERATURE short duration Soil sustainability differs across the landscape.
long duration millions of years PLATE TECTONICS TEMPORAL SCALES in Soil Taxonomy millennia centuries decades months hours/ weeks minutes PETROCALCIC HORIZON DEVELOPMENT CLAY ACCUMULATION IN SUBSOIL ORGANIC MATTER ACCUMULATION IN TOPSOIL SALT EFFLORESCENCE SOIL MOISTURE SOIL TEMPERATURE short duration Soil sustainability differs across the landscape.
long duration millions of years PLATE TECTONICS TEMPORAL SCALES in Soil Taxonomy millennia centuries decades months hours/ weeks minutes PETROCALCIC HORIZON DEVELOPMENT CLAY ACCUMULATION IN SUBSOIL ORGANIC MATTER ACCUMULATION IN TOPSOIL SALT EFFLORESCENCE SOIL MOISTURE SOIL TEMPERATURE short duration Soil sustainability differs across the landscape.
Present 30 0 30 Ron Blakey Northern Arizona Univ.
Miocene 30 0 30
Tertiary-Cretaceous 30 0 30
Late Jurassic 30 0 30
long duration millions of years millennia centuries decades months SCALE MOST CRITICAL FOR SUSTAINABILITY hours/ weeks minutes small short duration µm large mm meters km km x 1000s Soil sustainability differs across the landscape.
Soil Taxonomy Delivering Information
www.soils.usda.gov
www.soils.usda.gov
Soil Climate Data
Soil Taxonomy Soil Systems and Environmental Issues
Soil sustainability differs across the landscape. Soil systems approach
Mountains & Hills Mountains & Hills Basin Floor Jornada Exp. Range Headquarters Piedmont Slope (Bajada) Paleozoic sedimentary rocks Mountains & Hills Precambrian rocks Rio Grande Valley Tertiary plutonic rocks Basin Floors New Mexico State Univ. alluvial fill Tertiary volcanic rocks Gile et al. 1981
Soil sustainability differs across the landscape. Gulf Dead Zone NOAA Image of Sources of N and P linked to Gulf of Mexico Dead Zone Soil systems approach
Soil Taxonomy Do we need a Subaqueous Order?
Soil sustainability differs across the landscape both above and below water.
Soil sustainability differs across the landscape both above and below water.
Anguilla Series Marine sediments over sandy/gravelly outwash Ase --0 to 10 cm; black (N 2.5/) mucky sand; single grain; very fluid; 1 percent macroalgal fragments, 0 percent rubbed; sulfurous odor; strongly saline; neutral (ph 7.0); ultra acid (ph 3.4) after 8 weeks; clear boundary. ACse--10 to 40 cm; very dark greenish gray (10Y 3/1) mucky sand; single grain; very fluid; 1 percent macroalgal fragments, 0 percent rubbed; sulfurous odor; strongly saline; neutral (ph 7.1); ultra acid (ph 3.2) after 8 weeks; abrupt boundary. (Combined thickness of A and AC horizons is 30 to 70 cm.) 2Bwb--40 to 90 cm; olive brown (2.5Y 4/4) loamy sand; few fine prominent strong brown (7.5YR 4/6) masses of iron accumulation; single grain; nonfluid; 20 percent herbaceous fibers, 5 percent rubbed; 5 percent gravel; moderately saline; neutral (ph 7.0); very strongly acid (ph 4.9) after 8 weeks; abrupt boundary. (0 to 100 cm thick.) 3C--90 to 150 cm; very dark grayish brown (2.5Y 3/2) very gravelly coarse sand; single grain; nonfluid; 50 percent gravel; slightly saline; neutral (ph 7.0); strongly acid (ph 5.5) after 8 weeks.
Cross Section of Lagoon Pond
Depth (feet NAVD88) Washover Fan Flat Nagunt Series Washover Fan Slope Shallow Lagoon Bottom Fort Neck Series Mainland Submerged Beach Anguilla Series Lagoon Bottom Pishagqua Series
Curtis Monger USDA-NRCS Developments in Soil Taxonomy rice ANTHROPOCENE? Soil sustainability differs across the landscape. Ca
Curtis Monger USDA-NRCS Developments in Soil Taxonomy THANK YOU rice ANTHROPOCENE? Soil sustainability differs across the landscape. Ca