We studied the distribution of dissolved O-2, CO2, CH4, and N2O in a coasta
l swamp system in Thailand with the goal to characterize the dynamics of th
ese gases within the system. The gas concentrations varied spatially and se
asonally in both surface and ground waters. The entire system was a strong
source for CO2 and CH4, and a possible sink for atmospheric N2O. Seasonal v
ariation in precipitation primarily regulated the redox conditions in the s
ystem. However, distributions of CO2, CH4, and N2O in the river that receiv
ed swamp waters were not always in agreement with redox conditions indicate
d by dissolved O-2 concentrations. Sulfate production through pyrite oxidat
ion occurred in the swamp with thin peat layer under aerobic conditions and
was reflected by elevated SO42-/Cl- in the river water. When SO42-/Cl- was
high, CO2 and CH4 concentrations decreased, whereas the N2O concentration
increased. The excess SO42- in the river water was thus identified as a pot
ential indicator for gas dynamics in this coastal swamp system.