TY - BOOK
T1 - Investigations into aspects of nitrogen and carbon dynamics in grassland used for dairy production on a clay loam soil
AU - Necpalova, Magdalena
N1 - This was for the final master project
This is a placeholder note
PY - 2012
Y1 - 2012
N2 - Increasing concentrations of nitrogen (N) in the waterbodies along with increasing
concentrations of nitrous oxide (N2O) and carbon dioxide in the atmosphere have
become an international environmental concern. Permanent grasslands are important
sources of feed for intensively managed dairy and beef farming systems in North West
Europe and represent around 90% of agricultural land in Ireland. However, there is a
potential for substantial N losses following grazing during the winter when a significant
effective rainfall occurs. In addition, ploughing and reseeding of grassland in order to
increase its productivity may lead to a substantial decrease in soil organic matter (SOM)
followed by an increase in soil inorganic N. This two year study investigated (i) the
environmental impact of a dairy production system involving grazing over the winter
through calculations of soil surface N balances and its effect on soil N dynamics and N
loses to groundwater; (ii) the impact of permanent grassland renovation on soil N, N2O
emissions, N leaching and soil organic carbon (SOC) in a poorly drained clay-loam soil
at Solohead Research Farm. The correlations between grazing management and soil N
dynamics in the soil profile or N concentrations in the groundwater were difficult due to
high natural buffering capacity of the soils associated with heavy texture, high SOC,
high soil pH, anaerobic conditions and presence of shallow groundwater. For this
reason, grazing over the winter period had no effect on soil N dynamics and
groundwater quality on this site. In contrast, grassland renovation decreased topsoil
SOC and total N, increased oxidized N leaching to groundwater and N2O emissions
from the soil surface as a result of soil disturbance, enhanced decomposition of SOM
followed by nitrification and denitrification. Although, the overall losses due to net
SOM mineralisation were high (3 t N and 32 t C ha-1), the proportion lost via N leaching
and direct N2O emissions was low (27 kg N ha-1 y-1) suggesting that nitrate were
instantaneously reduced by dissimilatory nitrate reduction to ammonium or complete
denitrification.
AB - Increasing concentrations of nitrogen (N) in the waterbodies along with increasing
concentrations of nitrous oxide (N2O) and carbon dioxide in the atmosphere have
become an international environmental concern. Permanent grasslands are important
sources of feed for intensively managed dairy and beef farming systems in North West
Europe and represent around 90% of agricultural land in Ireland. However, there is a
potential for substantial N losses following grazing during the winter when a significant
effective rainfall occurs. In addition, ploughing and reseeding of grassland in order to
increase its productivity may lead to a substantial decrease in soil organic matter (SOM)
followed by an increase in soil inorganic N. This two year study investigated (i) the
environmental impact of a dairy production system involving grazing over the winter
through calculations of soil surface N balances and its effect on soil N dynamics and N
loses to groundwater; (ii) the impact of permanent grassland renovation on soil N, N2O
emissions, N leaching and soil organic carbon (SOC) in a poorly drained clay-loam soil
at Solohead Research Farm. The correlations between grazing management and soil N
dynamics in the soil profile or N concentrations in the groundwater were difficult due to
high natural buffering capacity of the soils associated with heavy texture, high SOC,
high soil pH, anaerobic conditions and presence of shallow groundwater. For this
reason, grazing over the winter period had no effect on soil N dynamics and
groundwater quality on this site. In contrast, grassland renovation decreased topsoil
SOC and total N, increased oxidized N leaching to groundwater and N2O emissions
from the soil surface as a result of soil disturbance, enhanced decomposition of SOM
followed by nitrification and denitrification. Although, the overall losses due to net
SOM mineralisation were high (3 t N and 32 t C ha-1), the proportion lost via N leaching
and direct N2O emissions was low (27 kg N ha-1 y-1) suggesting that nitrate were
instantaneously reduced by dissimilatory nitrate reduction to ammonium or complete
denitrification.
KW - Carbon dynamics
M3 - Doctoral Thesis
ER -