Curtis Monger USDA-NRCS Developments in Soil Taxonomy · 2015. 9. 8. · Btk4 Btk2 2Btk5 5/19/04...

76
Ca rice Curtis Monger USDA-NRCS Developments in Soil Taxonomy ANTHROPOCENE?

Transcript of Curtis Monger USDA-NRCS Developments in Soil Taxonomy · 2015. 9. 8. · Btk4 Btk2 2Btk5 5/19/04...

Page 1: Curtis Monger USDA-NRCS Developments in Soil Taxonomy · 2015. 9. 8. · Btk4 Btk2 2Btk5 5/19/04 Plane-polarized light Crossed-polarized light Clay films pore Calciargid

Ca

rice

Curtis Monger USDA-NRCS

Developments in Soil Taxonomy

ANTHROPOCENE?

Page 2: Curtis Monger USDA-NRCS Developments in Soil Taxonomy · 2015. 9. 8. · Btk4 Btk2 2Btk5 5/19/04 Plane-polarized light Crossed-polarized light Clay films pore Calciargid

Ca

rice

Curtis Monger USDA-NRCS

Developments in Soil Taxonomy

ANTHROPOCENE?Soil sustainability differs across the landscape.

Page 3: Curtis Monger USDA-NRCS Developments in Soil Taxonomy · 2015. 9. 8. · Btk4 Btk2 2Btk5 5/19/04 Plane-polarized light Crossed-polarized light Clay films pore Calciargid

Soil Taxonomy—

Historical Perspective

Page 4: Curtis Monger USDA-NRCS Developments in Soil Taxonomy · 2015. 9. 8. · Btk4 Btk2 2Btk5 5/19/04 Plane-polarized light Crossed-polarized light Clay films pore Calciargid

Whitney (1909)

Stressed soil textures within physiographic regions.

Soil sustainability differs across the landscape.

Page 5: Curtis Monger USDA-NRCS Developments in Soil Taxonomy · 2015. 9. 8. · Btk4 Btk2 2Btk5 5/19/04 Plane-polarized light Crossed-polarized light Clay films pore Calciargid

Curtis Marbut

Konstantin GlinkaV.V. Dokuchaev Nikolai Sibirtsev

Page 6: Curtis Monger USDA-NRCS Developments in Soil Taxonomy · 2015. 9. 8. · Btk4 Btk2 2Btk5 5/19/04 Plane-polarized light Crossed-polarized light Clay films pore Calciargid

Marbut (1935)

Stressed profile types within bioclimatic zones.

Soil sustainability differs across the landscape.

Page 7: Curtis Monger USDA-NRCS Developments in Soil Taxonomy · 2015. 9. 8. · Btk4 Btk2 2Btk5 5/19/04 Plane-polarized light Crossed-polarized light Clay films pore Calciargid

From Buol, Hole, McCracken 1973

Podzolic soil

Soil sustainability differs across the landscape.

Page 8: Curtis Monger USDA-NRCS Developments in Soil Taxonomy · 2015. 9. 8. · Btk4 Btk2 2Btk5 5/19/04 Plane-polarized light Crossed-polarized light Clay films pore Calciargid

Guy Smith and Soil Survey Staff (1960)

Stresses quantitative definitions based on soil properties.

Soil sustainability differs across the landscape.

Page 9: Curtis Monger USDA-NRCS Developments in Soil Taxonomy · 2015. 9. 8. · Btk4 Btk2 2Btk5 5/19/04 Plane-polarized light Crossed-polarized light Clay films pore Calciargid

Ultisols

―Zonal‖ origins are still apparent in Soil Taxonomy.

Page 10: Curtis Monger USDA-NRCS Developments in Soil Taxonomy · 2015. 9. 8. · Btk4 Btk2 2Btk5 5/19/04 Plane-polarized light Crossed-polarized light Clay films pore Calciargid

Soil Taxonomy—

A Language for Describing

Soils

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Taxonomic Divisions

fine, smectitic, thermic Vertic Torrifluvent

Page 12: Curtis Monger USDA-NRCS Developments in Soil Taxonomy · 2015. 9. 8. · Btk4 Btk2 2Btk5 5/19/04 Plane-polarized light Crossed-polarized light Clay films pore Calciargid

Taxonomic Divisions

fine, smectitic, thermic Vertic Torrifluventorder

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Taxonomic Divisions

fine, smectitic, thermic Vertic Torrifluventorder

suborder

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Taxonomic Divisions

fine, smectitic, thermic Vertic Torrifluventorder

suborder

great group

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Taxonomic Divisions

fine, smectitic, thermic Vertic Torrifluventorder

suborder

great group

subgroup

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Taxonomic Divisions

fine, smectitic, thermic Vertic Torrifluventorder

suborder

great group

subgroup

family

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Page 18: Curtis Monger USDA-NRCS Developments in Soil Taxonomy · 2015. 9. 8. · Btk4 Btk2 2Btk5 5/19/04 Plane-polarized light Crossed-polarized light Clay films pore Calciargid

Soil Taxonomy—

Applied Internationally

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Soil Taxonomy applied internationally

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Page 21: Curtis Monger USDA-NRCS Developments in Soil Taxonomy · 2015. 9. 8. · Btk4 Btk2 2Btk5 5/19/04 Plane-polarized light Crossed-polarized light Clay films pore Calciargid

Soil Taxonomy—

Moving Across Scales

Page 22: Curtis Monger USDA-NRCS Developments in Soil Taxonomy · 2015. 9. 8. · Btk4 Btk2 2Btk5 5/19/04 Plane-polarized light Crossed-polarized light Clay films pore Calciargid

small large

SOIL

PROFILE

SCALE

LAND-

SCAPE

SCALE

GLOBAL

SCALE

THIN

SECTION

SCALE

ELECTRON

MICROSCOPE

SCALE

mm meters km km x 1000sµm

SPATIAL SCALES

in Soil Taxonomy

Soil sustainability differs across the landscape.

Page 23: Curtis Monger USDA-NRCS Developments in Soil Taxonomy · 2015. 9. 8. · Btk4 Btk2 2Btk5 5/19/04 Plane-polarized light Crossed-polarized light Clay films pore Calciargid

small large

SOIL

PEDON

SCALE

LAND-

SCAPE

SCALE

GLOBAL

SCALE

THIN

SECTION

SCALE

ELECTRON

MICROSCOPE

SCALE

mm meters km km x 1000sµm

SPATIAL SCALES

in Soil Taxonomy

Soil sustainability differs across the landscape.

Page 24: Curtis Monger USDA-NRCS Developments in Soil Taxonomy · 2015. 9. 8. · Btk4 Btk2 2Btk5 5/19/04 Plane-polarized light Crossed-polarized light Clay films pore Calciargid

SOIL

PEDON

SCALE

Desert Project Tour (c. 1960)

Leland

Gile

Guy

Smith

Soil sustainability differs across the landscape.

Page 25: Curtis Monger USDA-NRCS Developments in Soil Taxonomy · 2015. 9. 8. · Btk4 Btk2 2Btk5 5/19/04 Plane-polarized light Crossed-polarized light Clay films pore Calciargid

2Bkb

3Byymb

3Byy1b

3Byy2b

C

2Ab

SOIL PEDON SCALE

Soil sustainability differs across the landscape.

Page 26: Curtis Monger USDA-NRCS Developments in Soil Taxonomy · 2015. 9. 8. · Btk4 Btk2 2Btk5 5/19/04 Plane-polarized light Crossed-polarized light Clay films pore Calciargid

small large

POLY-

PEDON

SCALE

GLOBAL

SCALE

THIN

SECTION

SCALE

ELECTRON

MICROSCOPE

SCALE

mm meters km km x 1000sµm

SOIL

PEDON

SCALE

SPATIAL SCALES

in Soil Taxonomy

Soil sustainability differs across the landscape.

Page 27: Curtis Monger USDA-NRCS Developments in Soil Taxonomy · 2015. 9. 8. · Btk4 Btk2 2Btk5 5/19/04 Plane-polarized light Crossed-polarized light Clay films pore Calciargid

Pedon Polypedon

(Soil Individual)

Profile

Soil sustainability differs across the landscape.

Page 28: Curtis Monger USDA-NRCS Developments in Soil Taxonomy · 2015. 9. 8. · Btk4 Btk2 2Btk5 5/19/04 Plane-polarized light Crossed-polarized light Clay films pore Calciargid

gypsum – inactive parabolic dunes

siliceous red sand

with coppice dunes

gypsic lake bed

POLYPEDONS—WHAT WE MAP

Page 29: Curtis Monger USDA-NRCS Developments in Soil Taxonomy · 2015. 9. 8. · Btk4 Btk2 2Btk5 5/19/04 Plane-polarized light Crossed-polarized light Clay films pore Calciargid

polypedon B

polypedon A

gypsic lake bed

B

B

B B

A A

Soil sustainability differs across the landscape.

Page 30: Curtis Monger USDA-NRCS Developments in Soil Taxonomy · 2015. 9. 8. · Btk4 Btk2 2Btk5 5/19/04 Plane-polarized light Crossed-polarized light Clay films pore Calciargid

small large

GLOBAL

SCALE

THIN

SECTION

SCALE

ELECTRON

MICROSCOPE

SCALE

mm meters km km x 1000sµm

POLY-

PEDON

SCALE

SOIL

PEDON

SCALE

SPATIAL SCALES

in Soil Taxonomy

Soil sustainability differs across the landscape.

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Mollisols

Soil sustainability differs across the landscape.

Page 32: Curtis Monger USDA-NRCS Developments in Soil Taxonomy · 2015. 9. 8. · Btk4 Btk2 2Btk5 5/19/04 Plane-polarized light Crossed-polarized light Clay films pore Calciargid

Aridisols

NRCS World Soil Resources

Page 33: Curtis Monger USDA-NRCS Developments in Soil Taxonomy · 2015. 9. 8. · Btk4 Btk2 2Btk5 5/19/04 Plane-polarized light Crossed-polarized light Clay films pore Calciargid

small large

GLOBAL

SCALE

THIN

SECTION

SCALE

ELECTRON

MICROSCOPE

SCALE

mm meters km km x 1000sµm

POLY-

PEDON

SCALE

SOIL

PEDON

SCALE

SPATIAL SCALES

in Soil Taxonomy

Soil sustainability differs across the landscape.

Page 34: Curtis Monger USDA-NRCS Developments in Soil Taxonomy · 2015. 9. 8. · Btk4 Btk2 2Btk5 5/19/04 Plane-polarized light Crossed-polarized light Clay films pore Calciargid

A

BA

Btk1

Btk3

Calciargid

Btk4

Btk2

2Btk5

5/19/04 Plane-polarized light

pore

Page 35: Curtis Monger USDA-NRCS Developments in Soil Taxonomy · 2015. 9. 8. · Btk4 Btk2 2Btk5 5/19/04 Plane-polarized light Crossed-polarized light Clay films pore Calciargid

A

BA

Btk1

Btk3

Btk4

Btk2

2Btk5

5/19/04 Plane-polarized light

Crossed-polarized light

pore

Calciargid

Page 36: Curtis Monger USDA-NRCS Developments in Soil Taxonomy · 2015. 9. 8. · Btk4 Btk2 2Btk5 5/19/04 Plane-polarized light Crossed-polarized light Clay films pore Calciargid

A

BA

Btk1

Btk3

Btk4

Btk2

2Btk5

5/19/04 Plane-polarized light

Crossed-polarized light

Clay films

pore

Calciargid

Page 37: Curtis Monger USDA-NRCS Developments in Soil Taxonomy · 2015. 9. 8. · Btk4 Btk2 2Btk5 5/19/04 Plane-polarized light Crossed-polarized light Clay films pore Calciargid

small large

GLOBAL

SCALE

THIN

SECTION

SCALE

ELECTRON

MICROSCOPE

SCALE

mm meters km km x 1000sµm

POLY-

PEDON

SCALE

SOIL

PEDON

SCALE

SPATIAL SCALES

in Soil Taxonomy

Soil sustainability differs across the landscape.

Page 38: Curtis Monger USDA-NRCS Developments in Soil Taxonomy · 2015. 9. 8. · Btk4 Btk2 2Btk5 5/19/04 Plane-polarized light Crossed-polarized light Clay films pore Calciargid

From Buck et al. 2006

gypsum crystals in soil

Page 39: Curtis Monger USDA-NRCS Developments in Soil Taxonomy · 2015. 9. 8. · Btk4 Btk2 2Btk5 5/19/04 Plane-polarized light Crossed-polarized light Clay films pore Calciargid

Sentry Btkyz3

gyp

gyp

gyp

gyp

gyp gyp

gyp

gyp

calcite

calc

ite calc

ite

quart

z

calc

ite

calc

ite

X-ray diffraction is used to

identify minerals

Page 40: Curtis Monger USDA-NRCS Developments in Soil Taxonomy · 2015. 9. 8. · Btk4 Btk2 2Btk5 5/19/04 Plane-polarized light Crossed-polarized light Clay films pore Calciargid

long duration

PLATE TECTONICS

SOIL TEMPERATURE

SOIL MOISTURE

ORGANIC MATTER ACCUMULATION IN TOPSOIL

CLAY ACCUMULATION IN SUBSOIL

SALT EFFLORESCENCE

PETROCALCIC HORIZON DEVELOPMENT

minutes

hours

months

decades

centuries

millennia

short duration

millions ofyears

TEMPORAL SCALES

in Soil Taxonomy

Soil sustainability differs across the landscape.

Page 41: Curtis Monger USDA-NRCS Developments in Soil Taxonomy · 2015. 9. 8. · Btk4 Btk2 2Btk5 5/19/04 Plane-polarized light Crossed-polarized light Clay films pore Calciargid

long duration

PLATE TECTONICS

SOIL TEMPERATURE

SOIL MOISTURE

ORGANIC MATTER ACCUMULATION IN TOPSOIL

CLAY ACCUMULATION IN SUBSOIL

SALT EFFLORESCENCE

PETROCALCIC HORIZON DEVELOPMENT

minutes

hours

months

decades

centuries

millennia

short duration

millions ofyears

TEMPORAL SCALES

in Soil Taxonomy

Soil sustainability differs across the landscape.

Page 42: Curtis Monger USDA-NRCS Developments in Soil Taxonomy · 2015. 9. 8. · Btk4 Btk2 2Btk5 5/19/04 Plane-polarized light Crossed-polarized light Clay films pore Calciargid

Temperature Change at 1 cm

White Sands, NM

Page 43: Curtis Monger USDA-NRCS Developments in Soil Taxonomy · 2015. 9. 8. · Btk4 Btk2 2Btk5 5/19/04 Plane-polarized light Crossed-polarized light Clay films pore Calciargid

long duration

PLATE TECTONICS

SOIL TEMPERATURE

SOIL MOISTURE

ORGANIC MATTER ACCUMULATION IN TOPSOIL

CLAY ACCUMULATION IN SUBSOIL

SALT EFFLORESCENCE

PETROCALCIC HORIZON DEVELOPMENT

minutes

months

decades

centuries

millennia

short duration

millions ofyears

hours/weeks

TEMPORAL SCALES

in Soil Taxonomy

Soil sustainability differs across the landscape.

Page 44: Curtis Monger USDA-NRCS Developments in Soil Taxonomy · 2015. 9. 8. · Btk4 Btk2 2Btk5 5/19/04 Plane-polarized light Crossed-polarized light Clay films pore Calciargid

long duration

PLATE TECTONICS

SOIL TEMPERATURE

SOIL MOISTURE

ORGANIC MATTER ACCUMULATION IN TOPSOIL

CLAY ACCUMULATION IN SUBSOIL

SALT EFFLORESCENCE

PETROCALCIC HORIZON DEVELOPMENT

minutes

months

decades

centuries

millennia

short duration

millions ofyears

hours/weeks

TEMPORAL SCALES

in Soil Taxonomy

Soil sustainability differs across the landscape.

Page 45: Curtis Monger USDA-NRCS Developments in Soil Taxonomy · 2015. 9. 8. · Btk4 Btk2 2Btk5 5/19/04 Plane-polarized light Crossed-polarized light Clay films pore Calciargid

Saline playa efflorescence at White Sands

For Example:

Page 46: Curtis Monger USDA-NRCS Developments in Soil Taxonomy · 2015. 9. 8. · Btk4 Btk2 2Btk5 5/19/04 Plane-polarized light Crossed-polarized light Clay films pore Calciargid

Saline playa efflorescence at White Sands

Page 47: Curtis Monger USDA-NRCS Developments in Soil Taxonomy · 2015. 9. 8. · Btk4 Btk2 2Btk5 5/19/04 Plane-polarized light Crossed-polarized light Clay films pore Calciargid

December 2011

Page 48: Curtis Monger USDA-NRCS Developments in Soil Taxonomy · 2015. 9. 8. · Btk4 Btk2 2Btk5 5/19/04 Plane-polarized light Crossed-polarized light Clay films pore Calciargid

February 2012

Page 49: Curtis Monger USDA-NRCS Developments in Soil Taxonomy · 2015. 9. 8. · Btk4 Btk2 2Btk5 5/19/04 Plane-polarized light Crossed-polarized light Clay films pore Calciargid

May 2012

Page 50: Curtis Monger USDA-NRCS Developments in Soil Taxonomy · 2015. 9. 8. · Btk4 Btk2 2Btk5 5/19/04 Plane-polarized light Crossed-polarized light Clay films pore Calciargid

long duration

PLATE TECTONICS

SOIL TEMPERATURE

SOIL MOISTURE

ORGANIC MATTER ACCUMULATION IN TOPSOIL

CLAY ACCUMULATION IN SUBSOIL

SALT EFFLORESCENCE

PETROCALCIC HORIZON DEVELOPMENT

minutes

months

decades

centuries

millennia

short duration

millions ofyears

hours/weeks

TEMPORAL SCALES

in Soil Taxonomy

Soil sustainability differs across the landscape.

Page 51: Curtis Monger USDA-NRCS Developments in Soil Taxonomy · 2015. 9. 8. · Btk4 Btk2 2Btk5 5/19/04 Plane-polarized light Crossed-polarized light Clay films pore Calciargid

long duration

PLATE TECTONICS

SOIL TEMPERATURE

SOIL MOISTURE

ORGANIC MATTER ACCUMULATION IN TOPSOIL

CLAY ACCUMULATION IN SUBSOIL

SALT EFFLORESCENCE

PETROCALCIC HORIZON DEVELOPMENT

minutes

months

decades

centuries

millennia

short duration

millions ofyears

hours/weeks

TEMPORAL SCALES

in Soil Taxonomy

Soil sustainability differs across the landscape.

Page 52: Curtis Monger USDA-NRCS Developments in Soil Taxonomy · 2015. 9. 8. · Btk4 Btk2 2Btk5 5/19/04 Plane-polarized light Crossed-polarized light Clay films pore Calciargid

long duration

PLATE TECTONICS

SOIL TEMPERATURE

SOIL MOISTURE

ORGANIC MATTER ACCUMULATION IN TOPSOIL

CLAY ACCUMULATION IN SUBSOIL

SALT EFFLORESCENCE

PETROCALCIC HORIZON DEVELOPMENT

minutes

months

decades

centuries

millennia

short duration

millions ofyears

hours/weeks

TEMPORAL SCALES

in Soil Taxonomy

Soil sustainability differs across the landscape.

Page 53: Curtis Monger USDA-NRCS Developments in Soil Taxonomy · 2015. 9. 8. · Btk4 Btk2 2Btk5 5/19/04 Plane-polarized light Crossed-polarized light Clay films pore Calciargid

long duration

PLATE TECTONICS

SOIL TEMPERATURE

SOIL MOISTURE

ORGANIC MATTER ACCUMULATION IN TOPSOIL

CLAY ACCUMULATION IN SUBSOIL

SALT EFFLORESCENCE

PETROCALCIC HORIZON DEVELOPMENT

minutes

months

decades

centuries

millennia

short duration

millions ofyears

hours/weeks

TEMPORAL SCALES

in Soil Taxonomy

Soil sustainability differs across the landscape.

Page 54: Curtis Monger USDA-NRCS Developments in Soil Taxonomy · 2015. 9. 8. · Btk4 Btk2 2Btk5 5/19/04 Plane-polarized light Crossed-polarized light Clay films pore Calciargid

Present

30°

30°

Ron Blakey – Northern Arizona Univ.

Page 55: Curtis Monger USDA-NRCS Developments in Soil Taxonomy · 2015. 9. 8. · Btk4 Btk2 2Btk5 5/19/04 Plane-polarized light Crossed-polarized light Clay films pore Calciargid

Miocene

30°

30°

Page 56: Curtis Monger USDA-NRCS Developments in Soil Taxonomy · 2015. 9. 8. · Btk4 Btk2 2Btk5 5/19/04 Plane-polarized light Crossed-polarized light Clay films pore Calciargid

Tertiary-Cretaceous

30°

30°

Page 57: Curtis Monger USDA-NRCS Developments in Soil Taxonomy · 2015. 9. 8. · Btk4 Btk2 2Btk5 5/19/04 Plane-polarized light Crossed-polarized light Clay films pore Calciargid

Late Jurassic

30°

30°

Page 58: Curtis Monger USDA-NRCS Developments in Soil Taxonomy · 2015. 9. 8. · Btk4 Btk2 2Btk5 5/19/04 Plane-polarized light Crossed-polarized light Clay films pore Calciargid

small large

mm meters km km x 1000sµm

long duration

minutes

months

decades

centuries

millennia

short duration

millions ofyears

SCALE MOST CRITICAL

FOR SUSTAINABILITY

hours/weeks

Soil sustainability differs across the landscape.

Page 59: Curtis Monger USDA-NRCS Developments in Soil Taxonomy · 2015. 9. 8. · Btk4 Btk2 2Btk5 5/19/04 Plane-polarized light Crossed-polarized light Clay films pore Calciargid

Soil Taxonomy—

Delivering Information

Page 60: Curtis Monger USDA-NRCS Developments in Soil Taxonomy · 2015. 9. 8. · Btk4 Btk2 2Btk5 5/19/04 Plane-polarized light Crossed-polarized light Clay films pore Calciargid

www.soils.usda.gov

Page 61: Curtis Monger USDA-NRCS Developments in Soil Taxonomy · 2015. 9. 8. · Btk4 Btk2 2Btk5 5/19/04 Plane-polarized light Crossed-polarized light Clay films pore Calciargid

www.soils.usda.gov

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Page 63: Curtis Monger USDA-NRCS Developments in Soil Taxonomy · 2015. 9. 8. · Btk4 Btk2 2Btk5 5/19/04 Plane-polarized light Crossed-polarized light Clay films pore Calciargid

Soil Climate Data

Page 64: Curtis Monger USDA-NRCS Developments in Soil Taxonomy · 2015. 9. 8. · Btk4 Btk2 2Btk5 5/19/04 Plane-polarized light Crossed-polarized light Clay films pore Calciargid

Soil Taxonomy—

Soil Systems and

Environmental Issues

Page 65: Curtis Monger USDA-NRCS Developments in Soil Taxonomy · 2015. 9. 8. · Btk4 Btk2 2Btk5 5/19/04 Plane-polarized light Crossed-polarized light Clay films pore Calciargid

Soil sustainability differs across the landscape.

Soil systems approach

Page 66: Curtis Monger USDA-NRCS Developments in Soil Taxonomy · 2015. 9. 8. · Btk4 Btk2 2Btk5 5/19/04 Plane-polarized light Crossed-polarized light Clay films pore Calciargid

Mountains & Hills

Piedmont Slope

(Bajada)

Basin Floor

Mountains & Hills

Rio Grande

Valley

Basin Floors

Mountains

& Hills

Jornada

Exp. Range

Headquarters

New Mexico

State Univ.

Gile et al. 1981

alluvial fill

Tertiary

volcanic

rocks

Tertiary

plutonic

rocks

Precambrian

rocks

Paleozoic

sedimentary

rocks

Page 67: Curtis Monger USDA-NRCS Developments in Soil Taxonomy · 2015. 9. 8. · Btk4 Btk2 2Btk5 5/19/04 Plane-polarized light Crossed-polarized light Clay films pore Calciargid

Gulf Dead Zone

NOAA Image of Sources of N and P linked to Gulf of Mexico Dead Zone

Soil sustainability differs across the landscape.

Soil systems approach

Page 68: Curtis Monger USDA-NRCS Developments in Soil Taxonomy · 2015. 9. 8. · Btk4 Btk2 2Btk5 5/19/04 Plane-polarized light Crossed-polarized light Clay films pore Calciargid

Soil Taxonomy—

Do we need a

Subaqueous Order?

Page 69: Curtis Monger USDA-NRCS Developments in Soil Taxonomy · 2015. 9. 8. · Btk4 Btk2 2Btk5 5/19/04 Plane-polarized light Crossed-polarized light Clay films pore Calciargid

Soil sustainability differs across the landscape—

both above and below water.

Page 70: Curtis Monger USDA-NRCS Developments in Soil Taxonomy · 2015. 9. 8. · Btk4 Btk2 2Btk5 5/19/04 Plane-polarized light Crossed-polarized light Clay films pore Calciargid

Soil sustainability differs across the landscape—

both above and below water.

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Page 72: Curtis Monger USDA-NRCS Developments in Soil Taxonomy · 2015. 9. 8. · Btk4 Btk2 2Btk5 5/19/04 Plane-polarized light Crossed-polarized light Clay films pore Calciargid

Anguilla SeriesMarine 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.

Page 73: Curtis Monger USDA-NRCS Developments in Soil Taxonomy · 2015. 9. 8. · Btk4 Btk2 2Btk5 5/19/04 Plane-polarized light Crossed-polarized light Clay films pore Calciargid

Cross Section of Lagoon Pond

Page 74: Curtis Monger USDA-NRCS Developments in Soil Taxonomy · 2015. 9. 8. · Btk4 Btk2 2Btk5 5/19/04 Plane-polarized light Crossed-polarized light Clay films pore Calciargid

Washover

Fan Flat

Nagunt Series

Washover

Fan Slope

Lagoon Bottom

Pishagqua Series

Shallow

Lagoon

Bottom

Fort Neck

Series

Mainland

Submerged

Beach

Anguilla Series

Depth

(fe

et N

AV

D88)

Page 75: Curtis Monger USDA-NRCS Developments in Soil Taxonomy · 2015. 9. 8. · Btk4 Btk2 2Btk5 5/19/04 Plane-polarized light Crossed-polarized light Clay films pore Calciargid

Ca

rice

Curtis Monger USDA-NRCS

Developments in Soil Taxonomy

ANTHROPOCENE?Soil sustainability differs across the landscape.

Page 76: Curtis Monger USDA-NRCS Developments in Soil Taxonomy · 2015. 9. 8. · Btk4 Btk2 2Btk5 5/19/04 Plane-polarized light Crossed-polarized light Clay films pore Calciargid

Ca

rice

Curtis Monger USDA-NRCS

Developments in Soil Taxonomy

ANTHROPOCENE?Soil sustainability differs across the landscape.

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