Soil Data Analysis and Presentation Muhs et al., 2001.

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Soil Data Analysis and Presentation Muhs et al., 2001

Transcript of Soil Data Analysis and Presentation Muhs et al., 2001.

Page 2: Soil Data Analysis and Presentation Muhs et al., 2001.

Algeo et al. (in submission) Elevated sediment fluxes in the Sverdrup Basin prior to the end-Permian mass extinction: A link to Siberian Traps volcanism?

Carbon and Sulfur In the Marine Setting:

Page 3: Soil Data Analysis and Presentation Muhs et al., 2001.

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Stanley, unmineralized

Stanley, mineralized

Womble

Glenwood Springs Quarry

normal marine

Stanley Shales

resi

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y = 72.679x + 120.53R2 = 0.842

y = 81.908x + 516.61R2 = 0.6181

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zinc

Angel Soils

Angel Soils and Ceramics

y = 0.06x + 1.0073R2 = 0.0108

y = -0.1534x + 2.6116R2 = 0.2464

Al2O3 (wt.%)

P2O

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Total organic carbon (TOC) in relation to selected trace elements

Comparison of total Al to P oxides in soils and ceramics

CarbonIn the Soil Setting:

Page 5: Soil Data Analysis and Presentation Muhs et al., 2001.

0.0 0.5 1.0 1.5 2.0 2.5 3.00

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f(x) = 281.424709354491 x + 109.948592380986R² = 0.28180285628463

A-horizonLinear (A-hori-zon)B-horizon

Corg (wt. %)

Ava

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e P

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Comparison of available P to TOC (Corg) in soils by individual horizon. Angel Mounds SHS

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The coldest, driest desert on Earth.The Dry Valleys are dry because very little snow falls here, the average water content is less than a centimeter. Yet a fully functioning ecosystem exists here, in the ice-covered lakes and the soils of the valley floor. Even though the ecosystem is all but invisible to the naked eye, it still has a basic food web: primary producers (mats of moss and algae in the lakes, bacteria, yeast, fungi and other microbial life in the soils ), grazers (microscopic invertebrates called rotifers and tardigrades), with the top of the food chain consisting of tiny nematode worms (roundworms ).

polarsoils.blogspot.com/2009/01/dry-valley

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Michael A. Poage, John E. Barrett, Ross A. Virginia, Diana H. Wall, 2008, The Influence of Soil Geochemistry on Nematode Distribution, McMurdo Dry Valleys, Antarctica: 40: 119-128.

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P. N. Ranasinghe, C. B. Dissanayake, D. V. N. Samarasinghe and R. Galappatti, 2007, The relationship between soil geochemistry and die back of montane forests in Sri Lanka: a case study: Environmental Geology ,51: 1077-1088. (Their Figure 4.)

Fe distribution map of Horton Plains.

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Pb in the environment

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Ritter, D.F. Process Geomorphology: Wm .Brown Co.: Iowa. 1978.

MAZZARIELLO, 2008, EVALUATION OF SOIL GEOCHEMISTRY IN THE VINEYARDS OF WALLA WALLA, WASHINGTON: 21st Annual Keck Symposium, 78-83.

Elevation (m)0 100 200 300 400 500 600

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www.fao.org/docrep/

Element Concentration

Plant and part Pollution source Country Excessive1 Background Cadmium 45 0.3 Lettuce, leaves Lead smelter Australia

4.2 0.08 Rice, grain Zinc smelter Japan 6.4 0.4 Spinach, leaves Zinc/lead smelter Zambia

Copper 64 8 Lettuce, leaves Copper smelter Australia 14 5 Radish, roots Urban garden United Kingdom 4 2.8 Rice, grain Irrigated farmland Japan

Lead 1000 2 Lettuce, leaves Lead smelter United Kingdom 57 1.8 Carrot, roots Lead smelter Poland 66 3 Spinach, leaves Zinc/lead smelter Zambia

Mercury 0.4 0.008 Lettuce, leaves Chlor-alkali work Switzerland

0.8 0.05 Carrot, roots Mercury mine Yugoslavia 0.6 0.01 Oats, grain Seed treatment Sweden

Zinc 710 25 Onion, bulb Lead smelter United Kingdom 316 40 Lettuce, leaves Zinc smelter Australia 114 35 Soybean, grain Sludged farmland United States

Table 3. Excessive levels of trace metals in food plants grown in contaminated sites (p.p.m. DW)

1Maximum found contents. Source: Kabata-Pendias and Pendias (in press).

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Saulius Marcinkonis, Bronislavas Karmaza, Eugenija Bakðienë, Liudmila Tripolskaja, Donatas Konèius, Danutë Oþeraitienë, Regina Repðienë, 2005, Long-term agrogenic impact on agricultural soil geochemistry in East and West Lithuania: GEOLOGIJA, 51: 1–9.

E W

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iopscience.iop.org

Pros-Release of nutrients,Removal of invasive species,Propagation adaptations

Cons-500 oC – all soil organic matter is destroyed and all clay minerals collapse120 o C – all soil microbes are killed176-288 o C – water repellent properties created

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Thomas H. Biggs and Lisa N. Florkowski, Philip A. Pearthree, Pei-Jen L. Shaner, 2005, The Effects of Fire Events on Soil Geochemistry in Semi-Arid Grasslands: USDA Forest Service Proceedings RMRS-P-503-507.