TY - JOUR
T1 - Spatial distribution characteristics of dissolved n2o in unconfi ned groundwater of an agricultural catchment affected by signifi cant fertilizer application
AU - Onishi, Koki
AU - Onodera, Shin Ichi
AU - Saito, Mitsuyo
AU - Shimizu, Yuta
AU - Yoshikawa, Masashi
PY - 2014
Y1 - 2014
N2 - Spatial distribution characteristics of nitrous oxide (N2O) in an unconfi ned aquifer were examined, based on changes in concentrations of N2O, nitrate-nitrogen (NO3--N) and other chemical components with the groundwater fl ow of an agricultural catchment affected by signifi cant fertilizer application. N2O concentrations were about 4μgN L-1 in the upstream area, and were positively correlated with NO3--N concentrations. These results suggest that the nitrifi cation process infl uences N2O concentrations in upstream areas. In the downstream area, N2O concentrations in deeper groundwater (> 15 m) were signifi cantly higher (13 μgN L-1), but they were very low in shallower groundwater (< 15 m), below the detection limit. Spatial distributions of dissolved oxygen (DO) and dissolved organic carbon (DOC) suggest that shallower groundwater is characterized by a strong reducing condition and high organic carbon content compared to deeper groundwater. These results suggest that a complete denitrifi cation process (NO3- → N2) occurs in shallower groundwater, whereas an incomplete denitrifi cation process causes the increase of N2O concentrations found in deeper groundwater.
AB - Spatial distribution characteristics of nitrous oxide (N2O) in an unconfi ned aquifer were examined, based on changes in concentrations of N2O, nitrate-nitrogen (NO3--N) and other chemical components with the groundwater fl ow of an agricultural catchment affected by signifi cant fertilizer application. N2O concentrations were about 4μgN L-1 in the upstream area, and were positively correlated with NO3--N concentrations. These results suggest that the nitrifi cation process infl uences N2O concentrations in upstream areas. In the downstream area, N2O concentrations in deeper groundwater (> 15 m) were signifi cantly higher (13 μgN L-1), but they were very low in shallower groundwater (< 15 m), below the detection limit. Spatial distributions of dissolved oxygen (DO) and dissolved organic carbon (DOC) suggest that shallower groundwater is characterized by a strong reducing condition and high organic carbon content compared to deeper groundwater. These results suggest that a complete denitrifi cation process (NO3- → N2) occurs in shallower groundwater, whereas an incomplete denitrifi cation process causes the increase of N2O concentrations found in deeper groundwater.
KW - Agricultural catchment
KW - Denitrifi cation
KW - Groundwater
KW - N2O
KW - Nitrifi cation
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U2 - 10.3739/rikusui.75.1
DO - 10.3739/rikusui.75.1
M3 - Article
AN - SCOPUS:84923299643
SN - 0021-5104
VL - 75
SP - 1
EP - 11
JO - Japanese Journal of Limnology
JF - Japanese Journal of Limnology
IS - 1
ER -