Effect of drainage on CO2 exchange patterns in an intensively managed peat pasture
[摘要] ABSTRACT: Eddy correlation measurements of CO
2 exchange were made in intensively managed peat pastures at 2 different groundwater tables during most of a growing season.
F was separated into a respiratory and an assimilatoryCO
2 flux. The fit of the Arrhenius temperature response to
Fr showed that
Fr was generally higher at low groundwater tables. The fit of a hyperbolic irradiance response to
Fa showed that
Fa was also generally higher at low groundwater tables, more than compensating for higher
Fr. The daily CO
2 balance suggested that the low groundwater pasture was a larger CO
2 sink or a smallerCO
2 source than the high groundwater pasture during the measurement period. The difference in
Fr between the groundwater tables was substantially less than the factor 2 difference in level of soil subsidence. This suggeststhat oxidization of soil organic matter was a relatively minor factor in soil subsidence.