Chemical Composition of Oceanic Water During Tertiary Time; Evidence from Pore-Water Studies on JOIDES Drill Cores: ABSTRACT

AAPG Bulletin ◽  
1970 ◽  
Vol 54 ◽  
Author(s):  
F. T. Manheim, K. M. Chan, F. L. Sa
Author(s):  
Marko Nehrig ◽  
Frank Wille ◽  
Annette Rolle ◽  
Konrad Linnemann

Packages for intermediate level waste (ILW) often contain residual water besides the actual waste. The water either exists as obvious free water or it may be bound physically or chemically, e.g. as pore water. A water driven gas generation could occur by vaporisation and by radiolysis. Steam as the result of vaporisation causes an increasing pressure inside a package and can affect corrosion. Vaporisation and condensation processes itself change the thermal behavior of the content especially during strongly unsteady thermal situations like accident fire situations. Radiolysis changes the chemical composition of the content which could cause an unexpected interaction, e.g. hydrogen embrittlement. Besides the pressure build-up the radiolysis of water generates hydrogen and oxygen, which can be highly flammable respectively explosive. The gas generation caused by vaporisation and radiolysis must be taken into account during the design and the safety assessment of a package. Pressure build-up, a changed thermal behavior and content chemistry, and especially the risk of accumulation of combustible gases exceeding the limiting concentration for flammability has to be considered in the safety assessment. Approaches to ensure the transportability of stored packages due to radiolysis will be discussed.


2013 ◽  
Vol 166 ◽  
pp. 52-64 ◽  
Author(s):  
X.P. Nguyen ◽  
Y.J. Cui ◽  
A.M. Tang ◽  
Y.F. Deng ◽  
X.L. Li ◽  
...  

2020 ◽  
Vol 195 ◽  
pp. 02004
Author(s):  
Angelica Tuttolomondo ◽  
Alessio Ferrari ◽  
Lyesse Laloui

An effective stress concept for active clays is formulated to improve the modelling of these materials under a variety of environmental conditions. In particular, the mechanical effects induced by a change in the chemical potential of pore water associated with a change of its pressure (even in the negative range), as well as a change of its chemical composition, are considered. Some implications of the proposed framework are shown with reference to shear strength results related to unsaturated conditions. The proposed approach allows to describe the shear strength envelope consistently by using a unique set of shear strength parameters irrespective of the pore water chemical composition and of the saturation state.


Island Arc ◽  
2008 ◽  
Vol 10 (3-4) ◽  
pp. 422-429
Author(s):  
Tatsuo Matsuda ◽  
Takashi Arai ◽  
Ryuji Ikeda ◽  
Kentaro Omura ◽  
Kenta Kobayashi ◽  
...  

Island Arc ◽  
2001 ◽  
Vol 10 (3-4) ◽  
pp. 422-429 ◽  
Author(s):  
Tatsuo Matsuda ◽  
Takashi Arai ◽  
Ryuji Ikeda ◽  
Kentaro Omura ◽  
Kenta Kobayashi ◽  
...  

1962 ◽  
Vol 14 ◽  
pp. 149-155 ◽  
Author(s):  
E. L. Ruskol

The difference between average densities of the Moon and Earth was interpreted in the preceding report by Professor H. Urey as indicating a difference in their chemical composition. Therefore, Urey assumes the Moon's formation to have taken place far away from the Earth, under conditions differing substantially from the conditions of Earth's formation. In such a case, the Earth should have captured the Moon. As is admitted by Professor Urey himself, such a capture is a very improbable event. In addition, an assumption that the “lunar” dimensions were representative of protoplanetary bodies in the entire solar system encounters great difficulties.


Sign in / Sign up

Export Citation Format

Share Document