P. Jermsawatdipong et al., METHANE EMISSION FROM PLOTS WITH DIFFERENCES IN FERTILIZER APPLICATION IN THAI PADDY FIELDS, Soil Science and Plant Nutrition, 40(1), 1994, pp. 63-71
Methane emission rates from plots with differences in fertilizer appli
cation (no fertilizer: NF-, chemical fertilizer: CF-, and organic mate
rials: OM-) in 3 typical Thai paddy fields (fresh water alluvial, acid
sulfate, and low humic gley paddy fields) were measured every week th
roughout the rice-growing period. The CH4 emission rates from the NF-
and CF-plots in the paddy field with acid sulfate soil were much lower
than the CH4 emission rates from similar plots in other countries, wh
ile those from the paddy field with low humic gley soil were much high
er. The CH4 emission rates from these plots in the paddy field with fr
esh water alluvial soil corresponded to the lower reported values. The
CH4 emission rates from the OM-plots in Thailand were within the rang
es of reported values or higher. Methane was mainly emitted in the fir
st half of the growth period in Thailand irrespective of the plots, in
contrast to reports stating that CH, emission was higher in the secon
d half of the growth period in the temperate region. The total amount
of CH4 emission (g C m-2) during the rice growing period ranged from 4
to 59 in the fresh water alluvial paddy field, 0.6 to 17 in the acid
sulfate paddy field, and 21 to 35 in the low humic gley paddy field, r
espectively.