Titlebook: Handbuch der Spurenanalyse; Die Anreicherung und Othmar G. Koch,Gertrud A. Koch-Dedic Book 1974Latest edition Springer-Verlag Berlin Heidel

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Othmar G. Koch,Gertrud A. Koch-Dedic The aim of this study is to develop a new proposal for the calculation of the buckling strength of partially encased columns, embedded on walls, under fire conditions. This proposal is based on the current calculation method proposed in Annex G of EN 1994-1-2. This study uses the finite element met

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Othmar G. Koch,Gertrud A. Koch-Dedic development of the economy of any country. With the advancement of process technologies and invention of new process and products, the risk associated with them is also increasing. This paper analyzes and quantifies the risk posed by an ammonia loading facility located north of a nearby residential

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Othmar G. Koch,Gertrud A. Koch-Dedicnvironment. Chlorine is one of the toxic gases, if released accidentally than the dispersion distance of the gas must be known by the people working around it to take decisions for safe evacuation distance for the general public. In the current analysis, a chlorine tank has been considered as the so

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Othmar G. Koch,Gertrud A. Koch-Dedicng has shifted from extensive to intensive industrial-scale production. However, this intensification has led to frequent occurrences of infectious diseases, hampering the development and profitability of fish farms. To control the persistent and emerging diseases and sustain the intensive fish prod

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Othmar G. Koch,Gertrud A. Koch-Dedic. Both areas were intruded by middle and late Cretaceous Byrd Coast Granites and experienced three distinct periods of low temperature cooling: from 100 to 85 Ma, from 75 to 60 Ma and since the Oligocene. The different cooling stages are related to a pulsing mantle plume, slowly wandering below MBL.

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Othmar G. Koch,Gertrud A. Koch-Dedic. Both areas were intruded by middle and late Cretaceous Byrd Coast Granites and experienced three distinct periods of low temperature cooling: from 100 to 85 Ma, from 75 to 60 Ma and since the Oligocene. The different cooling stages are related to a pulsing mantle plume, slowly wandering below MBL.

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