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土壤生态系统的结构与功能国际研讨会
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土壤生态系统的结构与功能国际研讨会

会议时间:2013-09-08 08:00:00至 2013-09-10 18:00:00结束

会议地点:南京  中国科学院南京土壤研究所  北京东路73

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Soil structure is a fundamental property of soil fertility with its ability to transport water, nutrients and gas, and to provide habitat for microorganisms and fauna. Aggregated soil structure can improve agronomic productivity and increase the resistance to soil erosion. The formation of soil structure (or aggregates) is the result of biotic (i.e., microorganisms, fauna, roots) and abiotic (i.e., tillage, wetting and drying, freezing and thrawing, clay, ion) factors and their interaction. The relation between soil structure and biotic agents may be the key mechanism to sequester C in soil. Recently, to mitigate global change and to secure food safety, soil structure has received much attention. However, the manifold of interactions between soil structure and factors is still hardly quantified. On the other hand, soil structure and its stability are dynamics with these environmental factors. Although aggregate formation and stability have been investigated in numerous studies, aggregate is not a surrogate of soil structure. With new technology (i.e., micro CT, NEXAFS), the natural heterogeneity of the soil as a three-dimension porous system can be characterized possibly. It may provide us with a chance to fully understand soil structure formation, stability and its functions on C sequestration, water transport, and soil erosion.

 

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  Before 30 June After 30 June and on site
Domestic participant 1200 RMB 1500 RMB
International participant 250 USD 300 USD
Student or Accompanying person 600 RMB or 120 USD 800 RMB or 160 USD
会议场地:中国科学院南京土壤研究所

标签: 土壤 生态

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