scholarly journals Seasonal Dynamics of Methane and Carbon Dioxide Evasion From an Open System Pingo: Lagoon Pingo, Svalbard

2019 ◽  
Vol 7 ◽  
Author(s):  
Andrew Jonathan Hodson ◽  
Aga Nowak ◽  
Kelly Robert Redeker ◽  
Erik S. Holmlund ◽  
Hanne Hvidtfeldt Christiansen ◽  
...  
1984 ◽  
Vol 30 (104) ◽  
pp. 44-48 ◽  
Author(s):  
A.G. Thomas ◽  
R. Raiswell

AbstractVariations in dissolved cations, total alkalinity, sulphate, and field pH are recorded for subglacial melt and bulk melt waters (those emerging from the portal) at Argentière (France), in peak and recession flow conditions. Calcium and bicarbonate are the major ions and the bulk melt waters are demonstrated to have acquired solutes by weathering and dissolution in a system open to atmospheric carbon dioxide. Subglacial melt waters have closed-system characteristics, are close to saturation with calcite and quartz, and must be in near-equilibrium with weathered particulates. Recession-flow bulk melt waters are chemically similar to subglacial melt but have open-system characteristics, either due to re-equilibration with the atmosphere for ground-water mixing.


1968 ◽  
Vol 107 (1) ◽  
pp. 7-18 ◽  
Author(s):  
B. Hodgson ◽  
J. D. McGarry

1. The identity of the organism previously known as Vibrio O1 (N.C.I.B. 8250) with a species of Moraxella is established. 2. The ability of cells to oxidize propionate is present only in cells with an endogenous respiration and this ability is increased 80-fold when the organism is grown with propionate. 3. Isocitrate lyase activity in extracts from propionate-grown cells is the same as that in extracts from lactate-grown cells, about tenfold greater than that in extracts from succinate-grown cells and slightly greater than half the activity in extracts from acetate-grown cells. 4. With arsenite as an inhibitor conditions were found in which the organism would catalyse the quantitative oxidation of propionate to pyruvate. When propionate was completely utilized pyruvate was metabolized further to 2-oxoglutarate. 5. The oxidation of propionate by cells was incomplete both in a ‘closed system’ with alkali to trap respiratory carbon dioxide and in an ‘open system’ with an atmosphere of oxygen+carbon dioxide (95:5). Acetate accumulated. Under these conditions [2−14C]- and [3−14C]-propionate gave rise to [14C]acetate. The rate of conversion of [2−14C]propionate into 14CO2, although much less than the rate of conversion of [1−14C]propionate into 14CO2, was slightly greater than the rate of conversion of [3−14C]propionate into 14CO2. 6. The oxidation of propionate by cells was complete in an ‘open system’ with an atmosphere of either oxygen or air. Under these conditions very little [1−14C]propionate was converted into 14C-labelled cell material. The conversion of [2−14C]- and [3−14C]-propionate into 14C-labelled cell material occurred at an appreciable rate, the rate for the incorporation of [3−14C]propionate being slightly more rapid. In the absence of a utilizable nitrogen source part of the [14C]propionate was incorporated into some reserve material, which was oxidized when added substrate had been completely utilized. 7. [14C]-Pyruvate produced from [14C]propionate was chemically degraded. The C(1) of propionate was found only in C(1) of pyruvate. At least 86% of C(2) of pyruvate was derived from C(2) of propionate and at least 92% of C(3) of pyruvate from C(3) of propionate. 8. These results are incompatible with the operation of any of the previously described pathways for propionate metabolism except the direct one, perhaps via an activated acrylate.


1984 ◽  
Vol 30 (104) ◽  
pp. 44-48 ◽  
Author(s):  
A.G. Thomas ◽  
R. Raiswell

AbstractVariations in dissolved cations, total alkalinity, sulphate, and field pH are recorded for subglacial melt and bulk melt waters (those emerging from the portal) at Argentière (France), in peak and recession flow conditions. Calcium and bicarbonate are the major ions and the bulk melt waters are demonstrated to have acquired solutes by weathering and dissolution in a system open to atmospheric carbon dioxide. Subglacial melt waters have closed-system characteristics, are close to saturation with calcite and quartz, and must be in near-equilibrium with weathered particulates. Recession-flow bulk melt waters are chemically similar to subglacial melt but have open-system characteristics, either due to re-equilibration with the atmosphere for ground-water mixing.


2013 ◽  
Vol 465 ◽  
pp. 48-55 ◽  
Author(s):  
Qiao-Qi Sun ◽  
Kun Shi ◽  
Peter Damerell ◽  
Charlotte Whitham ◽  
Guo-Hai Yu ◽  
...  

2019 ◽  
Vol 657 ◽  
pp. 1311-1322 ◽  
Author(s):  
T.R. Juhlke ◽  
R. Van Geldern ◽  
F. Huneau ◽  
E. Garel ◽  
S. Santoni ◽  
...  

2014 ◽  
Vol 106 (3) ◽  
pp. 789-792 ◽  
Author(s):  
Jeffrey T. Baker ◽  
Dennis C. Gitz ◽  
Paxton Payton ◽  
Katrina J. Broughton ◽  
Michael P. Bange ◽  
...  

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