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Soil Data Analysis and Presentation

Soil Data Analysis and Presentation. Muhs et al ., 2001. Carbon and Sulfur In the Marine Setting:. 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?. Stanley Shales.

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Soil Data Analysis and Presentation

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  1. Soil Data Analysis and Presentation Muhset al., 2001

  2. Carbon and Sulfur In the Marine Setting: 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?

  3. Stanley Shales resistant Corg normal marine

  4. Angel Soils 800 700 barium 600 y = 81.908x + 516.61 R 2 = 0.6181 500 (ppm) 400 300 zinc 200 y = 72.679x + 120.53 100 R 2 = 0.842 0 0.0 1.0 2.0 3.0 TOC (wt.%) Angel Soils and Ceramics 7 6 5 ceramics y = -0.1534x + 2.6116 y = 0.06x + 1.0073 R 2 = 0.2464 R 2 = 0.0108 4 soil P2O5 (wt.%) 3 2 1 0 10 12 14 16 18 20 22 24 26 Al2O3 (wt.%) Carbon In the Soil Setting: Total organic carbon (TOC) in relation to selected trace elements Comparison of total Al to P oxides in soils and ceramics

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

  6. 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

  7. 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.

  8. Sri Lanka This vegetation type can be seen above 1300m in Knuckles Range and can be seen areas such as Thangappuwa, Kalupahana and Gombaniya. During the year heavy mist can be seen in these types of forests. Montane forests are the most important catchments and water shed areas of the Knuckles Range. It plays a key role in providing a water supply to sustain the ecosystems and livelihoods through the year in the downstream areas. These types of the forests contribute a lot when it comes to the natural beauty in Knuckles Mountain Range.

  9. Fe distribution map of Horton Plains. 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.)

  10. Pb in the environment

  11. K concentrations Pb concentrations Ritter, D.F. Process Geomorphology: Wm .Brown Co.: Iowa. 1978. 0 100 200 300 400 500 600 Elevation (m) MAZZARIELLO, 2008, EVALUATION OF SOIL GEOCHEMISTRY IN THE VINEYARDS OF WALLA WALLA, WASHINGTON: 21st Annual Keck Symposium, 78-83.

  12. 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). www.fao.org/docrep/

  13. E W SauliusMarcinkonis, BronislavasKarmaza, EugenijaBakðienë, LiudmilaTripolskaja, DonatasKonèius, DanutëOþeraitienë, Regina Repðienë, 2005, Long-term agrogenic impact on agricultural soil geochemistry in East and West Lithuania: GEOLOGIJA, 51: 1–9.

  14. Pros- Release of nutrients, Removal of invasive species, Propagation adaptations Cons- 500 oC – all soil organic matter is destroyed and all clay minerals collapse 120 o C – all soil microbes are killed 176-288 o C – water repellent properties created iopscience.iop.org

  15. 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.

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