Titlebook: Ocean Margin Systems; Gerold Wefer,David Billett,Tjeerd C. E. Weering Book 2003 Springer-Verlag Berlin Heidelberg 2003 Benthic Biology.Flu

Entrancing

Physical Processes and Modelling at Ocean Marginsnce was the main reason to support integrated projects to understand and quantify the processes responsible for high biological productivities, in order to create the scientific knowledge required for its management. For long time it was believed that high productivity of ocean margin areas was a co

hermetic

Seabed Classification at Ocean Marginscance. These surveys deliver increasingly larger volumes of data, acquired by many types of techniques and sensors. Despite their importance, most of these data are still interpreted visually and qualitatively by skilled interpreters. Human interpretation is time-consuming and difficult to standardi

absolve

The Benthic Boundary Layere aggregation, biological mediated particle deposition and resuspension within the BBL is discussed. Theoretical and methodical aspects of BBL research are demonstrated and examples of modern continental margin studies are given.

人工制品

artifice

Slope Instability of Continental Marginsf up to 113,000 km.. Their wide spread distribution and their large dimensions make them important geological features, particularly as many of them are located within hydrocarbon exploration areas. The factors that are controlling slope stability are still poorly understood in spite of significant

仪式

DEMN

pulmonary-edema

珍奇

The Importance of Mineralization Processes in Surface Sediments at Continental Marginsediments. It is not meant to be a comprehensive overview of the whole subject. Instead, we will summarise the relevant subjects, present data from a number of well studied sites from different areas of the world ocean and focus on the aspects of lateral sediment advection, the role of oxygen minimum

哀悼

Numerical Modelling of Transport Processes in the Subsurfacetanding, can determine local or global budgets and are able to make predictions for changing conditions. The physical and mathematical model concepts are introduced for subsurface transport processes in a single phase, water, and, briefly in two phases, water and gas. The last model concept is requi