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Soil Science encompasses many aspects of soils study such as the disciplines of soil physics, soil chemistry, soil classification, soil microbiology, etc. One of these studies ispedology. Pedology is the study of soils in a three dimensional context in their natural setting across the landscape in terms of origins, morphology (forms), classifications, characteristics or attributes, profile or cross-section, surface and internal water relations, geology, plant ecology, etc. and interpretations for use and management.
OMICS International Organizes 1000+ Global Events Every Year across USA, Europe & Asia with support from 1000 more scientific societies and Publishes 700+ Open access journals which contains over 100000 eminent personalities, reputed scientists as editorial board and organizing committee members. The conference series website will provide you list and details about the conference organize worldwide.
Scope and Importance
Soil Science Conferences provides the scope for opportunities to learn progressed by international scientists and academicians. Soil Science Conference offers excessive quality content to suit the diverse professional development of science and technologies. It is a perfect platform to discuss the current discoveries and developments in the field of Soil Science.
Most soils develop from weathered mineral geologic materials and usually include some organic materials in their upper part. This is called the O horizon, and it is composed of organic material, generally not considered topsoil, but leaf litter and muck. The rock that the mineral part of the soil originates from is called the parent material. Through the further influence of the soil-forming processes of additions, removals, transfers and transformations the nature of the parent materials are altered to the extent that they become soils. The soil-forming processes are controlled by the soil forming factors of parent material, climate, living organisms, relief, and time. Thus the similarity or contrast of soils from place to place reflects the similarity or contrasts of the soil-forming processes and factors.
The primary convention for naming soils is to select a named geographic feature in the vicinity where the soil was first recognized and identified as a new soil, e.g.: the Dunkirk soil series for the village of Dunkirk near Lake Erie, NY. All soils found to have closely similar attributes are classified as Dunkirk wherever they are found. That distribution can be more localized or it can be somewhat more extensive. The description of the soil usually identifies attributes such as pH (degree of alkalinity or acidity), maturity (stage of pedogenic development), texture, consistence, color, gravel content and type, drainage class, and other soil features.
The United States and other nations have soil maps that show the soils in relation to one another as they occur across the landscape. On these maps each soil is characteristically related to a unique landscape position. Thus, the pattern of distribution and the location and extent of the soil type can be comprehended. Soil maps are a prime requisite for many users who need site information to make informed decisions on many aspects of use and management. Comparison of soil resources and their respective suitability and/or limitations can also be used to evaluate alternate sites for intended uses.
The global soil treatment market report highlights the market size for various soil treatment products in terms of both revenue and volume. The global soil treatment market revenue is estimated to reach $28.9 billion by 2017 with a CAGR of 8.5% from 2012 to 2017. Europe is the fastest growing market for aglime pH adjusters and it is projected to reach $269.4 million by 2017.
International symposium and workshops
1. 17th International Seismic Symposium, May 15-20, 2016, Scotland
2. EAGE Workshop on Seismic Reservoir Characterization, January 31 - 03 February, 2016 Kuwait City, Kuwait
3. SPE/EAGE Geosteering and Well Placement Workshop, February 08 – 10, 2016 Dubai, United Arab Emirates
4. International Coastal Symposium 2016 (ICS2016), March 6–11, 2016, Sydney, Australia
5. ISRM International Symposium - EUROCK 2016, August 29–31, 2016, Nevsehir, Turkey
2. 5th Biodiversity Conference, March 10-12, 2016 Madrid, Spain
4. 2ndGeology Conference, April 21-22, 2016 Dubai, UAE
5. 3rd Recycling Congress, Oct 06-07, 2016 Miami, USA
6. 2nd Green Energy Conference, Nov 28-30, 2016 Chicago, USA
8. 2nd Geologists Meeting, July 11-12, 2016 Brisbane, Australia
9. 2nd Recycling Conference, July 25-27, 2016 Berlin, Germany
10. 2nd Petroliferous Basins Conference, Oct 3-5, 2016 London, UK
11. Geophysics Conference, Sept 29-Oct 1, 2016 Vancouver, Canada
12. Geosciences Conference, Oct 6-7, 2016 Miami, USA
16. Coastal Zone Management Conference, May 16-18, 2016 Osaka, Japan
18. 18th International Conference on Earth Science and Climate Change, May 16 - 17, 2016 Montreal, Canada
19. 32nd Nordic Geological Winter Meeting, January 13-15 2016, Helsinki, Finland
20. International Geological Congress 2016August 27–September 04 2016, Cape Town, South Africa
21. International Symposium on Geodynamics and Earth Tides 2016, June 05–09 2016, Trieste, Italy
Relevant Society and Associations
1. Soil science Society of America
2. Indian Society of Soil science
3. American Society of Agronomy
4. British Society of Soil Science (BSSS)
5. Soil Science Australia
6. Canadian Society of Soil Science (CSSS)
7. Japanese Society of
8. Soil Science and Plant Nutrition
9. Egyptian Soil Science Society (ESSS)
10. East and Southeast Asia Federation of Soil Science Society
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This page was last updated on 16th Sep, 2015
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