Voltage-activated hydrogen ion currents

1994 ◽  
Vol 141 (3) ◽  
Author(s):  
T.E. DeCoursey ◽  
V.V. Cherny
Keyword(s):  
Nature ◽  
1982 ◽  
Vol 299 (5886) ◽  
pp. 826-828 ◽  
Author(s):  
R. C. Thomas ◽  
R. W. Meech

1989 ◽  
Vol 145 (1) ◽  
pp. 455-464 ◽  
Author(s):  
M. P. MAHAUT-SMITH

The effects of external Zn2+ on Ca2+ and H+ currents in the soma of intact Helix neurones were investigated using standard two-electrode voltage-clamp procedures. Cells were exposed to a 0Na+, tetraethylammonium (TEA+) saline and clamped with Cs+-filled electrodes, which allows separation of voltagedependent H+ and Ca2+ currents using different holding potentials. Outward H+ currents, activated by depolarizations from holding potentials in the range −15 to −10 mV, were rapidly blocked by low concentrations of external Zn2+ with a Kd of approximately 16μmol l−1. H+ current activation was also markedly slowed and the block was slow to reverse. Ca2+ currents, largely free from contamination by outward current, were activated by small depolarizations from a holding potential of −55 mV. Ca2+ currents were reduced by Zn2+, but the Kd for block was more than 80 times greater than for block of H+ currents. Thus, low concentrations of Zn2+ provide a method of selectively inhibiting H+ current in studies of Ca2+ current. This was demonstrated in cells which slowly acidified following exposure to 0Na+, TEA+ saline, leading to an increased outward H+ current. Washing with low concentrations of Zn2+ blocked the H+ current and uncovered the underlying Ca2+ current. The results also suggest that Zn2+ will be a useful tool in studies of the physiological role of the H+ pathway.


1988 ◽  
Vol 23 (4) ◽  
pp. 532-541
Author(s):  
G. D. Howell ◽  
P.E.J. Green ◽  
C.A. Field ◽  
B. Freedman

Abstract Twenty-eight rivers in Atlantic Canada are sampled monthly, and have periods of record dating back as far as 1965. Statistical analysis of water chemistry for rivers in areas of Nova Scotia and Newfoundland that are believed to be sensitive to acidification has revealed that pH was significantly lower during the late 1960’s and early 1970’s. Annual hydrogen ion export for selected rivers was also greater during this period. This period of relatively low pH and large hydrogen ion export corresponds to a peak of North American sulphur dioxide emission, suggesting that these rivers may be responding to atmospheric loading of anthropogenic mineral acids.


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