Canberra, ACT : The Australian National University
Doi
Abstract
Salinity is one of the most severe environmental
factors limiting the productivity of aquaculture and agriculture.
The worldwide area of salt-affected soils is predicted to become
even more widespread in the future due to climate change and
sea-level rise. However, the soil nitrogen and carbon dynamics
associated with soil-induced gas emissions under salinity are not
well understood. The main objective of this study was to
investigate changes of soil carbon and nitrogen cycling
associated with greenhouse gas emissions, plant growth and
fertilizer recovery under effects of different salinity levels.
This study addressed research issues with the following main
objectives. The main aim of the study reported in Chapter 2 was
to analyse greenhouse gas production from different soils with
different times of lid closure and to assess the effects of
different activation time on gas emissions from soils. The
results showed that the 20-min sampling interval at the closure
time of maximum 80 minutes had good results with less variance
either for soil types or monitored gases. Lengthening activation
times for the incubation study may affect emission rates due to
differences in soil properties. The study in Chapter 3 examined
the effects of salinity and additional sources of nitrogen and
carbon on soil nitrogen and carbon cycling in an acid sulphate
soil (ASS) and an alluvial soil. The findings of this study
demonstrated that salinity significantly decreased N2O emissions
from the acid sulphate soil but did not affect emissions from the
alluvial soil. The addition of glucose and nitrate enhanced N2O
production in both salt-affected soils. This investigation
indicated that salinity altered the carbon and nitrogen cycles in
the acid sulphate soil; it recommends that future fertiliser and
crop management will need to account for the changed nutrient
cycling caused by saline water intrusion and climate change. The
objective of the study reported in Chapter 4 was to identify a
relationship between induced-soil gas emissions and the abundance
of denitrification genes in a salt-affected soil. Increased
salinity caused a decrease in both flux and cumulation of the
N2O-N production and soil respiration from the incubated soil.
The study result also showed that elevated salinity increased the
denitrifying genes in the incubated acid sulphate soil. Abundance
of the nir genes was usually high between the first and second
week of incubation, while number of copies of the nosZ gene were
significantly low at those times. Another study presented in
Chapter 5 investigated changes in soil properties, the dynamics
of N and its effects on rice growth and yield under different
salinity levels by using a 15N label fertilizer technique.
Flooding soils for two weeks by saline water greatly decreased
rice yield and yield components in the acid sulphate soil. High
salinity significantly lowered the recovery of fertilizer N by
rice plants, especially in the acid sulphate soil where the crop
did not produce any grain. The loss of fertilizer nitrogen was
highly controlled by the interaction effect of soil types and
salinity. Findings from the thesis substantially and originally
contribute to the literature on salt-affected soils and will
assist in developing new managemental interventions and
strategies for soils where increased salinity is a real
possibility in the future