scholarly journals Comparison of membrane ATPases from extreme halophiles isolated from ancient salt deposits

1993 ◽  
Vol 23 (1) ◽  
pp. 53-64 ◽  
Author(s):  
Helga Stan-Lotter ◽  
Michael Sulzner ◽  
Eva Egelseer ◽  
Cynthia F. Norton ◽  
Lawrence I. Hochstein
2013 ◽  
Vol 154 (3) ◽  
pp. 387-395 ◽  
Author(s):  
Elmouldi Garoui ◽  
Ibtissem Ben Amara ◽  
Dorra Driss ◽  
Awatef Elwej ◽  
Semia Ellouze Chaabouni ◽  
...  

Geology ◽  
1980 ◽  
Vol 8 (2) ◽  
pp. 66 ◽  
Author(s):  
Roger Y. Anderson ◽  
Douglas W. Kirkland
Keyword(s):  

1992 ◽  
Vol 2 (2) ◽  
pp. 105-111 ◽  
Author(s):  
S. Sánchez-Nieto ◽  
R. Rodríguez-Sotres ◽  
P. González-Romo ◽  
I. Bernal-Lugo ◽  
M. Gavilanes-Ruíz

AbstractThe effectiveness of ATPase in germinated seed may play an important role in the vigour of germination. The activities of tonoplast and plasma membrane ATPases in two maize (Zea mays L.) lines with different vigour of germination were determined. ATP hydrolysis was measured in microsomal fractions from coleoptiles along with the responses to specific inhibitors for the plasma membrane, tonoplast and mitochondrial ATPases as well as for acid phosphatase. Nitrate-sensitive ATPase activity was 1.5–3.0 times lower in the low-vigour line than in the high-vigour line. Kinetic analysis of ATP hydrolysis at different substrate concentrations revealed the existence of two enzymes in the microsomal fractions of the two lines. The Vmax of enzyme 1 in the low-vigour line was a third of that in the high-vigour line. This enzyme was identified as the nitrate-sensitive or tonoplast ATPase on the basis of measurements of ATP hydrolysis in the presence of specific inhibitors at high (8.12mm) and low (0.77mm) ATP concentrations.


1981 ◽  
Vol 6 ◽  
Author(s):  
I-Ming Chou

Rock-salt deposits have been considered as a possible medium for the permanent storage of high-level radioactive wastes and spent fuel. Brine inclusions present in natural salt can migrate toward the waste if the temperature and the temperature gradients in the vicinity of the radioactive waste are large enough. This migration is due to the dissolution of salt at the hot side of the salt-brine interface, ion diffusion through the brine droplet, and the precipitation of salt at the cold side of the salt brine interface.


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